How to get 3-D accuracy with a 2-D stream-aquifer interaction model (or "The turning resistance factor in river seepage")

dc.contributor.author	Morel-Seytoux, Hubert J., author
dc.contributor.author	Colorado State University, publisher
dc.date.accessioned	2020-02-05T21:46:48Z
dc.date.available	2020-02-05T21:46:48Z
dc.date.issued	2008
dc.description	2008 annual AGU hydrology days was held at Colorado State University on March 26 - March 28, 2008.
dc.description.abstract	Close to a river the traditional groundwater Dupuit assumption of horizontal flow does not hold. In order to treat the problem accurately one would need to use a 3-dimensional numerical model with small cells in the vicinity of the river. Presented here is an analytic approximate way to avoid this extra complication and still describe accurately the exchange flow between the stream and the aquifer.
dc.format.medium	born digital
dc.format.medium	proceedings (reports)
dc.identifier.uri	https://hdl.handle.net/10217/200695
dc.identifier.uri	http://dx.doi.org/10.25675/10217/200695
dc.language	English
dc.language.iso	eng
dc.publisher	Colorado State University. Libraries
dc.relation.ispartof	Hydrology Days
dc.rights	Copyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.title	How to get 3-D accuracy with a 2-D stream-aquifer interaction model (or "The turning resistance factor in river seepage")
dc.title.alternative	Hydrology days 2008
dc.title.alternative	AGU hydrology days 2008
dc.type	Text

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