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Title: Cross-flows in observation boreholes induced by distant pumping of basalt aquifers: Eastern Snake River Plain, Idaho

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5450876
;  [1]; ;  [2]
  1. Boise State Univ., ID (United States)
  2. Idaho National Engineering Lab., Boise, ID (United States)

Vertical flow velocities up to 20 ft/minute occur in borehole between stratified permeable zones of basalt aquifers of the eastern Snake River Plain. Water is transferred vertically in wells across relatively impermeable zones 35 to 65 ft thick between permeable zones 515 feet deep and a zone 550 to 575 ft deep. Large rates of cross flows are caused by a well 2,000 feet distant which pumps 3,100 gallons/minute with a 2.0 hour on and a 3.5 hour off cycle. Impeller flow-meter logging shows the pump cycle produces reversals in flow direction within 120 seconds of pump switching. Preliminary results from packer isolation of the 500--515 ft zone indicates flow is induced by a hydraulic-head difference between permeable zones set up within 14 seconds of the pump turning on in the distant well. Distant pumping induces downward flow in the observation well, indicating the lower zone has a better connection to the pumped zone. When the pump is off, flow is upward at a lesser rate, suggesting the ambient hydraulic head in this system of aquifers decreases upward. Transmissivity of 1.5 [times] 10[sup 6] gallons/day/ft and storativity of 0.08 from well tests reported by others in this area of the Idaho National Engineering Laboratory do not predict such rapid response times for head changes over a distance of 2,000 feet. The authors suggest that the basalt aquifer system here behaves on a short time scale as a system of confined aquifers with storativity on the order of 10[sup [minus]5] rather than 0.08. The above observations on USGS wells no. 44 and 46 and pumping well CPP-2 show that cross-flow in boreholes provides a vertical path for ground water and contaminant movement between stratified basalt aquifers in the vicinity of the Idaho Chemical Processing Plant.

OSTI ID:
5450876
Report Number(s):
CONF-9305259-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 25:5; Conference: 89. annual meeting of the Cordilleran Section and the 46th annual meeting of the Rocky Mountain Section of the Geological Society of America (GSA), Reno, NV (United States), 19-21 May 1993; ISSN 0016-7592
Country of Publication:
United States
Language:
English