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Published byJemima Fitzgerald Modified over 8 years ago
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An extension of the Arc Hydro Groundwater Simulation feature dataset
MODFLOW Data Model An extension of the Arc Hydro Groundwater Simulation feature dataset
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Simulation Feature Data Set
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Boundary Polygon J I
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Cell2D and Node2D Features
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CELL3D Features
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Ancestral Streams
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Ancestral Streams
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Ancestral Streams
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Riverbank Model Layer 1 Middle to Late Pleistocene deposits (formerly the Victor Formation) Hardpan deposits are prevalent in this formation that inhibit vertical infiltration of recharge from applied water and precipitation Consists of sands, silts, and clays from floodplain and alluvial deposits Superjacent ancestral stream channels cut across this formation creating lateral channels of gravels and unconsolidated sediments
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Turlock Lake Laguna Formation
Model Layers 3,4 and 5 Early Pleistocene to late Pliocene deposits (formerly the Fair Oaks Formation) Characteristic feature: white to grey tuff and tuffaceous silts “white clay” Predominantly consists of sands, silts, and clays Superjacent ancestral stream channels cut across this formation, creating lateral channels of gravels and unconsolidated sediments
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Mehrten Formation Composed of two dominant units:
Model Layers 6,7 and 8 Pliocene deposits formed during an erosional sequence following chain of volcanic eruptions Significant water bearing unit Composed of two dominant units: Black andesitic sands “salt and pepper sand” and blue and brown clays Hard gray and black tuff-breccias “lava”
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Valley Springs Formation
Model Layer 9 Middle Miocene deposits formed during sequence of volcanic eruptions Characteristic features: olive green – greenish gray tone of clays, silts Consists of rhyolite ash, quartz sand , and ashy clay
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Ione Formation Consists of sandstone, silts, and clays Model Layer 10
Consists primarily of sandstone and clays deposited during the Eocene epoch, a time when the ancient sea became fresh to brackish. Generally low in permeability, although secondary fracturing near the outcrops Consists of sandstone, silts, and clays
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Interface Data Models
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MODFLOW Data Model Data standard for storing MODFLOW models in a GIS database Importing models built externally Building new MODFLOW models inside ArcGIS Custom scripts for analyzing/modifying models can be developed as geoprocessing tools
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MODFLOW Data Model
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MODFLOW Analyst Tools Developed as geoprocessing (GP) tools
Classes of tools Import Export Visualization/Map Layers Model editing Building package input Working with transient input/solutions
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Import MODFLOW Model Tool
INPUT OUTPUT
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Make MODFLOW Features Tool
+ Cell2D Node2D Or INPUT OUTPUT
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Map Layer – Computed Head
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Discretize: Spatial Temporal Build Package Input
Polygons K zones (overlay) Points K values (interpolate) Polylines River cells Points Wells Temporal Time Series Stress Periods
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Discretization of Features
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MODFLOW Array from Polygons
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Geoprocessing Tools
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Geoprocessing Tools
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Geoprocessing Tools - Workflows
GP tools enable the development of workflows as models or scripts Extendable – You can create your own workflows Leverage low-level tools to create new tools
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Model Domain Bear River Sierra Nevada Feather River Sacramento River
Mokelumne River
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Change from Non-urban to Urban
Land Use Patterns Farm Data Change from Non-urban to Urban Master Land Use File
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Water Unit Demand Factors
Agricultural Demand Factors (DWR) Model Output for Representative Water Years Urban Demand Factors Normalization Factor based on Water Year Index Monthly Conversion Factors Water Year Index 2002 ITRC Crop Evapotranspiration Rates for Eto Zone 14 ITRC Report , funded by CALFED and Agricultural Research Initiative of California State Univ.
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Calibration of Urban Demand Factors
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GSSHA Results 1 2 3 4 5 6 7
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Automated Workflow Total Recharge GSSHA simulations
Recharge coeff. for each STLU for each water year Master Land Use Files Water Unit Demand Factors Water Year Total Recharge GSSHA Simulation Recharge Coeffs Calculate Change in Land Use Calculate Recharge Model Total Applied Water and Precip Calculate Water Demand Calculate Total Applied Water Recharge to MODFLOW Total Flow from Ungaged Watersheds Water Budgeting and Accounting Calculate Demand Summary Lateral Inflow to MODFLOW Distribute Demand
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For more information (AHGW Wiki page) (Info on tools) Norm Jones
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