Well Package (WEL1)

©1995, 1996, Richard B. Winston

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Last modified on Monday, January 15, 1996 - 6:55:58 AM

Skip forward to Input instructions for the Well Package.

The original instructions for the Well Package are on page 8-3 of McDonald and Harbaugh (1988).

Introduction: The Well Package is used to simulate the withdrawal or recharge of water from or to aquifers by wells. The well package can also be used to simulate any other source of withdrawal or recharge which occurs at a known rate including specified flow boundaries. Unlike some other packages such as the Recharge or Evapotranspiration packages in which the withdrawal or recharge rates have units of length/time, the Well Package recharge rates are in units of length^3/time.

When preparing input files for the well package, remember that discharge values must be negative. Positive values represent recharge.

It's important to remember when interpreting MODFLOW output files, that the heads given for cells containing pumping wells are not the heads at those wells. The modeled heads more closely resemble the average head in the cell. Typically, the head observed at a pumping well is an extreme head; either a minimum head for pumping wells or a maximum head for recharge wells. Anderson and Woessner (1992) give the following formulas (Eq. 5.1 and 5.7) relating head in the well to modeled head in its cell for confined and unconfined aquifers.
For confined aquifers, hw = hm - (Q/2{pi}T)*ln(re/rw).
For unconfined aquifers, hw = SQRT[hm^2-(Q/{pi}K)*ln(re/rw)].
Where

For models which have a regular grid in the vicinity of the well re=0.208a where a=the length of the side of the cell. For other geometries, see Anderson and Woessner (1992).

Wells which are open to more than one layer can not be simulated directly by MODFLOW. Instead they must be treated as separate wells each of which is open to only one layer. The total discharge from the well must be divided among the layers. One way to do this is using the equation q = Q(t/T) where


Input Instructions

All input parameters should be right justified


Line 1, Spaces 1-10, Variable = MXWELL, Integer

MXWELL is the maximum number of wells that will be active at one time. You may have more than one well in a single cell.

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Line 1, Spaces 11-20, Variable = IWELCB, Integer

IWELCB is used to tell whether cell-by-cell flow terms should be printed, saved to disk or neither. You must also set ICBCFL in the Output Control option to print or save cell-by-cell flow terms. Back to Input instructions for the Well Package

Lines 2+, Spaces 1-10, Variable = ITMP, Integer

One copy of Lines 2+ followed by 0 or ITMP copies of Lines 3+ are read for each stress period. You may have more than one well in a single cell.

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Lines 3+, Spaces 1-10, Variable = Layer, Integer

"Layer" is the layer number of the cell containing the the well.
The number of copies of Lines 3+ depends on ITMP in Lines 2+

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Lines 3+, Spaces 11-20, Variable = Row, Integer

"Row" is the row number of the cell containing the the well.
The number of copies of Lines 3+ depends on ITMP in Lines 2+

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Lines 3+, Spaces 21-30, Variable = Column, Integer

"Column" is the column number of the cell containing the the well.
The number of copies of Lines 3+ depends on ITMP in Lines 2+

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Lines 3+, Spaces 31-40, Variable = Q

Q is the volumetric recharge rate to the aquifer. If Q is negative, it represents the volumetric discharge from the aquifer. Q remains constant within each stress period.
The number of copies of Lines 3+ depends on ITMP in Lines 2+

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©1995, 1996, Richard B. Winston,
rwinsto@lsuvm.sncc.lsu.edu
Dept. of Geology and Geophysics
Louisiana State University
Baton Rouge, La 70803
U.S.A.
504-388-2337
Fax 504-388-2302
http://scribe.geol.lsu.edu/rbwinston.html
ftp://aapg.geol.lsu.edu/pub/winston