Tungsten ore beneficiation (1)

First, the nature and use of tungsten
Belonging tungsten refractory metal, having a melting point of up to 3410 ± 20 ℃, the highest melting point metal, and having a vapor pressure high-temperature strength and hardness remain very low at a high temperature 2000 ~ 2500 ℃. Tungsten density 19.3 g / cm 3, 2.5 times that of steel, and gold is quite. Tungsten has good electrical conductivity, small expansion coefficient, high hardness, high modulus of elasticity and good ductility. Tungsten has strong corrosion resistance and does not work with any concentration of acid and alkali at room temperature; at 380~400 °C, tungsten trioxide begins to be reduced by hydrogen; above 630 °C, hydrogen can reduce tungsten dioxide to metal. Tungsten powder. Tungsten reacts with carbon and some carbon-containing gases at high temperatures to form hard, wear-resistant, refractory tungsten carbide with important industrial value.
Tungsten carbide-based hard alloys are used as cutting tools, die-cutting tools, drilling tools, rolls, armor-piercing warheads and heat-resistant wear parts; cast tungsten carbide for surfacing and coating of wear parts; tungsten carbide grain manufacturing No tooth saw blade. The consumption of tungsten in the form of tungsten carbide accounts for more than half of the total consumption of tungsten.
Tungsten is an important alloying element of steel, which increases the strength, hardness and wear resistance of steel. The main tungsten steels are high-speed tool steel, hot work die steel, series tools, die steel, ordnance steel, turbine steel, magnetic steel and so on. Application of a small amount of tungsten steel, accounting for about 20 to 30% of total consumption of tungsten.
Special alloys with tungsten as the main component are: refractory alloys for gas turbine blades, rocket nozzles, missiles, nuclear reactor components, etc.; high specific gravity alloys for heavy armor piercing warheads, navigation gyroscope rotors, flat street weights and automatic watches brakes; tungsten-nickel alloy, copper or the like is used as the X- and γ- rays shield, radiation material and other containers; tungsten copper, tungsten, silver alloy is a high-frequency electrical contact material; tungsten-rhenium alloy thermocouple measurable Temperatures range from room temperature to 2835 °C.
Metal tungsten materials, including wires, rods, strips, tubes and sheets, are important electrical light source materials, electronic components and high temperature materials for various lighting fixtures, tubes, X-ray tubes, non-consumable electrodes, Metal spraying and thermal components. Tungsten compounds can be used as the catalyst petrochemical industry, textiles, plastics industry flame retardants, mordant, pigments, dyes, fluorescent materials, decorative paints, solid lubricants and the like.
In short, tungsten is used in industries such as steel, machinery, mining, petroleum, rocket, aerospace, electronics, nuclear power, military and light industry in the form of alloying elements, tungsten carbide, metal materials or compounds. It is not a part of the national economy and cutting-edge technology. Missing important materials.
Second, the tungsten mineral nature of tungsten minerals have been found to have 20 kinds of industrial value which is wolframite (wolframite) and scheelite (scheelite) two kinds. Wolframite ore include tungsten (FeWO 4), wolframite ore (MnWO 4) and wolframite [(FeMn) WO 4], is a tungsten acid salts of iron and manganese continuous interstitial solid solution is a mixture of the same image, In fact, it rarely appears in a pure state. The tungsten-iron ore is a rich iron-tungsten mineral, the tungsten-manganese ore is a manganese-rich tungsten mineral, and the tungsten-manganese ore is a mixture of pure tungsten iron and tungsten manganese ore in a range of 20 to 80%. FeWO 4 : MnWO 4 ≤ 20: 80 is a tungsten manganese ore, and the ratio ≥ 80: 20 is tungsten iron ore.
The scheelite (CaWO 4 ) is a calcium tungstate with a tetragonal crystal. The molybdenum may replace the tungsten in the scheelite to form a similar calcium molybdate (CaMoO 4 ) ore. The scheelite emits a distinct blue-white fluorescence under the induction of ultraviolet radiation. When molybdenum is present in the mineral, it changes the color of the fluorescent light. As the content of molybdenum increases, it gradually changes from blue to beige, yellowish or orange. Table 1 shows the physical and chemical properties of the wolframite and scheelite.

Table 1 Physical and chemical properties of scheelite and scheelite

nature
Black tungsten ore (wolframite)
Scheelite
(scheelite)
Tungsten iron ore
(Ferberite)
Tungsten manganese ore
(Wolframite)
Tungsten manganese ore
(hubnerite)
Chemical formula
Contains WO 3 %
Mn%
Fe%
Crystal structure
Cleavage
Density, g/cm 3
colour
toughness
luster
Fracture
Hardness (Mohs)
magnetic
Streak
transparency
Occurrence
FeWO 4
76.3
0 to 3.6
18.5~14.7
Monoclinic system
Complete cleavage in one direction
7.5
black
Extremely brittle
Semi-metallic to metallic luster
Uneven
5
Micro to weak magnetic
Dark brown
Opaque to translucent
Crystallized bulk crystal
(FeMn)WO 4
76.5
3.6~14.5
14.7~3.7
Monoclinic system
Complete cleavage in one direction
7.1 to 7.5
Dark gray to black
Extremely brittle
Semi-metallic to metallic luster
Uneven
5 to 5.5
Micromagnetic
Dark brown
opaque
Irregular block, plate crystal, radial aggregate
MnWO 4
76.6
14.5~18.1
3.7~0
Monoclinic system
Complete cleavage in one direction
7.2 to 7.3
Reddish brown to black
Extremely brittle
Semi-metallic to metallic luster
Uneven
5
Slight magnetic
Brown red to green yellow
Opaque to translucent
Radial of thin plate crystal
Aggregate
CaWO 4
80.6
-
-
Orthogonal system
Good in four directions
5.4~6.1
Light yellow, brown, white
Extremely brittle
Glass to resin gloss
Uneven
4.5~5
Non-magnetic
white
Transparent to translucent
Generally square crystal
[next]
In addition to the above-mentioned main tungsten minerals, tungsten (WO 3 ) and tungsten-molybdenum ore [(CaMo) WO 4 ] are common in some black tungsten deposits and scheelite deposits. Lead minerals other secondary tungsten ore (PbWO 4), tungsten, bismuth (Bi 2 WO 6), tungsten wulfenite [Pb (MoW) O 4] , zinc, tungsten ore (ZnWO 4), copper-tungsten ore (CuWO 4 ), copper tungsten (Cu 2 (WO 4 ) (OH) 2 ], high-iron tungsten [Ca 2 Fe 2 (WO 4 ) 7 • 9H 2 O], tungsten ore (WS 2 ), and the like. These minerals have not yet found deposits with industrial value for exploitation.
Third, tungsten deposits, ore types
The formation of tungsten deposits is related to magma activity or metamorphism. Magmatic hydrothermal fluid, metamorphic hydrothermal fluid, sedimentation and reconstitution are the main mineralization effects. According to the genesis and occurrence of the deposit, combined with the mining and mineral processing technical conditions, the main tungsten deposits can be divided into four industrial types: quartz vein type tungsten deposit, skarn type scheelite deposit, fine vein disseminated tungsten deposit, and layer control. And layered tungsten deposits (Table 2).
Table 2 Main industrial types of tungsten deposits

The quartz vein type tungsten deposit is the most important tungsten deposit currently mined in China, accounting for more than 90% of the ore produced. The ore body is vein-like, fine veined, and vein-like in the granite and metamorphic rocks. The thickness of the veins can range from a few millimeters to a few meters, the depth of the veins ranges from tens of meters to a few hundred meters, and the length of the veins ranges from a few meters to a few hundred meters, or even kilometers. Some deposits such as the drift pond tungsten ore, the upper part is the fine vein zone or the thin vein group, and the lower part is merged into the large vein or the large vein group. In the quartz vein tungsten deposit, more than sixty kinds of minerals are seen. The tungsten minerals are mainly black tungsten ore, often containing scheelite, and other cassiterite , molybdenite, stibnite, chalcopyrite, Pyrite, galena, sphalerite, antimony ore, arsenopyrite, natural strontium, beryl, etc.; non-metallic minerals are mainly quartz, feldspar , mica , followed by tourmaline , fluorite , calcite , topaz , fluorine and carbonate apatite iron ore and the like. According to the content of useful minerals and the combination of minerals, it can be divided into the following types of veins: wolframite-quartz vein; wolframite, stibnite-quartz vein; wolframite, molybdenite-quartz vein; Black tungsten ore, cassiterite, sulfide ore-quartz vein; black tungsten ore, beryl, sulfide ore-quartz vein. In this type of vein, tungsten and its symbiotic metal minerals are born in the quartz vein and the vein wall. The surrounding rock generally does not contain useful minerals. The boundary between the vein and the surrounding rock is very obvious, the color is clear and easy to identify, so it can be manually selected. The waste rock will be abandoned in advance to create favorable conditions for the next step of mineral processing .
The skarn-type scheelite deposit is produced in or near the contact zone of granite intrusions and calcareous rocks. According to the combination characteristics of useful minerals and industrial utilization, it can be divided into two types of mineralization: one is sulfide ore and scheelite skarn type, and its main features are sulfide ore such as chalcopyrite, pyrite, and square. The content of lead ore, sphalerite and chalcopyrite is high, and the content of lead-zinc ore is high. It can be used as an independent ore deposit and has a high silver content. It is an important target for comprehensive utilization, so it is both a scheelite deposit and a Polymetallic sulphide deposits; the other type is scheelite skarn, the sulphide ore content is relatively less than the former, the mineral composition is relatively simple, the main industrial mineral is scheelite, and the sulphide ore is only used as a by-product comprehensive recovery. The skarn-type scheelite deposits are mostly in foreign countries, accounting for more than half of the foreign tungsten reserves.
Fine vein-disseminated tungsten deposits in which tungsten minerals are produced in fine veins and are produced on the tops and edges of granite, shale or porphyry bodies. The ore bodies are massive or layered, lenticular, and few It is distributed in a strip shape. The deposits are large in scale, from large to medium to large. The main metal minerals are hematite, scheelite, cassiterite, beryl, molybdenite, stibnite, chalcopyrite and strontium and barium minerals. The ore grade is generally moderate to poor.
For layered and layered tungsten deposits, the ore body is controlled by a certain stratigraphic horizon and lithology. The occurrence is basically the same as that of the strata. The ore-bearing layer consists of one layer to several layers. The general range is wider, but the scale of industrial ore bodies is sizes, such as Western main gold metallic minerals are scheelite, stibnite, natural gold, purple calcium occurs in sericite slate layer. Another example is the Austrian Mittel Silt stellite deposit in the volcanic sedimentary metamorphic rocks. [next]
The formation of this type of deposit in porphyry-type tungsten deposits is mainly related to the shallow-super-shallow intrusion of the weakly acidic calcium-alkali series in the late volcanic-subvolcanic action. The porphyries associated with tungsten mineralization are mainly granodiorite porphyry, feldspar porphyry, granite porphyry and quartz porphyry. Mineralization is mainly distributed in the rock mass, and some are produced in the contact zone between the porphyry body and the surrounding rock, and some are produced in the surrounding rock. Mineralization is characterized by fine veins, low grade, large scale, often associated with molybdenum ore, shallow ore body output, and surrounding rock alteration has a zoning phenomenon. The mineralization is in the form of disseminated, reticular and fine veins. The ore body often appears as layered, lenticular, and irregular, with no obvious boundary with surrounding rock. The ore minerals mainly include scheelite, wolframite and molybdenite, followed by chalcopyrite, sphalerite, stibnite and pyrite. The representative deposits are the Lianhuashan tungsten deposit in Guangdong and the Yangcangling tungsten deposit in Jiangxi.
Some large deposits often include several types, such as the Shizhuyuan tungsten deposit, including skarn type, fine vein disseminated granite type, Yunying rock network type and other composite tungsten-tin-molybdenum polymetallic deposits. The Yaogangxian tungsten deposit is composed of a quartz vein type black tungsten deposit and a skarn type scheelite deposit. The Luokeng tungsten deposit includes a quartz vein type and a fine vein network-disseminated type deposit.
Tungsten ore is generally classified into black tungsten ore (often containing scheelite) and scheelite ore according to the class of tungsten minerals. According to the mineral crystal nature, it can be divided into coarse grain inlay, fine grain inlay, uniform distribution and uneven distribution. These classifications are closely related to the mineral processing technology of tungsten.
IV. Production and Consumption of Tungsten in the World Thirty-four countries and regions in the world produce tungsten, mainly in China, the Soviet Union, Canada, South Korea, Bolivia, Australia, the United States and Portugal. China is the world's most abundant tungsten resource, with more than half of the world's reserves. It is mainly concentrated in Hunan, Jiangxi, Guangdong, and Fujian provinces in the eastern fold of the Nanzhao Mountain. The reserves, production, and export volume all rank first in the world. . The major consumers and regions of tungsten are the United States, the Soviet Union, Western Europe, Eastern Europe and Japan.
According to the report of the 18th session of the Tungsten Committee of the Commodity Committee of the United Nations Conference on Trade and Development in November 1986, the production and consumption of tungsten concentrates in the world in recent years are shown in Tables 3 and 4, respectively.
Table 3 World tungsten concentrate production, t tungsten content

Year, year
1981
1982
1983
1984
1985
1986
world
48701
45932
39810
44035
43528
39095
Developed market economy countries
Australia
Austria
Canada
France
Japan
Portugal
Spain
Sweden
United States
other
13961
3333
1450
2052
591
668
1396
441
365
3605
60
12062
2588
1406
2938
726
635
1343
556
349
1521
7
8092
2061
(1400)
328
793
475
1164
521
365
980
5
11715
1733
1400
3715
742
477
1486
569
365
1203
5
11403
1970
1565
3005
735
526
1737
462
402
996
5
(8817)
(1750)
(1400)
(1417)
(700)
(600)
(1200)
(450)
(400)
(900)
(—)
Developing country
Bolivia
Brazil
Myanmar
Mexico
Peru
South Korea
Rwanda
Thailand
other
10110
2778
1248
825
158
521
2742
281
1210
347
7583
2543
1365
844
78
654
2539
322
856
391
8538
2490
1026
930
147
703
2101
231
563
347
9170
1893
1101
1096
145
786
2702
291
742
414
8975
1643
1297
(1100)
282
798
2572
(300)
585
398
7328
(1100)
(800)
(1100)
(300)
(784)
(2200)
(300)
(464)
(380)
Asian socialist countries
(15700)
(15200)
(14000)
(14000)
(14000)
(13800)
Eastern European socialist countries
Soviet Union
other
(8930)
(8850)
(80)
(9080)
(9000)
(80)
(9180)
(9100)
(80)
(9150)
(9100)
(50)
(9150)
(9100)
(50)
(9150)
(9100)
(50)
Note: The numbers in parentheses are estimates.
Table 4 World tungsten concentrate consumption, t tungsten content

Year, year
1981
1982
1983
1984
1985
1986
world
47095
40022
39770
46967
44457
42075
Developed market economy countries
Austria
France
Federal Republic of Germany
Japan
Sweden
United Kingdom
United States
other
19371
1850
663
1348
2238
1432
879
9839
1122
12572
1304
653
1541
1826
994
660
4506
1088
13679
(1629)
520
2030
1977
774
560
5181
1008
20208
(2096)
815
2934
2302
765
610
8577
1109
17179
(2000)
806
2073
2616
820
(600)
6838
1424
(15345)
(2000)
(850)
(1600)
(2200)
(1220)
(600)
(5625)
(1250)
Developing country
Brazil
India
South Korea
other
2897
480
459
1898
60
2698
454
454
1742
48
2468
450
(400)
1555
63
3115
538
(400)
2070
107
3605
1048
(400)
2048
109
(3260)
(860)
(350)
1950
100
Eastern European socialist countries
Poland
Soviet Union
other
(18467)
427
(15870)
(2170)
(19152)
1312
(15870)
(1970)
(18623)
1073
(15600)
(1950)
(18664)
594
(16000)
(2070)
(18673)
603
(16000)
(2070)
(18670)
(600)
(16000)
(2070)
Asian socialist countries
(6360)
(5600)
(5000)
(5000)
(5000)
(4800)
V. Mineral processing products and quality requirements Tungsten ore is generally required to obtain 65% WO 3 or higher in impurities, and impurities meet the requirements of product specifications. At the same time, it is difficult to select low-grade (15-30% WO 3 ) ore. The latter is for chemical beneficiation. In addition to producing high-grade products in foreign countries, in order to ensure high recovery rate, it is often used to produce low-grade concentrates and then chemically treated to produce synthetic white tungsten or ammonium paratungstate.
Tungsten smelting has different requirements for the quality of tungsten concentrate due to different smelting methods and different purpose products. For example, tungsten concentrates for smelting tungsten iron and alloy steel by fire method have strict requirements on the content of sulfur, phosphorus and heavy metal elements, because these harmful elements cannot be removed during the smelting process, so that the produced tungsten steel is hot and brittle. Or cold and brittle to reduce mechanical properties; and the content of molybdenum is not limited, because molybdenum is a beneficial element of steel; the white tungsten contained in the black tungsten concentrate is also not strictly separated. However, when black tungsten concentrate is used as a raw material for hydrometallurgy, it is first processed into intermediate products such as ammonium paratungstate and tungsten oxygen, and then made into cemented carbide and tungsten products. In order to improve the decomposition rate of tungsten concentrate, it is required to separate black tungsten and white tungsten,

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