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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Transformation of metals migration and biogeochemical cycling under the influence of copper mining production (the Southern Urals)
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Transformation of metals migration and biogeochemical cycling under the influence of copper mining production (the Southern Urals)

机译:铜矿生产影响下金属迁移与生物地球化学循环的转化(南乌拉斯)

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摘要

This study aims to estimate the migration and accumulation of metals (Cu, Zn, Fe, Mn, Ni, Pb, Cd, Co, Cr, Zr, Ba, and Sc) in terrestrial and aquatic landscapes. The research is based on the results of a long-term study (1998-2018) in one of the copper mining centers in Russia in the vicinity of Sibay City in the Southern Urals. The metal contents in samples of water, bottom sediments, soils, plant shoots (total aboveground phytomass samples, agrobotanical group samples, and shoots of indicator terrestrial and aquatic species), and fish muscles are measured. It is found that within natural geochemical anomalies, the migration ability of chemical elements in the soil-plant system and general biogeochemical cycle is low because of the high soil buffer capacity (determined by the high humus content, high percentage of fine fractions in granulometric composition, and neutral pH) and the adaptation of local plants to ore mineralization. The ecosystems affected by low pollution maintain natural homeostasis, stabilize the flow of chemical elements, and preserve the natural features of geographic components. Metal pollution and the replacement of natural steppe vegetation with secondary herbaceousruderal communities in critical areas near copper-zinc mining objects can stimulate the mobilization and inclusion of chemical elements in biogeochemical cycling, as well as the disruption of bonds among landscape components. The water systems in catenae function as stabilizers through a system of geochemical barriers and low uptake of metals by hydrophytes, such as the common reed (Phragmites australis).
机译:本研究旨在估算陆地和水生景观中的金属(Cu,Zn,Fe,Mn,Ni,Pb,Cd,Co,Cr,Zr,Ba和Sc)的迁移和积累。该研究基于长期研究(1998-2018)在俄罗斯南部苏联南部的Sibay城市附近的铜矿中心之一。测量水,底部沉积物,土壤,植物芽样品中的金属含量(总面上植物样品,农生群样品和指示剂陆地和水生物种芽)和鱼类肌肉。发现在天然地球化学异常中,由于高土壤缓冲能力(由高腐殖质含量,粒度组合物中的高百分比确定的高腐殖质含量确定,所述土壤 - 植物系统和一般生物地球化学循环中的化学元素和一般生物地球化学循环的迁移能力低和中性pH值)和局部植物的适应矿石矿化。受低污染影响的生态系统维持天然稳态,稳定化学元素的流动,并保持地理成分的自然特征。金属污染和用次级草本族社区在铜 - 锌矿对象附近的关键区域中替代天然草原植被可以刺激生物地球化学循环中的化学元素的动员和包含化学元素,以及景观组分中的粘合。 Catenae的水系统通过地球化学障碍系统和疏水性的低吸收金属的水系统用作稳定剂,例如常见的芦苇(芦苇澳大利亚)。

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