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首页> 外文期刊>Eurasian Soil Science >Physicochemical properties and potassium state of the soils developed on dump rocks of coal mines.
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Physicochemical properties and potassium state of the soils developed on dump rocks of coal mines.

机译:煤矿排土场发育的土壤理化特性和钾态

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摘要

The main physicochemical parameters of soils formed on dumps composed of overburden rocks in a coalfield deposit have been compared with the properties of the zonal soils. For the first time, the potassium state of embryozems at different stages of development has been analyzed; the concentrations and profile distributions of different potassium compounds and the potential soil buffering capacity for potassium were studied. It was shown that the increase in the available potassium concentrations in the upper horizons of the embryozems was due to the higher intensity of the biological processes and the active weathering of the rocks transferred to the surface. The intensity of the biological accumulation of potassium was higher under the herbaceous cenoses than under the tree-shrub ones.Notes Translated from Pochvovedenie (2014) 1, 120-128 (Ru).
机译:将煤田矿床覆盖岩组成的堆积物上形成的土壤的主要理化参数与纬向土壤的性质进行了比较。首次分析了处于不同发育阶段的胚芽的钾状态。研究了不同钾化合物的浓度和分布,以及土壤对钾的潜在缓冲能力。结果表明,胚状体上部视野中有效钾浓度的增加是由于生物过程的强度更高以及转移到地表的岩石的主动风化所致。草本普查下钾的生物累积强度高于乔木灌木下的钾。注解自Pochvovedenie(2014)1,120-128(Ru)。

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