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Aluminum Mobilization by Sulfuric And Nitric Acids for smoe Folish Soils

机译:硫酸和硝酸对轻油污土壤中铝的活化作用

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Study was conducted to determine the influence of sulfuric an nitric acids on the Al solubility for brown, black, peat and calcareous soils. The results show that the amounts of labile aluminum mobilized depend significantly on the soil types and horizons. Much more labile aluminum is mobilized in the brown oil than in the black, peat and calcareous soils. The greatest difference in labile aluminum mobilization is betwee nagriculturally mangaed soils and unfertilized soils. It is apparent that long-term ammonium fertilization significantly increase soil aluminum solubility. The mobilization of labile aluminum inthe soil profile increases also with soil depth. The trivalent aqueous aluminum activity relative to the hydrogne ion activity does not comply with a gibbsite or gibbsite-like mineral solubility ocntrol. In most cases, aluminum mobilization by nitric acid is higher than by sulfuric acid. Nitric acid mobilized less aluminum than sulfuric acid only at high acid concentrations and in soils with high organic matter content.
机译:进行了研究以确定硫酸,硝酸对棕色,黑色,泥炭和石灰质土壤的Al溶解度的影响。结果表明,动员的不稳定铝的含量在很大程度上取决于土壤类型和层位。与黑色,泥炭和石灰质土壤相比,在棕色油中流动的铝要不稳定得多。不稳定的铝动员之间的最大差异是在农业耕作的土壤和未施肥的土壤之间。显然,长期施用铵肥会显着增加土壤铝的溶解度。土壤剖面中不稳定铝的迁移也随土壤深度的增加而增加。相对于水合氢离子活性的三价铝水溶液活性不符合三水铝石或三水铝石类矿物溶解度八氢萘酚。在大多数情况下,硝酸对铝的迁移率高于硫酸。仅在高酸浓度和高有机物含量的土壤中,硝酸迁移的铝少于硫酸。

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