The extent of lateral water movement in the sediments of a New England Salt Marsh

Models of depth‐averaged hydraulic head are used with data from a water balance study in a New England salt marsh to describe horizontal pore water water fluxes near a creek bank. Three hydrologically distinct regions are identified in the sediment. In the marsh studied, semidiurnal tides may drive...

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Veröffentlicht in:	Water resources research 1988-12, Vol.24 (12), p.2077-2085
1. Verfasser:	Nuttle, William K.
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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