Datapages, Inc.Print this page

Shallow Water Injection Monitoring in Vuggy Pores Using Ground-Penetrating Radar and Cross-Hole Tomography, Pipe Creek, Texas

Zahm, Chris 1; Tsoflias, Georgios P.2; Petersen, Kelly 2; Janson, Xavier 1
1 Bureau of Economic Geology, The University of Texas at Austin, Austin, TX.
2 Department of Geology, The University of Kansas, Lawerence, KS.

Large vuggy pores represent a significant challenge for flow property characterization in subsurface reservoirs. Touching vugs are fast permeability pathways and permeability calculations are highly scale dependent. We used both surface and down-hole ground-penetrating radar (GPR) to constrain the shape of a gravity-injected water plume at the Cretaceous (Albian) Pipe Creek site in Central Texas. Five wells were drilled to collect core for facies description and they were used to monitor pressure changes in a thin, perched aquifer during injection. Approximately 1300 gallons of water was injected in one well that was completed open hole from 1.5 to 7.6 meters depth below surface. Water pressure changes were monitored in the four other wells that were all spaced greater than 7.8 meters away from the injection well.

A 2D GPR grid was acquired prior to and near completion of the water injection. This grid was interpreted and processed for amplitude anomalies created by the water injection. Mapping the amplitude amoaly in the surface GPR reveals the areal extent of the water injection front. Downhole GPR was acquired in incremented time steps during injection. Zero offset profiles were processed to determine the lag time effect created by the injected water into the vuggy facies. From the cross-hole tomography we were able to determine the cross-sectional area that was affected during water injection. Integrating the surface and cross hole GPR data, along with the water injection rate, allows us to calculate a more precise effective permeability of 1.2 darcy for the rudist rudstone facies. This value is consistent with other measurements of this facies from conventional core analysis, but represents a three-fold increase from gas tracer experiments conducted within twinned wells spaced 1.5 meters apart.

 

AAPG Search and Discovery Article #90090©2009 AAPG Annual Convention and Exhibition, Denver, Colorado, June 7-10, 2009