Hydraulic fracturing stress measurements at Yucca Mountain, Nevada, and relationship to the regional stress field

Journal Article · Tue Sep 10 04:00:00 EDT 1985 · Journal of Geophysical Research

DOI:https://doi.org/10.1029/JB090iB10p08691· OSTI ID:59710

Stock, J M; Healy, J H; Hickman, S H; Zoback, M D

Hydraulic fracturing stress measurements and acoustic borehole televiewer logs were run in holes USW G-1 and USW G-2 at Yucca Mountain as part of the Nevada Nuclear Waste Storage Investigations for the U. S. Department of Energy. Eight tests in the saturated zone, at depths from 646 to 1288 m, yielded values of the least horizontal stress S/sub h/ that are considerably lower than the vertical principal stress S/sub v/. In tests for which the greatest horizontal principal stress S/sub H/ could be determined, it was found to be less than S/sub v/, indicating a normal faulting stress regime. The borehole televiewer logs showed the presence of long (in excess of 10 m), vertical, drilling-induced fractures in the first 300 m below the water table. These are believed to form by the propagation of small preexisting cracks under the excess downhole fluid pressures (up to 5.2 MPa) applied during drilling. The presence of these drilling-induced hydrofractures provides further confirmation of the low value of the least horizontal stresses. A least horizontal principal stress direction of N60{sup 0}W--N65{sup 0}W is indicated by the orientation of the drilling-induced hydrofractures (N25{sup 0}E--N30{sup 0}E), and the orientation of stress-induced well bore breakouts in the lower part of USW G-2 (N65 {sup 0}W). This direction is in good agreement with indicators of stress direction from elsewhere at the Neva da Test Site. The observed stress magnitudes and directions were examined for the possibility of slip on preexisting faults. Using these data, the Coulomb criterion for frictional sliding suggests that for coefficients of friction close to 0.6, movement on favorably oriented faults could be expected.

• Research Organization: Office of Earthquakes, Volcanoes, and Engineering, U. S. Geological Survey, Menlo Park, California
• Sponsoring Organization: USDOE
• OSTI ID: 59710
• Journal Information: Journal of Geophysical Research, Journal Name: Journal of Geophysical Research Journal Issue: B9 Vol. 90; ISSN 0022-1406; ISSN JGREA2
• Country of Publication: United States
• Language: English

Related Subjects

05 NUCLEAR FUELS
ACOUSTIC MEASUREMENTS
GEOLOGIC FAULTS
HYDRAULIC FRACTURING
NEVADA TEST SITE
SLIDING FRICTION
SLIP
STRESS ANALYSIS
STRESSES
UNDERGROUND DISPOSAL
Yucca Mountain Project