变差系数法在伊/蒙混层矿物混层有序性判断中的应用
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河北省自然基金项目(D2007000695,D2009000833)


Coefficient of variation and its application in orderliness judgment of illite-montmorillonite mixed-layer mineral
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    摘要:

    基于数理统计理论,利用变差系数对伊/蒙混层矿物的混层结构有序性进行判断。通过对样品进行X射线衍射测试,获得各个样品中伊/蒙混层矿物的特征峰值,并将所得数据作为统计对象,采用变差系数法对所得数据进行统计计算。结果表明6个样品的变差系数均小于0.75,据此可判断所有样品中伊/蒙混层矿物的混层结构为规则混层结构。与采用间隔层数法相比,差异系数法可以较为快捷而准确的判断伊/蒙混层矿物的混层有序性。

    Abstract:

    Order structure of illite-montmorillonite mixed-layer mineral was judged by coefficient of variation,based on mathematical statistics theory.Through the X-ray diffraction,characteristic peak height of illite-montmorillonite mixed-layer mineral was obtained.Being statistical object,these data were progressed in statistical calculation by coefficient of variation method.It was shown that coefficient of variation of 6 samples was below 0.75.Mixed-layer structure of illite-montmorillonite in all samples was regular mixed-layer.Difference coefficient method is rapid and accurate for the judgement of orderliness of illite-montmorillonite mixed-layer mineral,compared with interval coefficient method.

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徐博会,丁述理.变差系数法在伊/蒙混层矿物混层有序性判断中的应用[J].河北工程大学自然版,2009,26(2):59-61

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  • 收稿日期:2008-12-06
  • 最后修改日期:2008-12-06
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  • 在线发布日期: 2015-01-12
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