红壤中铝、锰和铁在酸雨作用下的释放特征
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X517 S153.6

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国家自然科学基金资助项目(批准号:49973031)


Release of Al, Mn and Fe from Red Soils under Influence by Simulated Acid Rain
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    摘要:

    酸雨作用下红壤中Al、Mn和Fe的释放大多具有阶段性特征,旦土壤不同,其阶段性特征存在明显的差异。多数情况下同一土壤中Al和Fe的阶段性释放特征较为相似。3种元素累积释放量(Q)随淋溶量(H)的变化符合二次模型:Q=A B1H B2H2。经过9150~10650mm的酸雨淋溶以后,与对照(pH5.6)相比,pH4.5的酸雨使Al累积释放量增加8.16%~87.49%,Mn增加-4.29%~24.75%,Fe增加5.78%~86.03%;pH3.5的酸雨使Al累积释放量增加68.59%~158.60%,Mn增加26.11%~205.53%,Fe增加8.48%~138.88%。3种元素对酸雨的敏感性依次是:Al>Fe>Mn。其累积释放量在不同土壤之间表现出基本一致的特点:Al和Mn的释放量较为接近,且远远大于Fe的释放量。

    Abstract:

    The releases of metal elements Al, Mn and Fe appeared phase characteristics, but the phase characteristics were very different among various soils. In most cases, the release processes of Al, Fe were very similar. The relation between cumulative release amount of the three metal elements can been described with Q=A B_1H B_2H~2. After simulating rainfall of 9 150~10 650 mm, compared with the control, pH4.5 acid rain enhanced cumulative release amount of Al 8.16%~87.49%,Mn -4.29%~24.75%, Fe 5.78%~86.03%. pH3.5 acid rain enhanced cumulative release amount of Al 68.59%~158.60%, Mn 26.11%~205.53%, Fe 8.48%~(138.88)%. The sensitivity of metal elements release to acid rain was Al>Fe>Mn. There was a similar characteristic of cumulative release of the three metal elements: the release amount of Al was close to the release amount of Mn, and was far bigger than that of Fe.

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许中坚 徐冬梅 刘广深 刘维屏.红壤中铝、锰和铁在酸雨作用下的释放特征[J].水土保持学报,2004,(3):20~23,27

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