Item talk:Q72654: Difference between revisions

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= Three-dimensional measurements of flow in uncased wells completed in basalt, Mountain Home Air Force Base, Idaho, March 2000 =
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Several ground-water monitoring wells on the Mountain Home Air Force Base in southwestern Idaho were constructed in February 2000 to replace existing monitoring wells that became ineffective as a result of declining water levels. Upon completion of the replacement wells, borehole geophysical logs were collected, including natural gamma radiation, electromagnetic induction, caliper, fluid temperature, and resistivity. A prototype borehole acoustic doppler velocimeter (B-ADV) was used to make experimental three-dimensional measurements of lateral and vertical flow in two of the replacement wells, MW11–2 and MW3–2, each 450 feet deep, to better understand ground-water flow in the basalt underlying this area. Measurements indicated two independent flow zones in each well: unit B, from about 380 to about 415 feet below land surface, and unit C, from about 415 to about 430 feet below land surface. In each well, direction of flow in unit B was north-northwest toward Canyon Creek and, in unit C, south-southwest toward the Snake River. Measurements also indicated downward intraborehole flow in both wells. Unit B appeared to represent a local-scale flow regime; unit C appeared to represent a regional flow regime. This information suggests the existence of a complex three-dimensional hydrogeologic setting that cannot be discriminated easily on conventional waterlevel maps. Although data from only two wells are insufficient to construct a conceptual model of the ground-water flow regime, these experimental results demonstrate the capability of the B-ADV to obtain detailed flow measurements that, combined with data from other types of geophysical logs, discrete measurements of hydraulic head, and water chemistry, would aid in future studies and management of the ground-water resources, including contaminant transport and remediation.
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      "name": "Three-dimensional measurements of flow in uncased wells completed in basalt, Mountain Home Air Force Base, Idaho, March 2000",
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          "value": "10.3133/wri014259",
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      "datePublished": "2002",
      "dateModified": "2012-12-04",
      "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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Latest revision as of 04:20, 15 August 2024

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