Encyclopedia of Hydrological Sciences 2005
DOI: 10.1002/0470848944.hsa153
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Groundwater as an Element in the Hydrological Cycle

Abstract: Groundwater commonly is portrayed in diagrams of the hydrological cycle as a single pool of water with simple transfers of water to and from the land surface, oceans, and atmosphere. In reality, groundwater is an integral part of a complex hydrological cycle that involves the continuous movement of water on Earth. We begin with a global perspective on the importance of groundwater in the hydrological cycle and then address the importance of understanding the dynamics of groundwater‐flow systems. We next turn o… Show more

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Cited by 7 publications
(9 citation statements)
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“…Podzemna voda se pojavlja skoraj povsod pod zemeljskim površjem in predstavlja najobčutljivejšo in največjo razpoložljivo zalogo sladke vode v tekočem stanju na Zemlji (Quevauviller, 2008;Lerner, Harris, 2009;Alley, La Baugh, Reilly, 2005). Zaradi velikih zalog, geografske razširjenosti, kakovosti ter neobčutljivosti na sezonska nihanja predstavlja podzemna voda razpoložljiv, varen in obnovljiv vodni vir.…”
Section: Upravljanje S Podzemno Vodo V Slovenijiunclassified
“…Podzemna voda se pojavlja skoraj povsod pod zemeljskim površjem in predstavlja najobčutljivejšo in največjo razpoložljivo zalogo sladke vode v tekočem stanju na Zemlji (Quevauviller, 2008;Lerner, Harris, 2009;Alley, La Baugh, Reilly, 2005). Zaradi velikih zalog, geografske razširjenosti, kakovosti ter neobčutljivosti na sezonska nihanja predstavlja podzemna voda razpoložljiv, varen in obnovljiv vodni vir.…”
Section: Upravljanje S Podzemno Vodo V Slovenijiunclassified
“…So, even if theoretically the rate of natural recharge is irrelevant, it has an indirect influence on the capture: the natural recharge controls the natural predevelopment groundwater discharge, which is subject to capture by pumping wells (Konikow and Leake ). The topic of the influence of the natural recharge in determining the rate of pumping is discussed by several authors (Alley et al ; Kalf and Woolley ; Sophocleous ; Zhou ). According to Zhou (), when the new steady‐state conditions are reached, the following equation can be written: R0+ΔR=Q+Dr where D r is the residual discharge: Dr=D0ΔD …”
Section: Basic Concepts Of Sustainable Yieldmentioning
confidence: 99%
“…The exchange of water between streams and aquifers influences the quality and quantity of water within both domains according to the fluxes and water chemistry of the water moving through the streambed and the changes that occur at the groundwater-surface water interface (Ruehl et al, 2006). These interactions are essential for water supply, water quality and aquatic ecosystems (Sophocleous, 2002;Alley et al, 2006) and thus they are important for the sustainable management of water resources.…”
Section: Figures Back Closementioning
confidence: 99%
“…In lowland rivers, complex heterogeneities Figures of the sediment and therefore the hydraulic conditions, pose a major challenge to use this approach (Krause et al, 2012). Individual precipitation events may change the direction of water exchange between the surface and subsurface on a daily or even shorter time horizon, due to localized recharge near the stream banks, flood peaks moving downstream or transpiration by river bank vegetation (Alley et al, 2006). Highly variable exchange fluxes are reported for intense precipitation seasons (Mendoza et al, 2008;Bartsch et al, 2014).…”
Section: Figures Back Closementioning
confidence: 99%