Published on Hazen Research (https://www.hazenresearch.com)


Patent Number/Link: 
6,173,840 Beneficiation of saline minerals

111111111111111111111111111111111111111111111111111111111111111111111111111

US006173840Bl

(12) United States Patent

Pruszko et al.

(10) Patent No.:

(45) Date of Patent:

US 6,173,840 Bl

Jan. 16,2001

(52) U.S. CI. 209/214; 209/3; 209/218;

209/11

(51) Int. CI? B03C 1/00; B07B 1/00;

B03B 1/00

(73) Assignee: Environmental Projects, Inc., Casper,

WY(US)

(21) Appl. No.: 09/027,043

(22) Filed: Feb. 20, 1998

Related U.S. Application Data

(60) Provisional application No. 60/038,759, filed on Feb. 21,

1997.

4,054,513 * 10/1977 Windle 209/223.1

4,214,984 * 7/1980 MacElvain 209/214

4,236,640 12/1980 Knight 209/587

4,277,329 * 7/1981 Cavanagh 209/223.1

4,294,690 * 10/1981 Kollenz 209/214

4,324,577 * 4/1982 Sepehri-Nik 209/214

4,341,744 * 7/1982 Brison 423/206

4,363,722 12/1982 Dresty, Jr. et al. 209/3

4,375,407 * 3/1983 Kronick 209/8

4,375,454 * 3/1983 Imperto et al. 209/214

4,388,179 6/1983 Lewis 208/177

4,512,879 4/1985 Attia et al. 209/3

4,609,109 * 9/1986 Good 209/223.1

4,668,591 * 5/1987 Minemura et al. 209/223.1

4,737,294 * 4/1988 Kukuck 209/223.1

4,772,383 * 9/1988 Christensen 209/223.1

4,781,298 * 11/1988 Hemstock et al. 209/214

4,814,151 * 3/1989 Beuke 423/206

4,874,508 10/1989 Fritz 209/214

4,902,428 * 2/1990 Cohen 209/214

4,943,368 7/1990 Gilbert et al. 209/2

5,238,664 * 8/1993 Frint et al. 423/206.2

(List continued on next page.)

Primary Examiner-Donald P. Walsh

Assistant Examiner-Daniel K Schlak

(74) Attorney, Agent, or Firm---8heridan Ross Pc.

Under 35 U.S.c. 154(b), the term of this

patent shall be extended for 0 days.

(54) BENEFICIATION OF SALINE MINERALS

(75) Inventors: Rudolph Pruszko, Green River, WY

(US); Roland Schmidt, Lakewood;

Dale Lee Denham, Jr., Arvada, both of

CO (US)

( *) Notice:

(58) Field of Search 209/3, 4, 7, 9,

209/10, 11,214,218,223.1,225,226,

227,908

U.S. PATENT DOCUMENTS

References Cited

(57) ABSTRACT

Processes for purification of saline minerals using magnetic

separation are disclosed. In particular, saline minerals can

include trona, borates, potash, sulfates, nitrates and chlorides.

The magnetic separation can include high intensity

magnetic separation which can be conducted at greater than

about 20,000 Gauss and up to greater than about 50,000

Gauss. Other embodiments of the invention include calcination

of a saline mineral in an inert atmosphere or in an

oxygen-containing atmosphere at a high temperature prior to

magnetic separation. A further embodiment of the invention

includes pre-alignment of particles on a surface to align the

particles of high magnetic force during a magnetic separation

step. Also disclosed are various embodiments of magnetic

separation which include subjecting an ore to a preliminary

magnetic field prior to magnetic separation.

8 Claims, 9 Drawing Sheets

Uhlig.

Koren 209/223

Cavanagh et al. 241/24

Haseman .. 241/24

Laurila 209/214

Mayer et al. 209/111.8

Fraas 209/214

Coglaiti 209/12.2

Seglin et al. 23/63

Lee et al. 209/8

Sproul et al. 423/206.2

Frangiskos 209/3

Boom et al. 209/39

Noll 209/214

3/1921

5/1955

6/1961

2/1962

4/1966

10/1966

5/1968

9/1970

4/1972

1/1975

3/1975

2/1976

6/1976

* 11/1976

1,371,825

2,708,034

2,990,124

3,022,956

3,246,753 *

3,276,581

3,382,977 *

3,528,766 *

3,655,331 *

3,860,514

3,869,538 *

3,936,372 *

3,966,590

3,990,642

(56)

10

Feedstream/

:~ ~16__26

~24

US 6,173,840 Bl

Page 2

U.S. PATENT DOCUMENTS

5,470,554 * 11/1995 Schmidt et al. 423/206.2

5,651,465 * 7/1997 Schmidt et al. 209/12.2

5,736,113 * 4/1998 Hazen et al. 423/206.2

5,911,959 * 6/1999 Wold et al. 423/206.2

* cited by examiner

u.s. Patent Jan. 16,2001 Sheet 1 of 9 US 6,173,840 Bl

- ~ ro

en •

-..Q...-.). (!) 0 0 -c -lJ-.-. <D

LL

r- -c -c J-+--+---I---l-l--+---t---t----t-----j

c: Q)

:::J ....... o u '- ro

0> '-

~u.....c....

ro :::J

..c en

0 co CD """ N 0 N """ CD co 0

0 0 0 0 ~ ...- a a 0 0 a 0 0 0 a a a0 aa a0 a0 a0 a0 a a a a a I I I I I

(nwa) UOlleZ!lau6eV\l

Na

I

"a""I

u.s. Patent Jan. 16,2001 Sheet 2 of 9 US 6,173,840 Bl

Na

-..

ro C'\I

00

Q.) • --- (!) 0 -- c:i "'0 """-

Q.) LL u..

NaI

"'0 "'0 C Q.)

:::::J --- .0... ruo 0) ....

~u..-c--

ro :::::J ..cOO -.::t

I- aI

0 co (.0 -.::t N 0 N -.::t (.0 co 0

0r- o 0 0 0 0 0 0 0 0 ~

0 0 0 0 0 0 0 0 0 0 0

a a a a a a 0 a a a a I I I I I

(nwe) uOneZlleu6eV\l

u.s. Patent Jan. 16,2001 Sheet 3 of 9 US 6,173,840 Bl

..--. ro

00 (\j (],) --- 0 -- •

d "'C <!> (],) -- u.. LL

N

d

I

'"C c: "'C Q)

~ 0 -u--

e~n ro ~

...:::.:::: u..-Q-- , ro ..q ..cO:O::J dI

N ..q CD ex:> 0

.0.- ex:> CD ..q N 0 0 0 0 0 ..- a 0 0 0 a 0 0 a a a a 0 0 0 0 0 0 0 0 d 0 d d d d d d I I I I I

(nW8) UO!leZll8UBelJ\l

u.s. Patent Jan. 16,2001 Sheet 4 of 9 US 6,173,840 Bl

\

~

~

\

-ro

en ~

Q) ...... • 0 - c::i -c (!)

Q) """-

LL ll.

N

o

I

Naa

c::i

aa

a

c::i

Nao

c::i

I

oo;:t

oo

c::i I

u.s. Patent Jan. 16,2001 Sheet 5 of 9 US 6,173,840 Bl

\

'\

'"~

~

~""""\

,

a CX) CD "'¢ N a N "'¢ CD CX) a

...... a a a a a a a a a ......

a a a a a a a a a a 0

a a a a a 0 0 ci ci 0 ci

I I I I I

(nwa) UOneZllauBe1"J

...--..

ro

..eQ.n.). lC')

a ....- .

a ""0 (!)

Q) -- u.. u...

Na

I

"'¢ aI

u.s. Patent Jan. 16,2001 Sheet 6 of 9 US 6,173,840 Bl

N

o

-CU

..CC.J.D.) <0

~ --- •

0 ""C <!>

CD -- i.L LL

NoI

""C ""C C CD :::J ...... e c..:>

ro C) '-

~ ......

c..:> .c

ro :::J

.c CJ)

I

0 co c.D oo:::t N 0 N oo:::t

........ 0 0 0 0 0 0 0

0 0 q q 0 0 0 0

0 0 0 0 0 0 0 0

I I

(nW8) UOll8Z!l8u5ev-J

c.D oooI

co ooo

I

oo:::t

ciI

o........ ooI

u.s. Patent Jan. 16,2001 Sheet 7 of 9 US 6,173,840 Bl

1

-c-c

C Q) :::J ......... V o (.)

L- CO

0) L-

~ .........

(,,)..0

co :::J

..0 (J)

~

...-

co ~

(J)

Q) ......... •

0 -- -c C!)

Q) u: LL

~

I

LO

~ooo

o

~ooa

LO oooo o

oooa

LO oooa

I

o

~oq9

N

I

LO

~ooa

I

u.s. Patent Jan. 16,2001 Sheet 8 of 9 US 6,173,840 Bl

~I'--

---...,~

J

N

c:i

N

c:i I

CD ooo

c:i

oo::t ooo

c:i

Nooo

c:i

oooo

c:i

Nooo

c:i

I

oo::t ooo

c:i

I

CD ooo

c:i

I

(nwe) UOneZlleu6eV\J

u.s. Patent Jan. 16,2001

o

~\

Ero

Q)

..'.-...

CJ)

-C

Q)

Q)

LL

Sheet 9 of 9

c.o

N

o

N

US 6,173,840 Bl

•

Q) .......

LL

US 6,173,840 B1

2

SUMMARY OF THE INVENTION

One embodiment of the invention is a process for recovering

a saline mineral from an ore which contains saline

mineral and impurities. The method includes separating a

first portion of impurities from the ore by magnetic separation

which includes subjecting the ore to a magnetic flux

density of greater than about 20,000 Gauss. In a preferred

embodiment, the saline mineral selected from trona, borates,

potash, sulfates, nitrates and chlorides, and most preferably

is trona. In other embodiments, the process includes such a

method of magnetic separation of impurities, wherein an

impurity selected from shortite and pyrite are separated. In

these embodiments, at least about 25% of the impurity and

up to more than 75% of the impurity is removed.

In a further embodiment of the present invention, a

process is provided for recovering saline mineral from an

ore which includes saline mineral and impurities. The

method includes calcining the saline mineral in an inert

atmosphere and the separating a portion of the impurities

from the ore by magnetic separation. In a preferred

embodiment, the inert atmosphere is any nonoxygencontaining

atmosphere and can be selected from carbon

dioxide, nitrogen, and water vapor. In an alternative

embodiment, calcination is conducted in an oxygencontaining

atmosphere at a temperature of greater than about

1500 C. and subsequently separating a portion of the impurities

by magnetic separation. A further embodiment of the

present invention includes a process for the purification of

saline minerals in an ore which includes saline mineral and

50 impurities by magnetic separation in a first magnetic field,

wherein the first magnetic field has positions of higher

intensity and lower intensity. The process includes prealigning

the ore on a surface with respect to one or more of

said positions of higher intensity of said first magnetic field

before separation. The process further includes separating a

portion of the impurities from the ore by magnetic separation

in the first magnetic field.

In a further embodiment of the present invention, a

process is provided for removing magnetic impurities from

an ore which contains a saline mineral and magnetic impurities

and has a particle size of less than 100 mesh. The

process includes subjecting the ore to a magnetic flux

density of greater than about 20,000 Gauss whereby magnetic

impurities are separated from the saline mineral. This

process can include recovering greater than about 25 wt. %

of the magnetic impurities and up to greater than about 75

wt. % of the magnetic impurities.

beneficiating trona or soda ash that generally comprises the

step of density separation, and optionally includes electrostatic

separation and/or magnetic separation. U.S. Pat. No.

5,470,554 is incorporated herein by reference in its entirety.

5 The resulting product can have trona or soda ash purities on

the order of 97-98% or more. Although this process works

quite satisfactorily, there is always a desire to reduce the

number of steps, and thereby reduce the costs, associated

with separation processes. In addition, there is always a

10 desire to improve the recovery of beneficiation processes.

As such, it can be appreciated that it would be desirable

to be able to beneficiate trona or soda ash utilizing a low cost

dry beneficiation process to obtain trona or soda ash purities

of about 97-98% or higher and recoveries on the order of

15 90-95%. Accordingly, it is an object of the present invention

to provide a dry process for the beneficiation of trona or soda

ash resulting in higher purities and lower costs than many

existing dry beneficiation processes, and which is simpler

and less expensive than known wet beneficiation processes.

FIELD OF THE INVENTION

CROSS-REFERENCE TO RELATED

APPLICATIONS

BACKGROUND OF THE INVENTION

1

BENEFICIATION OF SALINE MINERALS

The present invention relates to the beneficiation of saline

minerals and, more specifically, trona, by methods of magnetic

separation.

This application claims priority from U.S. Provisional

Application Ser. No. 60/038,759, filed Feb. 21, 1997,

entitled "BENEFICIATION OF SALINE MINERALS."

Many saline minerals are recognized as being commercially

valuable. For example, trona, borates, potash and

chlorides are mined commercially. After mining, these minerals

need to be beneficiated to remove naturally occurring

impurities. 20

With regard to trona (Na2C03.NaHC03 .2H2 0), highpurity

trona is commonly used to make soda ash, which is

used in the production of glass, paper and other goods.

Naturally-occurring trona, or crude trona, is found in large 25

deposits in the western United States, such as in Wyoming

and California, and also in Egypt, Kenya, Botswana, Tibet,

China, Venezuela and Turkey. The largest deposit of trona in

the world is located in the Green River Basin in Wyoming.

Crude trona ore from Wyoming is typically between about 30

80% and about 90% trona, with the remaining components

including shortite, pyrite, quartz, dolomite, mudstone, oil

shale, kerogen, mica, nahcolite and clay minerals.

Many areas of the glass and paper making industries

require soda ash produced from trona having a purity of 99% 35

or more. In order to obtain such a high purity, wet beneficiation

processes have been used. Such processes generally

involve crushing the crude trona, solubilizing the trona,

treating the solution to remove insolubles and organic

matter, crystallizing the trona, and drying the trona which 40

may subsequently be calcined to produce soda ash.

Alternatively, the crude trona can be calcined to yield crude

sodium carbonate, which is then solubilized, treated to

remove impurities, crystallized and dried to produce sodium

carbonate monohydrate or calcined to produce soda ash. 45

While the above-described wet processes can produce with

high purity, they tend to be time consuming and expensive

to perform, and therefore result in a product which is much

more expensive than products produced using known dry

processes.

Not all industries which use trona or soda ash require such

a highly purified form. For example, certain grades of glass

can be produced utilizing soda ash having less than 97%

purity. For this purpose, U.S. Pat. No. 4,341,744 discloses a

dry beneficiation process which is less complex and less 55

expensive than the above-described wet beneficiation process.

Such a dry beneficiation process generally includes

crushing the crude trona, classifying the trona by particle

size, electrostatically separating certain impurities, and

optionally magnetically separating other impurities. Such a 60

process can yield trona or soda ash having up to 95% to 97%

purity with a 60-74% recovery, depending on the quantity

and type of impurities present in the crude trona ore.

There are uses for trona or soda ash, for example in certain

applications in the glass industry, requiring a purity of at 65

least 97%, yet not needing a purity over 99%. To accomplish

this, U.S. Pat. No. 5,470,554 discloses a dry method for

US 6,173,840 B1

3

BRIEF DESCRIPTION OF THE DRAWINGS

FIG. 1 is a graph of the magnetic properties of pyrite from

trona calcined at low temperature.

FIG. 2 is a graph of the magnetic properties of pyrite from

trona calcined at low temperature and washed with hydrochloric

acid.

FIG. 3 is a graph of the magnetic properties of pyrite from

uncalcined trona.

FIG. 4 is a graph of the magnetic properties of pyrite from

an ore body other than trona from Climax, Colo.

FIG. 5 is a graph of the magnetic properties of pyrite from

an ore body other than trona from Vulcan, Colo.

FIG. 6 is a graph of the magnetic properties of pyrite from

an ore body other than trona in Argentina.

FIG. 7 is a graph of the magnetic properties of shortite

from a non-magnetic fraction of uncalcined trona.

FIG. 8 is a graph of the magnetic properties of shortite

from a magnetic fraction of uncalcined trona.

FIG. 9 is an illustration of a design for an open gradient

magnetic separator.

DETAILED DESCRIPTION

The present invention is a dry beneficiation process for

recovering saline minerals from an ore containing the saline

mineral and impurities, and takes advantage of previously

unrecognized characteristics of such ore. As used herein and

in the mineral processing industry, the term "saline mineral"

refers generally to any mineral which occurs in evaporite

deposits. Saline minerals that can be beneficiated by the

present process include, without limitation, trona, borates,

potash, sulfates, nitrates, chlorides, and preferably trona.

The purity of saline minerals within an ore depends on the

deposit location, as well as on the area mined at a particular

deposit. In addition, the mining technique used can significantly

affect the purity of the saline minerals. For example,

by selective mining, higher purities of saline minerals can be

achieved. Regarding the saline mineral trona, deposits are

located at several locations throughout the world, including

Wyoming (Green River Basin), California (Searles Lake),

Egypt, Kenya, Venezuela, Botswana, Tibet, China and Turkey

(Beypazari Basin). For example, a sample of trona ore

from Searles Lake has been found to have from about 50%

to about 90% by weight (wt. %) trona and a sample taken

from the Green River Basin in Wyoming has been found to

have from about 70 wt. % to about 92 wt. % trona. The

remaining 8 wt. % to 30 wt. % of the ore in the Green River

Basin sample comprised impurities including shortite,

pyrite, shale consisting predominantly of dolomite, clay,

quartz and kerogen, and traces of other impurities. Other

samples of trona ore can include different percentages of

trona and impurities, as well as include other impurities.

Particular aspects of the present invention will be

described in the context of the saline mineral trona. Such

descriptions are not intended to limit the general applicability

of the present invention to only trona. Moreover, as

discussed herein, trona is often processed by calcination to

produce soda ash (Na2C03 ). It should be noted that, unless

specifically indicated otherwise, use of the term trona herein

can refer to both trona (i.e., Na2C03.NaHC03 .2H20) and

trona which has been processed by calcination to form soda

ash. In addition, it should be recognized that descriptions of

other processing steps herein (e.g., magnetic separation)

should be construed to include processing of calcined and

uncalcined trona. More particularly, it should be noted that,

4

in preferred embodiments, calcined trona is used for magnetic

separations and density separations described herein.

It has now been discovered that saline minerals, such as

trona, do not have a constant distribution of impurities

5 throughout the saline mineral particles. That is, crushed

saline mineral ore particles have a variety of impurity

contents ranging from no impurities in some particles to

almost total impurities in other particles. It is believed that

this characteristic of saline minerals was not previously

10 recognized. Therefore, until the recognition of the present

invention, there has been no suggestion or teaching to

conduct aspects of the present process. It has been discovered

that the impurities in saline mineral ores, such as trona

containing ores, are typically concentrated in a relatively

15 small percentage of the particles, while the rest of the saline

mineral particles can be of relatively high purity. For

example, under microscopic examination, most of the particles

of crushed trona after calcination are almost completely

white (i.e., substantially white), indicating highly

20 pure trona, while others are distinctly yellowish-brown,

indicating the presence of interstitial impurities. Such particles

can be selectively separated (e.g., manually sorted) to

yield a high purity fraction (e.g., about 97% or more saline

mineral) and a low purity fraction (e.g., less than about 97%

25 saline mineral).

It can be appreciated that, while the above-described

manual sorting process produces a suitable product, the

process can be impractical for high volume separation. The

process of the present invention, however, includes all

30 methods for selectively separating high and low purity

products whether manual or automated. That is, more

commercially-viable processes for separating the high purity

saline mineral from the low purity saline mineral also fall

within the scope of this invention. Thus, the process of the

35 present invention includes a process for selectively separating

a low purity fraction having more than about 3%

impurity content from a high purity fraction having less than

about 3% impurity content. Such separation is based upon

differences in the properties of the particles at the level of

40 impurities present in the particles.

In a preferred embodiment of the present invention, the

step of separating impurities from an ore containing saline

mineral and impurities includes the step of ultra-high magnetic

separation. The ultra-high magnetic separation step

45 subjects the ore to conditions such that materials of different

magnetic susceptibilities (e.g., trona and shale) separate

from each other into a recovered stream and an impurity

stream. In accordance with the present invention, the ultrahigh

intensity of the magnetic flux during the magnetic

50 separation step is at least about 20,000 Gauss, preferably at

least about 30,000 Gauss, and more preferably at least about

50,000 Gauss. It should be noted that 10,000 Gauss is

equivalent to 1 tesla and these units can be used interchangeably.

Such ultra-high magnetic fluxes are in contrast to the

55 above-described standard intensity magnetic separation at

less than about 20,000 Gauss because such standard intensities

are not sufficient to separate particles having both

magnetic (e.g., shale) and non-magnetic (e.g., saline

mineral) components. In order to generate such an ultra-high

60 magnetic flux, superconducting electromagnetic field generators

can be utilized. For example, an open gradient

superconducting magnet can be used. It should be appreciated

that other types of magnetic separators may be used, as

long as the required ultra-high magnetic flux can be

65 obtained. For example, it is recognized that some rare earth

magnets can now achieve a magnetic flux of up to about

28,000 Gauss. With regard to the beneficiation of trona,

US 6,173,840 B1

5 6

intensity separation as described herein. Alternatively, water

can be added to such a stream to dissolve the small crystals

therein. In addition, the liquid medium can be an alcohol or

other suitable medium.

In a further aspect of the present invention, it has been

surprisingly found that during high intensity magnetic

separation, as described above, impurities not previously

recognized as being susceptible to magnetic separation can

be separated. In one such embodiment, this process includes

10 subjecting a saline mineral containing ore to high intensity

magnetic separation, whereby the impurity shortite is separated

from the saline mineral. In another such embodiment,

the impurity pyrite is separated. In this process, at least about

25 wt. % of the impurity is separated, more preferably at

15 least about 50 wt. %, and most preferably at least about 75

wt.%.

As noted above, magnetic separation at under about

20,000 Gauss is known. It has been appreciated, however,

that there are limits on the effectiveness of such processes.

20 It has previously been thought that at 20,000 Gauss the

primary separation is between liberated impurities and trona

containing particles. As noted above, it has now been

identified that impurities in saline mineral are typically not

evenly distributed throughout the saline mineral particles.

25 However, it has been determined that, in performing a

magnetic separation on crushed trona ore using a 20,000

Gauss magnetic field, no appreciable separation or difference

in magnetic susceptibilities between high and low

purity particles occurred. At 23,000 Gauss, an identifiable

30 difference in magnetic susceptibility was noted between the

high purity particles and the low purity particles. In a

subsequent test, a 28,000 Gauss magnetic field was found to

give remarkable separation between the high purity particles

and the low purity particles. The high purity particles were

35 subsequently subjected to density separation at a 2.3 specific

gravity cut-off. The resulting purity of the product was on

the order of about 97%-98%, and the recovery was as high

as about 90%-95%. Therefore, in addition to discovering

that crushed trona ore actually comprises a large percentage

40 of high purity particles, it has also been discovered that a

high purity, high recovery trona product can be obtained by

subjecting crushed trona ore to ultra-high intensity magnetic

separation. (See, for example, Examples 1, 4 and 8.) Such a

process provides significant advantages because acceptable

45 purity levels and recoveries can be achieved without the

significantly greater expense associated with recrystallization

processes. It should be noted that high intensity magnetic

separation processes are more effective at separating

pyrite from trona ore having a wide size fraction (e.g., 6x20

50 mesh or 20x100 mesh) than, for example, density separations

such as air tabling. Therefore, a dry separation process

using only high intensity separation could be more useful

than a dry separation process using density separation when

the desired product must be low in pyrite so long as

55 moderate amounts of shortite can be tolerated. For example,

it is contemplated by the present inventors that some amount

of shortite may be desirable in soda ash in certain

applications, such as the production of glass. Alternatively,

high intensity magnetic separations can be conducted in

60 combination processes which also include density

separations, electrostatic separations or recrystallization

processes.

In a further aspect of the present invention it has been

surprisingly found that saline mineral particles of -100 mesh

65 can be efficiently separated by high intensity magnetic

separation, as described above. It is generally recognized

that conventional magnetic separation for such small partypical

impurities that can be removed during the magnetic

separation step include shale and impure trona with interstitial

dolomite and paramagnetic clay-type materials, which

have higher magnetic susceptibilities than pure trona. In

addition, other impurities may be separated by the present 5

process due to their association with the magnetic impurities.

As noted, any type of high intensity magnetic separator is

suitable for use in the present invention. More particularly,

either dry or wet high intensity magnetic separators can be

used. Dry separation refers to any process in which dry

particles are subjected to a high intensity magnetic field for

separation of magnetic impurities. Wet separation refers to

any process in which magnetic impurities are separated

from, e.g., crystals of a saline mineral in a saturated brine in

a high intensity magnetic field. Alternatively, the wet

medium can include other liquids, such as an alcohol.

Suitable high intensity magnetic separators can be of any

known design. For example, magnetic separators can be of

a type wherein a feedstream is fed in free fall in proximity

to a high intensity magnet so that magnetic particles tend to

migrate toward the magnet and non-magnetic particles do

not. In this manner, as the particles are collected on either

side of a splitter, the magnetic particles will physically

separate from the non-magnetic particles. With particular

regard to FIG. 9, a particular apparatus is illustrated. The

feedstream 10 is fed to a dropoff point 12 in free fall. At the

dropoff point 12, the feedstream is in close proximity to the

magnet 14. As the feedstream 10 falls, the magnetic particles

16 migrate toward the magnet 14 and the non-magnetic

particles 18 do not migrate toward the magnet 14. After the

particles are separated and fall further toward the splitter 20,

the magnetic particles 16 fall on one side of the splitter,

while the non-magnetic particles 18 fall on the other side of

the splitter 20. The horizontal distance between the dropoff

point 12 and the magnet 14 defines the gap width 22. The

horizontal distance between the splitter and a point on the

magnet face which is closest to the arc of the feedstream

defines the splitter gap width 24. The magnet angle 26 is

defined by the angle between the bottom surface of the

magnet and the horizontal. In an alternative high intensity

magnetic separator design for dry separations, particles can

be fed onto a matrix, such as a steel wool or wire mesh

screen matrix in proximity to a high intensity magnet. Such

a matrix can be made of any metal, such that in the presence

of a magnetic flux, the metal can act as a magnet. The metal

can be in any configuration having a high surface area such

as a wool or screen. The magnetic particles in the feed

stream will become attached to the matrix, whereas nonmagnetic

particles will migrate through the matrix and be

removed from the bottom of the matrix. This apparatus

design is particularly well suited for fine particles, such as

feedstreams having a particle size of less than 100 mesh.

In a further apparatus design for use with wet high

intensity magnetic separations, a matrix in a vessel filled

with a liquid is provided. The matrix is subjected to the

magnetic field of a high intensity magnet. The liquid can be,

for example, a saturated brine solution of a saline mineral.

For example, such a liquid can be from a saturated brine

recrystallization process, such as is described in PCT application

PCT/US96/00700, which is incorporated herein by

reference in its entirety. Such a stream can include the entire

size range of crystals generated by the process or can be

generated by separating large crystals from insoluble impurities

and smaller crystals on a size separation basis. The

resulting stream of a saturated brine solution with insoluble

impurities and small crystals can be treated by wet high

US 6,173,840 B1

7 8

density separation effect. For example, it has been found

that, in order to get adequate density separation using an air

table, the particle size distribution ratio should be about 3.0

or less, preferably about 2.8 or less, and more preferably

5 about 2.2 or less.

As discussed above, density separation is conducted by

subjecting the ore to conditions such that materials of

different densities separate from each other. The mineral

stream having materials of varying densities is separated by

10 a rougher pass into a denser and a lighter stream, or into

more than two streams of varying densities. Typically, in the

case of beneficiating trona, the separation is made at a

specific gravity of about 2.3, and trona is recovered in the

lighter stream. The purity of a saline mineral recovered from

15 density separation can be increased by reducing the weight

recovery of the recovered stream from the feed stream. At

lower weight recoveries, the recovered stream will have a

higher purity, but the rougher pass will also have a reduced

yield because more of the desired saline mineral will report

20 to the impurity stream. Such a "high purity" process may be

beneficial in that it requires less subsequent processing (e.g.,

separation) of the ore and, in addition, may be of higher

value because it can be used in other applications where high

purity saline minerals are required.

In an alternative embodiment, the impurity stream from

density separation can go through one or more scavenger

density separation step(s) to recover additional saline mineral

to improve the overall recovery. The scavenger separation

is similar to the above-described density separation

30 step. The scavenger step treats the impurity stream from the

rougher pass and recovers a portion of the saline mineral

therefrom. The recovered scavenger portion is combined

with the above-described recovered stream to increase the

overall recovery from density separation, or recycles it to

35 other steps in the process, with or without further size

reduction.

In a further alternative embodiment, the recovered stream

from the rougher pass density separation can go through one

40 or more cleaning density separation steps to further remove

impurities from the recovered stream and improve the purity

of the final product. The cleaning step is similar to the

above-described density separation process in that impurities

are removed from the stream by density separation. In

45 both scavenging and cleaning passes, the feed stream into

those passes can undergo further size reduction, if desired,

for example, to achieve higher liberation.

With regard to the beneficiation of trona, which, prior to

calcination, has a density of 2.14 and after calcination has an

50 apparent density of about 1.5, impurities that are removed

during the density separation step of the present invention

include shortite, having a density of 2.6, dolomite, having a

density of 2.8-2.9 and pyrite, having a density of 5.0. Each

of these is separable from the trona ore because of differ-

55 ences in density from trona. By practice of the present

invention, of the total amount of shortite, dolomite, pyrite

and, if present, potentially valuable heavy minerals in the

trona ore, the density separation step can remove at least

about 10 wt. % and more preferably, about 50 wt. %, and

60 most preferably, about 90 wt. % of the heavy impurity.

In an alternative embodiment, impurities removed during

the density separation process can be recovered as a product

for commercial use. For example, in the beneficiation of

trona, the impurities removed during the air tabling step can

65 comprise as much as 90% shortite. Such shortite may be

acceptable, for example, for certain applications where it can

be used for neutralization of acids or removal of sulfur from

ticles is not effective. It is believed that static charges on the

particles prevent effective separation between magnetic and

non-magnetic particles. In addition, it is believed that such

small particles do not efficiently separate because of a weak

magnetic force. However, such small particles can be effectively

separated by high intensity magnetic separation. High

intensity magnetic separators using a matrix, such as steel

wool, are believed to be particularly effective for such small

particles. Without intending to be bound by theory, it is

believed that the metal matrix functions to physically break

up associations between magnetic and non-magnetic particles.

In addition, it is believed that the metal matrix is able

to dissipate static charges which otherwise hold such particles

together. In this aspect of the invention, at least about

25 wt. % of magnetic impurities are separated from the -100

mesh particles, more preferably at least about 50 wt. %, and

most preferably at least about 75 wt. %.

Other processes may be utilized to practice the present

invention to selectively separate high and low purity portions

instead of ultra-high intensity magnetic separation. For

example, the process of selectively separating low purity

saline mineral from high purity saline mineral comprise

performing colorimetric separation. More specifically, for

example in the separation of trona, the low purity particles

may be separated based upon their darker color than the high 25

purity particles utilizing an automated colorimetric sorting

process. Such a process may utilize a video imager in

conjunction with appropriately-timed blasts of pressurized

gas to deflect the darker colored particles away from the high

purity particles.

The impurity stream from the selective separation step,

such as ultra-high intensity magnetic separation, can go

through one or more scavenger steps to improve the overall

recovery. The scavenger step recovers a portion of the

impurity stream from the rougher pass through magnetic

separation and combines it with the above-described recovered

stream or recycles it to the process with or without

further size reduction to increase the overall recovery of the

magnetic separation step. Furthermore, the recovered stream

from magnetic separation can go through one or more

magnetic cleaning steps to further remove impurities from

the recovered stream and improve the purity of the final

product.

The present process may further include removing impurities

from the ore containing saline minerals by a density

separation method. Density separation methods are based on

subjecting an ore to conditions such that materials of different

densities physically separate from each other.

Thereby, certain impurities having a different density than

the desired saline mineral can be separated. The density

separation step of the present invention is most preferably a

dry process; however, wet density separation processes,

such as heavy media separation, can be used as well. In dry

density separation processes, the need for processing in a

saturated brine solution, solid/brine separation, and drying

of the product is eliminated. Consequently, dry processes

according to the present invention tend to be cheaper and

less complex than wet processes. Any known density separation

technique could be used for this step of the present

invention, including air tabling or dry jigging.

During such dry separation steps, it is important to

maintain a narrow particle size distribution with a particular

fraction. That is, the ratio of the largest particle within a

fraction of the smallest particle within that fraction should

be relatively small. Without such a small ratio of particle

size distribution, the differences in particle sizes could tend

to dominate the separation process, thereby reducing the

US 6,173,840 B1

9 10

three size fractions of 6 mesh by 20 mesh, 20 mesh by 100

mesh, and minus 100 mesh, the two larger size fractions are

preferably treated using an apparatus in which particles free

fall while subject to a high intensity magnet and are col-

5 lected on either side of a splitter. Such an apparatus is also

known as an open gradient magnetic separator ("OGMS").

The smallest size fraction is preferably treated by a high

intensity magnetic separator having a metal matrix.

In yet another embodiment of the present invention, the

10 ore is dried prior to the separation processes set forth above.

The drying step removes surface moisture from the ore to

better enable the ore to be separated. Drying can be accomplished

by any conventional mineral drying technique,

including rotary kiln, fluid bed or air drying. The ore can be

dried to less than about 2%, and preferably less than about

15 1% surface moisture content. During the drying process, it

is preferred that the saline mineral is not raised to such a

temperature for such a period of time that it is calcined. In

the case of trona, the drying temperature should remain

below about 40 degrees centigrade to avoid calcination.

In still another embodiment of the present invention, a

de-dusting step is added to the basic beneficiation process to

remove fines before the selective separation step (e.g.,

magnetic separation). Such a de-dusting step can be conducted

before, during or after one or more of the crushing

25 and sizing steps, but preferably before the electrostatic

separation, magnetic separation and density separation

steps. The fines produced during the processing of trona are

relatively high purity trona and are useful in several industrial

applications. For example, trona recovered by

30 de-dusting can have a purity of greater than about 94%,

preferably greater than about 96% and more preferably

greater than about 98%. Fines can be collected in de-dusting

steps by use of a baghouse, or other conventional filtering

device, and sold as purified trona without further processing.

35 In a further aspect of the present invention, the magnetic

separation achieved by any magnetic separation step of the

present invention, including high intensity magnetic separation

and conventional intensity magnetic separation, can

be improved by subjecting the ore that is being processed to

a preliminary magnetic field prior to separation and subse-

40 quently separating a portion of impurities from the ore by

magnetic separation. Without being bound by theory, it is

believed that by subjecting particles being processed to a

preliminary magnetic field before physical separation of

magnetic from non-magnetic particles, the magnetic tractive

45 force on particles during magnetic separation is greater. In

this manner, more efficient separations can be achieved

during magnetic separation steps.

The term "preliminary magnetic field" refers to a magnetic

field to which a feed stream being processed is sub-

50 jected prior to physical separation of magnetic from nonmagnetic

particles. A feed stream being processed can be

subjected to a preliminary magnetic field using conventional

apparatus known to those in the art. For example, a feed

stream can be transported along a conveyor belt and sub-

55 jected to a magnetic field during linear transport on the

conveyor belt. Subsequently, particles will reach the end of

the conveyor belt and drop off of the conveyor belt while

being subjected to the primary magnetic field for separation.

In this embodiment of the present invention, the preliminary

magnetic field typically has a magnetic flux density of

60 greater than about 2000 Gauss, more preferably greater than

about 5000 Gauss, and most preferably greater than about

20,000 Gauss. Further, the step of subjecting particles to a

preliminary magnetic field is conducted for at least about 1

second, more preferably at least about 30 seconds, and most

65 preferably at least about 60 seconds. The positive effect of

a preliminary magnetic field can be further enhanced by

increased temperatures. More particularly, the process is

flue gases. In addition, for some trona deposits, potentially

valuable heavy minerals may be present. Such minerals can

be separated by the method and recovered.

It should be appreciated that the above-identified process

steps could be performed along with other process steps. For

example, such other process steps can include low or standard

intensity magnetic separation, electrostatic separation,

or any other suitable separation technique. In addition, the

above-identified process steps could be performed in any

order. Further, calcination can be conducted at any point in

the sequence of process steps and preferably is conducted

prior to any magnetic or density separation steps.

In a further embodiment of the present invention, the

saline mineral-containing ore can be crushed to achieve

liberation of impurities prior to the separation steps. The

crushing step of the present invention can be accomplished

by any conventional technique, including impact crushing

(e.g., cage or hammer mills), jaw crushing, roll crushing,

cone crushing, autogenous crushing or semi-autogenous

crushing. Autogenous and semi-autogenous crushing are

particularly beneficial because the coarse particles of ore 20

partially act as the crushing medium. Moreover, because

saline minerals are typically soft, these methods are suitable

for use in the present process. In addition, these two crushing

methods allow for the continuous removal of crushed material

and high grade potentially saleable dust.

In general, crushing to smaller particle size achieves

better liberation of impurities and thus improves recovery.

However, if the particle size after crushing is too fine, there

may be adverse effects upon subsequent separation steps. In

addition, over-crushing is not needed for many applications

of the present invention and merely increases the costs

associated with the crushing step. It has been found that

acceptable liberation for the present process can be achieved

by crushing the ore to at least about 6 mesh. Preferably, the

particle size range after crushing is from about 6 to about

100 mesh and, more preferably, from about 6 to about 65

mesh.

In another embodiment of the present invention, the ore is

sized into size fractions prior to the separation steps. Each

size fraction is subsequently processed separately. In

general, the narrower the range of particle size within a

fraction, the higher the efficiency of removal of impurities.

This is particularly true if air tabling is used as a density

separation step, wherein small particle size distribution

ratios are desired. On the other hand, a larger number of

fractions will increase the efficiency, but may increase the

cost of the overall process. The use of from 1 to 10 fractions

has been found to be acceptable. Preferably, the number of

fractions is from 4 to 10 and, more preferably, the number

of fractions is 8. Any conventional sizing technique can be

used for the present process, including screening or air

classification. For dividing into 8 fractions, the fractions

typically have the following particle size ranges: 6 to 8

mesh; 8 to 10 mesh; 10 to 14 mesh; 14 to 20 mesh; 20 to 28

mesh; 28 to 35 mesh; 35 to 48 mesh; 48 to 65 mesh (Tyler

mesh). Utilizing these fractions, the particle size distribution

ratio for each fraction is about 1.42. It should be noted that

a smaller number of size fractions, including only one size

fraction (such as 6 meshx100 mesh or 6 meshxO) or two size

fractions (such as 6 mesh by 20 mesh and 20 mesh by 0), can

be used for high intensity magnetic separations. Without

intending to be bound by theory, it is believed that the effects

of particle size are reduced under high intensity magnetic

separator apparatus designs. Thus, high intensity magnetic

separation can be conducted on a size fraction from 6 or 8

mesh by 20, 65 or 100 mesh.

In a further embodiment, the different size fractions can

be treated with high intensity magnetic separations using

different equipment. For example, in the instance of using

US 6,173,840 B1

11 12

EXAMPLES 1-8

Eight tests were performed on trona-containing ore in

accordance with the present invention. The tests were performed

on samples generated from ore mined from the

Green River Basin in Wyoming. The ore received was

crushed to nominal 50 mesh. The ore was screened into size

fractions, and the 20x35 fraction was used as the supply for

the eight tests. Referring to Table 1, the original 20x35

fraction comprised 94.01% soluble matter (i.e., trona) and

5.99% insoluble matter (i.e., impurities). The 20x35 fraction

was subjected to standard magnetic separation utilizing a

rare earth separator at its maximum intensity of less than

about 20,000 Gauss. The standard magnetic separation step

65 resulted in removal of 3.0% of the weight of the original

sample in a magnetic fraction, and the remaining nonmagnetic

fraction comprised 95.7% trona.

magnetic separation. For example, in a preferred

embodiment, the magnetic separation is conducted by feeding

ore onto a conveyor belt which then transports the ore

toward one end of the conveyor belt. The magnet creating

the first magnetic field is positioned in the rollers at the end

of the belt towards which the ore is transported. In this

manner, there will be one or more positions along the length

of the roller which have higher or maximum intensity of

magnetic force compared to other portions of the roller.

Thus, in order for the ore to be pre-aligned such that it is

primarily contacted with the portion of the roller having a

higher intensity magnetic field, it is necessary for the ore to

be aligned in the direction of travel of the belt in alignment

with the one or more positions of higher intensity. In this

embodiment, the step of pre-aligning can be accomplished

by a variety of means. For example, in the above example in

which an ore feed stream is fed onto a belt which is

transported toward a first end of the belt, pre-alignment can

be accomplished by subjecting the ore, for alignment purposes

only, to a second magnetic field in the vicinity of the

portion of the belt at which the ore is fed onto the belt. In this

manner, as ore particles are fed onto the belt and are settling

to a static position, magnetic particles will tend to migrate

and settle in alignment with one or more magnets placed

under the belt at the position desired for alignment. Thus, as

the ore is subsequently transported toward the end of the belt

toward the first magnetic field for purposes of magnetic

separation, the magnetic particles will be aligned with the

desired position of higher intensity of the first magnetic

field. Alternatively, alignment can be accomplished by

simple mechanical means of feeding the ore onto the belt at

one or more discrete locations across the width of the belt

such that as the belt is advanced, a line of ore is laid down

on the belt. Thus, alignment is accomplished by aligning the

discrete feed discharge point with the one or more positions

of higher intensity of the first magnetic field.

The foregoing process including pre-alignment of ore on

a surface for magnetic separation can be used alone or in

conjunction with other aspects of the present invention.

The foregoing description of the present invention has

been presented for purposes of illustration and description.

Furthermore, the description is not intended to limit the

invention to the form disclosed herein. Consequently, variations

and modifications commensurate with the above

teachings, and the skill or knowledge of the relevant art, are

within the scope of the present invention. The embodiment

described hereinabove is further intended to explain the best

mode known for practicing the invention and to enable

others skilled in the art to utilize the invention in such, or

other, embodiments and with various modifications required

by the particular applications or uses of the present invention.

It is intended that the appended claims be construed to

50 include alternative embodiments to the extent permitted by

the prior art.

conducted at temperatures of at least about 1000 c., more

preferably 1500 c., and most preferably 2000 C.

In a further embodiment of the present invention, a saline

mineral can be calcined prior to magnetic separation. More

particularly, in one aspect of this embodiment, the saline 5

mineral is calcined in an inert atmosphere prior to separating

impurities from the ore. In a second aspect of this

embodiment, the saline mineral is calcined in an oxidizing

atmosphere at a temperature of greater than about 1500 C.

prior to separating impurities from the ore. In this embodiment

of the present invention, it has been surprisingly found 10

that by calcination under the conditions identified above

(i.e., an inert atmosphere or an oxidizing atmosphere at high

temperature), the subsequent magnetic separation is more

efficient than in the absence of such calcining conditions.

As used herein, reference to the term "inert atmosphere" 15

refers to a non-oxidizing atmosphere (i.e., an atmosphere

substantially free of oxygen). More particularly, an inert

atmosphere is any non-oxygen containing atmosphere and in

particular, can comprise carbon dioxide, nitrogen, or water

vapor. In a further preferred embodiment, carbon dioxide

used for providing an inert atmosphere for calcination 20

purposes can be carbon dioxide which is recycled from an

exhaust stream from the calcination process. For example, in

the instance of calcination of trona, the byproducts of

calcination include carbon dioxide and water. Thus, the

water can be condensed from the exhaust stream and the 25

carbon dioxide recycled for use as the calcination gas, for

example, in a fluidizing bed.

When using an inert atmosphere in this embodiment, the

calcination temperatures typically range between about 430

C. and about 4000 c., more preferably between about 1000 30

C. and about 3500 c., and most preferably between about

1500 C. and about 2600 C.

In the aspect of this embodiment of the present invention

in which an oxidizing atmosphere is used during calcination,

the atmosphere most typically includes air but can include

other oxygen containing gases as well. Further, the calcina- 35

tion temperature in this aspect of the invention is at least

about 1500 c., more preferably at least about 2500 c., and

most preferably at least about 5000 C.

Subsequent to the calcination step as described above, the

saline mineral containing ore is then subjected to magnetic 40

separation. Such magnetic separation can include high intensity

magnetic separation as generally described herein, or

conventional intensity magnetic separation as described

herein and otherwise described in the art. In a further

preferred embodiment, the process of calcining saline min- 45

eral in an inert atmosphere or in an oxidizing atmosphere at

a high temperature followed by magnetic separation can also

include the step of subjecting the calcined ore to a preliminary

magnetic field prior to magnetic separation, as generally

described above.

A further embodiment of the present invention includes a

process for the purification of saline mineral by magnetic

separation in an ore comprising saline mineral and impurities.

In this embodiment, the magnetic separation is conducted

in a first magnetic field having positions of higher 55

intensity and lower intensity. The process includes prealigning

the ore on a surface with respect to one or more of

the positions of higher intensity of the first magnetic field

before separation of impurities and separating a first portion

of impurities from the ore by magnetic separation in the first

magnetic field. In this manner, higher efficiency of magnetic 60

separation is achieved because the ore is conducted through

the first magnetic field at the positions of highest magnetic

intensity. Therefore, magnetically susceptible particles are

subject to a higher magnetic tractive force and thereby are

more readily separated.

The manner in which the step of pre-aligning is conducted

will depend, in large part, upon the apparatus used for

US 6,173,840 B1

13 14

TABLE 1

Analysis of Original 20 x 35 Fraction from Trona Ore

Weight Water Insol. Water Soluble

Product

% of % of % of Assay Dist.

Feed Prod. * Spl. ** % Prod. *

Dist.

Spl**

Assay

%

Dist.

Prod.

Dist.

Spl.**

1.3

98.7

100.0

1.3

98.7

100.0

NOTE: The feed to the superconductor was processed with the International Process Systems RE

Belt Magnet, giving the following results:

3.0 3.0 60.3 30.2 30.2 39.7

97.0 97.0 4.31 69.8 69.8 95.7

100.0 100.0 5.99 100.0 100.0 94.01

Magnetic

Non-Mag.

Feed Calc.

*Feed to Separation as 100%

**Original Sample as 100%

The effectiveness of the 28,000 Gauss magnetic separation

in improving trona purity (i.e., compared to only using

20,000 Gauss magnetic separation) can be seen by comparing

the Water Soluble Assay % in the "Non Mag" row (i.e.

before density separation) to the Water Soluble Assay % in

the "Feed Calc" row.

The data generated from the foregoing beneficiation processes

is shown in Table 2. As can be seen from the Table,

the purity of trona in the final product (shown as Water

20 Soluble Assay %-2.3 Float) ranged from 97.20 in Tests 1

and 2 to 98.17 in Test 4. In addition, the recoveries (i.e., the

amount of final product divided by the amount of the

original sample, shown as Weight % of Spl.-2.3 Float) for

the whole process ranged from 67.1 in Test 4 to 95.0 in Test

25 1.

The non-magnetic fraction from the previous step was

then divided into seven (7) samples to be used in eight (8)

tests (test 8 was performed on the output from test 7). Each

of the eight (8) tests included a two-step separation process:

(1) magnetic separation at 28,000 Gauss; and (2) density

separation at 2.3 specific gravity on the non-magnetic fraction

from the previous step. The density separation was

performed with a heavy liquid which simulates density

separation with commercial air tables. The heavy liquid used

was a mixture of acetylene tetrabromide and kerosene.

Each of the first seven tests had essentially identical feed

compositions, and the input to the eighth test was the output

from the seventh test. The major difference between the tests 30

was the depth of the impurity cut. In general, the deeper the

cut, the higher the purity and the lower the recovery.

TABLE 2

Data From Second Series of Super Conducting Magnetic Separations

Feed 20 x 35 Mesh Non-Magnetic Ore

Weight Fe as Fe203 Water Insol. Water Soluble

Test #/ % of % of % of Assay Dist. Assay Dist., Dist. Assay Dist., Dist.

Product Feed Prod. Spl. % % % Prod. Spl. % Prod. Spl.

Test 1

Magnetic 1.0 0.9 1.44 17.1 57.3 13.0 9.1 42.7 0.4 0.4

Non-Mag. 100.0 99.0 96.1 82.9 3.74 87.0 60.7 96.26 99.6 98.3

2.3 Float 98.9 98.0 95.0 0.069 2.80 64.4 44.9 97.20 99.5 98.2

2.3 Sink 1.1 1.1 1.0 90 22.6 15.8 10 0.1 0.1

Feed Calc. 100.0 97.0 0.082 100.0 4.26 100.0 69.8 95.74 100.0 98.7

Test 2

Magnetic 1.3 1.3 1.27 19.7 50.4 15.3 10.7 49.6 0.7 0.7

Non-Mag. 100.0 98.7 95.7 80.3 3.66 84.7 59.1 96.34 99.3 98.1

2.3 Float 99.0 97.7 94.8 0.069 2.80 64.1 44.7 97.20 99.2 98.0

2.3 Sink 1.0 1.0 0.9 90 20.6 14.4 10 0.1 0.1

Feed Calc. 100.0 97.0 0.084 100.0 4.27 100.0 69.8 95.73 100.0 98.7

Test 3

Magnetic 7.3 7.1 0.53 42.5 19.0 32.6 22.7 81.0 6.2 6.1

Non-Mag. 100.0 92.7 89.9 57.5 3.10 67.4 47.1 96.90 93.8 92.6

2.3 Float 99.0 91.8 89.1 0.057 2.25 48.5 33.9 97.75 93.7 92.5

2.3 Sink 1.0 0.9 0.9 90 18.9 13.2 10 0.1 0.1

Feed Calc. 100.0 97.0 0.091 100.0 4.50 100.0 69.8 95.74 100.0 98.7

Test 4

Magnetic 30.3 29.4 0.20 65.1 8.88 60.2 42.0 91.1 28.9 28.5

Non-Mag. 100.0 69.7 67.6 34.9 2.56 39.8 27.8 97.44 71.1 70.2

2.3 Float 99.2 69.1 67.1 0.047 1.83 28.3 19.7 98.17 71.0 70.1

2.3 Sink 0.8 0.6 0.6 90 11.6 8.1 10 0.1 0.1

Feed Calc. 100.0 97.0 0.093 100.0 4.47 100.0 69.8 95.53 100.0 98.7

Test 5

Magnetic 12.0 11.6 0.40 49.5 14.9 41.0 28.6 85.1 10.7 10.5

US 6,173,840 B1

15 16

TABLE 2-continued

Data From Second Series of Super Conducting Magnetic Separations

Feed 20 x 35 Mesh Non-Magnetic Ore

Weight Fe as Fe203 Water Insol. Water Soluble

Test #/ % of % of % of Assay Dist. Assay Dist., Dist. Assay Dist., Dist.

Product Feed Prod. Spl. % % % Prod. Spl. % Prod. Spl.

Non-Mag. 100.0 88.0 85.4 50.5 2.93 59.0 41.2 97.07 89.3 88.2

2.3 Float 99.1 87.3 84.6 0.056 2.17 43.4 30.3 97.83 89.3 88.1

2.3 Sink 0.9 0.8 0.7 90 15.6 10.9 10 0.1 0.1

Feed Calc. 100.0 97.0 0.097 100.0 4.37 100.0 69.8 95.63 100.0 98.7

Test 6

Magnetic 3.5 3.4 0.91 35.3 32.2 50.1 18.2 67.8 2.5 2.4

Non-Mag. 100.0 96.5 93.6 64.7 3.30 73.9 51.6 96.70 97.5 96.3

2.3 Float 99.0 95.5 92.7 0.061 2.43 53.8 37.6 97.57 97.4 96.2

2.3 Sink 1.0 1.0 0.9 90 20.0 14.0 10 0.1 0.1

Feed Calc. 100.0 97.0 0.090 100.0 4.31 100.0 69.8 95.69 100.0 98.7

Test 7

Magnetic 8.0 7.8 0.54 45.5 18.9 35.0 24.4 81.1 6.8 6.7

Non-Mag. 100.0 92.0 89.2 54.5 3.06 65.0 45.4 96.94 93.2 92.0

2.3 Float 99.0 91.1 88.3 0.057 2.20 46.2 32.3 97.80 93.1 91.9

2.3 Sink 1.0 0.9 0.9 90 18.7 13.1 10 0.1 0.1

Feed Calc. 100.0 97.0 0.095 100.0 4.33 100.0 69.8 95.67 100.0 98.7

Test 8

Magnetic 4.4 4.3 0.30 23.8 11.3 17.6 8.0 88.7 4.4 4.0

Non-Mag. 100.0 87.6 84.9 76.2 2.67 82.4 37.4 97.33 95.6 88.0

2.3 Float 99.1 86.7 84.1 0.049 1.88 56.9 25.8 98.14 95.5 87.9

2.3 Sink 0.9 0.8 0.8 90 25.5 11.6 10 0.1 0.1

Feed Calc. 92.0 89.2 0.056 100.0 3.08 100.0 45.4 96.92 100.0 92.0

A summary of the tests results is provided in Table 3. The

Table gives the weight recovery of the overall process using

the original sample as 100% (Weight, %), the amount of

impurities in the final product (% H20 Insol), the amount of

iron as Fe20 3 in the final product (Fe2 0 3 , %), and the

amount of the original trona remaining in the final product

(Trona Dist., %).

TABLE 3

The process of Test #8 exceeds 98% purity, while still

having a recovery greater than 80%. This was accomplished

35 by performing a two-stage ultra-high intensity magnetic

separation. More specifically, the non-magnetic fraction

from test #7 was run through the ultra-high intensity magnetic

separation process a second time. The result is a

process which gives a purity almost as good as the best

results (test #4), with a satisfactory recovery.

40

Non- Distributions Based on 20 x 35 Mesh as 100%*

Summary of Non-Magnetic Product

From Superconducting Magnetic Separations

on 20 x 35 Mesh Non-Magnetic Trona Ore

*Air tabling simulated by heavy liquid separations (SG ~ 2.3) on NonMag.

**Non-Magnetic was not treated with heavy liquid.

***Calculated assay of calcined product based on assay of water insoluble

residue.

EXAMPLE 9

This example demonstrates that both pyrite and shortite

are magnetic.

Six examples of pyrite identified as P-l through P-6 and

two samples of shortite identified as S-1 and S-2 were

evaluated for magnetic susceptibility. A description of the

samples is provided below in Table 4.

TABLE 4

Pyrite From trona calcined at 1500 C.

Pyrite from trona calcined at 1500 C. and washed with

hydrochloric acid

Pyrite from uncalcined trona

Pyrite from an ore other than trona from Climax, Colorado

Trona from ore other than trona from Vulcan, Colorado

Pyrite from an ore other than trona from Argentina

Shortite from a non-magnetic fraction of uncalcined trona

Shortite from a magnetic fraction from a rare earth

magnetic separation of uncalcined trona

P-l

P-2

P-3

P-4

P-5

P-6

S-l

S-2

45

60

50

55

Weight, % H20 Fe20 3 , Trona Dist.,

% Sol*** %*** %

97.0 95.69** 0.09* * 98.7

95.0 97.20 0.069 98.2

94.8 97.20 0.069 98.0

89.1 97.75 0.057 92.5

67.1 98.17 0.047 70.1

84.6 97.83 0.056 88.1

92.7 97.57 0.061 96.2

88.3 97.80 0.057 91.9

84.1 98.14 0.049 87.9

Feed

Test #1

Test #2

Test #3

Test #4

Test #5

Test #6

Test #7

Test #8

Magnetic

From:

As can be seen from the values in Table 3, test #4 resulted

in excellent purity (98.17%), which is uncharacteristic of

most dry separation processes, while achieving moderate

recovery (67.1 %). Test #1 resulted in outstanding recovery

(95.0%) while still achieving a purity (97.2%) in excess of

97%. These two tests illustrate the excellent purities that can

be achieved by practicing the present invention.

The samples were all less than 1 mm in diameter. The

testing was done on a vibrating sample magnetometer having

a maximum field of 12 tesla. All data were gathered at

room temperature, with a time constant of 0.3 seconds and

65 ramping the magnetic field at 20 Oersted/sec. (to 0.4 tesla)

or 150 Oersted/sec. (to 2 tesla). Other than for strongly

magnetic samples (such as P-5), an appropriate background

US 6,173,840 B1

18

TABLE 7

Not Calcined in C02 at:

5 Calcined 1500 C. 3000 C. 4500 C. 600 0 C.

Water Insoluble 6.25 5.95 5.84 4.42 2.34

Assays - Non Mag.

Water Soluble 93.8 94.1 94.2 95.6 97.7

Assays - Non Mag.

10 Total Iron Assays 0.168 0.177 0.186 0.057 0.026

as Fe - Non Mag.

subtraction was performed. For the measurements on

samples P-5 and S-2, the materials were weighed and

wrapped with PTFE tape which was then formed into an

approximately spherical ball before packing into the sample

holder. The resulting ball of material was approximately 5

mm in diameter. The other samples, and also sample P-5,

were weighed into gelatin capsules and packed down with

cotton wool. The capsule was then locked into a sample

holder for measurement. The results of these tests are shown

below in Table 5 and in FIGS. 1-8. As can be seen from the

results, the magnetic properties of the samples varied from

diamagnetic through paramagnetic to weakly ferromagnetic.

17

TABLE 5

SUSCEPTI- SATURATION

MASS BILITY MOMENT

SAMPLE (g) emu/g. tesla emu/G. PROPERTY

Pl 0.1417 0.0128 paramagnetic

P2 0.1480 0.0038 paramagnetic

P3 0.1215 0.020 paramagnetic

P4 0.1135 0.032 ferromagnetic

P5 0.1263 0.058 ferromagnetic

(capsule)

P5 0.1777 0.060 ferromagnetic

(tape)

P6 0.1788 0.0056 paramagnetic

Sl 0.1357 0.00031 diamagnetic

S2 0.0784 0.0062 ferromagnetic

with hysteresis

EXAMPLE 10

The foregoing results illustrate that at higher temperatures

15 of calcination, significantly improved results in magnetic

separation is attained.

EXAMPLE 11

20 This example illustrates magnetic separation with high

intensity magnetic separation of impurities from calcined

trona which had previously been treated by two passes of

over a rare earth magnetic separator.

The initial product was prepared by calcining trona and

25 passing the calcined product over a rare earth magnetic

separator to yield magnetic fraction and a non-magnetic

fraction. The non-magnetic fraction was again passed over a

rare earth magnetic separator to yield a magnetic fraction

and a non-magnetic fraction. The non-magnetic fraction

30 from the second pass was used as the initial feed for this

experiment. The feed was tested using an OGMS superconducting

magnet set at 2 tesla. Four runs were conducted,

varying the feed rate, magnet angle and feed gap. The

parameters for each run are listed below in Table 8.

35

TABLE 9

Feed Water Insoluble Water Soluble Fe as Fe2 0 3

TABLE 8

Run Feed Rate Magnet Angle Feed Gap

Number (tph/m) (degrees) (em)

1 2.5 5 1

2 10 5 1

3 10 15 1

4 10 15 0.7

The magnetic and non-magnetic portions from each of

runs 1-4 were then analyzed for water insoluble and water

soluble contents, as well as for iron. In addition, each of the

non-magnetic and magnetic fractions from runs 1-4 were

examined to determine the mineralogy of each of the

samples. The results of the analytical testing and mineralogy

are shown below in Tables 9 and 10.

40

55

This example illustrates the effect of calcination temperature

on subsequent magnetic separation of impurities from

trona ore.

Trona ore was treated, in both air and in CO2 , by

calcination at 1500 c., 3000 c., 4500 c., or 6000 C. The trona

ore was treated by magnetic separation. A control was run on

trona with no calcining. Magnetic separation was conducted 45

on a rare earth roll magnet at about 20,000 Gauss. The

magnetic and non-magnetic fractions were then assayed for

water insoluble content (i.e., impurities) and for water

soluble content (i.e., sodium carbonate values). The magnetic

and non-magnetic fractions were also assayed for total 50

iron. The results of these experiments are shown below in

Table 6 (Calcination in Air) and Table 7 (Calcination in

CO2 ). All separations were done at same RPM and splitter

settings.

TABLE 6 Dist., Assay Dist.

Desc. % % %

Not Calcined in Air at:

Feed Sample 3.91

Calcined 1500 C. 3000 C. 4500 C. 600 0 C. 60

Run 1, 97.2 3.41 82.6

Non Mags

Water Insoluble 6.25 4.93 4.67 3.43 2.34 Run 1, Mags 2.8 24.99 17.4

Assays - Non Mag. Run 2, 91.1 3.16 75.2

Water Soluble 93.8 95.1 95.3 96.6 97.7 Non Mags

Assays - Non Mag. Run 2, Mags 8.9 10.58 24.8

Total Iron Assays 0.168 0.164 0.153 0.046 0.030 Run 3, 97.1 3.36 86.2

as Fe - Non Mag. 65 Non Mags

Run 3, Mags 2.9 17.94 13.8

Assay Dist. Assay Dist.

% % % %

96.09 0.114

96.59 97.6 0.083 86.1

75.01 2.2 0.472 13.9

96.84 91.7 0.159 87.0

89.42 8.3 0.242 13.0

96.62 97.5 0.079 87.0

82.06 2.5 0.394 13.0

US 6,173,840 B1

19

TABLE 9-continued

Feed Water Insoluble Water Soluble Fe as Fe20 3

5

Dist., Assay Dist. Assay Dist. Assay Dist.

Desc. % % % % % % %

Run 4, 97.0 3.29 83.7 96.71 97.5 0.104 86.1

10

Non Mags

Run 4, Mags 3.0 20.78 16.3 79.22 2.5 0.459 11.9

20

Mineralogy

TABLE lO-continued

Essentially all fine tan shale, minor

Shortite (less Shortite than Run 2, non-mags,

also some fine), Searlesite and dark brown

shale. Trace pyrite. Increase in dark brown

compact shale (15 to 10%)

Description

Run 4

Mags

25

This example illustrates the magnetic separation of impurities

from either trona or calcined trona using an OGMS.

Seventeen runs were conducted using a feedstream of

either trona or calcined trona calcined at 1500 C. The

30 feedstreams were either a size fraction of 6 mesh by 20 mesh

or 20 mesh by 100 mesh. The experimental setup varied the

gap width and the splitter gap width. The gap width is the

horizontal distance between the drop-off point of the feed

and the magnet. The splitter gap width is the horizontal

distance between the splitter and a point on the magnet face

35 which is closest to the arc of the feedstream. The separations

were conducted at a magnetic field strength of 4 tesla, with

a magnet angle of 11o.

The percentage of pyrite in the feed was calculated and,

for some runs, determined by analysis. In addition, the

40 percent pyrite in the non-magnetic fraction was analyzed. In

addition, the weight-percent recovery in the non-magnetic

fraction was calculated, as was the weight-percent recovery

of soluble material in the non-magnetic fraction.

The various gap and splitter gap widths as well as the

experimental results are shown below in Table 11.

The foregoing results demonstrate that at a magnet~c

strength of 2 tesla, an OGMS superconducting magnetlc

separator improved the purification of a non-magnetic fraction

from a rare earth magnetic separator with a high

recovery. Moreover, the mineralogical evaluation of the

15 sample showed that even at 2 tesla, some pyrite and shortite

showed up in the magnetic fraction. The use of high intensity

magnetic separation provided improved separation of impurities

compared to the use of rare earth magnetic separation

with the same size fraction and magnetic strength. The use

20 of an OGMS superconducting magnetic separator has the

advantage of eliminating centrifugal forces found with conventional

roll type magnetic separators. Centrifugal forces

can cause particles to report to the far side of the splitter due

to mass considerations rather than magnetic susceptibility.

EXAMPLE 12

Essentially all fine tan shale, minor

Shortite (less Shortite than Run 2, non-mags,

also some fine), searlesite and dark brown

shale. Trace pyrite.

Essentially all fine tan shale, minor

Shortite (less Shortite than Run 2, non-mags,

also some fine), Searlesite and dark brown

shale. Trace pyrite.

Mostly tan shale, subordinate dark brown

shale. Minor Shortite frequently inter grown

with dark brown shale, but also liberated.

Minor to trace northupite, fine grained

pyrite frequently inter grown with dark brown

shale. Trace Searlesite.

Essentially all fine tan shale, minor

Shortite, Searlesite and dark brown shale.

Trace pyrite.

Essentially all fine tan shale, minor

Shortite (less Shortite than Run 2, non-mags,

also some fine), Searlesite an dark brown

shale. Trace pyrite.

Essentially all fine tan shale, minor

Shortite (less Shortite than Run 2, non-mags,

also some fine), Searlesite and dark brown

shale. Trace pyrite.

Essentially all fine tan shale, minor

Shortite (less Shortite than Run 2, non-mags,

also some fine), Searlesite and dark brown

shale. Trace pyrite. Increase in dark brown

compact shale (15 to 10%)

Essentially all fine tan shale, minor

Shortite, Searlesite and dark brown shale.

Trace pyrite.

TABLE 10

Mineralogy

Run 1

Mags

Description

Run 1

Non Mags

Run 2

Non Mags

Run 3

Non Mags

Feed Sample

Run 3 Mags

Run 4

Non Mags

Run 2

Mags

TABLE 11

% Fe20 3 NM%

in feed Soluble

Size Test as as % Fe20 3 NM%wt H2O GAP SPLITTER

Material Mesh # anal. calc. inNM Rec. Rec. MM* GAPMM

Trona 6 x 20 1 N/A 0.39 0.15 89.7 96 15 16

Trona 6 x 20 2 N/A 0.31 0.19 93.5 99.4 20 18

Trona 6 x 20 3 N/A 0.34 0.11 80.6 89.8 15 32

Trona 6 x 20 4 0.31 0.32 0.1 89.7 97.4 15 16

Trona 6 x 20 5 0.31 0.37 0.12 44.9 49.5 15 25

Trona 6 x 20 6 0.31 0.38 0.13 85.1 93.5 15 22

Trona 20 x 100 7 0.82 0.97 0.2 50.6 56.9 15 24

Trona 20 x 100 8 0.82 0.47 0.23 92.3 95.4 15 21

Trona 20 x 100 9 0.82 0.94 0.35 96.7 96.5 25 18

Cal. 6 x 20 10 N/A 0.41 0.09 67.1 73.8 15 30

Trona

Cal. 6 x 20 11 N/A 0.41 0.11 81.6 87.9 15 25

Trona

Cal. 6 x 20 12 0.31 0.39 0.12 74.5 81.6 15 21

Trona

US 6,173,840 B1

21 22

TABLE ll-continued

% Fe20 3 NM%

in feed Soluble

Size Test as as % Fe20 3 NM%wt H2O GAP SPLITTER

Material Mesh # anal. calc. inNM Rec. Rec. MM* GAPMM

Cal. 6 x 20 13 0.31 0.29 0.14 88.6 95.6 15 25

Trona

Cal. 20 x 100 14 N/A 0.15 0.13 98.7 99.7 15

Trona

Cal. 20 x 100 15 N/A 0.15 0.1 95.7 97.9 15 30

Trona

Cal. 20 x 100 16 0.82 0.91 0.22 79.7 88.3 15 16

Trona

Cal. 20 x 100 17 0.82 1.1 0.24 86.6 94.2 15 15

Trona

The samples from each of the runs were weighed and

analyzed for insoluble material. The insoluble material was

analyzed by microscopic examination and by chemical

analysis. The analytical results for this example are shown in

Tables 13 and 14. These test results show that using high

intensity magnetic separation with a metal matrix makes

separations of finer size fractions possible. Conventional

technology only permits narrow size ranges to be separated

to a level of purity that was achieved with use of high

intensity magnetic separation in a matrix material using a

large size range (20x100 mesh). Also, the separation of

material of less than 150 mesh is now possible when

conventional rare earth and induced roll magnetic separation

cannot process those size fractions.

35

The next three samples were recovered by reducing the

20 magnetic field from 3 to 2 tesla, from 2 to 1 tesla, and from

1 to 0 tesla. A final magnetic sample was recovered by

shaking the unit at 0 tesla.

Run 3 was conducted to determine whether a second pass

through the magnetic separator would improve the purity of

25 the non-magnetic fraction. A feedstream of about 150 g was

used.

Run 4 was similar to Run 2, except that calcined trona was

used instead of trona. In addition, instead of ten portions of

100 g, Run 4 included five samples of 160 g. Further, the

30 magnetic samples included a division of the 5-3 tesla sample

into a 5-4 tesla and a 4-3 tesla sample.

Run 5 was conducted to confirm the results obtained from

Run 4 and determine repeatability of the test method.

Run 6 used the heavy portion of a density separation of

calcined trona. The heavy portion of such a density separation

included a large percentage of shortite, shale and pyrite.

Thus, the feed material is enriched in these impurities. A

feedstream of 200 g of this material was used. However, the

40 matrix became blocked as a result of the coarse nature of the

feed material.

Run 7 repeated Run 6 except that a higher frequency on

the vibrator was used to allow all of the feed material to pass

through the matrix.

Run 8 repeated Run 7 but less feed material (i.e., 100 g of

feed material) was used. After the first pass, the magnetic

fraction was removed from the matrix before running the

non-magnetic fraction through for a second pass.

Run 9 was conducted to evaluate the effect of magnetic

separation on very fine material. Due to the poor flow

characteristics of this feed material, the matrix became

blocked.

TABLE 12

Run Size Range

Number Type Material (Tyler Mesh)

1 T-50 Calcined Trona 100 x 150

2&3 T-50 Trona 20 x 150

T-50 Calcined Trona 20 x 150

6,7 & 8 Air Table Heavies Calcined Trona 28 x 35

9 T-50 Calcined Trona 100 x 0

These results show a separation using high intensity magnetic

separation, such as OGMS, can, with a wide size

fraction (e.g., 6x20 mesh or 20x100 mesh), produce equal or

better purification when compared to conventional magnetic

separation using multiple narrow size factions (e.g., lx8

mesh, 8xlO mesh, lOx20 mesh, etc.).

EXAMPLE 13

The feedstream was introduced at a feed rate of 25 cm3 Is. 45

The magnetic field was set at 5 tesla. The matrix material in

this test was an expanded metal matrix having a matrix size

of Y4 inch. Non-magnetic material exited the bottom of the

unit while the magnetic fraction was held in the matrix.

Run 1 was conducted to determine the effect of vibration 50

on the flow of material through the magnetic separator. The

frequency of a vibrator of the matrix was varied from 40 HZ

to 25 HZ, and then 10 HZ. Approximately 100 g of feed was

fed through at each frequency setting. The non-magnetic

fraction from each run was collected and the final magnetic 55

fraction from the total of the three settings was also collected.

Run 2 was conducted to evaluate the capacity of the

matrix and how the purity of the non-magnetic fraction was

affected as the matrix was loaded up with a magnetic 60

fraction. The magnetic separator was fed 100 g of feedstream

at a time until 1000 g had been run through the matrix

without removing any magnetic fraction from the matrix.

After the last 100 g had been run through the matrix, the

magnetic fraction was removed from the matrix by ramping 65

down the magnetic coil in tesla increments. The first sample

was produced by reducing the field from 5 tesla to 3 tesla.

This example illustrates the use of magnetic separation of

impurities from soda ash or trona using a superconducting

magnet with a metal matrix to remove impurities from a dry

feedstream.

Nine test runs were conducted in this experiment. The

feed material for each test run is described below in Table

12.

TABLE 13

Analytieal Test Results on a Soda Ash Basis

Water

Sample Feed Insoluble, (%) Water Soluble, (%) Fe as Fe20" (%) Ca as CaO, (%) Mg as MgO, (%) K as K2 0, (%) Al as A120" (%) Si as Si02 , (%) Total S as S, (%)

# Description Dist. % Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist.

Calcined Trona

la Run 1, Feed 3.06 96.94 0.115

N~

Sample

Ib Run 1, 40 HZ 25.6 1.67 14.1 98.33 25.9 0.024 5.4

Non Mags

Ie Run 1, 25 HZ 30.1 1.74 17.3 98.26 30.5 0.026 6.9

Non Mags

Id Run 1, 10 HZ 40.3 1.82 24.3 98.18 40.8 0.029 10.1

Non Mags

Ie Run 1, Mags 2.8 46.40 43.4 53.60 1.6 2.960 72.4

If Run 1, Mags 1.2 2.02 0.8 97.98 1.2 0.115 5.3 0.022 e Cleanout

4a,5a Runs 4 and 5 6.22 93.78 0.153 1.06 0.61 0.21 0.081 C/J

Feed Sample vO\

4b Run 4, 1st Non 17.8 2.82 7.4 97.18 18.6 0.080 8.4 0.59 0.17 0.04 f-l.

Mag -..l

W 4e Run 4, 2nd Non 18.4 2.99 8.1 97.01 19.2 0.059 6.4 00 Mag ~

4d Run 4, 3rd Non 18.3 3.11 8.4 96.89 19.0 0.059 6.4 0

Mag 4e Run 4, 4th Non 18.3 3.20 8.7 98.80 19.0 0.068 7.3 OJ f-l.

Mag

4f Run 4, 5th Non 18.2 3.48 9.4 96.52 18.8 0.077 8.2

Mag

4g Run 4, Mag 0 1.1 35.26 5.7 64.74 0.8 1.128 7.2 4.23 3.67 1.39 2.10 10.51 0.681

Tesla Shake

4h Run 4, 3.7 58.86 31.8 41.14 1.6 1.672 36.1 6.89 6.59 2.58 0.854

Mag 1-0 Tesla

4i Run 4, 2.0 42.26 12.3 57.74 1.2 1.069 12.4 5.03 4.48 1.80 0.562

Mag 2-1 Tesla

4j Run 4, 0.9 54.96 7.1 45.04 0.4 1.292 6.6 6.87 5.25 2.02 0.747 N

Mag 3-2 Tesla ~

4k Run 4, 1.1 5.74 0.9 94.26 1.1 0.148 0.9 0.90 0.44 0.15 0.093

Mag 4-3 Tesla

41 Run 4, 0.3 4.25 0.2 95.75 0.3 0.060

Mag 5-4 Tesla

5b Run 5, Non Mag 88.8 2.94 41.1 97.06 92.0 0.056 31.4

5e Run 5, Mag 11.2 33.33 58.9 66.67 8.0 0.977 68.6

6a,7a, Runs 6, 7, 8 40.48 59.52 0.963 8.34 3.04

8a Feed Sample

6b Run 6, Non Mag 28.2 23.01 16.2 76.99 36.2 0.235 7.3 7.64 27.2 0.34 3.2

6e Run 6, Mag 71.8 46.67 83.8 53.33 63.8 1.176 92.7 8.03 72.8 4.01 96.8

7b Run 7, Non Mag 66.9 24.39 40.1 75.61 85.2 0.249 17.8 8.20 66.6 0.33 7.5

TABLE 13-continued

Analytical Test Results on a Soda Ash Basis

Water

Sample Feed Insoluble, (%) Water Soluble, (%) Fe as Fep" (%) Ca as CaO, (%) Mg as MgO, (%) K as Kp, (%) Al as Alp" (%) Si as SiOh (%) Total S as S, (%)

# Description Dist. % Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist.

7c Run 1, Mag 33.1 73.43 59.9 26.57 14.8 2.313 82.2 8.30 33.4 8.30 92.5

8b Run 8, Non Mag 59.2 22.43 33.7 77.57 75.7 0.185 11.3 7.49 0.29

after 2nd Pass

8c Run 8, Mag after 34.4 70.99 62.1 29.01 16.5 2.194 78.4 7.95 7.88 N

1 Pass

Ul

8d Run 8, Mag after 6.4 25.41 4.1 14.59 7.9 1.540 10.2

2nd Pass

9a Run 9, 93.4 8.37 95.9 91.63 93.2 0.187 96.8

Feed Sample

9b Run 9, 6.6 5.08 4.1 94.92 6.8 0.087 3.2

Non Mag

Trona ---

2a,3a Runs 2, 3 8.34 91.66 0.221 1.47 0.66 0.23 0.35 1.89 0.147 e

Feed Sample C/J

2b Run 2, 1st Non 8.3 4.17 4.2 95.83 8.6 0.085 3.1 1.07 0.20 0.05 0.08 0.61 0.059 vO\

Mag f-l.

2c Run 2, 2nd Non 8.9 4.06 4.5 95.94 9.3 0.094 3.7 -..l

Mag W

2d Run 2, 3rd Non 9.1 4.19 4.7 95.81 9.5 0.097 3.9 00

Mag ~

2e Run 2, 4th Non 9.1 4.08 4.5 95.92 9.5 0.100 4.0

0

Mag OJ

2f Run 2, 5th Non 9.0 4.29 4.8 95.71 9.4 0.108 4.3 f-l.

Mag

2g Run 2, 6th Non 9.2 4.33 4.9 95.67 9.6 0.113 4.6

Mag

2h Run 2, 7th Non 9.2 4.36 4.9 95.64 9.5 0.116 4.7

Mag

2i Run 2, 8th Non 9.0 4.43 4.9 95.57 9.4 0.117 4.7

Mag

2j Run 9th Non 8.9 4.82 5.3 95.18 9.3 0.142 5.6

Mag N

2k Run 2, 10th Non 8.9 5.26 5.7 94.74 9.2 0.146 5.7 0'1

Mag

21 Run 2, Mag 0 2.6 40.63 12.7 59.37 1.6 1.329 15.0 4.83 3.92 1.54 2.41 12.39 0.825

Tesla Shake

2m Run 2, Mag 0 3.8 57.44 26.9 42.56 1.8 1.660 27.9 6.72 5.80 2.31 3.56 17.52 0.988

Tesla

2n Run 2, Mag 2-1 2.3 33.45 9.4 66.55 1.7 0.937 9.5 3.95 3.17 1.27 1.92 9.93 0.559

Tesla

20 Run 2, Mag 3-2 0.8 15.59 1.5 84.41 0.7 0.536 1.8 0.329

Tesla

2p Run 2, Mag 5-3 0.9 8.85 1.0 91.14 0.9 0.377 1.5 0.199

Tesla

Sample

TABLE 13-continued

Analytical Test Results on a Soda Ash Basis

Water

Feed Insoluble, (%) Water Soluble, (%) Fe as Fep" (%) Ca as CaO, (%) Mg as MgO, (%) K as Kp, (%) Al as Alp" (%) Si as SiOh (%) Total S as S, (%)

# Description Dist. % Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist.

3b

3c

3c

Run 3, Non Mag

after 1 Pass

Run 3, Non Mag

after 2nd Pass

Run 3, Mag after

2nd Pass

15.9

67.9

16.2

4.22 8.5

3.83 32.8

28.90 58.8

95.78

96.17

71.10

16.5

71.0

12.5

0.084

0.077

1.087

5.5

21.7

72.8

0.98

3.53

0.17

2.95

0.05

1.16

0.07 0.51

0.054

0.052

N

-..J

N

QIO

e

C/J

vO\

f-l.

-..l

W

00

~o

OJ

f-l.

29

US 6,173,840 B1

TABLE 14

Mineralogy of Test Samples

30

Sample # Description

Calcined Trona

1a Run 1, Feed Sample

1b Run 1, 40 HZ Non Mags

1c Run 1, 25 HZ Non Mags

1d Run 1, 10 HZ Non Mags

1e Run 1, Mags

1f Run 1, Mags Cleanout

4a,5a Runs 4 and 5

4b Run 4, 1st Non Mag

4c Run 4, 2nd Non Mag

4d Run 4, 3rd Non Mag

4e Run 4, 4th Non Mag

4f Run 4, 5th Non Mag

4g Run 4, Mag 0

Tesla Shake

4h Run 4,

Mag 1-0 Tesla

4i Run 4,

Mag 2-1 Tesla

4j Run 4,

Mag 3-2 Tesla

4k Run 4,

Mag 4-3 Tesla

41 Run 4,

Mag 5-4 Tesla

5b Run 5, Non Mag

5c Run 5, Mag

6a, 7a, 8a Runs 6, 7, 8

Feed Sample

6b Run 6, Non Mag

6c Run 6, Mag

7b Run 7, Non Mag

8b Run 6, Non Mag after

2nd Pass

8c Run 8, Mag after 1 Pass

8d Run 8, Mag after

9a Run 9. Feed Sample

9b Run 9, Non Mag

Trona

2a,3a Runs 2, 3

Feed Sample

2b Run 2, 1st Non Mag

2c Run 2, 2nd Non Mag

2d Run 2, 3rd Non Mag

Mineralogy

Mostly fine shale and shortite, minor to trace sepiolite, northupite, searlesite, fairly abundant tarnished pyrite.

Mostly fine shale and shortite, minor to trace sepiolite, northupite, searlesite. No obvious pyrite

Mostly fine shale and shortite, minor to trace sepiolite, northupite, searlesite. Trace pyrite.

Mostly fine shale and shortite, minor to trace sepiolite, northupite, searlesite. Trace very fine pyrite.

Quite different. Mostly compact but fine tan-greenish shale not powdery like fine shale in other samples. Also,

abundant fine compact dark brown shale. Abundant northupite, minor shortite, trace pyrite and searlesite.

Mostly shartite (60 to 70%) and fine tan shale with subordinate strongly magnetic "rust" particles with fused

appearing surfaces. Minor (1 to 3%) pyrite with highly tarnished surfaces, narthupite, both discrete and admixed

with shale (dolomite) and sepiolite.

Mostly fine tan shale and subordinate shortite and dark brown compact shale (appreciably mare than

in Sample #4b). Minar to trace pyrite (more than Sample #4b) and searlesite.

Mostly fine shale and much coarse shortite. Subordinate to minor dark brown particulate shale. Trace

searlesite and pyrite.

Mostly fine shale and much coarse shortite. Subordinate to minor dark brown particulate shale. Trace

searlesite and pyrite.

Mostly fine shale and much coarse shortite, but less than previous sample. Subordinate to minor dark brown

particulate shale. Trace searlesite and pyrite.

Mostly fine shale and much coarse shortite. Subordinate to minor dark brown particulate shale. Trace

searlesite and pyrite.

Mostly fine shale and much coarse shortite. Subordinate to minor dark brown particulate shale. Trace

searlesite and pyrite.

Virtually all shale, tan more abundant than dark brown. Both contain admixed northupite. Minar sepiotite and

shartite and traces of searlesite, sugary northupite and pyrite both liberated and locked with shale. Pyrite

appears fresh. Possibly more shortite than Sample #4i.

Virtually all shale, tan more abundant than dark brown. Both contain admixed northupite. Minar sepiolite and

shartite and traces of searlesite, sugary northupite and pyrite both liberated and locked with shale.

Pyrite appears fresh with slightly more tarnished pyrite. Possibly less shortite than Sample #4i.

Virtually all shale, tan more abundant than dark brown. Both contain admixed northupite. Minar sepiolite and

shartite and traces of searlesite, sugary northupite and pyrite both liberated and locked with shale. Pyrite

appears fresh.

Virtually all shale, tan more abundant than dark brown. Both contain admixed northupite. Minar sepiolite and

shartlife and traces of searlesite, sugary narthupite and pyrite both liberated and locked with shale. Pyrite

appears fresh.

Majarity is shale (both types) and ± 30% shortite and minor searlesite (more than Sample #4i). Both shales

contain admixed northupite. Also more sepiolite than Sample #4i. Traces of searlesite, sugary

northupite and pyrite both liberated and locked with shale. Pyrite appears fresh.

Majarity is shale (both types) and 40 to 50% shartite and minar searlesite (mare than Sample #4i). Both shales

contain admixed northupite. Also more sepiolite than Sample #4i. Sepiolite conspicuous causing

more tangled up lumps. Traces of searlesite, sugary northupite and pyrite both liberated and locked with shale.

Pyrite appears fresh.

Mostly fine shale and much coarse shortite. Subordinate to minor dark brown particulate shale. Trace searlesite

and pyrite.

Distinctly different from Sample #5b. Predominantly (60 to 70%) tan-greenish compact relatively coarse shale and

and 30 to 40% dark brown compact shale. Minar (2-3%) shortite and trace pyrite, fairly frequently locked with

dark brown compact shale, searlesite and sepiolite.

About 60 to 70% shortite, balance tan-greenish shale (both compact cellular and fine) and dark brown compact

shale and 1% pyrite mostly as liberated cubes, less frequently lock with dark brown shale.

About 90 to 95% shortite, balance mostly fine tan shale, 1% liberated and locked (with shortite) pyrite. Some

pyrite is tarnished. Trace searlesite.

About 60% shale, mostly tan-greenish compact, less dark brown compact, 40% shortite, 1% pyrite.

About 90 to 95% shortite, balance mostly fine tan shale. About 0.5 to 1% pyrite mostly as liberated cubes, less

commonly locked with shortite.

Mostly shartite (90 to 95%), balance mostly fine tan shale. Trace (5 to 1%) pyrite and searlesite.

Mostly compact fairly coarse tan-greenish shale (80%), 10% dark brown compact shale, 10% shortite. 1% pyrite

both relatively coarse liberated cubes, also tarnished fragments and frequently locked with dark brown

compact shale.

Predominantly shartite (80%), subardinate fine shale and northupite and minar pyrite (3 to 5%). The pyrite is

slightly tarnished and is mostly liberated but also frequently locked with shale and shartite.

Mostly fine tan shale and rather fine shortite, subordinate dark brown compact shale. Trace pyrite and

searlesite.

Predominantly shartite (60 to 70%), subordinate fine shale and about 10% strongly magnetic fused appearing

"rust". Minar searlesite, northupite and pyrite (1% ar less). Similar to Sample #1f.

Mostly shartite and shale (both fine tan an particulate dark brown), minor searlesite, narthupite, sepiolite and

pyrite.

Mostly shortite and tan fine shale. Dark brown particulate almost absent. Minor searlesite, northupite, sepiolite

and pyrite. Pyrite reduced compared to Sample #2a, 3a.

Mostly shartite and tan fine shale. Dark brown particulate almost absent, but slight increase over Sample #2b.

Minor searlesite, northupite, sepiolite and pyrite. Pyrite reduced compared to Sample #2a, 3a.

Mostly shartite and tan fine shale. Dark brown particulate almost absent, but slight increase over Sample #2b.

Minor searlesite, northupite, sepiolite and pyrite. Pyrite reduced compared to Sample #2a, 3a.

US 6,173,840 B1

31 32

TABLE 14-continued

Mineralogy of Test Samples

Sample # Description

2e Run 2, 4th Non Mag

2f Run 2, 5th Non Mag

2g Run 2, 6th Non Mag

2h Run 2, 7th Non Mag

2i Run 2, 8th Non Mag

2j Run 2, 9th Non Mag

2k Run 2, 10th Non Mag

21 Run 2, Mag 0

Tesla Shake

2m Run 2, Mag 0 Tesla

2n Run 2, Mag 2-1 Tesla

20 Run 2, Mag 3-2 Tesla

2p Run 2, Mag 5-3 Tesla

3b Run 3, Non Mag after

1 Pass

3c Run 3, Non Mag after

2nd Pass

3d Run 3, Mag after

2nd Pass

Mineralogy

Mostly shartite and tan fine shale. Dark brown particulate almost absent, but slight increase over Sample #2b.

Minor searlesite, northupite, sepiolite and pyrite. Pyrite reduced compared to Sample #2a, 3a.

Mostly shartite and tan fine shale. Dark brown particulate almost absent, but slight increase over Sample #2b.

Minor searlesite, northupite, sepiolite and pyrite. Pyrite reduced compared to Sample #2a, 3a, but possibly

slight increase in pyrite over Sample #2c.

Mostly shartite and tan fine shale. Dark brown particulate almost absent, but slight increase over Sample #2b.

Minor searlesite, northupite, sepiolite and pyrite. Pyrite reduced compared to Sample #2a, 3a.

Mostly shartite and tan fine shale. Dark brown particulate almost absent, but slight increase over Sample #2b.

Minor searlesite, northupite, sepiolite and pyrite. Pyrite reduced compared to Sample #2a, 3a.

Mostly shartite and tan fine shale. Dark brown particulate almost absent, but slight increase over Sample #2b.

Minor searlesite, northupite, sepiolite and pyrite. Pyrite reduced compared to Sample #2a, 3a.

Significant increase in shartite (60 to 70%) and some increase in dark brown particulate shale compared to

Sample

#2i. Minor searlestite, northupite, sepiolite and pyrite. Pyrite reduced compared to Sample #2a, 3a, but

slight increase over Sample #2e.

Significant increase in shartite (60 to 70%) and some increase in dark brown particulate shale compared to

Sample

#2i. Minor searlestite, northupite, sepiolite and pyrite. Pyrite decreased to trace.

Mostly shale (60% tan greenish, now particulate and mostly finer and 40% dark brown particulate), trace shartite,

searlesite, sepiolit3 and pyrite. The maj arity of the pyrite occurs locked in dark brown particulate shale with a

litle more liberated pyrite.

Mostly shale (60% tan greenish, now particulate and 40% dark brown particulate), trace shortite, searlesite,

sepiolite and pyrite. The majarity of the pyrite occurs locked in dark brown particulate shale.

Roughly 1:1 mixture of tan-greenish particulate and dark brown particulate shale. Quite coarse grained. Trace

shartite (liberated), searlesite4 and pyrite mostly locked with dark brown shale and rarely liberated.

Roughly 1:1 mixture of tan-greenish particulate and dark brown particulate shale. Tan-greenish shale more

cellular as though derived from trona interslices. Quite coarse grained. Slightly more shartite (liberated),

searlesite and slightly more pyrite and sepiolite.

Shortite 40%, balance tan-greenish cellular and dark brown particulate shale. Minar pyrite (1 %) and minor to

trace searlesite and sepiolite.

Shortite 70%, balance mostly fine tan-greenish shale. Minar searlesite, northupite, sepiolite and mostly

liberated pyrite (2 to 3%).

Mostly shartite and fine dispersed tan-greenish shale. Dark brown particulate almost absent. Minor

searlesite, northupite, and sepiolite. Trace liberated pyrite.

About 70% compact tan-greenish shale, 25% dark brown compact shale, 3 to 5% shortite, 2 to 3% pyrite,

some as coarse liberated cubes and fragments and frequently finely locked with dark brown compact shale.

Trace searlestite and sepiolite.

EXAMPLE 14

40 TABLE 16

Run Size Range

Number Slurry Type Prescreened (Tyler Mesh 60

1,2 & 3 calcined trona Yes 100 x 150

4 calcined trona No 20 x 100

5 filter cake No 100 x 0

Test Parameters

Magnetic Matrix

Run Feed Rate Field Matrix Matrix Size Diameter

Number (cm3 /s) (tesla) Material (mm) (mm)

1 25 5 Square Wire 2.5 64

2 25 5 Square Wire 1.0 & 1.7 64

3 25 5 Steel Wool 110* 64

4 25 5 Square Wire 2.5 64

5 25 5 Square Wire 1.0 & 1.7 64

*Microns, not millimeters

65

45

The test material was fed into the unit and flowed through

the matrix in a 5 tesla magnetic field. No vibrator of the

apparatus was used. The non-magnetic material exited the

55 bottom of the unit while the magnetic fraction was held in

the matrix. The current was ramped down to 0, reducing the

magnetic field to o. When the magnetic field was at 0, the

matrix was flushed with water to remove any magnetic

material that was still adhering to the matrix and internal

ledges. It was necessary to preheat the magnetic separator

unit and matrix material to prevent crystals from forming in

the matrix. The recovered samples were diluted with water

to remove any crystals that formed during the run and then

filtered on 1 micron filter paper to remove insolubles.

In Run 1, a 2.5 mm square wire matrix was used.

In Run 2, a matrix composed of alternating pieces of 1.7

mm and 1.0 mm square wire material was used.

Feed Material

TABLE 15

The feed material for four test runs of this example was

produced by dissolving about 6,000 g of soda ash prepared

by calcining trona in 4 gallons of warm water. This slurry

was screened at 100 mesh to remove the +100 mesh

50

insolubles. A fifth test run slurry was made by dissolving

filter cake from a sodium carbonate recrystallization process

to make a saturated -100 mesh insolubles slurry. The feed

materials for this example are shown in Table 15.

The test parameters in terms of feed rate, magnetic field and

matrix material are shown in Table 16.

This example illustrates the use of magnetic separation

using a superconducting magnetic separator process having

a metal matrix for capture of particles wherein the feedstream

is a wet slurry.

US 6,173,840 B1

33 34

TABLE 19-continued

Mineralogy

Mineralogy of Test Samples

Essentially all fine tan shale with a small amount

of dark brown shale, traces of searlesite, fine

pyrite, etc. Slight increase in pyrite compared to

Run 1 Non Mag.

Essentially all fine tan shale, traces of

searlesite, fine pyrite, etc.

Essentially all fine tan shale, traces of

searlesite, fine pyrite, etc.

Description

Run 3 Mag

Run 3 Non Mag

10 Run 4

Run 5 Non Mag

In Run 3, the non-magnetic product from Run 2 was used

as the feed. The matrix was changed to a 110 micron steel

wool.

In Run 4, a 2.5 mm square wire material was used as a

matrix. The feed material included the +100 mesh 5

insolubles, that had previously been screened out of the

slurry in Runs 1, 2 and 3. The matrix plugged at the

beginning of the run.

Run 5 included alternating pieces of a 1.7 mm and a 1.0

mm square wire material as the matrix.

The insoluble materials recovered from the various runs

were analyzed by microscopic examination and chemical

analysis. The results of these analyses are provided in Tables

17, 18 and 19.

TABLE 17

Analytical Test Results on an Insoluble Basis

Water insoluble, Water Soluble,

(%) (%) Fe as Fe2 0 3 • (%) Ca as CaO. (%) Mg as MgO. (%) K as K2 0. (%) Total S as S. (%)

Description Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist.

Run 1 45.5 1.660 38.9 13.60 46.0 10.10 39.5 3.60 46.2 0.159 23.3

Non Mag

Run 1 54.5 2.180 61.1 13.30 54.0 12.90 60.5 3.50 53.8 0.436 76.7

Mag

Run 2 64.4 1.870 69.6 13.20 63.8 12.60 73.1 3.75 68.5 0.332 71.6

Mag

Run 3 19.9 1.320 15.2 13.50 20.2 6.89 12.4 3.43 19.4 0.161 10.7

Non Mag

Run 3 15.7 1.670 15.2 13.50 16.0 10.20 14.5 2.70 12.1 0.334 17.6

Mag

Run 4

Run 5 79.8 1.470 68.0 19.40 82.0 7.74 77.1 2.70 79.6 0.363 51.0

Non Mag

Run 5 20.2 2.740 32.0 16.80 18.0 9.11 22.9 2.74 20.4 1.380 49.0

Mag

TABLE 18

Cryo Filter Analytical Test Results on a Soda Ash Basis

Water insoluble, Water Soluble,

(%) (%) Fe as Fe2 0 3 • (%) Ca as CaO. (%) Mg as MgO. (%) Kas Kp. (%) Total S as S. (%)

Description Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist. Assay Dist.

Run 1 3.67 45.5 96.3 90.0 0.061 38.9 0.50 46.0 0.37 39.5 0.13 46.2 0.006 23.3

Non Mag

Run 1 29.09 54.5 70.9 10.0 0.634 61.1 3.87 54.0 3.75 60.5 1.02 53.8 0.127 76.7

Mag

Run 2 19.77 64.4 80.2 8.0 0.370 69.6 2.61 63.8 2.49 73.1 0.74 68.5 0.066 71.6

Mag

Run 3 1.64 19.9 98.4 90.0 0.022 15.2 0.22 20.2 0.11 12.4 0.06 19.4 0.003 10.7

Non Mag

Run 3 1.45 15.7 98.5 2.0 0.024 15.2 0.20 16.0 0.15 14.5 0.04 12.1 0.005 17.6

Mag

55

TABLE 19 TABLE 19-continued

Mineralogy of Test Samples Mineralogy of Test Samples

Description Mineralogy 60

Description Mineralogy

Run 1 Non Mag Essentially all fine tan shale, traces of

searlesite, fine pyrite, etc.

Run 1 Mag Essentially all fine tan shale, traces of

searlesite, fine pyrite, etc.

Run 2 Mag Essentially all fine tan shale, traces of

searlesite, fine pyrite, etc.

65

Run 5 Mag Roughly 1:1 mixture of mostly fine shartite and fine

tan shale and dark brown compact shale in roughly

equal amounts. Possible increase of fine pyrite

compared to other samples. Trace searlesite.

35

US 6,173,840 B1

36

These test results show that the reduction of impurities

was obtained by use of wet high intensity magnetic separation.

This eliminates or reduces the need to remove

insoluble impurities by conventional means such as filtration

from a saturated sodium carbonate solution. It also allows

the removal of these impurities found in trona without the

need to remove sodium carbonate monohydrate first to

prevent loss of crystals in a filter cake or rejection stream.

The foregoing description of the present invention has

been presented for purposes of illustration and description.

Furthermore, the description is not intended to limit the

invention to the form disclosed herein. Consequently, variations

and modifications commensurate with the above

teachings, and the skill or knowledge of the relevant art, are

within the scope of the present invention. The embodiment

described hereinabove is further intended to explain the best

mode known for practicing the invention and to enable

others skilled in the art to utilize the invention in such, or

other, embodiments and with various modifications required

by the particular applications or uses of the present invention.

It is intended that the appended claims be construed to

include alternative embodiments to the extent permitted by

the prior art.

What is claimed is:

1. A process for recovering a saline mineral from an ore

containing said saline mineral and impurities which comprises

shortite, pyrite or mixtures thereof, comprising calcining

said saline mineral in an inert atmosphere and separating

a first portion of impurities from said ore by magnetic

separation, wherein said step of calcination produces carbon

dioxide as a waste product and further comprising the step

of recycling carbon dioxide produced by said step of calcination

to provide said inert atmosphere.

2. A process, as claimed in claim 1, wherein said inert

atmosphere further comprises a composition selected from

the group consisting of nitrogen and water vapor.

3. A process, as claimed in claim 1, wherein said saline

5 mineral is calcined at a temperature between about 43° C.

and about 400° C.

4. A process, as claimed in claim 3, further comprising the

step of subjecting said saline material to a preliminary

10 magnetic field prior to said step of separating.

5. A process for the purification of a saline mineral in an

ore comprising saline mineral and impurities, which comprises

shortite, pyrite or mixtures thereof, by magnetic

separation in a first magnetic field having positions of higher

15 intensity and lower intensity, said process comprising prealigning

said ore on a surface with respect to one or more of

said positions of higher intensity of said first magnetic field

prior to separation of said impurities; and separating a first

portion of impurities from said ore by magnetic separation

20 in said first magnetic field.

6. A process, as claimed in claim 5, wherein said surface

comprises a belt and said ore is pre-aligned in the direction

of travel of said belt.

7. A process, as claimed in claim 6, wherein said step of

25 pre-aligning comprises subjecting said ore on said belt to a

second magnetic field.

8. A process, as claimed in claim 6, wherein said step of

pre-aligning comprises feeding said ore onto a portion of

30 said belt which is aligned with said one or more higher

intensity positions of said first magnetic field.

* * * * *


Source URL: https://www.hazenresearch.com/6173840-beneficiation-saline-minerals