Mitigating Land Subsidence in the Coachella Valley, California, USA: An Emerging Success Story
<p>Groundwater has been a major source of agricultural, municipal, and domestic water supply since the early 1920s in the Coachella Valley, California, USA. Land subsidence, resulting from aquifer-system compaction and groundwater-level declines, has been a concern of the Coachella Valley Wate...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2020-04-01
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Series: | Proceedings of the International Association of Hydrological Sciences |
Online Access: | https://www.proc-iahs.net/382/809/2020/piahs-382-809-2020.pdf |
Summary: | <p>Groundwater has been a major source of agricultural,
municipal, and domestic water supply since the early 1920s in the Coachella
Valley, California, USA. Land subsidence, resulting from aquifer-system
compaction and groundwater-level declines, has been a concern of the
Coachella Valley Water District (CVWD) since the mid-1990s. As a result, the
CVWD has implemented several projects to address groundwater overdraft that
fall under three categories – groundwater substitution, conservation, and
managed aquifer-recharge (MAR). The implementation of three projects in
particular – replacing groundwater extraction with surface water from the
Colorado River and recycled water (Mid-Valley Pipeline project), reducing
water usage by tiered-rate costs, and increasing groundwater recharge at the
Thomas E. Levy Groundwater Replenishment Facility – are potentially linked
to markedly improved groundwater levels and subsidence conditions, including
in some of the historically most overdrafted areas in the southern Coachella
Valley. Groundwater-level and subsidence monitoring have tracked the effect
these projects have had on the aquifer system. Prior to about 2010, water
levels persistently declined, and some had reached historically low levels
by 2010. Since about 2010, however, groundwater levels have stabilized or
partially recovered, and subsidence has stopped or slowed substantially
almost everywhere it previously had been observed; uplift was observed in
some areas. Furthermore, results of Interferometric Synthetic Aperture Radar
analyses for 1995–2017 indicate that as much as about 0.6 m of
subsidence occurred; nearly all of which occurred prior to 2010. Continued
monitoring of water levels and subsidence is necessary to inform the CVWD
about future mitigation measures. The water management strategies
implemented by the CVWD can inform managers of other overdrafted and
subsidence-prone basins as they seek solutions to reduce overdraft and
subsidence.</p> |
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ISSN: | 2199-8981 2199-899X |