Definition
Wells are excavations into the earth for developing groundwater, oil, brine, gas, and engineering geology operations (Driscoll 1986; Hunt 2005).
Water wells are dug, driven, bored, or drilled into the saturated zone of water-bearing formations (aquifers) to extract groundwater for drinking and irrigation (Barrocu 2014; Campbell and Lehr 1973).
Shallow water wells are excavated into lose and soft rocks by hand, or mechanically, mainly in unconfined aquifers. They are rarely deeper than 50–60 m, normally with a circular section of 1–3.5 m in diameter. One supports their walls with masonry or a precast concrete ring lining to prevent collapsing. The lining often extends above the ground to prevent people from falling into the well and to reduce contamination.
In dug wells , if the water table lowers below their bottom, one can use the existing well as the fore shafts of new wells drilled down below the new water level (Fig. 1). In the ancient past, water was brought to the...
References
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Barrocu G (2014) Chapter 12, groundwater hydrology: saturation zone. In: Eslamian S (ed) Handbook of engineering hydrology, fundamentals, and applications, vol 1. CRC Press/Taylor & Francis Group, Boca Raton, pp 221–249. ISBN:13: 978-1-4665-5244-9 (eBook – PDF)
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Barrocu, G., Eslamian, S., Ostad-Ali-Askari, K., Singh, V.P. (2018). Wells. 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_297-1
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