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WELL PACKAGE

WELL PACKAGE. Simulates the discharge or recharge of water from wells. Simulates a prescribed flow boundary (Neuman) condition. Given that Q is the rate of flow to or from the well or boundary, negative Q represent discharge and a positive Q represent discharge.

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WELL PACKAGE

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  1. WELL PACKAGE • Simulates the discharge or recharge of water from wells. • Simulates a prescribed flow boundary (Neuman) condition. • Given that Q is the rate of flow to or from the well or boundary, negative Q represent discharge and a positive Q represent discharge. • The user specifies the discharge associated with each individual well, and these are summed within the program to obtain a total discharge from a cell. WEL6

  2. WELL PACKAGE • The well package does not accommodate wells which are open to more than one layer of the model. • Well perforated in multiple layers are represent as a group of single-layer wells, • each opened to one of the layers tapped by the multi-layered, • each having an individual Q term specified for each stress period , WEL6

  3. WELL PACKAGE • The discharge of the multi-layer well must be apportioned in in some way among the individual layers, externally to the model program • A common method of external apportionment is to divide the well discharge in proportion to layer transmissivity, where Qijbis the discharge from layer b to a particular i,j well in a given stress period, Qwijis the well discharge in that stress period, Tijb is the transmissivity of layer b, ΣT represents the sum of the transmissivites of all layers penetrated by the well, and m to n includes all of the subscripts for layers open to the well. WEL6

  4. Head at a Well in a Single Layer The head value at the node in a cell is representative of the average value of head throughout the cell. If a well is present in a cell, this average head value can be considered to be the head at some distance re from the well. The distance reis calculated as follows, The area of the cell is equal to DELRj×DELCi WELL PACKAGE Node ij DELCi Well DELRj WEL6

  5. The area is converted to that of a circle, therefore, giving, Thus the head at re is hij, the head at the node We use Theim’s Equation to calculate head at the well. If, hw is the head at the well, hij is the head at radius re Qw is the pumping (-) or injection (+) rate, T is the transmissivity of the cell, and rw is the well radius, then for a Confined aquifer, Unconfined aquifer, WELL PACKAGE Well re DELCi DELRj WEL6

  6. WELL PACKAGE Head in a Well Perforated Through a Multi-Aquifer System • MODFLOW calculates the head in each layer of a well perforation, however, the measured water level in a well, hw, is an integrated head over all the perforated layers and is given by, where Qw is the total pumping , Tijb is the transmissivity of cell i,j,b, hijb is the head in cell i,j,b, reb is the converted radial distance in cell b, and rw is the radius of the well. The indices m to n includes all of the subscripts for zones open to the well. WEL6

  7. Pumpage for Multi-Aquifer System For most multiple-aquifer systems the equation, is sufficient to estimate the distribution of pumping over the perforated layers. A more accurate method involves external iterations, 1. Estimate Qijb from the above equation 2. Calculate hijb with MODFLOW using the calculated Qijb 3. Calculate hw from 4. Calculate a new Qijb using the equation, 5. Return to step 2. WELL PACKAGE WEL6

  8. WELL PACKAGE • The primary source of groundwater recharge into low-land basins is mountain front recharge. • Mountain front recharge is the water that infiltrates into the zones of coarse material that extend from the base of the mountain into the basin (alluvial fans) • The quantity of water potentially available for recharge is assumed to be equal to the precipitation minus evapotranspiration. WEL6

  9. WELL PACKAGE • As an example, a mountain front recharge estimate developed for the Upper San Pedro Basin by Anderson et al (USGS) is, where qrechis the recharge rate per unit area (inches/year), and P is the precipitation for a catchment in excess of 8 inches per year. • The figure on the right shows the average precipitation within each mountain catchment that contributes to the Upper San Pedro basin. Note: this equation is applicable only to the Upper San Pedro Basin WEL6

  10. WELL PACKAGE • For each catchment, the product of qrech with the area gives the amount of recharge water. • The recharge from these catchments is then distributed to active cells along the outside edge of the model boundary. • The recharge into these boundary cell is modeled using recharge wells. • A well is present at each of the boundary cells unless it is a no-flow boundary WEL6

  11. WELL PACKAGE NPWEL—is the number of well parameters. MXL—is the maximum number of wells using parameters. MXACTW—is the maximum of wells in use during any stress period, including those defined using parameters. WEL6

  12. WELL PACKAGE IWELCB—is a flag and unit number IWELCB>0, unit number to which cell-by-cell terms will be written when SAVE BUDGET or a non-zero value of ICBCFL is specified in output control. IWELCB=0, cell-by-cell terms not written. IWELCB<0, well pumping for each well will be written when SAVE BUDGET or a non-zero value of ICBCFL is specified in output control WEL6

  13. WELL PACKAGE [Option]—is an optional list of character values. AUXILIARY abc or AUX abc—defines an auxiliary variable named abc, which is read for each well as part of Items 4 and 6. Up to 5 variable can be specified, each preceded by AUXLIARY or AUX. CBCALLOCATE or CBC—indicates that memory should be allocated to store cell-by-cell flows for each well in order to make these flows available for use in other packages. WEL6

  14. WELL PACKAGE PARNAM—is the name of a parameter. This name can consist of 1 to 10 characters, and is not case specific. PARTYP—is parameter type. There is only one parameter type for the WEL Package—thevolumetric discharge rate, Q. Parval—is the parameter value. NLST—is the number of wells that are included in the parameter. WEL6

  15. WELL PACKAGE ITMP—is a flag and a counter. ITMP<0, non-parameter well data from last stress period will be reused. ITMP≥0, ITMP will be the number of non-parameter wells read for current stress period. NP—is the number of parameters in use in current stress period. Layer—is the layer number of the cell that contains the well Row—is the row number of the cell that contains the well. Column—is the column number of the cell that the contains the well. WEL6

  16. WELL PACKAGE Qfact—is the factor used to calculate the well discharge rate from the parameter value. The discharge rate is the product of Qfact and the parameter value. Q—is the volumetric discharge rate. A positive value is recharge and a negative value is discharge. [xyz]—represent the value of any auxiliary variable for a well that has been defined in Item 2. The auxiliary variable must be present in each repetition of of Item 4 and 6 if they are defined in Item 2. Pname—is the name of the parameter being used in the current stress period. NP parameter names are read. WEL6

  17. WELL PACKAGE No Parameters WEL6

  18. WELL PACKAGE Parameters WEL6

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