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• W2150517102 abstract "The effects of earthquakes on baseflow, the component of streamflow provided by groundwater, are analyzed for streams that exhibit large coseismic increases in streamflow and discharge large volumes of excess water. Although discharge Q may increase rapidly, the rate of baseflow recession dlogQ/dt is unchanged suggesting that the hydraulic conductivity of groundwater system providing baseflow does not change. For (at least) the studied streams, the coseismic increase of discharge therefore requires increased hydraulic head gradients resulting from the rapid release of water from some source of storage. The relationship between the response of streams, earthquake magnitude, and the distance of the drainage basin from the epicenter, is consistent with subsurface liquefaction being the mechanism that increases head gradients." @default.
• W2150517102 created "2016-06-24" @default.
• W2150517102 creator A5004170702 @default.
• W2150517102 date "2001-05-15" @default.
• W2150517102 modified "2023-10-16" @default.
• W2150517102 title "Origin of postseismic streamflow changes inferred from baseflow recession and magnitude-distance relations" @default.
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• W2150517102 doi "https://doi.org/10.1029/2000gl012481" @default.
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