Physics
Scientific paper
Oct 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30ssde1b&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 19, pp. SDE 1-1, CiteID 1976, DOI 10.1029/2003GL017929
Physics
4
Physical Properties Of Rocks: Acoustic Properties, Geomagnetism And Paleomagnetism: Magnetic Fabrics And Anisotropy, Physical Properties Of Rocks: Transport Properties, Physical Properties Of Rocks: Permeability And Porosity
Scientific paper
Pore fabric anisotropy is a common feature of many sedimentary rocks. In this paper we report results from a comparative study on the anisotropy of a porous sandstone (Crab Orchard) using anisotropy of magnetic susceptibility (AMS), acoustic wave velocity and fluid permeability techniques. Initially, we characterise the anisotropic pore fabric geometry by impregnating the sandstone with magnetic ferro-fluid and measuring its AMS. The results are used to guide subsequent measurements of the anisotropy of acoustic wave velocity and fluid permeability. These three independent measures of anisotropy are then directly compared. Results show strong positive correlation between the principal directions given from the AMS, velocity anisotropy and permeability anisotropy. Permeability parallel to the macroscopic crossbedding observed in the sandstone is 240% higher than that normal to it. P and S-wave velocity anisotropy and AMS show mean values of 19.1%, 4.8% and 3.8% respectively, reflecting the disparate physical properties measured.
Benson Philip M.
Meredith Philip G.
Platzman Ellen S.
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