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Acid and Mineral Components Determining the Exchangeable Acidity in Mineral Horizons of Taiga Soils of the Komi Republic

机译:酸和矿物成分决定了科米共和国针叶林土壤中矿物交换层的酸度

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摘要

Analysis of acid components in soil-KCl suspension filtrates from the mineral horizons was performed on the basis of analytical data reported between 1958 and 2003, including the data on more than 60 soil profiles (about 300 horizons) from the taiga zone of the Komi Republic. It was shown that the acid ions Al~(3+), H~+ (exchangeable hydrogen), and Fe~(3+) and the basic ion H_3siO_4~- are the main components determining the pH of filtrates. Groups of horizons with the predominance of specific ions were separated.
机译:根据1958年至2003年间报告的分析数据,包括来自科米共和国塔加地区的60多个土壤剖面(约300个视野)的数据,对来自矿物视野的土壤KCl悬浮液滤液中的酸成分进行了分析。 。结果表明,酸性离子Al〜(3 +),H〜+(可交换氢),Fe〜(3+)和碱性离子H_3siO_4〜-是决定滤液pH值的主要成分。具有特定离子优势的水平视场被分离。

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