SCHLICH MINERALOGICAL ANALYSIS FOR RESEARCH OF MODERN BOTTOM SEDIMENTS

V. Ivanchenko, L. Berozkina, V. Stetsenko, L. Kovalchuk
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Abstract

Gold and other heavy minerals often form scaly, leafy, needle-like or split crystals, dendrites of complex shape, individuals and aggregates with a large number of internal cavities. Significant mobility of these particles in water and air streams causes their separation from the psammitic component of sediment and deposition together with clay minerals. During preparatory stages for mineralogical analysis, such crystals of heavy minerals fall into slime part. According to classical algorithm of schlich mineralogical analysis slime part is thrown away. So it leads to losses of rich minerals and an incorrect analysis. The main purpose of the article is to present the new algorithm for the preparation of the bottom sediments samples for the mineralogical analysis and to demonstrate practical benefits of it. Authors propose the meliorated methods of mineralogical analysis considering comprehensive study of test material. The real natural composition of ore minerals in the sediments consists of adding the data "heavy concentrate-1" and "heavy concentrate-2". This provides an increase in industrial value of minerals by 10-30%, compared with the methods of prospecting that operate today. Such detailed analysis showed that modern bottom sediments include both natural components and man-made materials (plastic, polyethylene, synthetic fibers and fabrics, fuel, various types of petroleum products, metallurgical and household waste). Mineralogical analysis can be used as an ecological method for assessing the environmental pollution and reviewing the types of pollutants. The estimation of mineral reserves according to new methodology opens opportunities for profitable field development of poor polymetallic deposits. The study of bottom sediments by such a method indicates the need to clean hydrogeoecosystems and stimulates the development of new recycling methods in the economy and the waste-free production, for example, cleaning beaches from heavy metals and waste, complex sludge processing after dredging works in riverbeds, berths and port waters.
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现代海底沉积物研究中的Schlich矿物学分析
金等重矿物常形成鳞片状、叶状、针状或裂状晶体、形状复杂的树突、具有大量内腔的个体和集合体。这些颗粒在水和气流中的显著流动性导致它们与沉积物的沙质成分分离,并与粘土矿物一起沉积。在矿物学分析的准备阶段,这类重矿物晶体落入泥态。根据经典的施里希矿物学分析算法,将矿泥部分丢弃。因此,它会导致丰富矿物质的损失和错误的分析。本文的主要目的是提出一种制备用于矿物学分析的海底沉积物样品的新算法,并论证其实际效益。提出了综合研究试验材料的矿物学分析改进方法。沉积物中矿石矿物的真实自然组成是“重精矿-1”和“重精矿-2”数据的相加。与目前使用的勘探方法相比,这种方法使矿物的工业价值增加了10-30%。这种详细的分析表明,现代海底沉积物既包括天然成分,也包括人造材料(塑料、聚乙烯、合成纤维和织物、燃料、各种石油产品、冶金和家庭废物)。矿物学分析可以作为一种评价环境污染和审查污染物类型的生态学方法。根据新方法估计矿产储量为贫多金属矿床的有利可图的油田开发提供了机会。用这种方法对底部沉积物的研究表明,需要清洁水文地质生态系统,并刺激经济和无废物生产中新的回收方法的发展,例如,清除海滩上的重金属和废物,在河床、泊位和港口水域进行疏浚工程后处理复杂的污泥。
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