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Title: Sonic and electrical properties of partially saturated tight-gas sands. Final report

Technical Report ·
DOI:https://doi.org/10.2172/6350056· OSTI ID:6350056

This study was aimed at relating the seismic and the electrical properties of tight-gas rocks to their pore-space geometry, permeability, and level of water saturation. Here we report results of a laboratory experimental study of wave propagation in Cotton Valley and Spirit River Sandstones as a function of partial water saturation (SW) and wave frequency. We find that wave velocities and the velocity ratio are sensitive to the presence of gas. Furthermore, wave attenuation is sensitive to the amount of gas in the pore space. Ultrasonic measurements in tight-gas sands tend to yield higher velocity values, due to the inability of the pore fluid pressure to homogenize during the passage of waves. Laboratory measurements were made also of the complex electrical response of selected tight rocks, and compared with normal permeability Berea Sandstone. The results show that the dielectric property of tight-gas sands is very sensitive to partial water saturation, and may give not only insight into the nature of the pore space, but also provide a practical measure of S/sub w/ in situ. 35 figures, 2 tables.

Research Organization:
Stanford Univ., CA (USA). Dept. of Geophysics
DOE Contract Number:
AS19-81BC10498
OSTI ID:
6350056
Report Number(s):
DOE/BC/10498-5; ON: DE83009472
Resource Relation:
Other Information: Portions are illegible in microfiche products. Original copy available until stock is exhausted
Country of Publication:
United States
Language:
English