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Transactions of the INDIAN CERAMIC SOCIETY   Vol. 51  1992
X-ray Diffraction Study of Layer Shift in Chlorites by Fourth Moment
A.K.DE
Pages : 35-36
DOI : 10.1080/0371750X.1992.10804529
Abstract
An expression connecting the fourth central moment or an X -ray diffraction line profile with the particle size and stacking disorders of the type ortayerdisplacement In the specimen studied, has been derived on the supposition that the line broadening Is due to particle size as well as stacking disorders of the above type. It has been shown that from a single reflection, the defect parameter can be easily calculated and the method can be utilised as widely as the method of second moment (I.e. variance) in the study or disorders In layer silicate clay minerals.
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