Describes geological materials rich in clay: shales for example. Not normally applied to soils, the roughly equivalent term in pedology being argillic, as in argillic horizon. Soils developed on argillaceous materials tend to be heavy, with clay minerals inherited or derived from sheet silicates in the parent rock. Where soils have developed on so-called “black” (i.e., organic-rich) shales, elements such as Cu, Mo, Ni, Zn, Cr, V, As and F, may be present in toxic amounts (e.g., Fang et al., 2001).
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Bibliography
Fang, W., Hu, R., and Wu, P., 2001. Influence of black shales on soils and edible plants in the Ankang Area, Shaanxi Province, P. R. of China. Environ. Geochem. Health, 24: 35–46.
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2008 Springer
About this entry
Cite this entry
(2008). Argillaceous. In: Chesworth, W. (eds) Encyclopedia of Soil Science. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3995-9_35
Download citation
DOI: https://doi.org/10.1007/978-1-4020-3995-9_35
Published:
Publisher Name: Springer, Dordrecht
Print ISBN: 978-1-4020-3994-2
Online ISBN: 978-1-4020-3995-9
eBook Packages: Earth and Environmental ScienceReference Module Physical and Materials ScienceReference Module Earth and Environmental Sciences