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• W1999973399 abstract "[1] We know little regarding how geomorphological features along the surface-groundwater interface collectively affect water quality and quantity. Simulations of surface water-groundwater exchange at increasing scales across bed forms, bars and bends, and basins show that groundwater has a power-law transit time distribution through all these features, providing a purely mechanistic foundation and explanation for temporal fractal stream chemistry. Power-law residence time distributions are almost always attributed to spatial variability in subsurface transport properties- something we show is not necessary. Since the different geomorphological features considered here are typical of most landscapes, fractal stream chemistry may be universal and is a natural consequence of water exchange across multifaceted interfaces." @default.
• W1999973399 created "2016-06-24" @default.
• W1999973399 creator A5049326709 @default.
• W1999973399 date "2008-04-17" @default.
• W1999973399 modified "2023-10-10" @default.
• W1999973399 title "Surface water-groundwater interface geomorphology leads to scaling of residence times" @default.
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• W1999973399 doi "https://doi.org/10.1029/2008gl033753" @default.
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