磁铁矿石英岩分散产物对环境的潜在影响

O. Lavrynenko, V. Yatsenko, B. Shabalin, I. Yatsenko
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引用次数: 0

摘要

利用XRF、TG-DTA、化学和沉积分析等方法,对克罗热热N矿选矿厂磁铁矿石英岩的选矿产物进行了对比分析,对比原矿样品,追踪了磁选4个阶段的样品和尾矿的物相和化学组成的变化,揭示了分散过程对环境的潜在影响。热重研究显示阶段转换的磁铁矿磁赤铁矿(250 - 340°C),多态转换的铁氧化物和破坏矿物(430 - 480°C),α-石英转换成测试阶段(564 - 568°C),脱羟基铁和镁氢氧化物(385°C),转换的石英beta-cristobalite(970°C)。在浓缩过程中,有一个损失的增加样品的质量,这是%:0.06(我);1.46 (2);1.9 (III)和2.6 (IV).根据x射线衍射,矿石矿物主要为磁铁矿,造岩矿物为石英。次生矿物有硫化物、明矾、放光石等。结果表明:在第1阶段,原生矿物和次生矿物全部存在于样品中;在第2阶段,硫化物从样品中消失;在第3阶段,次生矿物消失;在第4阶段,石英保留在样品中,并与磁铁矿形成团聚体。磁铁矿的晶格参数在8.397 ~ 8.403 nm之间变化,其相干散射区域(CSR)为31.4 ~ 35.6 nm。研究发现,在磨矿过程中,二次矿物的破坏是伴随着破坏产物的去除而发生的,尾矿中出现了分散的石英。根据沉降分析数据,在前20秒内,24-28 μm的颗粒有一半以上从矿浆中沉降,3分钟后,8-9 μm的颗粒沉降,6分钟后- 6-7 μm的颗粒沉降。在30分钟内,4.5 ~ 2.7 μm的颗粒几乎完全析出。尾矿水力分级结果表明,分选机第一室和第二室主要沉积石英颗粒,第三室分离放线石和白云母颗粒,第四室分离明辉石、黑云母和绿泥石颗粒。分散产物的化学成分分析表明,Si、Ca和Na在尾矿中积累,而Ti被去除,可能进入环境。结果表明,尾矿和分离产物使锌含量增加,尾矿中富集了对环境有害的砷和铌。同时,其它元素的浓度在加工的各个阶段都保持稳定。
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Potential impact of dispersion products of magnetite quartzites on the environment
Using XRF, TG-DTA, chemical and sedimentation analysis of the products of processing of magnetite quartzites from the N Ore Processing Plant of Krivorozhye, changes in the phase and chemical composition of samples of four stages of magnetic separation and tailings were traced compared to a sample of the raw ore, and the potential impact of the dispersion process on the environment was revealed. Thermogravimetric studies indicate phase transformations of magnetite to maghemite (250-340 ° C), polymorphic transformations of iron oxides and destruction of rock-forming minerals (430-480 ° C), conversion of alpha quartz to beta-form (564-568 ° C), dehydroxylation of iron and magnesium oxyhydroxides (385 ° C), conversion of beta-quartz to beta-cristobalite (970 ° C). In the process of enrichment, there is an increase in the loss of mass of the samples, which is %: 0.06 (I); 1.46 (II); 1.9 (III), and 2.6 (IV). According to X-ray diffraction, the main ore mineral is magnetite, the rock-forming mineral is quartz. Among the secondary minerals are sulfides, cummingtonite, actinolite, and others. It is shown that at the first stage of enrichment all primary and secondary minerals are present in the samples, at the 2nd stage sulfides disappear from the sample, at the 3rd stage secondary minerals disappear, and at the 4th stage quartz remains in the sample and it forms aggregates with magnetite. The parameter of the crystal lattice of magnetite varies between 8.397-8.403 nm, its coherent scattering region (CSR) is 31.4-35.6 nm. It is found that in the course of ore grinding the destruction of secondary minerals takes place with the removal of destruction products, as evidenced by the occurrence of disperse quartz in the tailings. According to sedimentation analysis data, in the first 20 seconds, more than half of the particles with a size of 24-28 μm were deposited from the pulp, after 3 minutes, particles with a size of 8-9 μm settled, after 6 minutes - particles with a size of 6-7 μm. Within 30 minutes, almost complete precipitation of particles with sizes of 4.5-2.7 μm was observed. Hydraulic classification of the tailings showed the deposition of mainly quartz particles in the first and second chambers of the separator, actinolite and muscovite particles were separated in the third chamber, and cummingtonite, biotite and chlorite in the fourth chamber. Analysis of the chemical composition of the dispersion products indicates that Si, Ca, and Na accumulate in the tailings, whereas Ti is removed, and could potentially enter the environment. It is shown that the tailings and separation products increase the content of Zn, and the tailings accumulate environmentally hazardous As, and Nb. At the same time, the concentrations of other elements remain stable at all stages of processing.
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