Factors influencing surface water and groundwater interaction in alluvial fan

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Case studies of groundwater – surface water interactions and scale relationships in small alluvial aquifers

An alluvial aquifer can be described as a groundwater system, generally unconfined, that is hosted in laterally discontinuous layers of gravel, sand, silt and clay, deposited by a river in a river channel, banks or flood plain. In semi-arid regions, streams that are associated with alluvial aquifers tend to vary from discharge water bodies in the dry season, to recharge water bodies during cert...

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ژورنال

عنوان ژورنال: Journal of Water and Climate Change

سال: 2020

ISSN: 2040-2244,2408-9354

DOI: 10.2166/wcc.2020.174