4.2 Article

Iron-bearing smectites: a revised relationship between structural Fe, b cell edge lengths and refractive indices

期刊

CLAY MINERALS
卷 48, 期 1, 页码 97-103

出版社

MINERALOGICAL SOC
DOI: 10.1180/claymin.2013.048.4.06

关键词

smectite; montmorillonite; beidellite; structural iron; cell edge length b; refractive index; turbidity measurement; VIS

资金

  1. German Federal Ministry of Education and Research (BMBF) [03G0707A]

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Structural iron in smectites correlates with the cell edge length b and increases the refractive index. The cell edge length b is usually obtained from the position of the (060) reflection, but in this work we show that such b values differ from the values obtained from Rietveld fits because contributions from (hkl) reflections shift the position of the (060) reflection. The correlation between Fe and cell edge length b was significant (r(2) > 0.99); the relationship is b [angstrom] = 8.9977(0.0035) + 0.1117(0.0032) x Fe-tot. Furthermore, we present for the first time measurements of the refractive index n of Fe-bearing smectites, applying a recently published turbidity method (Weidler & Friedrich, 2007). The refractive index correlates both with structural iron (r(2) = 0.64) and with b (r(2) = 0.94).

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