Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Vionnet, Leticia Beatriz"'
Publikováno v:
Provided by the Department of Hydrology and Water Resources..
The Colorado River Delta (CRD) is a large sedimentary complex within a tectonically active structurally controlled basin. The CRD lies across the U.S.-Mexico international boundary and is traversed by the Colorado River on is way to the Gulf of Calif
Externí odkaz:
http://hdl.handle.net/10150/615772
http://arizona.openrepository.com/arizona/handle/10150/615772
http://arizona.openrepository.com/arizona/handle/10150/615772
Autor:
Vionnet, Leticia Beatriz
A finite element numerical model is developed for the modeling of coupled surface-water flow and ground-water flow. The mathematical treatment of subsurface flows follows the confined aquifer theory or the classical Dupuit approximation for unconfine
Externí odkaz:
http://hdl.handle.net/10150/187414
http://arizona.openrepository.com/arizona/handle/10150/187414
http://arizona.openrepository.com/arizona/handle/10150/187414
Publikováno v:
Provided by the Department of Hydrology and Water Resources..
A finite element numerical model is developed for the modeling of coupled surface-water flow and ground-water flow. The mathematical treatment of subsurface flows follows the confined aquifer theory or the classical Dupuit approximation for unconfine
Externí odkaz:
http://hdl.handle.net/10150/615700
http://arizona.openrepository.com/arizona/handle/10150/615700
http://arizona.openrepository.com/arizona/handle/10150/615700
Publikováno v:
Provided by the Department of Hydrology and Water Resources..
Many hydrologic basins in the southwest have seen their perennial streamflows turn to ephemeral, their riparian communities disappear or be jeopardized, and their aquifers suffer from severe overdrafts. Under -management of ground -water exploitation
Externí odkaz:
http://hdl.handle.net/10150/614152
http://arizona.openrepository.com/arizona/handle/10150/614152
http://arizona.openrepository.com/arizona/handle/10150/614152
Ground-water exploitation in the Upper San Pedro Basin has produced the formation of a cone of depression around the Sierra Vista-Fort Huachuca area. A portion of the mountain front recharge that otherwise would reach the San Pedro River is being int
Externí odkaz:
http://hdl.handle.net/10150/278134
Publikováno v:
Hydrogeology Journal; Jun1998, Vol. 6 Issue 1, p24-32, 9p