Using hydraulic head, chloride and electrical conductivity data to distinguish between mountain-front and mountain-block recharge to basin aquifers

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Mountain-Block Hydrology and Mountain-Front Recharge

In semiarid climates, a significant component of recharge to basin aquifers occurs along the mountain front. Traditionally called “mountain-front recharge” (MFR), this process has been treated by modelers of basins as a boundary condition. In general, mountain-front recharge estimates are based on the general precipitation characteristics of the mountain (as estimated, e.g., by the chloride mas...

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WATER ABOVE THE MOUNTAIN FRONT – ASSESSING MOUNTAIN-BLOCK RECHARGE IN SEMIARID REGIONS By

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Seasonal recharge components in an urban/agricultural mountain front aquifer system using noble gas thermometry

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ژورنال

عنوان ژورنال: Hydrology and Earth System Sciences

سال: 2018

ISSN: 1607-7938

DOI: 10.5194/hess-22-1629-2018