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Read Full Article (file size: 1104195 bytes) Cited by
WATER RESOURCES RESEARCH,
VOL. 43,
W08421,
doi:10.1029/2006WR005389,
2007
Analysis of pumping-induced unsaturated regions beneath a perennial river
Grace W. Su
Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California, USA
James Jasperse
Sonoma County Water Agency, Santa Rosa, California, USA
Donald Seymour
Sonoma County Water Agency, Santa Rosa, California, USA
James Constantz
U.S. Geological Survey, Menlo Park, California, USA
Quanlin Zhou
Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California, USA
Abstract
The presence of an unsaturated region beneath a streambed during groundwater pumping near streams can reduce the pumping capacity,
change flow paths, and alter the types of biological transformations in the streambed sediments. A three-dimensional, multiphase
flow model of two horizontal collector wells along the Russian River near Forestville, California, was developed to investigate
the impact of varying the ratio of the aquifer to streambed permeability on (1) the formation of an unsaturated region beneath
the stream, (2) the pumping capacity, (3) stream water fluxes through the streambed, and (4) stream water traveltimes to the
collector wells. The aquifer to streambed permeability ratio at which the unsaturated region was initially observed ranged
from 10 to 100. The size of the unsaturated region beneath the streambed increased as the aquifer to streambed permeability
ratio increased. The simulations also indicated that for a particular aquifer permeability, decreasing the streambed permeability
by only a factor of 2–3 from the permeability where desaturation initially occurred resulted in reducing the pumping capacity.
In some cases, the stream water fluxes increased as the streambed permeability decreased. However, the stream water residence
times increased and the fraction of stream water that reached that the wells decreased as the streambed permeability decreased,
indicating that a higher streambed flux does not necessarily correlate to greater recharge of stream water around the wells.
Received 31
July
2006;
accepted 24
May
2007;
published 22
August
2007.
Keywords: surface-groundwater interactions.
Index Terms: 1830 Hydrology: Groundwater/surface water interaction; 1847 Hydrology: Modeling; 1880 Hydrology: Water management (6334).
Read Full Article (file size: 1104195 bytes) Cited by
Citation: Su, G. W., J. Jasperse, D. Seymour, J. Constantz, and Q. Zhou
(2007),
Analysis of pumping-induced unsaturated regions beneath a perennial river,
Water Resour. Res.,
43,
W08421,
doi:10.1029/2006WR005389.
Copyright 2007 by the American Geophysical Union.
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