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Migration behavior of base metal elements in Andosols and the controlling factors

机译:基础金属元素的迁移行为及控制因子

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摘要

Migration behavior of base metal elements in volcanic ash soil (Andosols) profile at two (A and B) sites in Hadano, Kanagawa Prefecture, central Japan was investigated. It was found that the base metal elements in A site which is composed only of Andosols and B site which is composed of Andosols and Loam dissolve considerably from the parent-rock but partially adsorb onto secondary minerals in Andosols. The order of elemental mobility in A site is similar to the adsorption tendency of base metal elements onto iron oxy-hydroxides. It is thought that the migration behavior in A site is controlled by the adsorption onto iron oxyhydroxide, but that in B site is fractionation of solution composition influenced by the adsorption onto iron oxyhydroxide and the ion exchange reaction between downward migrating soilsolution and clay minerals.
机译:日本中部,日本中部,日本中,日本中,日本中部两(A和B)位点的火山灰土壤(Andosols)谱系中基础金属元素的迁移行为。 发现仅由Andosols和B位点组成的位点中的基本金属元素从母体岩石中溶解并且部分地吸附在沙糖溶胶中的二次矿物上。 部位中的元素迁移率的顺序与基础金属元素的吸附趋势类似于铁氧 - 氢氧化物上。 据认为,部位的迁移行为由吸附在铁羟基氧化铁上的吸附来控制,但是在B位点是受吸附在铁羟基氧化铁中受吸附的溶液组合物的分馏和向下迁移的泥土污垢和粘土矿物之间的离子交换反应。

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