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User's guide of Proceessing Modflow 5.0

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Processing <strong>Modflow</strong> 91<br />

For the case that h is greater than H , Q is negative. It means that water flows from the<br />

RIV RIV<br />

aquifer into the river and is removed from the groundwater model. When h has fallen below the<br />

bottom <strong>of</strong> the riverbed, the rate <strong>of</strong> leakage through the riverbed is given by eq. 3.20.<br />

Q RIV ' C RIV @(H RIV & R BOT ) h#R BOT<br />

The value C <strong>of</strong> a river-cell is <strong>of</strong>ten given by<br />

RIV<br />

C RIV ' K·L·W<br />

M<br />

(3.20)<br />

(3.21)<br />

where K is the hydraulic conductivity <strong>of</strong> the riverbed material, L is the length <strong>of</strong> the river within<br />

a cell, W is the width <strong>of</strong> the river and M is the thickness <strong>of</strong> the riverbed. If C is unknown, it<br />

RIV<br />

must be adjusted during a model calibration.<br />

MODFLOW < Streamflow-Routing<br />

The Streamflow-Routing package (Prudic, 1989) is designed to account for the amount <strong>of</strong> flow<br />

in streams and to simulate the interaction between surface streams and groundwater. Streams are<br />

divided into segments and reaches. Each reach corresponds to individual cells in the finite-<br />

difference grid. A segment consists <strong>of</strong> a group <strong>of</strong> reaches connected in downstream order.<br />

Streamflow is accounted for by specifying flow for the first reach in each segment, and then<br />

computing streamflow to adjacent downstream reaches in each segment as inflow in the upstream<br />

reach plus or minus leakage from or to the aquifer in the upstream reach. The accounting scheme<br />

used in this package assumes that streamflow entering the modelled reach is instantly available<br />

to downstream reaches. This assumption is generally reasonable because <strong>of</strong> the relatively slow<br />

rates <strong>of</strong> groundwater flow.<br />

Streamflow into a segment that is formed from tributary streams is computed by adding the<br />

outflows from the last reach in each <strong>of</strong> the specified tributary segments. If a segment is a<br />

diversion, then the specified flow into the first reach <strong>of</strong> the segment is subtracted from flow in<br />

the main stream. However, if the specified flow <strong>of</strong> the diversion is greater than the flow out <strong>of</strong><br />

the segment from which flow is to be diverted, then no flow is diverted from that segment.<br />

In the Data Editor, you can press the right mouse button and specify the following required<br />

cell values in the Streamflow-Routine Package dialog box (Fig. 3.23). The specified cell values<br />

will be shown from left to right on the status bar.<br />

< Segment is a number assigned to a group <strong>of</strong> reaches. Segments must be numbered in<br />

downstream order. The maximum number allowed in PMWIN is 25.<br />

3.6.1 MODFLOW

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