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Estimating specific yield and storage change in an unconfined aquifer using temporal gravity surveys
Author(s) -
Gehman Carter L.,
Harry Dennis L.,
Sanford William E.,
Stednick John D.,
Beckman Nathaniel A.
Publication year - 2009
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2007wr006096
Subject(s) - groundwater recharge , aquifer , groundwater , water table , hydrology (agriculture) , water level , geology , drawdown (hydrology) , infiltration (hvac) , environmental science , soil science , geotechnical engineering , geography , meteorology , cartography
Two high‐precision gravity surveys were conducted to determine groundwater mass changes at a managed groundwater recharge site in northeastern Colorado. Gravity data were collected during pumping and two months after pumping ceased. During pumping, gravity was lower by as much as 46 μ Gal near the pumping wells and higher by as much as 90 μ Gal near the recharge ponds in comparison to data collected after pumping had ceased. These differences are attributed to changes in groundwater mass associated with drawdown and infiltration. Inverse modeling of the gravity data indicates a 5.1 × 10 5 m 3 decrease in storage beneath the recharge ponds between the two surveys, which we attribute to dissipation of the groundwater mound created by recharge during pumping. This estimate of the change in groundwater storage is made independently of assumptions of physical properties of the aquifer. Dividing the change in water volume per unit area determined from the gravity modeling by the change in water level measured in wells provides an estimate of specific yield (S y ) of 0.21 ± 0.03, which is within the range of specific yield estimates derived from aquifer tests at the site. Water level changes predicted from the gravity data agree on average to within ±0.45 m of those measured, which we take to be an estimate of the uncertainty in water table depth predictions that can be obtained from gravimetric data in unconfined aquifers. The study covers a 3.2 km 2 area, providing a prototype for similar studies at larger scales.