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伊利石结晶度 Ku ¨bler ,Weaver 和Weber 指数关系式常数的确定与应用

王河锦1,陶晓风2,Rahn Meinert3   

  1. 1. 北京大学 地球与空间科学学院, 北京 100871;2. 成都理工大学 地球科学学院, 成都 610059;3. 瑞士核安全委员会HSK, 5232 Villigen, Switzerland
  • 收稿日期:2007-09-20 修回日期:2007-09-20 出版日期:2007-09-20 发布日期:2007-09-20

Determination of Constants C 1-C 14 in 14 Equations of the Relationships between the K¨ubler,Weaver and Weber Indices and Their Applications

WANG He-jin1, TAO Xiao-feng2, RAHN Meinert3   

  1. 1. School of Earth and Space Sciences, Peking University, Beijing 100871, China;2. College of Earth Sciences, Chengdu University of Technology; Manufacture and Technology Division, Chengdu 610059, China;3. Hauptabteilung fur die Sicherheit der Kernanlagen, 5232 Villigen-HSK, Switzerland
  • Received:2007-09-20 Revised:2007-09-20 Online:2007-09-20 Published:2007-09-20

摘要: 根据衍射峰具有的不同分布特点推导出了14个伊利石结晶度K¨ubler 指数,Weaver 指数和Weber 指数关系式中常数项C 1-C 14的数值,提出了PearsonVII分布中形态参数μ 与C 5,C 6,C 11,C 12的4个定量方程。由此,14个伊利石结晶度指数关系式可直接用于实际计算。根据阿尔卑斯复理石伊利石形态特征Sc=0.731,由这些关系式进 行近变质带上下界线的转换得出与K¨ubler 指数0.42~0.25。△2θ 界线对应的Weaver 指数和Weber 指数的界线值分别为5.8~17.6和300~179。讨论了在自然干燥状态下直接进行伊蒙混层鉴定的基本原理。

Abstract: Constants C 1-C 14 in 14 equations of the relationships between the K¨ubler,Weaver and Weber indices were deduced and calculated. Four formulae of the relationships between exponent u of the Pearson VII function and C 5, C 6, C 11, C 12 were deduced also. Therefore, those 14 equations can be directly used for actual converting analysis. According to the shape parameter Sc=0.731 for the XRD peak of illite from Alpine flysch and using these equations the boundaries of anchizone of Weaver and Weber indices were calculated as 5.8-17.6 and 300-179, respectively.Application in distinguishing illite/smectite mixed-layer phase in air-dried condition was discussed on the basis of the added principle of XRD peaks.