Changes in the permeability, streaming potential and resistivity of a claystone from the Nankai prism under stress

Details Changes in the permeability, streaming potential and resistivity of a claystone from the Nankai prism under stress Changes in the permeability, streaming potential and resistivity of a claystone from the Nankai prism under stress

Jan 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994georl..21..149j&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 21, no. 2, p. 149-152

Physics

11

Clays, Deformation, Fluid Flow, Geomorphology, Infiltration, Ocean Bottom, Permeability, Pressure Effects, Sedimentary Rocks, Shear Properties, Streams, Stress Measurement, Triaxial Stresses, Brittleness, Electrical Resistivity, Graphs (Charts), Kinetics, Ocean Currents, Oceanography, Sampling, Sea Water

Scientific paper

Permeability is the critical factor governing fluid flow in accretionary prisms. Accretionary wedges are highly deformed, so permeability changes in an indurated claystone sample from the Nankai accretionary prism were measured during a triaxial stress experiment by the pulse decay method. Three zones were identified from the loading test. In zone I, the sample has deformed less than 1.3% and its permeability was 5.10(exp -20) sq m. In zone II, the deformation reached 1.5% and the permeability was unstable with time. In zone III, the sample deformation reached 2% and its permeabilty reached 3.8 10(exp -18) sq m. The permeability strongly decreased (from 3.2 10(exp -18) sq m to 1.7 (10 (exp -19) sq m) with increasing effective pressure (from 2.3 to 10.8 MPa) after the sample was well deformed (zone III). The streaming potential was not measurable when the sample had a low permeability (zone I), but clearly occured when the permeability increased (zone III): the streaming potential measured was 6 mV when the pore pressure pulse applied was about 1.17 MPa and the permeability 3.8 10(exp -18) sq m. Our experiments suggest that shear deformation under low effective pressure increased the vertical permeability of sediments above the decollement. This increase in permeability may be detected by measuring the streaming potential. Variations of flow rate of expelled fluid in accretionary wedges may be detected by monitoring changes of electrokinetic potential, giving new insights on the state of stress related to the seismic cycles.

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