狭缝系统与伊利石结晶度Kuebler指数的测定及相关问题讨论
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P581 P588.3

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本文为国家自然科学基金资助项目(编号 49872033)成果之一。


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    摘要:

    根据实验结果,衍射峰半高宽随接收狭缝增大而呈二次工线线性增大。扫描速度与扫描步长的确定应遵守Wang(1994)提出的关系式,并确定在相对误差小于〈5%的范围内。固定样品条件,选定最优实验条件下使用国际标样标定系统偏差是伊利石结晶测量中必不可少的重要步骤。不固定样品条件和实验条件,同一样品的伊利石工值将因条件的变化而不同;固定样品和实验条件而不使用国际标样标定系统偏差,则无法与他人数据进行对比,其

    Abstract:

    Based on the analysed result, there established a curve relationship between the receiving slit (Rs) of a diffractometer and FWHM, i. e. FWHM = ARs2 BRs C. The methods based on Wang's formulae (1994) to evaluate the error levels caused by the scanning speed and step size in FWHM and maximum intensity of an XRD peak were described. These errors induced by the step size and scanning speed should be below 5 %. Reviews of sample preparation, X-ray diffraction setting and the role played by interlaboratory IC standards were given, involving (1) determining sample geometric conditions, choosing optimum instrumental settings and using interlaboratory illite crystallinity standards are the most important procedures in the measurement of illite crystallinity; (2) the IC value from the same sample will vary with the changes of such geometric conditions and instrumental settings; (3) IC values without correction for the IC standards (Kisch, 1991, Warr et al. , 1994) cannot be comparable with each other and (4) this will mislead the research when the boundaries of the anchizone are derived from these uncorrected IC values.

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王河锦 徐庆生.2000.狭缝系统与伊利石结晶度Kuebler指数的测定及相关问题讨论[J].地质论评,46(6):588-593,[DOI].
Wang Hejing Zhu Mingxin Xu Qingsheng Liu Chuxiong Bian Zhihong) Department of Geology, Peking University, Beijing,) Institute of Mineral Deposits, Chinese Academy of Geological Sciences, Beijing, ) Hubei Experimental Institute of Geology, Wuhan,.2000.[J]. Geological Review,46(6):588-593.

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