HR: 09:30h
AN: G41A-07    [PDF]
TI: A Coupled Inversion of Pressure and Surface Displacement
AU: * Vasco, D W
EM: dwvasco@lbl.gov
AF: Berkeley Laboratory, Earth Sciences Division/Bldg. 90 1 Cyclotron Road, Berkeley, CA 94720 United States
AU: Karasaki, K
EM: kkarasaki@lbl.gov
AF: Berkeley Laboratory, Earth Sciences Division/Bldg. 90 1 Cyclotron Road, Berkeley, CA 94720 United States
AU: Kishida, k
EM: kishida@toshi.kuciv.kyoto-u.ac,jp
AF: Kyoto University, Department of Civil Engineering, Kyoto, 606-8501 Japan
AB: A coupled inversion of transient pressure observations and surface displacement measurements provides an efficient technique for estimating subsurface permeability variations. The methodology has the advantage of utilizing surface observations, which are typically much less expensive than measurements requiring boreholes. Furthermore, unlike many other geophysical observables, the relationship between surface deformation and reservoir pore fluid volume changes is relatively well understood. Our treatment enables us to partition the estimation problem into a sequence of three linear sub-problems. An application of the approach to a set of tilt and borehole pressure data from the Raymond field site in California illustrates it's efficiency and utility. The observations are associated with a well test in which fluid is withdrawn from a shallow fracture zone. During the test thirteen tiltmeters recorded the movement of the ground surface. Simultaneously, nine transducers measured pressure changes in boreholes intersecting the fracture system. We are able to image a high permeability, north trending channel located within the fracture zone. The existence and orientation of this high permeability feature is substantiated by a semi-quantitative analysis of some 4,000 transient pressure curves.
DE: 1294 Instruments and techniques
DE: 3260 Inverse theory
SC: Geodesy [G]
MN: 2003 Fall Meeting