HR: 0800h
AN: H21F-1094    [Abstracts]
TI: Estimating Natural Recharge in a Desert Environment Facing Increasing Ground-Water Demands
AU: * Nishikawa, T
EM: tnish@usgs.gov
AF: U.S. Geological Survey, 5735 Kearny Villa Rd. Suite O, San Diego, CA 92123 United States
AU: Izbicki, J A
EM: jaizbick@usgs.gov
AF: U.S. Geological Survey, 5735 Kearny Villa Rd. Suite O, San Diego, CA 92123 United States
AU: Hevesi, J A
EM: jhevesi@usgs.gov
AF: U.S. Geological Survey, 6000 J St. Placer Hall, Sacramento, CA 95819 United States
AU: Martin, P
EM: pmmartin@usgs.gov
AF: U.S. Geological Survey, 5735 Kearny Villa Rd. Suite O, San Diego, CA 92123 United States
AB: Ground water historically has been the sole source of water supply for the community of Joshua Tree in the Joshua Tree ground-water subbasin of the Morongo ground-water basin in the southern Mojave Desert. Joshua Basin Water District (JBWD) supplies water to the community from the underlying Joshua Tree ground-water subbasin, and ground-water withdrawals averaging about 960 acre-ft/yr have resulted in as much as 35 ft of drawdown. As growth continues in the desert, ground-water resources may need to be supplemented using imported water. To help meet future demands, JBWD plans to construct production wells in the adjacent Copper Mountain ground-water subbasin. To manage the ground-water resources and to identify future mitigating measures, a thorough understanding of the ground-water system is needed. To this end, field and numerical techniques were applied to determine the distribution and quantity of natural recharge. Field techniques included the installation of instrumented boreholes in selected washes and at a nearby control site. Numerical techniques included the use of a distributed-parameter watershed model and a ground-water flow model. The results from the field techniques indicated that as much as 70 acre-ft/yr of water infiltrated downward through the two principal washes during the study period (2001-3). The results from the watershed model indicated that the average annual recharge in the ground-water subbasins is about 160 acre-ft/yr. The results from the calibrated ground-water flow model indicated that the average annual recharge for the same area is about 125 acre-ft/yr. Although the field and numerical techniques were applied to different scales (local vs. large), all indicate that natural recharge in the Joshua Tree area is very limited; therefore, careful management of the limited ground-water resources is needed. Moreover, the calibrated model can now be used to estimate the effects of different water-management strategies on the ground-water subbasins.
DE: 1655 Water cycles (1836)
DE: 1803 Anthropogenic effects
DE: 1829 Groundwater hydrology
SC: Hydrology [H]
MN: 2004 AGU Fall Meeting