Item talk:Q72654
From geokb
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"abstract": "Several ground-water monitoring wells on the\nMountain Home Air Force Base in southwestern Idaho\nwere constructed in February 2000 to replace existing\nmonitoring wells that became ineffective as a result of\ndeclining water levels. Upon completion of the replacement\nwells, borehole geophysical logs were collected,\nincluding natural gamma radiation, electromagnetic\ninduction, caliper, fluid temperature, and resistivity.\nA prototype borehole acoustic doppler velocimeter\n(B-ADV) was used to make experimental three-dimensional\nmeasurements of lateral and vertical flow in two\nof the replacement wells, MW11\u20132 and MW3\u20132, each\n450 feet deep, to better understand ground-water flow\nin the basalt underlying this area.\nMeasurements indicated two independent flow\nzones in each well: unit B, from about 380 to about\n415 feet below land surface, and unit C, from about\n415 to about 430 feet below land surface. In each well,\ndirection of flow in unit B was north-northwest toward\nCanyon Creek and, in unit C, south-southwest toward\nthe Snake River. Measurements also indicated downward\nintraborehole flow in both wells. Unit B appeared\nto represent a local-scale flow regime; unit C appeared\nto represent a regional flow regime.\nThis information suggests the existence of a\ncomplex three-dimensional hydrogeologic setting that\ncannot be discriminated easily on conventional waterlevel\nmaps. Although data from only two wells are\ninsufficient to construct a conceptual model of the\nground-water flow regime, these experimental results\ndemonstrate the capability of the B-ADV to obtain\ndetailed flow measurements that, combined with data\nfrom other types of geophysical logs, discrete measurements\nof hydraulic head, and water chemistry,\nwould aid in future studies and management of the\nground-water resources, including contaminant transport\nand remediation.",
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