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• W2134429079 abstract "Measurements of the upward advection and pore-water profiles of salinity were made at three coastal settings (the Venice Lagoon, Italy; Jamaica Bay, New York; and Mattituck, New York). Coincident measurements of seepage rates using vented benthic chambers and profiles of salinity in pore water collected with a piezometer are used to quantify the coefficient of dispersive mixing. Three mathematical methods were used to quantify this coefficient: a simple, linearized salt balance and two analytical solutions to the steady-state, one-dimensional, advection-diffusion equation in either a slab or a semi-infinite medium. The majority of dispersive mixing coefficients in fine- to medium-grained silty sand were calculated to be between 0.04 and 0.8 m2 d-1. In some cases, the dispersive mixing seemed to involve small-scale preferred pathways for vertical transport, such as would be the case for bioirrigation, gravitational convection, or salt fingering." @default.
• W2134429079 created "2016-06-24" @default.
• W2134429079 creator A5011878132 @default.
• W2134429079 creator A5032574258 @default.
• W2134429079 date "2009-03-01" @default.
• W2134429079 modified "2023-09-26" @default.
• W2134429079 title "The effect of groundwater advection on salinity in pore waters of permeable sediments" @default.
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• W2134429079 doi "https://doi.org/10.4319/lo.2009.54.2.0630" @default.
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