TY - GEN
T1 - Problem for the maximum stress estimation by hydrofracturing method and its potential solution
AU - Ito, T.
AU - Igarashi, A.
AU - Ito, H.
AU - Sano, O.
N1 - Funding Information:
The research fund for the present work was granted by the Earthquake Research Institute, University of Tokyo. The authors wish to thank the kind support by Nittetsu Mining Co. Ltd. and Kamaishi Mining Co. Ltd..
Publisher Copyright:
Copyright 2005, ARMA, American Rock Mechanics Association.
PY - 2005
Y1 - 2005
N2 - For the stress measurement by hydrofracturing, the observed borehole pressures of Pr and Ps, i.e. the reopening and shut-in pressures, should be related independently to the maximum stress SH and the minimum stress Sh, and the independent relationships give the principle for the two values of SH and Sh to be determined from the two observations of Pr and Ps. However, the data of field tests so far indicate that the measured reopening pressure lies close to the shut-in pressure, i.e. Pr = Ps, are far more numerous than can reasonably be expected. To examine such a paradox, we carried out field tests of hydrofracturing, and then we confirmed that borehole pressure is fairly influenced by the hydraulic compliance of test equipments, C, as expected from our theoretical model which has been developed so far. The model suggests that if the C will be reduced small enough, then the measured reopening pressure Pr (a) approaches the true reopening pressure, Pr0, i.e. the borehole pressure at which the fracture truly begins to open from its mouth at the borehole wall. Thus we could measure Pr0 approximately from Pr (a) by using stiff hydrofracturing system. The detected Pr0 allows us to estimate SH on condition that the magnitude of Sh is known from the shut-in pressure.
AB - For the stress measurement by hydrofracturing, the observed borehole pressures of Pr and Ps, i.e. the reopening and shut-in pressures, should be related independently to the maximum stress SH and the minimum stress Sh, and the independent relationships give the principle for the two values of SH and Sh to be determined from the two observations of Pr and Ps. However, the data of field tests so far indicate that the measured reopening pressure lies close to the shut-in pressure, i.e. Pr = Ps, are far more numerous than can reasonably be expected. To examine such a paradox, we carried out field tests of hydrofracturing, and then we confirmed that borehole pressure is fairly influenced by the hydraulic compliance of test equipments, C, as expected from our theoretical model which has been developed so far. The model suggests that if the C will be reduced small enough, then the measured reopening pressure Pr (a) approaches the true reopening pressure, Pr0, i.e. the borehole pressure at which the fracture truly begins to open from its mouth at the borehole wall. Thus we could measure Pr0 approximately from Pr (a) by using stiff hydrofracturing system. The detected Pr0 allows us to estimate SH on condition that the magnitude of Sh is known from the shut-in pressure.
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M3 - Conference contribution
AN - SCOPUS:85041257148
SN - 9781604234541
T3 - American Rock Mechanics Association - 40th US Rock Mechanics Symposium, ALASKA ROCKS 2005: Rock Mechanics for Energy, Mineral and Infrastructure Development in the Northern Regions
BT - American Rock Mechanics Association - 40th US Rock Mechanics Symposium, ALASKA ROCKS 2005
PB - American Rock Mechanics Association (ARMA)
T2 - 40th US Rock Mechanics Symposium: Rock Mechanics for Energy, Mineral and Infrastructure Development in the Northern Regions, ALASKA ROCKS 2005
Y2 - 25 June 2005 through 29 June 2005
ER -