Геохимические свойства и трансформация микроэлементного состава почв при разработке коренных месторождений алмазов в Якутии

IF 2.4 Q2 MINING & MINERAL PROCESSING
Yana Legostaeva, Anna Gololobova, V. Popov, V. Makarov
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Abstract

Extraction of diamonds from primary deposits in Siberia is associated with the development of kimberlite pipes in challenging environmental conditions, accompanied by a complex impact on the environment. The article presents the results of monitoring the soil cover of the Nakyn kimberlite field  in the Yakutia diamond province, which is affected by the facilities of the Nyurba Mining and Processing Division. Development of primary diamond deposits has a large-scale impact on the subsoil, topography, and soil cover: creation of the world's largest quarries, formation of dumps more than 100 m high, arrangement of extensive tailings, formation of solid and liquid industrial wastes of various chemical composition. The research is aimed at studying the spatial and temporal patterns of the technogenic impact on the soil cover, identifying the nature and level of transformation of the microelement composition of soils based on the analysis of the intra-profile and lateral distribution of mobile forms of trace elements. The study targets in 2007-2018 were zonal types of permafrost soils of northern taiga landscapes, cryozems, occupying 84 % of the total study area, which are characterized by biogenic accumulation of mobile forms of Ni, Mn, and Cd in the upper AO, Acr horizons, and Cr, Ni, Co, Mn, Cu in the suprapermafrost CR horizon. We found out that the contamination of the soil cover of the industrial site at the Nyurba Mining and Processing Division is of a multielement nature with local highly to very highly contaminated areas. Over a ten-year observation period, areas of stable soil contamination are formed, where the main pollutants are mobile forms of Mn, Zn, Ni. We suggest that against the background of a natural geochemical anomaly associated with trap and kimberlite magmatism, technogenic anomalies are formed in the surface horizons of soils. They are spatially linked to technogenically transformed landscapes. One of the sources of pollutants is the dispersion of the solid phase of dust emissions in the direction of the prevailing winds, which leads to the formation of soils with abnormally high contents of mobile forms of Mn, Zn, Ni.
地化学性质和土壤微量元素组成的转变,以开发雅库茨亚的钻石基岩
从西伯利亚原生矿床中提取钻石与金伯利岩管道在具有挑战性的环境条件下的发展有关,并伴随着对环境的复杂影响。本文介绍了雅库特钻石省纳金金伯利岩矿区受纽尔巴采矿和加工司设施影响的土壤覆盖监测结果。原生钻石矿床的开发对底土、地形和土壤覆盖产生了大规模的影响:创造了世界上最大的采石场,形成了100多米高的垃圾场,排列了大量的尾矿,形成了各种化学成分的固体和液体工业废物。研究技术对土壤覆盖影响的时空格局,在分析微量元素流动形态的内剖面分布和横向分布的基础上,确定土壤微量元素组成变化的性质和程度。2007-2018年的研究对象为占研究总面积84%的北方针叶林景观冻土带地带性土壤类型,其特征是在AO上部、Acr层中以Ni、Mn、Cd的流动形态为生物积累,在冻土带上层Cr层中以Cr、Ni、Co、Mn、Cu的流动形态为生物积累。我们发现,纽尔巴采矿和加工部门工业场地的土壤覆盖污染具有多元素性质,局部污染程度高到非常高。在10年的观测期内,形成了稳定的土壤污染区,主要污染物为Mn、Zn、Ni的流动形式。我们认为,在圈闭和金伯利岩岩浆作用相关的自然地球化学异常背景下,在土壤表层形成了技术成因异常。它们在空间上与经过技术改造的景观相联系。污染物的来源之一是粉尘排放的固相在盛行风方向上的分散,这导致形成了Mn, Zn, Ni的流动形态含量异常高的土壤。
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来源期刊
Journal of Mining Institute
Journal of Mining Institute MINING & MINERAL PROCESSING-
CiteScore
7.50
自引率
25.00%
发文量
62
审稿时长
8 weeks
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