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Compression

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Encyclopedia of Engineering Geology

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

Synonyms

Compressibility; Consolidation; Deformation; Settlement; Volume reduction

Definition

Reduction of volume primarily through rearrangement of soil grains in a soil mass from shear and sliding at inter-particle contacts, disruption of particle aggregations, grain crushing, and expulsion of water from the voids of the soil.

Introduction

Soil is a multiphase medium consisting of mineral grains which enclose voids that may be filled with gas, liquid, or a combination of both. For most soils, the gas is air and the liquid is water. When stress is applied to a soil sample, its volume decreases. Loads giving rise to stresses can be due to weight of foundations, superstructure, chemical and moisture environments, and temperature. The effects of stress changes are generally the most important and the most studied. Change in volume of the soil mass may be due to: (a) compression of the solid soil particles, (b) compression of liquid/water and air within the voids, or (c) escape of water...

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Correspondence to Joseph B. Adeyeri .

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Adeyeri, J.B. (2018). Compression. 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_63

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