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Article Dans Une Revue Groundwater Année : 2012

Field Test of the Superconducting Gravimeter as a Hydrologic Sensor

Résumé

We report on a field test of a transportable version of a superconducting gravimeter (SG) intended for groundwater storage monitoring. The test was conducted over a 6-month period at a site adjacent to a well in the recharge zone of the karstic Edwards Aquifer, a major groundwater resource in central Texas. The purpose of the study was to assess requirements for unattended operation of the SG in a field setting and to obtain a gravimetric estimate of aquifer specific yield. The experiment confirmed successful operation of the SG, but water level changes were small (<0.3 m) leading to uncertainty in the estimate of specific yield. Barometric pressure changes were the dominant cause of both water level variations and non-tidal gravity changes. The specific yield estimate (0.26) is larger than most published values and dependent mainly on low frequency variations in residual gravity and water level time series.

Dates et versions

insu-00702687 , version 1 (31-05-2012)

Identifiants

Citer

Clark R. Wilson, Bridget R. Scanlon, John Sharp, Laurent Longuevergne, Hongqiu Wu. Field Test of the Superconducting Gravimeter as a Hydrologic Sensor. Groundwater, 2012, 50 (3), pp.442-449. ⟨10.1111/j.1745-6584.2011.00864.x⟩. ⟨insu-00702687⟩

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