Seismic attenuation in a partially saturated, artificial crack due to restricted contact line motion

Geophysical Research Letters

Volumn 24, Issue 24, 1997, Pages 3309-3312

  Waite, W ^a,c   Moerig, R ^b   Spetzler, H ^a,c  

^a Univ of Colorado ^*  (United States)

^b WESTERNGECO   (United States)

^c UNIVERSITY OF COLORADO   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

DEIONIZED WATER; FLOW OF FLUIDS; STIFFNESS; ATTENUATION; CALCULATIONS; CRACKS; MATHEMATICAL MODELS; MEASUREMENTS; SEISMOLOGY; WAVE EFFECTS;

CONTACT LINE MOTION; FREQUENCY INDEPENDENT; PARTIALLY SATURATED; PHYSICO-CHEMICAL INTERACTIONS; SEISMIC ATTENUATION; STIFFNESS MEASUREMENTS; SURFACE CONTAMINATIONS; THREE PHASE BOUNDARY;

CRACKS; SEISMIC WAVES;

PARTIALLY SATURATED ARTIFICIAL CRACKS;

ATTENUATION; CRACKED MEDIUM; PARTIALLY SATURATED MEDIUM; STIFFNESS; WAVE PROPAGATION;

EID: 0031393967     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/97GL03308     Document Type: Article

References (4)

1. Adamson, A. W., Physical Chemistry of Surfaces, Fifth Ed., Wiley-Interscience, 1990.
2. Cernica, J. N., Strength of materials. Holt, Rinehart and Winston, 1977.
3. White, J. E., Computed seismic speeds and attenuation in rocks with partial gas saturation, Geophysics, 40, 224-232, 1975.
4. Young, G. W., S. H. Davis, A plate oscillating across a liquid interface: Effects of contact angle hysteresis, J. Fluid Mech., 174, 327-356, 1987.