Senior Lecturer, Department of Metallurgy, Navoi State Mining and Technology University, Republic of Uzbekistan, Navoi
DEVELOPMENT OF A TECHNOLOGY FOR ENRICHMENT OF VERMICULITE ORE OF THE KARAUZYAK DEPOSIT
ABSTRACT
The article indicates the main properties of natural vermiculite, analyzes the analysis of the mineralogical and technological features of vermiculite of sungulite raw materials. Information is given that the first appeared vermiculite ores of the Karauzyaksky deposit, as well as the development of a beneficiation scheme, the purpose of which is to obtain raw materials for heat-insulating and facing tiles.
АННОТАЦИЯ
В статье указаны основные свойства природного вермикулита, рассмотрены анализы минералого-технологических особенностей вермикулитового сырья. Приведены сведения о вермикулитовых рудах Караузякского месторождения. А также рассмотрены вопросы разработки схемы обогащения, целью которой является получение сырья для теплоизоляционных и облицовочных плиток.
Keywords: minerals, vermiculite, effluent separator, pneumatic separator, crushing, screening, drying, thermal insulation, temperature, extraction.
Ключевые слова: минералы, вермикулит, выхретоковой сепаратор, пневматический сепаратор, дробление, грохочение, сушка, теплоизоляция, температура, извлечения.
Introduction. In the Republic of Uzbekistan, the production of vermiculite and materials based on it is just beginning to develop. High porosity, low volumetric weight and low coefficient of thermal conductivity, as well as a mineral composition that provides high fire resistance and biostability, put it in one of the first places among other heat-insulating materials. Dry construction mixtures are prepared from it, fire-retardant boards and paints are produced, it is used to insulate heating units, to soundproof rooms, when pouring steel, etc. In the industry of economically developed countries, vermiculite is used for the production of more than a hundred types of products. [1].
Research methods and results. Vermiculite ores of the Karauzyaksky deposit are typical formations of the weathering crust. In the near-surface part, they are represented by loose fine - medium-grained rocks, often with a lumpy structure. The lumps are 3-7 cm in size and easily crumble into small particles. At depth, the rocks are denser, but also poorly cemented. [2].
The granulometric composition of the ores is variable (Table 1). In general, the fraction of less than 5 mm prevails (from 55 to 98%, on average about 83%). The content of the fraction more than 10 mm (mostly soft lumps) is from a few percent to 15-30%, the fraction of 5-10 mm is mainly at the level of 2-5%, the content of fractions 5-0.6 and 0.6-0 mm is approximately equal.
Table 1.
Granulometric composition of ores of the Karauzyaksky deposit
No. p\p |
Sample No. |
Fractions, mm, % |
|||||
+10 |
-10+5 |
+5 |
-5+0 |
Including |
|||
-5+0,6 |
-0,6+0 |
||||||
1 |
S-01t |
31,2 |
24,8 |
56,0 |
44,0 |
39,5 |
4,5 |
2 |
S -02t |
0,7 |
1,2 |
1,9 |
98,1 |
42,9 |
55,2 |
3 |
S -03t |
2,0 |
2,8 |
4,8 |
95,2 |
45,9 |
49,3 |
4 |
S -04t |
2,2 |
4,0 |
6,2 |
93,8 |
52,8 |
41,0 |
5 |
S -35 |
- |
- |
33,6 |
66,4 |
41,6 |
24,8 |
6 |
S -36 |
- |
- |
2,2 |
97,8 |
62,1 |
35,7 |
7 |
S -41 |
- |
- |
14,9 |
85,1 |
58,2 |
26,9 |
8 |
S-49 |
- |
- |
45,0 |
55,0 |
40,7 |
14,3 |
9 |
S-48 |
- |
- |
22,5 |
77,5 |
42,1 |
35,4 |
10 |
S-50 |
3,3 |
2,3 |
56 |
94,4 |
46,1 |
48,3 |
The main minerals of the ores are vermiculite, pyroxene, amphibole, minor ones - carbonate, titanomagnetite, iddingsite, hydrochlorite, montmorillonite, chrysotile - asbestos, gypsum, iron oxides. Titanomagnetite is largely martitized. Its content ranges from 0.5-1.0 to 5-10%, less often 15-20%. In terms of mineral composition, ores are predominantly vermiculite-pyroxene with a pyroxene content of 60 to 90% [3].
The chemical composition of ores (Table 2) largely inherits the composition of ore-forming unweathered rocks, differing only in the higher content of Fe2O3, CO2 sulfate sulfur and loss on ignition, which is typical for the hypergenesis zone.
Table 2.
The chemical composition of vermiculite ores
Components |
Content, % |
Components |
Content, % |
SiO2 |
41,13 |
Na2O |
1,0 |
TiO2 |
1,11 |
K2O |
0,62 |
Al2O3 |
6,25 |
P2O5 |
0,03 |
Fe2O3 |
7,36 |
SO3 |
0,29 |
FeO |
3,76 |
п.п. |
6,18 |
MgO |
15,04 |
H2O |
1,31 |
CaO |
17,7 |
CO2 |
2,55 |
X-ray phase analysis of the crushed vermiculite sample was carried out on an X-ray diffractometer DRON-3. Radiation - CuKα, detector - scintillation counter. The recording was carried out in the range of angles 2Θ – 5–70 ° С with a step of 0.1°. The X-ray diffraction pattern of crushed vermiculite is shown in Fig. 1. A difference has been established in the behavior of finely ground vermiculite and relatively large aggregates of vermiculite concentrate selected in the sample, the diameter of which is about 2 mm, and they are folded in a number of tightly adjacent layers.
According to the analysis data, the main role in the composition of vermiculite is played by mica of the intermediate stage of hydration, represented by mixed layered formations with alternating layers of hydrobiotite and vermiculite. Actually, vermiculite sometimes consists of only small flakes of mica. By the nature of the exchangeable cations, magnesium is noted, magnesium - calcium vermiculite and sodium vermiculite and hydrobiotite. In large micaceous scales, their sodium varieties predominate, in small magnesium - calcium ones.
W – vermiculite, F – phlogopite, B – biotite
Figure 1. Diffraction pattern of crushed vermiculite
The content of vermiculite in ores is extremely uneven - from the first tenths of a percent to 35-38%, in vein-like accumulations up to 50-65%. A clear pattern of distribution of vermiculite to depth is not observed.
The vermiculite content was determined by rock firing and air separation of expanded vermiculite. Most of the samples were analyzed using special equipment (tubular vibroelectric furnace LHE TP-1, vibro-jet air separator VEP-1), which significantly increased the accuracy of analyzes.
According to the vermiculite content, ores can be conditionally subdivided into 3 types: lean ores with a content of 5-10%, medium (10-20%) and rich (more than 20%). However, the delineation of ores with different vermiculite content due to the unevenness of its distribution is not possible.
Given the relatively low content of vermiculite in the ores, laboratory tests were carried out to determine the possibility of their preliminary enrichment on a jig. The tests were carried out on two samples weighing 7.1 and 8.1 kg with a vermiculite content of 8.12 and 11.62%. The content of vermiculite in the obtained concentrates (light fractions) was 18.49 and 28.35%, respectively, with a yield of 25.7 and 27.6%. Extraction of vermiculite in concentrate 58-67%. Bulk bulk density of expanded vermiculite is 166-178 kg/m3. The research results are shown in Fig. 2.
Figure 2. Dependence of the extraction of vermiculite into concentrate on the pulsation frequency of the jig
With an increased content of titanomagnetite in ores, it is possible to simultaneously obtain its concentrate by magnetic separation of ores at the head of the technological process. According to laboratory tests, the content of Fe2O3 in magnetite concentrates is 24.7-50% and they can be used as an iron additive in the production of cement.
As can be seen from the data presented, when enrichment on jigging machines, the enrichment indices are low. To create an optimal beneficiation scheme, the vermiculite ore of the Karauzyaksky deposit with a vermiculite content of 10.16% was tested for washability according to the developed scheme (Fig. 3).
The technological scheme includes one-stage crushing, extraction of iron-containing, non-ferrous metals and other impurities from ores, sorting on screens into the resulting fractions and air separation.
Figure 3. Technological scheme of dry concentration of vermiculite ores
To separate the fraction over 4mm, the ore was screened. Fraction over 4mm is fed to the crusher for crushing, followed by the return of the crushed product to screening. Under mechanical action, vermiculite grains easily unfold along cleavage planes, forming very thin, weakly swelling scales, therefore, during crushing, excessive splitting of vermiculite must be excluded.
In its structure and properties, vermiculite differs significantly from other natural stone materials, crushing of which can be successfully carried out on hammer, jaw and roller crushers. The ability of vermiculite to stratify into thin plates and, in some cases, a rather high viscosity does not allow the use of existing crushing plants for crushing it. The physical properties of vermiculite, as well as the above requirements for crushed material, require that vermiculite be crushed not by impact or crushing action, but by cutting or simultaneously acting by cutting and impact.
The process of crushing vermiculite ore of the Karauzyaksky deposit was carried out in jaw, roll and hammer crushers in order to study the crushing performance.
The studies carried out on crushing vermiculite made it possible to establish that good results can be obtained when using hammer crushers with cutting blades. Their use makes it possible to reduce the degree of crushing, increase the thickness of the crushed vermiculite grains and reduce the specific work, thereby increasing the crushing performance.
To remove moisture, before electromagnetic separation, the -4 + 1 mm fraction was dried in a drying drum with a cyclone at a temperature of 150 ℃. The removal of nonferrous metals was carried out in an electromagnetic field using an exhaust current separator. From there, the vermiculite product goes for classification in screens for sieving into fractions -4 + 2mm, -2 + 1mm, and -1mm.
Further, vermiculite concentrate was obtained in air separators (Fig. 4.) by dry dressing. To increase the enrichment indicators and the efficiency of the separator, each size class was separated separately. The experiments were carried out on a CAD-4 air separator with a change in the air flow rate.
When separating vermiculite ore, minerals are separated by specific gravity. Minerals with a large specific gravity enter the first receiver (Fig. 4.), vermiculite, the fact that it has a small specific gravity compared to other minerals in the ore, is carried away by the air flow and enters the distant receiver. The results of the study show (Fig. 5.) that the initial speed of the main air stream for separating vermiculite grain from waste rock should be in the range of 25-30 m/s. From Figure 5 it can be seen that with an increase in the speed of the air stream, the extraction of the class
-4 + 2 mm and -2 + 1 mm into the concentrate increases. With enrichment of class
-1 + 0.5 mm, the extraction of vermiculite grain into concentrate increases with an increase in the air stream velocity up to 20 m / s, further increase in the flow velocity negatively affects the recovery, since fine particles are carried away with the exhaust air stream from the separator
Figure4. Trajectory of movement of minerals by specific gravity inside the separator
1 – base module; 2 – feed hopper; 3 – vibrating tray; 4 – main fan; 5 – jet generator; 6 – working chamber; 7 – collection of factions (1- for heavy fractions, 2,3 - for fraction of intermediate density, 4,5 - for light fractions); 8 – swivel shutters; 9 – aspiration unit; 10 – cyclone. а – collection of major factions; б – collection of intermediate fractions.
Figure 5. Dependence of the extraction of vermiculite into concentrate on the air flow rate of the air separator
Table 3
Distribution of vermiculite concentrate by fractions
Fraction |
Concentrate yield, % |
Vermiculite content in concentrate, % |
Extraction of vermiculite into concentrate, % |
-4+2 mm |
4,0 |
85,0 |
33,46 |
-2+1 mm |
3,97 |
85,0 |
33,21 |
-1+0 mm |
3,50 |
85,0 |
29,28 |
Total |
11,47 |
85,0 |
95,95 |
Thus, as a result of the studies carried out according to the developed scheme, a vermiculite concentrates of fractions -4 + 2mm, -2 + 1mm and -1mm with extraction of vermiculite in concentrate 95.95%, concentrate yield 11.47% and vermiculite content in concentrate 85%. The distribution of vermiculite concentrate by fractions is shown in table 3.
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