Relative contributions of transient and steady state infiltration during ephemeral streamflow-Reference-Cited by-同舟云学术

Relative contributions of transient and steady state infiltration during ephemeral streamflow

Published:2006-08 Issue:8 Volume:42 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Blasch Kyle W.¹,Ferré Ty P. A.²,Hoffmann John P.¹,Fleming John B.¹

Affiliation:

1. Arizona Water Science Center; U.S. Geological Survey; Tucson Arizona USA

2. Department of Hydrology and Water Resources; University of Arizona; Tucson Arizona USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2005WR004049/fullpdf

Reference34 articles.

1. Recharge to ground water from floods in a typical desert wash, Pinal County, Arizona;Babcock;Trans., AGU,1942

2. Bailey , M. 2002 Analysis of one-dimensional vertical infiltration using heat as a tracer in Rillito Creek, Tucson, Arizona Univ. of Ariz. Tucson

3. Bartolino , J. R. R. G. Niswonger 1999 Numerical simulation of vertical ground-water flux of the Rio Grande from ground-water temperature profiles, central New Mexico U.S. Geol. Surv. Water Resour. Invest. Rep. 99-4212

4. Temperature and moisture content profiling of an ephemeral stream channel in a semiarid watershed: Comparison of vertical infiltration velocities at the onset and cessation of flow;Blasch;Eos Trans. AGU,2000

5. Water Sci. and Appl. Ser.;Blasch,2004

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