Bc. Haimson et al., STRESS MEASUREMENTS AT THE SITE OF THE SM3 HYDROELECTRIC SCHEME NEAR SEPT-ILES, QUEBEC, International journal of rock mechanics and mining sciences & geomechanics abstracts, 33(5), 1996, pp. 487-497
Citations number
7
Categorie Soggetti
Geochemitry & Geophysics","Mining & Mineral Processing
A set of 10 complete hydraulic fracturing stress measurements in an an
orthosite was conducted as part of the site investigation of the SM3 h
ydroelectric project, located some 800 km northeast of Montreal, Quebe
c. These were the first such measurements in that region of Canada. Th
e vertical test hole was N-size, 260 m deep and adjacent to the future
powerhouse. Within the relatively short depth range tested two appare
nt stress regimes were detected. In the 160-220 m range all three prin
cipal in situ stresses approach being lithostatic, suggesting stress r
elief probably induced by natural fracturing in the rock as evidenced
by considerable jointing in the extracted core. At depths comparable t
o those of the planned powerhouse (220-255 m) the least horizontal str
ess is quite consistent and averages 11.0 (+/-1.4) MPa, the maximum ho
rizontal stress averages 17.7 (+/-3.1) MPa and acts in a NE-SW directi
on, and the vertical stress is 7.5 (+/-0.4) MPa. Thus, Patios of 1.6:1
between the two horizontal principal stresses and of 2.5:1 between th
e maximum horizontal and vertical stresses, can be expected, and shoul
d be carefully considered in design, as should the fact that both hori
zontal stresses are substantially larger than the vertical stress. The
northeastern direction of the maximum horizontal stress, as well as t
he compressive nature of the measured stresses are in accord with most
measurements in eastern North America. Copyright (C) 1996 Elsevier Sc
ience Ltd