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Head Dependent Boundaries

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Presentation on theme: "Head Dependent Boundaries"— Presentation transcript:

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

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

3 Drain Package

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

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

6 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.

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

8 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)

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

10 Transient Simulations require:
Initial Conditions Storage Coefficient Time step

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


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