When rock is cored at depth by drilling, anisotropic expansion occurs with the relief of anisotropic rock stresses, resulting in a sinusoidal variation of core diameter with a period of 180 deg. in the core roll angle. The circumferential variation of core diameter is given theoretically as a function of rock stresses. These new findings can lead ideas to estimate the rock stress from circumferential variation of core diameter measured after the core retrieving. When several core samples with different orientation are available, all of three principal components of 3D rock stress can be estimated. If we apply an advanced technology of the rotary sidewall coring tool, we can have cores with the orientation of core axis deviated from the originally-drilled borehole axis by a right angle, 90 deg.. By using both of a sidewall core and a core of the originally-drilled borehole, we can determine absolute magnitude of 3D in-situ stress. The theoretical relationship between the core expansion and rock stress has been verified through the examination of core samples prepared in laboratory experiments and retrieved field cores.
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52nd U.S. Rock Mechanics/Geomechanics Symposium
June 17–20, 2018
Seattle, Washington
A New Method of Stress Measurement Based on Elastic Deformation of Sidewall-Core With Stress Relief During Coring
Paper presented at the 52nd U.S. Rock Mechanics/Geomechanics Symposium, Seattle, Washington, June 2018.
Paper Number:
ARMA-2018-672
Published:
June 17 2018
Citation
Ito, T., Fukusawa, S., Funato, A., Tamagawa, T., and K. Tezuka. "A New Method of Stress Measurement Based on Elastic Deformation of Sidewall-Core With Stress Relief During Coring." Paper presented at the 52nd U.S. Rock Mechanics/Geomechanics Symposium, Seattle, Washington, June 2018.
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