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contributor authorCarlos G. Ochoa
contributor authorAlexander G. Fernald
contributor authorSteven J. Guldan
contributor authorVincent C. Tidwell
contributor authorManoj K. Shukla
date accessioned2017-05-08T21:49:42Z
date available2017-05-08T21:49:42Z
date copyrightOctober 2013
date issued2013
identifier other%28asce%29he%2E1943-5584%2E0000739.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/63623
description abstractIrrigation percolation can be an important source of shallow aquifer replenishment in arid regions of the southwestern United States. Aquifer recharge derived from irrigation percolation can be more significant in fluvial valleys overlying shallow aquifers, where highly permeable soils allow rapid water infiltration and aquifer replenishment. This study used data from various irrigation experiments and data at the piezometric level to assess the irrigation percolation effects on the recharge of a shallow aquifer in an agricultural valley of northern New Mexico. The water balance method (WBM) and the water table fluctuation method (WTFM) were used to estimate aquifer recharge at the field scale (
publisherAmerican Society of Civil Engineers
titleShallow Aquifer Recharge from Irrigation in a Semiarid Agricultural Valley in New Mexico
typeJournal Paper
journal volume18
journal issue10
journal titleJournal of Hydrologic Engineering
identifier doi10.1061/(ASCE)HE.1943-5584.0000718
treeJournal of Hydrologic Engineering:;2013:;Volume ( 018 ):;issue: 010
contenttypeFulltext


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