Observations of time-dependent meniscus behavior with implications for seismic attenuation in three-phase systems

Details Observations of time-dependent meniscus behavior with implications for seismic attenuation in three-phase systems Observations of time-dependent meniscus behavior with implications for seismic attenuation in three-phase systems

May 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001georl..28.1867b&link_type=abstract

Geophysical Research Letters, Volume 28, Issue 9, p. 1867-1870

Physics

2

Hydrology: Groundwater Quality, Physical Properties Of Rocks: Wave Attenuation

Scientific paper

Meniscus dynamics causing strain energy dissipation in three-phase systems, e.g., partially saturated rocks, is being studied as a method of detecting changes in the chemical composition of these systems. New observations of dynamic menisci and thin films on contaminated and clean surfaces have been made. Thin films on contaminated surfaces were observed to exhibit time-dependent relaxation. We propose that this relaxation is responsible for a poorly understood attenuation peak previously observed in partially saturated, contaminated systems.

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