Titlebook: Clay Mineralogy: Spectroscopic and Chemical Determinative Methods; M. J. Wilson (Head) Book 1994 Chapman & Hall 1994 chemical analysis.min

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Infrared methods,e is so versatile that it can be used both as a source of the physical parameters of crystal lattice determinations, and as a means of eliciting purely empirical qualitative relationships between specimens. It is an intrinsically simple technique that deserves to be more widely used in clay mineralo

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館長(zhǎng)

Electron paramagnetic resonance spectroscopy,nments. It is able to provide information on materials in both liquid and solid phases. The technique is extremely sensitive and under favourable circumstances the detection limit for paramagnetic centres can be as low as 10.–10. spins/g, i.e. well below 1 part per billion (Wertz and Bolton, 1986).

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Chemical analysis, instrumental techniques, such as X-ray diffraction and thermal methods, the identification of clay-mineral phases was accomplished by chemical analysis, supplemented where possible by optical data and physical characteristics such as specific gravity, colour, hardness, etc. However, fine-grained ma

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