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Capillarity

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Encyclopedia of Engineering Geology

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

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Definition

Capillarity in soils refers to the upward flow of water above the groundwater table.

This natural phenomenon of prevailing ascent of water in soil pores was compared, from the first decades of research, with the capillary rise of water in fine bore tubes (Fredlund and Rahardjo 1993). In order to describe this state of water movement in soils, a capillary model must be defined in terms of capillary height and capillary pressure (see Fig. 1).

Capillarity, Fig. 1
figure 35 figure 35

Capillary model. (a) Natural situation. (b) Thin tube filled with fine sand. (c) Water pressure distribution. (d) Capillary water distribution

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References

  • Brooks RH, Corey AT (1966) Properties of porous media affecting fluid flow. J Irrig Drain E-ASCE 92(IR2):61–88

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  • Florea MN (1980) Soil and rock mechanics. Ed. Tehnicã, Bucharest. (in Romanian)

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  • Fredlund DG, Rahardjo H (1993) Soil mechanics for unsaturated soils. Wiley, New York

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  • van Genuchten MT (1980) A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Sci Soc Am J 44(5):892–898

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  • Hogentogler CA, Barber ES (1941) Discussion in soil water phenomena. Proc HWY Res Board 21:452–465

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Correspondence to Mihaela Stãnciucu .

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Stãnciucu, M. (2018). Capillarity. 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_42

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