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Groundwater Modeling – 3 Transient Models Groundwater Hydraulics Daene C. McKinney
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Remember Your Old Model? Find the file that you used for the example model from the previous class Or recreate it by reviewing the overhead slides from that assignment. – See file: 07_Groundwater_Modeling_2.pptx
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Example Boundaries – North & South: No-flow – East & West: Constant-head Layer 1 – unconfined (13 m) – K h = 5x10 -3 m/s; K v = 5x10 -4 m/s – Porosity = 0.25 Layer 2 – confined (5 m) – K h = 1x10 -3 m/s; K v = 1x10 -4 m/s – Porosity = 0.25 No-flow Boundary Constant Head Boundary (h = 9 m) Constant Head Boundary (h = 8 m) Pumping Well 600 m Adapted from Chiang, W-H and W. Kinzelbach, Processing Modflow: A Simulation System For Modeling Groundwater Flow and Pollution, 1996 Pumping Well Layer 1 Layer 2 5 13 10 m -3 m -8 m N
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Results – Remember? To get contours of water table, check this box Always check the box for Cell-by-Cell flow
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Transient Groundwater Models Transient models simulate changes over time – Necessary when boundary conditions vary with time (e.g., pumping rates, recharge, river stage, etc.) Stress period: – Period of time during which boundary conditions are constant – Stress periods can have multiple time steps – Boundary conditions can change at the beginning of a stress period Stress period Time Steps Stress period Time Steps Stress period Time Steps Time Pumping and boundary conditions can change e.g., one month e.g., one day
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Transient Model Convert you steady-state model to a transient model Open your model Select: Model MODFLOW Package Options Select: Basic Package Tab Uncheck: Steady-State checkbox Enter: Number of stress periods = 12 Select: Days Select: OK Do you want to copy data? Select: Yes Do you want to set up stress periods? Select: Yes
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Stress Periods Use 12 stress periods, one for each day for 12 days Enter – Length of each stress period (= 1 day) – Number of time steps (= 1) – Time step multiplier (= 1.0)
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Pumping Conditions Select: Layer 1 Select: BC Well Select: BC Modify Layer Uncheck: “Steady-state Boundary Condition” Press: “Transient Data” Uncheck this box Press this button
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Pumping Conditions Change the pumping rates from “m 3 /sec” to “m 3 /day” Enter: Starting and Ending Stress Period Numbers Enter: Q = 0 m 3 /d for stress periods 1, 2, and 3 Enter: Q = -159,840 m 3 /d for stress periods 4 - 12 Repeat for layer 2:Q = 0 m 3 /d in stress periods 1, 2 and 3; Q = -1296 m 3 /d in periods 4 - 12
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Hydraulic Conductivity Change the hydraulic conductivity values from “m/sec” to “m/day” Select: Props – Hydraulic Conductivity Select: Props – Property Values – Database Enter: – Zone 1: Kx = 432 m/d Ky = 432 m/d Kz = 43.2 m/d – Zone 2: Kx = 86.4 m/d Ky = 86.4 m/d Kz = 8.64 m/d
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Storage/Porosity Select: Props – Storage/Porosity Select: Props – Property Values – Database Enter: – Zone 1 and Zone 2: S s = 0.0001 S y = 0.15 Porosity = 0.15
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Leakance Select: Props – Leakance Select: Props – Property Values – Database Enter: – Zone 1 and Zone 2: Leakance = 864 m/day
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Monitoring Wells Select: AE Well Select: Row 15, Column 24 Select: Top layer = 1, and Bottom Layer = 2 Change: Pumping rate = 0.0 Check box: Monitor Head/Concentration vs. Time Select: Well Name button – Enter MW-1 Select: OK Add another Monitoting Well (MW-2) in cell (15, 18)
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Model with Monitoring Wells
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Run Simulation Select: Calculator button Would you like to process the results? Select: Yes Select: Cell-by-cell flows
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Switching Between Time Steps There are several options that allow switching between time steps in a transient run: – Import Results (Plot->Import Results) Ctrl+Shift+I – Next Time Step (Plot->Next Time Step) Ctrl+Shift+N – Previous Time Step (Plot->Previous Time Step) Ctrl+Shift+P Selecting the next time step will bring in the next set of heads, drawdowns, and cell-by-cell flows
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Results – Stress Period 12
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Monitoring Wells Select: Plot – Hydrograph - Monitoring Well Select: Your Monitoring Wells Row 7 Column 9 Row 2 Column 9
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