1887

Abstract

Crosswell seismic and radar data were acquired at the Boise Hydrogeophysical Research<br>Site (BHRS) as part of an effort to characterize the hydrological property distribution in a<br>heterogeneous alluvial aquifer. The dielectric constant and amplitude attenuation values<br>obtained from inversion of the radar data, as well as the seismic P-wave velocity values<br>obtained from inversion of the seismic data, reveal similar spatial patterns. Comparison of<br>this tomographic information with coincident wellbore logs suggest that the geophysical<br>attributes are sensitive to hydrogeological variations. Information obtained from the radar<br>tomography data were used to produce 2-D, high-resolution images of porosity and electrical<br>conductivity. Comparison of these images with coincident log data reveal that these estimates<br>are reasonable and suggests that the tomography data will be useful at this site for delineating<br>variations in hydrological parameters.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.202.1999_070
1999-03-14
2024-04-28
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.202.1999_070
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error