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Two piezometers have been placed along the direction of low in a confined
aquifer that is 30.0 m thick. The piezometers are 280 m apart.
The difference in piezometric head bewteen the two is 1.4 m. The aquifer
hydraulic conductivity is 50 m/d and the porosity is 20%. Estimate
the travel time for water to flow between the two piezometers.
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An artesian aquifer 5 m thick with a piezometeric surface 65 m above the
bottom confining layer is being pumped by a fully penetrating well.
Thie aquifer is a mixture of sand and gravel, with a hydraulic conductivity
of 6.1x10-4 m/s. A steady-state drawdown of 7 m is observed
at a nonpumping well located 10 m away. If the pumping rate is 0.020
m3/s, how far away is a second nonpumping well that has an observed
drawdown of 2 m?
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Drawdown at a 0.20 m diameter, fully penetrating well, which has been pumping
at the rate of 1000 m3/day for a long enough time that steady-state
conditions have been reached, is determined to be 0.75 m. The aquifer
is unconfined and 12.0 m thick. An observation well 10 m away has
been drawn down by 0.30 m.
a.) Determine the hydraulic conductivity of the aquifer.
b.) What is the drawdown at an observation well 25 m away?
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Suppose a spill of 5200 L of trichloroethylene (TCE) distributes itself
evenly throughout an aquifer 10.0 m thick, forming a rectangular plume
2000 m long and 250 m wide (see figure below). The aquifer has porosity
of 0.40, hydraulic gradient of 0.001, and hydraulic conductivity of 0.001
m/s.
a.) What would be the concentration of TCE (in mg/L) in this
idealized groundwater plume? Could this much TCE be totally dissolved in
the aquifer at equlibrium, given the solubility of TCE?
b.) Using capture zone curves, design an extraction field to pump out
the plume under the assumption that the wells are lined up along
the leading edge of the plume, with each well to be pumped at the same
rate, not to exceed 0.003 m3/s per well. What is the smallest
number of wells that could be used to capture the entire plume? What
minimum pumping rate would be required for each well?
c.) What would the optimal spacing be between the wells, at the minumum
pumping rate?
d.) What are the assumptions made in designing this well field?
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If the transmissivity of an aquifer is 2.51x10-3 m2/s
and the storativity is 2.86x10-4, calculate the drawdown that
will result at the end of two days of pumping a 0.5 m diameter well at
a rate of 0.0194 m3/s.
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