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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> 83<br />

boundaries between pairs <strong>of</strong> adjacent cells in the finite-difference grid. Refer to Hsieh and<br />

Freckleton (1993) for the numerical implementation <strong>of</strong> the Horizontal-Flow Barrier package.<br />

A horizontal-flow barrier is defined by assigning the following values to a model cell in the<br />

Horizontal-Flow Barrier Package dialog box (Fig. 3.18):<br />

- Barrier Direction [-]; and<br />

-1<br />

- (Hydraulic Conductivity/Thickness) <strong>of</strong> the barrier TDW [T ] for unconfined layers or<br />

-1<br />

(Transmissivity/Thickness) <strong>of</strong> the barrier TDW [LT ] for confined layers.<br />

Fig. 3.18 The Horizontal-Flow Barrier Package dialog box<br />

The barrier direction indicates the cell face where the barrier is located. To erase an existing<br />

barrier, use zero for the barrier direction. The second value TDW gives the hydraulic<br />

characteristic <strong>of</strong> the barrier. If a layer is unconfined (type 1 or 3), TDW is the barrier hydraulic<br />

conductivity divided by the thickness <strong>of</strong> the barrier. If a layer is confined (type 0 or 2), TDW is<br />

the barrier transmissivity divided by the thickness <strong>of</strong> the barrier. The barrier thickness is included<br />

implicitly in TDW.<br />

MODFLOW < Interbed Storage<br />

For steady state flow simulations, this menu item is not used and is therefore dimmed.<br />

Groundwater is released from storage under conditions <strong>of</strong> decreasing hydraulic head. The<br />

released water volume is proportional to the compressibility <strong>of</strong> the soil matrix and water, because<br />

a reduction <strong>of</strong> the hydraulic head results in an increase in the effective stress on the soil skeleton<br />

and a decrease <strong>of</strong> the water pressure. Increasing effective stress on the soil skeleton results to<br />

deformation (compaction) <strong>of</strong> the soil matrix. The Interbed Storage package (Leake and Prudic,<br />

1991) calculates the water volume released from storage and simulates elastic and inelastic<br />

3.6.1 MODFLOW

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