Central Valley Aquifer, Chapters A and B - MAE Class Websites

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190 Groundwater Availability of the Central Valley Aquifer, California 0 50 100 Miles 0 50 100 Kilometers Shaded relief derived from U.S. Geological Survey National Elevation Dataset, 2006. Albers Equal Area Conic Projection EXPLANATION Stream cell hydraulic conductivity, in feet per day— 0.0413406 0.0564332 0.16405 0.193579 0.326131 0.3281 0.479026 0.588939 1.29271 2.71358 3.31381 5.63676 32.81 328.133 (K_SACRIVN) (K_TRIB_NWB) (K_SACRIV) (K_TRIB_SW) (K_TRIB_NE) (K_OTHER1) (K_SJRIV) (K_TRIB_SEB) (K_TRIB_NEB) (K_SO_RIV) (K_TRIB_SE) (K_TRIB_NW) (K_OTHER2) (K_TRIB_SEC) Active model grid boundary Model water-balance subregions Inflow locations Figure C26. Distribution of cells used for streams, colored by streambed hydraulic conductivity values for cells estimated during calibration.
Sensitivity Analysis - limited the use of systematic parameter-estimation techniques - estimation techniques based on perturbation approaches for used to identify the parameters to include in the parameter - - ( K - - - - Simulation Results and Budget 191 Simulation Results and Budget - 42-year simulation. This chapter focuses on the simulation of are the focus of . aquifer-system compaction and land subsidence. ( and
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GROUNDWATER RESOURCES PROGRAM Groun
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Groundwater Availability of the Cen
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Foreword An adequate supply of grou
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Contents Chapter A Introduction, Ov
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Chapter C Numerical Model of the Hy
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Figures Chapter A Figure A1. Map of
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Figure B12. Map of altitude of the
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Figure C28. Pie chart and histogram
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Conversion Factors Inch/Pound to SI
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Chapter A. Introduction, Overview o
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- - precipitation. -
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40° 39° 38° 37° 36° 35° Klama
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Texture Model DATA Centralized Geos
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Hydrology Water Well Information Aq
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Table A1. Water-balance subregions
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B Red Bluff 0 50 100 Miles 0 50 100
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Delta and Eastside Streams ).
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for about 30 percent of the annual
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0 50 100 Miles 0 50 100 Kilometers
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A Coast Ranges Clayey lenses Fault
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- the distribution of these pro
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C DEPTH TO MIDPOINT OF INCREMENT, I
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). The southern part, referred , in
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3-D Model of Percentage of Coarse-G
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A Layer 1 EXPLANATION Central Valle
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C Layer Corcoran Clay EXPLANATION C
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E Layer 9 EXPLANATION Central Valle
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Geomorphic province— Basin Delta
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San Joaquin Valley ),
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- Water supplied from aquifers
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C Figure A16. Continued. 3.54% 5.45
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CUMULATIVE DEPARTURE OF PRECIPITATI
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CUMULATIVE DEPARTURE OF STREAMFLOW
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700 500 600 400 200 160 0 50 100 Mi
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B 0 50 100 Miles 0 50 100 Kilometer
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Water Budget per year (
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References Cited 55 -
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References Cited 57 - - 2009, at
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60 Groundwater Availability of the
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