Head Dependent Boundaries

Slides:



Advertisements
Similar presentations
Simulation of groundwater response to development: CENTRAL PASSAIC RIVER BASIN, NJ Fatoumata Barry 1,2, Duke Ophori 1, Jeffrey L. Hoffman 2 and Robert.
Advertisements

The Drainage Basin System
EARTHS WATER SUPPLY. SOME QUICK FACTS 70% of the Earths surface is covered with water 70% of the Earths surface is covered with water 97% of Earths water.
Water in a river drainage system
Groundwater Hydraulics Daene C. McKinney
Groundwater Flow Equations
Groundwater Modeling - 1
1 Using SUB model to predict long-term land subsidence in Yunlin and Chiayi areas Presenter : Chiou-Shiang Hung Adviser : Chuen-Fa Ni Date : 2010/10/07.
The Sacramento Regional Groundwater Model Derrick Whitehead Roseville City - Roseville, CA Norm Jones Aquaveo - Provo, UT Michelle Smilowitz Heatwave Data.
2 A J B F 5 6 E 8 C G 10 4 I 26 H D N Legend Source drains into the ditch here. Data point directly.
Boundaries and Superposition
(e.g., the Toth Problem) z x z x h = c x + z o Profile Models.
General governing equation for transient, heterogeneous, and anisotropic conditions Specific Storage S s =  V / (  x  y  z  h)
Boundary Conditions A steady state solution with all specified flux boundary conditions (including no flow) without specified head or head-dependent internal.
GHB61 GENERAL HEAD BOUNDARY PACKAGE The General Head Boundary Package is used to, –Simulate head-dependent recharge or discharge across an aquifer boundary,
Transient Simulations require: Initial Conditions Storage Coefficient Time step.
Today’s Lecture: Grid design/boundary conditions and parameter selection. Thursday’s Lecture: Uncertainty analysis and Model Validation.
Engineering Hydrology (ECIV 4323)
Figure taken from Hornberger et al. (1998). Linear flow paths assumed in Darcy’s law True flow paths.
GLY 521- Hydrogeology Modflow Packages. Block Center Flow (BCF) Package The BCF package is the central package for all solutions Specify the way each.
Figure from Hornberger et al. (1998) Darcy’s data for two different sands.
Types of Boundary Conditions
EEOS 350: Quantitative hydrogeology Lecture 2 Water balance.
Integrated Water Management Modeling Framework in Nebraska Association of Western State Engineers Spring Workshop Salt Lake City, Utah June 9, 2015 Mahesh.
MODFLOW – Introduction Organization & Main Packages
The Islamic University of Gaza Faculty of Engineering Approaches to Groundwater Modeling Conceptual Model.
III. Ground-Water Management Problem Used for the Exercises.
Representing Groundwater in Management Models Julien Harou University College London 2010 International Congress on Environmental Modelling and Software.
These notes are provided to help you pay attention IN class. If I notice poor attendance, fewer notes will begin to appear on these pages 1.
Local Groundwater Flow Model Addendum Guadalupe Restoration Project San Luis Obispo County October
 These slides were presented to the Hood River Basin Water Planning Group on May 1, 2013 by Jon Rocha and Jennifer Johnson.  Slides contain animations.
Grid design/boundary conditions and parameter selection USGS publication (on course website): Guidelines for Evaluating Ground-Water Flow Models Scientific.
Modflow, GWVistas MODular three-dimensional finite- difference ground-water FLOW model
Studying the effects of an irrigation/drainage network on groundwater table fluctuations using 3D groundwater flow modeling Mohammad Zare Manferd Koch.
Surface Water – Groundwater Interaction in San Acacia Reach
CE EN 547 – BRIGHAM YOUNG UNIVERSITY.  River  Stream-Aquifer Interaction  General Head  Changing Head Boundary  Horizontal Flow Barrier.
Modflow Simulation on Savannah River GIS For Water Resources Term Project (CE 394) Seyoum Asemenaw.
The Islamic University of Gaza Faculty of Engineering Civil Engineering Department EENV 5326 Groundwater Modeling.
Model Status Update July 01, Agenda Purpose Model Development Update Model Calibration Status Next Steps Schedule Public Input.
Transient Simulations require: Initial Conditions Storage Coefficient Time step.
IX. Transient Forward Modeling. Ground-Water Management Issues Recall the ground-water management issues for the simple flow system considered in the.
CE EN 547 – BRIGHAM YOUNG UNIVERSITY. 1. Build conceptual model object 2. Build coverages 3. Define grid frame 4. Build grid 5. Initialize MODFLOW 6.
Groundwater Flow Equations Groundwater Hydraulics Daene C. McKinney.
Flow to Wells - 1 Groundwater Hydraulics Daene C. McKinney.
CE 3354 Engineering Hydrology Lecture 2: Surface and Groundwater Hydrologic Systems.
Objective: conceptual model definition and steady state simulation of groundwater flow.
Building Transient MODFLOW Models
Radial Flow to an Unconfined Aquifer From Mays, 2011, Ground and Surface Water Hydrology.
CHAPTER 11 - WATER Section 1 – Water Resources – Pt 1.
Groundwater Modeling Assignment #2. Parts A and B.
Engineering Hydrology (ECIV 4323)
Transient Water Balance Eqn.
Test 1 Review Chapter 1, Hydrologic cycle and the water balance
Remediation of a Leaking Landfill Site
Dewatering Solutions using MODFLOW
GROUNDWATER.
The Islamic University of Gaza Faculty of Engineering Approaches to Groundwater Modeling Conceptual Model.
Anisotropy – Key ideas Effective conductivity that represents aggregate effect of flow through a layered system Effective conductivity is different parallel.
2.1 Basic hydrology.
Lessons Learned in the Decade Since the San Pedro Capture Map
Boundary Conditions Sources and Sinks Based on Slides Prepared By
Fresh Water and River Systems
Transient Models See Anderson and Woessner Chapter 7
The hydrologic cycle.
The Location & Movement of Water on Earth’s Surface
GLOBAL PROCESS DATA Name File: Contains the names of most input and output files and controls the parts of the model program that are active. Discretization.
Chapter 5 Sources and Sinks
2New Jersey Department of Environmental Protection
Fresh Water and River Systems
GHOST (Generic Hydrologic Overland-Subsurface Toolkit)
Presentation transcript:

Head Dependent Boundaries in MODFLOW88 Q = C h River Package Drain Package General Head Boundary (GHB) Package ET Package

River Package Q = C (hR – hijk) where C =KvLw/m

Drain Package

Drain Package Q = C (hijk-d) Q = 0 if hijk<d where d = head in the drain. Q = 0 if hijk<d

General Head Boundary Package Boundary cell hB L h Q= C (hB-h) C = K A /L

Lake Model hB L GHB Q = C (hB - h) C = Conductance = K A/L K is the hydraulic conductivity of the aquifer between the model and the lake; A is the area of the boundary cell, perpendicular to flow.

Evapotranspiration (EVT) Package …to be discussed later, when we do the Final Project

New MODFLOW Packages to simulate dynamic interchange between groundwater and surface water • Stream Package (Prudic, 1989) • MODBRANCH (Swain, 1993) • Lake Package (Cheng and Anderson, GW,1993) (Council, 1998) (Merritt and Konikow, 2000) • Wetland Module (Restrepo et al., GW,1998)

Lake (LAK) Package Change in Storage = Outflow - Inflow Change in lake level = Change in Storage/Area

Transient Simulations require: Initial Conditions Storage Coefficient Time step

Types of Initial Conditions Static steady state Dynamic steady state Dynamic cyclic conditions (Time distant conditions)