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2014 | OriginalPaper | Buchkapitel

3. Nature of Sensitive Clays from Québec

verfasst von : Jacques Locat, Daniel St-Gelais

Erschienen in: Landslides in Sensitive Clays

Verlag: Springer Netherlands

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Abstract

Quantitative mineralogical analyses of sediment samples from 18 sites in Québec indicate that plagioclase is the most abundant mineral in all soils and that chlorite is generally the dominant clay mineral followed by illite and expandable clays consisting of mixed-layer clays minerals involving vermiculite. The study also illustrates how specific surface area and constitutive water content can be used to evaluate departures from average in the mineralogical composition of sensitive clays. The relationship between activity and specific surface area of sensitive clays shows that when compared to soils from different sedimentary basins that have different mineralogy, they are characterized by a much lower activity and specific surface area.

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Vorheriges Kapitel Chemistry, Sensitivity and Quick-Clay Landslide Amelioration

Nächstes Kapitel Three-Dimensional Quick-Clay Modeling of the Gothenburg Region, Sweden

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Titel: Nature of Sensitive Clays from Québec
verfasst von: Jacques Locat
Daniel St-Gelais
Verlag: Springer Netherlands
Buch: Landslides in Sensitive Clays
Print ISBN: 978-94-007-7078-2

Electronic ISBN: 978-94-007-7079-9

Copyright-Jahr: 2014
DOI: https://doi.org/10.1007/978-94-007-7079-9_3