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Microelements in solonchaks of the western Trans-Baikal region

机译:贝加尔湖西部地区的独白中的微量元素

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摘要

Distribution patterns of microelements (Mn, Zn, Ni, Cu, Cr, Co, Pb, and Cd) in solonchaks of the western Trans-Baikal region were studied. It was found that their concentrations in typical solonchaks of haloxerophytic steppe differed from those in solonchaks of moistened habitats (playa, gleyed, and dark solonchaks) because of the differences in their landscape positions and ecological conditions. A general rise in the contents of the microelements was observed from the northeast to the southwest in agreement with changes in the parent materials. Different degrees of correlation of the contents of the microelements and their exchangeable forms with the contents of soluble salts, humus, and physical clay in the soils and the soil reaction were found. The average and extreme concentrations of the microelements were determined. The studied typical solonchaks differed from the zonal chestnut soils in the higher contents of Co, Cr, and Cd; whereas solonchaks of moistened habitats were enriched in Mn, Co, and Cd.
机译:研究了贝加尔河西部地区独生舟中微量元素(Mn,Zn,Ni,Cu,Cr,Co,Pb和Cd)的分布规律。结果发现,由于其景观位置和生态条件的差异,它们在典型的盐生植物草原独角兽中的浓度与在潮湿栖息地(普拉亚,灰色和深色独角兽)的独角兽中的浓度不同。从东北到西南,微量元素的含量普遍增加,这与母体材料的变化一致。发现土壤中微量元素及其交换形式与可溶性盐,腐殖质和物理黏土的含量以及土壤反应之间存在不同程度的相关性。确定了微量元素的平均浓度和极限浓度。 Co,Cr,Cd含量较高时,所研究的典型独角cha与带状栗土不同。而潮湿栖息地的独行客富含锰,钴和镉。

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