Borehole Geophysical Characterization of Hydraulic Stimulation of Fractured Bedrock Aquifers

Paillet FL and Hanscomb H. 2000. Borehole Geophysical Characterization of Hydraulic Stimulation of Fractured Bedrock Aquifers. In Symposium on the application of geophysics to environmental and engineering problems

Portions of abstract are copied below: 'Changes induced by typical hydraulic stimulation procedures were monitored in two adjacent boreholes at a site in northeastern Maine by comparing geophysical well logs run before and after stimulation. Caliper and acoustic televiewer logs run before stimulation indicated a few faint, impermeable-looking horizontal and vertical fractures, but inflow before treatment was too weak to detect with a heat-pulse flowmeter. Caliper and televiewer logs run after stimulation showed no significant differences comparedto the pre-stimulation logs. Flow logs run after stimulation demonstrate that inflow in both boreholes is associated with a faint horizontal fracture on the televiewer logs near 60 m in depth, which appears no different from several other similar fractures. A cross-borehole flow experiment confirms that the stimulated zone is a single horizontal fracture connecting the two boreholes. These results demonstrate that the hydraulic stimulation produced at least a 10-fold increase in well capacity from less than 0.5 to more than 5.0 liters per minute. The results also agree with previous studies where fractures affected by stimulation: 1) were present before treatment; 2) showed no obvious changes in the imediate vicinity of the borehole after stimulation; and 3) experienced a 10 to 20 fold increase in permeability attributed to the treatment.' /STUDY LOCATIONS:/ /MOUNT DESERT ISLAND/

Type
Conference Proceeding Paper
Authors
Paillet, Frederick; Hanscomb, Harry
Units
ACAD
Keywords
Drilling, Groundwater, Mount Desert Island, Wells

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