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Studies on the mechanisms of fixation and release of ammonium in paddysoils after flooding. I. Effect of iron oxides on ammonium fixation

机译:淹水后水稻土中铵盐固定和释放机理的研究。 I.铁氧化物对铵固定的影响

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Experiments were conducted with two typical paddy soils from China and a vermiculite to study the influence of iron oxides on the fixation and release of ammonium. Removing iron oxides, especially amorphous iron oxides, from the soils favoured the release of non-exchangeable NH4-N and stimulated the fixation of NH4-N in the presence of added (NH4)(2)SO4 Addition of artificial goethite and hematite to the original soils or to the soils free of iron oxides reduced the fixation of NH4+-ions. This effect was also observed with vermiculite. We conclude that the coating of clay minerals with iron oxides has an impact on the diffusion of NH4+-ions into and out of the interlayers of the clay minerals. The reduction and dissolution of iron oxides induced by low redox potential (E-h) after flooding of paddy soils is assumed to be an important mechanism controlling NH4+-fixation in paddy fields.
机译:在中国两种典型的水稻土和a石上进行了实验,研究了氧化铁对铵盐固定和释放的影响。从土壤中去除铁氧化物,特别是非晶态铁氧化物有利于释放不可交换的NH4-N,并在添加(NH4)(2)SO4的情况下刺激了NH4-N的固定。原始土壤或不含铁氧化物的土壤都会减少NH4 +离子的固定。 ver石也观察到了这种效果。我们得出的结论是,用氧化铁对粘土矿物进行涂层处理会影响NH4 +离子向粘土矿物中间层中的扩散和扩散。稻田水淹后低氧化还原电势(E-h)引起的铁氧化物的还原和溶解被认为是控制稻田中NH4 +固着的重要机制。

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