Grant Ferguson
University of Saskatchewan
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ABSTRACT:
Permeabilities were measured on core from the White Rim Sandstone of the Cutler Group at the Utah Geological Survey’s Core Laboratory. Measurements were made using a TinyPermTM air permeameter. Forty-nine measurements were taken from core from the Altex Government 1 (API 43-055-300290000) well between depths of 432 and 508 m below ground surface and 15 measurements were taken from core from the Romex Bullfrog Creek 1 well (API 43-017-300190000) between depths of 906 and 927 m below ground surface. Results are also presented as hydraulic conductivities in m/yr assuming viscosity and density of low salinity water at standard temperature and pressure.
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Created: March 20, 2023, 7:30 p.m.
Authors: Ferguson, Grant · McIntosh, Jennifer
ABSTRACT:
Permeabilities were measured on core from the White Rim Sandstone of the Cutler Group at the Utah Geological Survey’s Core Laboratory. Measurements were made using a TinyPermTM air permeameter. Forty-nine measurements were taken from core from the Altex Government 1 (API 43-055-300290000) well between depths of 432 and 508 m below ground surface and 15 measurements were taken from core from the Romex Bullfrog Creek 1 well (API 43-017-300190000) between depths of 906 and 927 m below ground surface. Results are also presented as hydraulic conductivities in m/yr assuming viscosity and density of low salinity water at standard temperature and pressure.