淹水对两种水稻土氧化层和还原层铁氧化物转化和磷吸附的影响

在实验室条件下对两种水稻土在为期6周的淹水过程中,其氧化层和还原层土壤中还原物质总量(TRS)、草酸盐可提取铁(Fe0)、连二亚硫酸钠-柠檬酸-碳酸氢钠可提取铁(FeDCB)和磷吸附的变化进行了研究。结果表明:淹水可急剧增加新鲜土样中的TRS、Fe0和土壤对磷的吸附,并且还原层土壤的TRS、Fe0和土壤对磷的吸附明显高于氧化层土壤。TRS、Fe0和磷吸附之间存在着极显著的相关关系,表明淹水过程中土壤Eh的下降、致使FeDCB向结晶度差的Fe0转化是导致土壤对磷吸附显著增加的主要原因。...

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Veröffentlicht in:Zhejiang daxue xue bao. Journal of Zhejiang University. Agriculture and life sciences. Nong ye yu sheng ming ke xue ban 2002, Vol.28 (5), p.485-491
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container_title Zhejiang daxue xue bao. Journal of Zhejiang University. Agriculture and life sciences. Nong ye yu sheng ming ke xue ban
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creator 章永松 林咸永
description 在实验室条件下对两种水稻土在为期6周的淹水过程中,其氧化层和还原层土壤中还原物质总量(TRS)、草酸盐可提取铁(Fe0)、连二亚硫酸钠-柠檬酸-碳酸氢钠可提取铁(FeDCB)和磷吸附的变化进行了研究。结果表明:淹水可急剧增加新鲜土样中的TRS、Fe0和土壤对磷的吸附,并且还原层土壤的TRS、Fe0和土壤对磷的吸附明显高于氧化层土壤。TRS、Fe0和磷吸附之间存在着极显著的相关关系,表明淹水过程中土壤Eh的下降、致使FeDCB向结晶度差的Fe0转化是导致土壤对磷吸附显著增加的主要原因。
doi_str_mv 10.3321/j.issn:1008-9209.2002.05.005
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subjects 土壤吸附
氧化层
水稻土
淹水
物质转化
磷吸附
还原层
铁氧化物
title 淹水对两种水稻土氧化层和还原层铁氧化物转化和磷吸附的影响
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