Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Effects of single fractures on seismic wave propagation

Conference ·
OSTI ID:7041898
 [1];  [2];  [3]
  1. Lawrence Berkeley Lab., CA (USA)
  2. Purdue Univ., Lafayette, IN (USA). Dept. of Earth and Atmospheric Sciences
  3. Lawrence Berkeley Lab., CA (USA) California Univ., Berkeley, CA (USA). Dept. of Materials Science and Mineral Engineering

Detection and characterization of fractures, joints and faults remains an important problem in mining and geotechnical engineering, as well as in petroleum reservoir engineering. A theoretical model has been developed which predicts the amplitude and group time delay of the transmitted, reflected, and converted waves resulting from a plane wave incident upon a single fracture. It is assumed that seismic stresses are continuous across the interface. Seismic particle displacements, however, are assumed to be discontinuous. For completely dry conditions, the magnitude of the displacement discontinuity is given by the ratio of the seismic stress to the stiffness, {kappa}, of the fracture. If a fluid is present in the fracture, we postulate that, in addition to the displacement discontinuity, a velocity discontinuity exists which is equal to the ratio of the seismic stress to specific viscosity, {eta}. The wave equation has been solved for two sets of boundary conditions, with each set incorporating both specific stiffness and specific viscosity. These boundary conditions have been designated as Kelvin and Maxwell models. 12 refs., 5 figs.

Research Organization:
Lawrence Berkeley Lab., CA (USA)
Sponsoring Organization:
DOE/ER; DOE/RW
DOE Contract Number:
AC03-76SF00098
OSTI ID:
7041898
Report Number(s):
LBL-28442; CONF-900640--4; ON: DE90009191
Country of Publication:
United States
Language:
English