2015
DOI: 10.3133/ofr20151026
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Evaluation of aquifer interconnection from aquifer characteristics computed by using specific capacity data within the vicinity of the Tremont Barrel Fill site, Clark County, Ohio

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Cited by 2 publications
(2 citation statements)
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“…Moreover, it is more expensive to regulate the total performance of aquifer tests. Although the data and equations have applied to identify the transmissivity with its inherent limitations and errors as potential (Gahala, 2015). Partial penetration of well, well loss and hydrogeological boundaries, values of transmissibility that have been calculated from specific capacity data by underestimate of actual values effect on the pumping tests unfavorably (Misstear & Beeson, 2000).…”
Section: Specific Capacitymentioning
confidence: 99%
“…Moreover, it is more expensive to regulate the total performance of aquifer tests. Although the data and equations have applied to identify the transmissivity with its inherent limitations and errors as potential (Gahala, 2015). Partial penetration of well, well loss and hydrogeological boundaries, values of transmissibility that have been calculated from specific capacity data by underestimate of actual values effect on the pumping tests unfavorably (Misstear & Beeson, 2000).…”
Section: Specific Capacitymentioning
confidence: 99%
“…Until the drawdown stabilized, it is measures every test temporary changes in water levels at every step (Kruseman, De Ridder, & Verweij, 1970). Moreover, some researchers (Gahala, 2015;Louwyck, Vandenbohede, & Lebbe, 2010) studied that the analytical process of step-drawdown test assists to identify the quantify aquifer mechanisms which evaluate the rate of flow into the well laminar/turbulent. The discharge rate (Q) and time are proportional to the resistance of formation on the water-bearing zone.…”
Section: Introductionmentioning
confidence: 99%