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Southwest Kansas Groundwater Management District #3 Model Kansas Water Office Contract A Kansas Water Plan Project Progress Report March 29, 2010
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Major Progress PEST Calibration – 16 runs 1) Power functions for recharge-precipitation 2) Five-year water level differences 3) Weighting factor change for streamflow
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Power P-R Functions P 0 is threshold precipitation after which groundwater recharge occurs. For each recharge zone, P 0, a and b are calibrated.
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PEST Runs D-J D: Change linear P-R segments to power functions. Other settings same as Run B in TAC020810. E: Change water-level difference targets from 1 year to 5-year intervals. Other settings same as D. Different runs derived from E - F: Fix P-R power functions, calibrate PST+ K and Sy. G: Fix P-R power functions and Sy, calibrate K. H: Fix P-R power functions and K, calibrate Sy. I: Use optimal values from H and recalibrate all parameters. J: Use optimal values from I and calibrate all parameters, but lower the maximum limit for Sy (the calibrated Sy for sands and gravels from I was 39%).
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PEST Runs K-S K: Double the weighting factor for streamflow targets. Other setting same as J. L: Use log for K. Other settings same as J. M: Decrease the weighting factor for streamflow targets by half. Use log for K. N: Increase precipitation recharge for zone 3. Calibrated recharge for zone 3 too small. O: Change precipitation recharge parameter settings for zone 2. Calibrated recharge for zone 2 not physically reasonable. P: Further modify recharge parameter settings. Calibrated recharge for zone 2 from O still not physically reasonable. Q: Further modify recharge parameter and specific yield settings. Precipitation recharge curve for zone 2 not reasonable. The Sy values considered a little too high after KGS internal team discussion. R and S: Similar to Q, fix K and Sy and further improve recharge parameters.
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PEST Run RMS Summary Overall Predevelopment Heads (ft) Water Level Difference (ft) Streamflows log(cfs) B (TAC020810) 26.7621.10 4.80 (1-yr interval) 0.85 D27.5621.70 4.85 (1-yr interval) 1.01 E36.9826.29 9.40 (5-yr interval) 1.29 F32.2621.699.371.20 G31.3221.089.310.94 H31.2821.089.270.93 I31.2121.149.220.84 J31.3121.249.220.85 K31.2821.189.250.84 L31.0620.999.220.85
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PEST Run RMS Summary Overall Predevelopment Heads (ft) Water Level Difference (ft) Streamflows log(cfs) E36.9826.299.401.29 F32.2621.699.371.20 G31.3221.089.310.94 H31.2821.089.270.93 I31.2121.149.220.84 J31.3121.249.220.85 K31.2821.189.250.84 L31.0620.999.220.85 M31.0921.039.220.84 N30.8020.789.180.85 O30.9920.949.200.85 P30.8120.819.160.84 Q31.3821.139.320.93 R31.2321.189.220.83 S32.5322.539.160.83
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Comparison to Previous Models Model Changes Head Statistics Streamflows Log(cfs) RMS RMS (ft)MAR (ft)RMAE(%) TAC 0917200935.6925.331.441.07 PEST Run TAC 02082010 33.9923.811.360.85 PEST Run R TAC 03282010 33.3823.521.340.83
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Model Results from PEST Run R
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Current Model Recharge Zones Row Column Zone 1
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Calibrated P-R Curves
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Calibrated Synonymy K (ft/day) and Sy
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Parameter Sensitivity
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Predevelopment T ft 2 /d
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1996-2007 T ft 2 /d
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Predevelopment-1966 Sy
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1997-2007 Sy
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Predevelopment Precipitation Recharge in/yr
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2007 Precipitation Recharge in/yr
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Simulated vs. Observed Water Levels The RMS (root mean square), MAR (mean absolute residual) and RMAE (relative mean absolute error) are: 33.38 ft and 23.52 ft and 1.34%.
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Simulated vs. Observed Water Level Changes 5 Years 10 Years
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Simulated Vs. Observed Ark River Flows Syracuse RMS = 0.08 Deerfield RMS = 0.63 Garden City RMS = 0.46 Dodge City RMS = 0.85
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Cimarron River and Crooked Creek Flows Crooked Creek RMS = 0.40 Cimarron RMS = 0.10
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Well Hydrographs Paleo KearnyFinneyArkN GrayArkN KearnyFinneyArkS HoFo GrHsCimN GrayArkS-CC Stanton MT StSeCimS ME
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Well Hydrographs - Paleo Ark Valley
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Well Hydrographs – Kearny & Finney North of Ark
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Well Hydrographs – Gray North of Ark
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Well Hydrographs – Kearny & Finney South of Ark
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Well Hydrographs – Hodgeman & Ford
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Well Hydrographs - Stanton
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Well Hydrographs – Grant & Haskell North of Cimarron
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Well Hydrographs - Gray South of Ark to Crooked Creek
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Well Hydrographs - Morton The first well is in bedrock although the water level is slightly above bedrock surface; the second well is also in thinly saturated area on the tri-state border.
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Well Hydrographs - Stevens & Seward South of Cimarron
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Well Hydrographs - Meade
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GMD3 Model Boundaries Red – Specified Fluxes (Represented by a series of artificial wells)
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Water Budgets Across Boundaries (Accumulative)
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Water Budgets Across Boundaries (Annual)
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Bedrock Head Boundary Budgets (Accumulative)
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Bedrock Head Boundary Budgets (Annual)
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Arkansas River Flow Predevelopment 2007
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Crooked Creek Flow Predevelopment 2007
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Cimarron River Flow Predevelopment 2007
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Simulated Groundwater Budgets (Accumulative)
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Simulated Groundwater Budgets (Annual)
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Next Major Steps A few more PEST runs to check if the calibrated model can be further improved. Scenario simulation under different climatic and water use conditions.
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