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User's guide of Proceessing Modflow 5.0

User's guide of Proceessing Modflow 5.0

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Processing <strong>Modflow</strong> 259<br />

6.2.8 Simulation <strong>of</strong> Lakes<br />

Folder: \pm5\examples\basic\basic8\<br />

Overview <strong>of</strong> the Problem<br />

Fig. 6.32 shows an unconfined aquifer with the boundary conditions and the location <strong>of</strong> a<br />

planned open-cast mining site. The aquifer is bounded by a no-flow zone to the north and to the<br />

south. To the west and east exist fixed-head boundaries with the hydraulic heads h = 100 m and<br />

50 m; the elevations <strong>of</strong> the aquifer top and bottom are 100 and 0 m, respectively.<br />

The aquifer is homogeneous and isotropic with a measured horizontal hydraulic<br />

conductivity <strong>of</strong> 0.0001 m/s and vertical hydraulic conductivity <strong>of</strong> 0.00001 m/s. The specific<br />

yield and effective porosity are assumed to be 0.25. The specific storage coefficient S = 0.0001.<br />

s<br />

In the final mining phase, the hydraulic head within the mining site must be drawn down at<br />

the level <strong>of</strong> h = 21 m. Afterwards, the mining site will be filled with water to form an artificial<br />

lake. Your task is to<br />

1. construct a steady-state flow model and calculate the necessary abstraction rate (= inflow<br />

into the mining site) for holding the head at 21 m, and<br />

2. use the calculated steady-state head as the initial hydraulic head and calculate the temporoal<br />

development curve <strong>of</strong> the water level (head vs. time) in the artificial lake for the case that<br />

the abstraction within the mining site is turned <strong>of</strong>f.<br />

Fig. 6.32 Plan view <strong>of</strong> the model area<br />

6.2.8 Simulation <strong>of</strong> Lakes

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