Fe (Ⅱ)存在条件下氧化铁-高岭石复合物的形成与转化
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国家自然科学基金项目(40671088, 40471071)和教育部新世纪优秀人才支持计划项目(NCET-08-0781)资助


Formation and transformation of iron oxide-kaolinite association in the presence of Fe (II)
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    摘要:

    氧化铁-高岭石复合物是我国南方土壤的重要组分,也是影响这些土壤理化性质的主要因子。本文以Fe(Ⅱ)为添加剂,研究了晶质氧化铁-高岭石复合物的形成与转化过程及其影响因素。结果表明,Fe(Ⅱ)可加速晶质氧化铁-高岭石复合物的形成,在一定程度上克服了高岭石对晶质氧化铁形成的抑制作用。当Fe(Ⅱ)/Fe(Ⅲ)摩尔比(R)在0.04~0.06时,Fe(Ⅱ)可加速纤铁矿、针铁矿、赤铁矿-高岭石复合物的形成;当R≥0.1时,可快速形成磁铁矿-高岭石复合物。在温度50~60℃、pH5~6条件下,Fe(Ⅱ)可加速纤铁矿、针铁矿-高岭石复合物的形成;温度80℃及中性附近时,可加速赤铁矿-高岭石复合物的形成;pH9时,则形成了磁铁矿-高岭石复合物。高岭石的存在减弱了Fe(Ⅱ)对晶质氧化铁形成的催化效果,也可影响产物类型和结晶形貌。上述结果可为自然环境中氧化铁以及氧化铁-高岭石复合物的形成转化过程提供重要参考。

    Abstract:

    Iron oxide-kaolinite association is an important component of the soils in South China and a critical factor influencing physical and chemical properties of these soils. Hence, formation and transformation processes of crystalline iron oxide-kaolinite association and their influencing factors were studied with Fe (II) as catalyst. Results show that Fe(II) accelerated association of crystalline iron oxide with kaolinite, which offset the inhibiting action of kaolinite to some extent on the formation of crystalline iron oxides When the molar ratio ( R ) of Fe (II) to Fe (III) was in the range of 0.04~0.06, Fe(II) accelerated association of kaolinite with lepidocrocite, goethite and hematite, and when R ≥0.1, magnetite-kaolinite association readily formed. In addition, Fe(II) accelerated association of kaolinite with lepidocrocite and goethite at pH 5~6 and 50~60℃, with hematite at 80℃ and neutral pH, and with magnetite at pH 9. Kaolinite reduced the catalytic effect of Fe(II) on formation of crystalline iron oxides and influenced type and morphology of the iron oxides formed. These findings may serve as valuable reference for the study on formation and transformation of iron oxides and iron oxides-kaolinite associations in natural environments.

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魏世勇,刘茜,刘凡,冯雄汉,谭文峰. Fe (Ⅱ)存在条件下氧化铁-高岭石复合物的形成与转化[J].土壤学报,2010,47(6):1134-1143. DOI:10.11766/trxb200905220230 weishiyong. Formation and transformation of iron oxide-kaolinite association in the presence of Fe (II)[J]. Acta Pedologica Sinica,2010,47(6):1134-1143.

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  • 收稿日期:2009-05-22
  • 最后修改日期:2009-09-09
  • 录用日期:2009-10-09
  • 在线发布日期: 2010-08-31
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