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Pedogenic and Anthropogenic Influence on Calcium and Magnesium Behaviors in Stagnic Anthrosols

机译:生土和人为因素对滞滞性人类气溶胶中钙和镁行为的影响

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摘要

The formation of Stagnic Anthrosols is closely related to rice planting and parent materials. Six representative pedons, two from each of three Stagnic Anthrosol subgroups, Vertic Haplic-, Vertic Gleyic-, and Sulfic Gleyic-Stagnic Anthrosols, from different parent materials and soil formation processes, from Liaoning Province, China, were selected and used along with additional supporting data to assess the potential impact in each soil subgroup combination of both pedogenic and anthropogenic factors on the migration and geochemical characteristics of calcium (Ca) and magnesium (Mg) and their relations to soil particle-size composition. Results revealed that exchangeable Mg was correlated positively with clay and silt content, but negatively with sand content, suggesting that clay and silt could retain more exchangeable Mg than sand. Also, in the six pedons exchangeable Ca/Mg ratios generally decreased with depth, which was most likely due to the preferential retention of Mg below the Ap1 horizon and the effects of bio-cycling in rice-soil systems. The pedons with high pH had smaller exchangeable Ca/Mg ratios than those with low pH. Thus, it was concluded that exchangeable Ca/Mg ratios could be helpful in classification of Stagnic Anthrosols.
机译:雄性炭疽气溶胶的形成与水稻种植和母本材料密切相关。从中国辽宁省的不同母体和土壤形成过程中,选择了六个有代表性的脚趾,分别来自三个不同的雄性炭疽亚种,分别是垂直的Haplic-,垂直的Glyic-和硫酸的Ggic-Stagnic的两个亚群。支持性数据,用于评估成因和人为因素在每种土壤亚组组合中对钙(Ca)和镁(Mg)的迁移和地球化学特征及其与土壤粒度组成的关系的潜在影响。结果表明,可交换的镁与黏土和泥沙含量呈正相关,而与沙子含量呈负相关,这表明黏土和粉土比沙子能保留更多的可交换镁。同样,在六个脚架中,可交换的Ca / Mg比例通常随深度而降低,这最有可能是由于Mg优先保留在Ap1水平以下以及水稻-土壤系统中生物循环的影响。高pH值的脚踏板与低pH值的脚踏板相比,可交换的Ca / Mg比更小。因此,得出的结论是,可交换的Ca / Mg比值可能有助于对滞滞性人类气溶胶的分类。

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