TIDAL FLUCTUATIONS IN A LEAKY CONFINED AQUIFER: LOCALISED EFFECTS OF AN OVERLYING PHREATIC AQUIFER

dc.contributor.author	Li L.
dc.contributor.author	Jeng D.S.
dc.contributor.author	Barry D.A.
dc.date.accessioned	2021-04-19T23:58:30Z
dc.date.available	2021-04-19T23:58:30Z
dc.date.issued	2002
dc.description.abstract	Damping of tidal head fluctuations in a leaky confined coastal aquifer is enhanced by leakage into an overlying phreatic aquifer. We show that the phreatic aquifer is, however, resistant to the leakage flow and in particular, a deep phreatic aquifer can reduce the leakage effects significantly. An analytical solution, based on a vertical flow model for the phreatic aquifer, is derived for quantifying the role of this upper free water body in tidal propagation in the lower semi-confined aquifer.
dc.identifier	https://www.elibrary.ru/item.asp?id=1106323
dc.identifier.citation	Journal of Hydrology, 2002, 265, 1-4, 283-287
dc.identifier.issn	0022-1694
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/28111
dc.subject	SEMI-CONFINED AQUIFER
dc.subject	PHREATIC AQUIFER
dc.subject	TIDAL FLUCTUATIONS
dc.subject	LEAKAGE
dc.title	TIDAL FLUCTUATIONS IN A LEAKY CONFINED AQUIFER: LOCALISED EFFECTS OF AN OVERLYING PHREATIC AQUIFER
dc.type	Статья

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