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Glen Feshie (1.1 kyr soil): Crystallization of clays Elsewhere the amorphous reaction products have crystallized K-aluminosilicates:
Conclusions The FIB-TEM technique enable detailed characterisation of naturally weathered mineral surfaces in cross-section. Shap grains weather by stoichiometric dissolution centered on sites reactive by virtue of their composition and/or strain. Any ‘leached layers’ must be
Page 1 and 2: High-resolution characterization of
Page 3 and 4: Models for feldspar weathering
Page 5 and 6: Models for feldspar weathering
Page 7 and 8: Our approach: 100 nm thick cross-se
Page 9 and 10: FIB cross-sectioning Using a 30 kV
Page 11 and 12: FIB milling artifacts Modeling show
Page 13 and 14: Shap alkali feldspars: Reactive sit
Page 15 and 16: Shap alkali feldspars: Etch pit net
Page 17 and 18: Shap alkali feldspars: Microstructu
Page 19 and 20: Glen Feshie alkali feldspars Most g
Page 21 and 22: Glen Feshie feldspars: Weathering p
Page 23: Glen Feshie (1.1 kyr soil): Reconst

presentation (pdf) - University of Glasgow

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