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Residual Soils

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Encyclopedia of Engineering Geology

Synonyms

Alteration products; Lateritic soils; Saprolites; Weathering products

Definition

Residual soil is the material resulting from the in situ weathering of the parent rock.

Residual soils are distributed throughout many regions of the world, such as Africa, South Asia, Australia, Southeastern North America, Central and South America, and considerable regions of Europe. The largest areas and thickness of these soils occur normally in humid tropical regions, such as Brazil, Nigeria, South India, Singapore, and the Philippines.

Characteristics

According to Duarte (2002), the diversity exhibited by residual soils is due, not so much to the lithology of the original rock, but mainly to external factors such as climate, topography, and vegetation cover; factors that provide distinctive weathering processes and, consequently, distinctive weathering products – the residual soils. At the first International Conference on Tropical Residual Soils, it was proposed to divide such soils into...

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References

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  • Duarte IMR (2002) Solos residuais de rochas granitóides a Sul do Tejo. Características geológicas e geotécnicas [Residual soils of granitoid rocks to south of the Tagus River. Geological and geotechnical characteristics]. (Unpublished Doctoral Dissertation, in Portuguese). University of Évora, Évora, Portugal

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Correspondence to Isabel M. R. Duarte .

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Duarte, I.M.R., Rodrigues, C.M.G. (2018). Residual Soils. In: Bobrowsky, P.T., Marker, B. (eds) Encyclopedia of Engineering Geology. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-73568-9_237

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