摘要
对含硒(Se)土样进行淹水培养,运用连续提取法和X射线光电子能谱分析(XPS)技术,揭示淹水处理过程中土壤硒和铁氧化物的形态转化过程。结果表明,土壤氧化还原电位(Eh值)对土壤硒形态转化起主导作用,淹水培养过程中的水溶态和可交换态硒含量逐渐降低,元素态和残渣态硒含量逐渐增高;XPS分析结果表明,淹水15 d后土壤中Se(Ⅳ)占总硒的百分比由59.7%下降到48.3%,元素态和金属硒化物的含量分别升高了6.3百分点和5.1百分点。同时,淹水过程中土壤还原性铁含量增加,且铁氧化物晶体结构发生了变化。综上所述,土壤Eh值为影响硒活性的主要因素,Eh值对土壤硒形态转化起主导作用,土壤氧化性越强,土壤中硒的活性也越强。在淹水条件下土壤处在还原状态,土壤中硒的移动性逐渐减弱,生物有效性降低。
引文
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