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Definition
An aquitard is a leaky confining bed that transmits water at a very slow rate to or from an adjacent aquifer.
Characteristics
Due to their reduced hydraulic conductivity, aquitards permit water to move through at very slow rate as compared to the adjacent aquifers. In particular they permit the vertical (upward or downward) flow of water between underlying and overlying aquifers, depending on the hydraulic gradient. Aquitards differ from aquicludes in that the latter prevent water transmission and can act as a barrier to regional groundwater flow.
Aquitards may transmit quantities of water that are significant in terms of regional groundwater flow, but from which negligible supplies of groundwater can be obtained. Examples of aquitards include fluvial, glaciofluvial, and lacustrine deposits, or poorly fractured sedimentary and crystalline rock.
Water flow through aquitards depends on the hydraulic conductivity and...
References
Cushman JH, Tartakovsky DM (eds) (2017) The handbook of groundwater engineering, 3rd edn. CRC Press/Taylor and Francis Group, Boca Raton, 1092 pages
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Guerra, M. (2018). Aquitard. In: Bobrowsky, P., Marker, B. (eds) Encyclopedia of Engineering Geology. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-12127-7_18-1
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DOI: https://doi.org/10.1007/978-3-319-12127-7_18-1
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