14.07.2013 Views

User's guide of Proceessing Modflow 5.0

User's guide of Proceessing Modflow 5.0

User's guide of Proceessing Modflow 5.0

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

282 Processing <strong>Modflow</strong><br />

6.5.4 Cut-<strong>of</strong>f Wall<br />

Folder: \pm5\examples\geotechniques\geo4\<br />

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

As shown in Fig. 6.53, a highly contaminated area is located in the first stratigraphic unit <strong>of</strong> an<br />

unconfined aquifer. To the west and east <strong>of</strong> the aquifer exist fixed-head bounaries with the<br />

hydraulic head h = -0.4 m and +0.5 m. The aquifer consists <strong>of</strong> five stratigraphic units. Each unit<br />

is horizontally isotropic with uniform thickness. The elevations and horizontal hydraulic<br />

conductivities are illustrated in Fig. 6.53. The vertical hydraulic conductivities are assumed to<br />

be a tenth <strong>of</strong> the horizontal hydraulic conductivities. The effective porosity <strong>of</strong> the aquifer is<br />

-8<br />

0.15. The recharge rate is 1 × 10 m/s.<br />

Because <strong>of</strong> the unpayable cost, the contaminants cannot be removed. Your task is to<br />

develop a strategy to isolate the contamination. There are four steps to be done.<br />

1. Construct a groundwater flow model and perform a steady-state flow simulation by using<br />

the data given above and the model grid given in Fig. 6.53.<br />

2. Geotechnical measures, such as cut-<strong>of</strong>f wall, impervious cover, drain etc., can be<br />

considered as an alternative. Calculate flowlines for the case that a cut-<strong>of</strong>f wall has been<br />

built to a depth <strong>of</strong> -8m and the recharge rate within the cut-<strong>of</strong>f wall is reduced to zero by an<br />

impervious cover. The location <strong>of</strong> the cut-<strong>of</strong>f wall is given in Fig. 6.53. When calculating<br />

the flowlines, particles should be started from the contaminated area.<br />

3. Repeat step 3 for the case that the cut-<strong>of</strong>f wall reaches the depth -10m.<br />

4. Use a pumping well located in the cell [6, 12] to capture the contaminants. Calculate the<br />

required pumping rate and penetration depth.<br />

Modeling Approach and Simulation Results<br />

The aquifer is simulated using a grid <strong>of</strong> 5 layers, 23 columns and 23 rows. All layers have the<br />

same layer type 3: confined/unconfined (Transmissvity varies). The cut-<strong>of</strong>f wall is modelled<br />

by using the Horizontal-flow Barriers package. An impervious cover can be easily simulated by<br />

reducing the recharge rate. Fig. 6.54 and Fig. 6.55 show the flowlines by performing forward<br />

and backward particle tracking with PMPATH. The particles are initially placed in the center <strong>of</strong><br />

each cell, which is located in the first model layer and within the cut-<strong>of</strong>f wall. It is obviously<br />

that the contaiminants will be “washed out”, even if the cut-<strong>of</strong>f wall is going deeper.<br />

The contaminated area can be captured by using a pumping well (located in the cell [6,12])<br />

6.5.4 Cut-<strong>of</strong>f Wall

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!