Publication: Research - peer-review › Conference abstract in proceedings – Annual report year: 2009
A change in soil water content is a change in mass stored in the subsurface. Given that the mass change is big enough, the change can be measured with a gravity meter. Attempts have been made with varying success over the last decades to use ground-based time-lapse gravity measurements to infer hydrogeological parameters. These studies focused on the saturated zone with specific yield as the most prominent target parameter. Any change in storage in the vadose zone has been considered as noise. Our modeling results show a measureable change in gravity from the vadose zone during a forced infiltration experiment on 10m by 10m grass land. Simulation studies show a potential for vadose zone model calibration using gravity data in conjunction with other geophysical data, e.g. cross-borehole georadar. We present early field data and calibration results from a forced infiltration experiment conducted over 30 days and discuss the potential for gravity measurements in vadose zone model parameter estimation.
|Title of host publication||AGU Fall Meeting Abstracts|
|Publisher||American Geophysical Union|
|State||Published - 2009|
|Event||American Geophysical Union Fall Meeting 2009 - San Francisco, United States|
|Conference||American Geophysical Union Fall Meeting 2009|
|Period||14/12/2009 → 18/12/2009|