首页> 美国卫生研究院文献>International Journal of Environmental Research and Public Health >Immobilization of Lead Migrating from Contaminated Soil in Rhizosphere Soil of Barley (Hordeum vulgare L.) and Hairy Vetch (Vicia villosa) Using Hydroxyapatite
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Immobilization of Lead Migrating from Contaminated Soil in Rhizosphere Soil of Barley (Hordeum vulgare L.) and Hairy Vetch (Vicia villosa) Using Hydroxyapatite

机译:利用羟基磷灰石固定化大麦(Hordeum vulgare L.)和毛V菜(Vicia villosa)的根际土壤中污染土壤中的铅迁移

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摘要

This study conducted plant growth tests using a rhizobox system to quantitatively determine the distance of immobilization lead migrating from contaminated soil into uncontaminated rhizosphere soil, and to assess the lead phases accumulated in rhizosphere soil by sequential extraction. Without the hydroxyapatite, exchangeable lead fractions increased as the rhizosphere soil got closer to the contaminated soil. Exchangeable lead fractions were higher even in the rhizosphere soil that shares a boundary with the root surface than in the soil before being planted. Thus, plant growth of hairy vetch was lower in the soil without the hydroxyapatite than in the soil with the hydroxyapatite. The presence of hydroxyapatite may immobilize the majority of lead migrating from contaminated soil into the rhizosphere soil within 1 mm from the contaminated soil. The dominant lead fraction in the rhizosphere soil with the hydroxyapatite was residual. Thus, plant growth was not suppressed and the lead concentration of the plant shoot remained at the background level. These results indicate that the presence of hydroxyapatite in the rhizosphere soil at 5% wt may immobilize most of the lead migrating into the rhizosphere soil within 1 mm from the contaminated soil, resulting in the prevention of lead migration toward the root surface.
机译:这项研究使用根瘤菌系统进行了植物生长试验,定量确定了固定化铅从污染土壤迁移到未污染根际土壤的距离,并通过顺序提取来评估在根际土壤中积累的铅相。如果没有羟基磷灰石,可交换的铅含量会随着根际土壤越来越靠近污染土壤而增加。甚至在与根表面具有边界的根际土壤中,可交换的铅含量也比种植前的土壤中的高。因此,在没有羟基磷灰石的土壤中,有毛紫菜的植物生长低于在有羟基磷灰石的土壤中的生长。羟基磷灰石的存在可能会使大部分铅从污染土壤迁移到距污染土壤1毫米内的根际土壤中。残留的含羟基磷灰石的根际土壤中的铅占主导地位。因此,植物生长没有受到抑制,并且植物茎中的铅浓度保持在背景水平。这些结果表明,在根际土壤中5%重量的羟基磷灰石的存在可能使大部分铅迁移到距污染土壤1毫米内的根际土壤中,从而防止了铅向根表面迁移。

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