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Field Observed Relationship between Soil Metal Speciation and Precipitation Events: What It Implies?

机译:现场观察到的土壤金属形态与降水事件之间的关系:这意味着什么?

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@@ INTRODUCTION Metals in soil, especially the heavy metals in arable land, has raised wide concerns about its spatial translocation and entrance to crops. Either of the two aspects is intimately connected to the metals' lability, the nature to migrate, which is determined in large part by the chemical status of the metals. Specifically, one metal in soil can have 4 species with residual component disregarded, the exchangeable component, the carbonates bound component, the Fe-Mn oxides bound component, and the organic bound component. From the perspective of lability, the exchangeable species is the most migratory, followed by the carbonates bound species, which is readily transformed to the exchangeable under a weakly acidic environment; in contrast, the Fe-Mn oxides bound component and the organic bound component are generally more reluctant to migrate. Hence, it is critical to discover the law underlying the variation among the metal species in actual cropland soil.
机译:@@引言土壤中的金属,尤其是耕地中的重金属,引起了人们对其空间易位和农作物进入的广泛关注。这两个方面中的任何一个都与金属的不稳定性,迁移的性质紧密相关,这在很大程度上取决于金属的化学状态。具体而言,土壤中的一种金属可以具有4种物质,而忽略了残留组分,可交换组分,碳酸盐结合的组分,Fe-Mn氧化物结合的组分和有机结合的组分。从不稳定性的角度来看,可交换物种是最易迁徙的,其次是碳酸盐键合物种,在弱酸性环境下,它们很容易转变为可交换物种。相反,Fe-Mn氧化物结合的组分和有机结合的组分通常更不迁移。因此,至关重要的是要发现实际农田土壤中金属种类之间的差异所依据的定律。

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