Item talk:Q75586
From geokb
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"name": "Streamflow gains and losses in the lower Boise River basin, Idaho, 1996-97",
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"abstract": "Information on streamflow gains and losses \nin the lower Boise River Basin is needed by the \nIdaho Department of Water Resources to determine recharge to and discharge from the ground- \nwater system. A method was developed to select \ncanal and creek reaches such that a minimum of \ntwo reaches were measured in each of 12 different \nareas that share a set of common environmental \ncharacteristics. After a large number of environmental characteristics were evaluated, soil type, \nland use, and canal density were selected to define \nthe 12 areas.\nSeepage runs were made on 39 irrigation \ncanal and creek reaches in the lower Boise River \nBasin in June-July and September 1996. During \nthe June-July seepage runs, irrigation canals \ngained and lost water, whereas in September, most \nreaches lost. No substantial differences were noted \nin the median and spread of flow gains and losses \nwithin the 12 areas; therefore, no direct relation \ncould be defined between seepage and environmental areas.\nSeepage runs were made on three reaches of \nthe lower Boise River in November 1996 to identify flow gains and losses after the irrigation season. The two upstream reaches had net gains, \nwhereas the most downstream reach, near the confluence with the Snake River, had a net loss. The \ntotal gain to the river from the three reaches was \n90.71 cubic feet per second.\nBecause of potential flooding in March 1997, \nwater was diverted from the Boise River into the \nNew York Canal to reduce flows in the river. This \nallowed a seepage run on the canal when there \nwere no irrigation diversions or return flows. Subsequently, two seepage runs were made in March \nwhen flows near Diversion Dam were about 440 \nand 860 cubic feet per second. Both gains and \nlosses were measured along the canal, but losses \nwere dominant. Total loss from the canal during \nthe first seepage run was -54 cubic feet per second; \nduring the second, -143 cubic feet per second. Sixteen wells near the canal were measured weekly \nfrom the last week in February through mid-June. \nGenerally, water levels decreased from February \nto mid-April and then increased through June. \nPaired wells near the canal indicated downward \nmovement of water, probably recharge from canal \nlosses.\nStudy results indicate that additional seepage \nruns are needed on irrigation canals and creeks, \nthe Boise River, and the New York Canal. Piezometers installed at different depths are needed to better define vertical ground-water movement and \ngradients. Additional work is needed to determine \nhow seepage in canals and streams relates to environmental characteristics.",
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