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🆕The Recharge Zone Podcast – Season 2, Episode 8 | EAA's Plan to Excel Aquifer Education at its Anticipated Education Outreach Center (EOC)

🆕The Recharge Zone Podcast – Season 2, Episode 8 | EAA's Plan to Excel Aquifer Education at its Anticipated Education Outreach Center (EOC)

266 viewsAug 27, 2021

FacebookEdwards Aquifer Authority (EAA)

SOLVED:The governing equation for an unconfined aquifer with flow… | Numerade

SOLVED:The governing equation for an unconfined aquifer with flow… | Numerade

How filter data using slicer in excel #exceltips #exceltricks #spreadsheet #finance #accounts #corporate #sheets #viralreels #viral | Ather Naqvi

How filter data using slicer in excel #exceltips #exceltricks #spreadsheet #finance #accounts #corporate #sheets #viralreels #viral | Ather Naqvi

305K views2 months ago

FacebookAther Naqvi

SOLVED: A pump test was conducted on a test well in an unconfined aquifer, with the results as shown in Figure 5-14. If water was pumped at a steady flow of 185 gal / min, determine the coefficient of permeability of the permeable soil. FIGURE CANT COPY Figure 5-14 | Numerade

SOLVED: A pump test was conducted on a test well in an unconfined aquifer, with the results as shown in Figure 5-14. If water was pumped at a steady flow of 185 gal / min, determine the coefficient of permeability of the permeable soil. FIGURE CANT COPY Figure 5-14 | Numerade

Solving Laplace Equation for Simulation of Groundwater Flow in Confined Aquifer: Excel Model

Solving Laplace Equation for Simulation of Groundwater Flow in Confined Aquifer: Excel Model

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Derive the following expression for the length of time required for groundwater to flow from an observation well to a pumped well in a confined aquifer: t=(πB η)/(Q)(R^2-rw^2) where B= thickness of the confined aquifer η= aquifer porosity R= radial distance from the observation well to the pumped well rw= radius of the pumped well Q= pumping rate Hint: Combine (54), Q=2 πr B K(d hc / d r), with the average linear velocity from Eq. (48): ν^'=-(K)/(η)((d hc)/(d r))=(d r)/(d t) | Numerade

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