1989
DOI: 10.3133/ofr89582
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Streamflow, specific-conductance, and temperature data for Bayou and Little Bayou Creeks near Paducah, Kentucky, August 15 and 16, 1989

Abstract: Discharge, temperature, and specific conductance measurements were made August 15 and 16, 1989, at 74 main channel sites and seven tributaries on Bayou and Little Bayou Creeks in the vicinity of the Paducah Gaseous Diffusion Plant. These measurements were made during base flow conditions to provide data for analysis of the interaction of surface and ground water. The discharge of Bayou Creek was 0.30 cubic feet per second (ft 3 /s) at the most upstream site, and 5.8 ft 3 /s at the most downstream site. Total m… Show more

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Cited by 3 publications
(10 citation statements)
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“…Although Evaldi and McClain (1989) located the transition from no-net-discharge to gaining conditions between LB3 and LB6, and mixing calculations indicate discharge upstream ofLB6, evidence of gaining conditions between LB6 and LB2 is equivocal. Seeps along the east bank of Little Bayou…”
Section: Gaining Reaches Of Creeksmentioning
confidence: 95%
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“…Although Evaldi and McClain (1989) located the transition from no-net-discharge to gaining conditions between LB3 and LB6, and mixing calculations indicate discharge upstream ofLB6, evidence of gaining conditions between LB6 and LB2 is equivocal. Seeps along the east bank of Little Bayou…”
Section: Gaining Reaches Of Creeksmentioning
confidence: 95%
“…and Mather (1957) for 1969-1989data, CH2M Hill (1992 calculated that potential evapotranspiration exceeds actual evapotranspiration (and precipitation) from June through September and that no water is available for infiltration or runoff from June through October. During our study, the minimum air temperature at Barkley Airfield was -19 °Con January 11, 1997, andthe maximum was 37 °Con July 27, 1997 (National Weather Service [NWS], unpublished data).…”
Section: Northeast Plumementioning
confidence: 99%
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“…T r 29 30 discharge to the streams and to distinguish between re-emergence of channel underflow and other spring flows (Evaldi and McClain, 1989). As with temperature, it is hypothesized that stream water conductivity containing reemerging underflow would be higher if it had mixed with ground water, or if the water had traveled through small cracks in the upper bedrock zone.…”
Section: Specific Conductivitymentioning
confidence: 99%