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Groundwater pumping to remediate groundwater pollution. March 5, 2002. TOC . 1) Squares 2) FieldTrip: McClellan 3) Finite Element Modeling. First: Squares. Oxford Dictionary says “a geometric figure with four equal sites and four right angles”. Squares.
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Groundwater pumping to remediate groundwater pollution March 5, 2002
TOC • 1) Squares • 2) FieldTrip: McClellan • 3) Finite Element Modeling
First: Squares • Oxford Dictionary says • “a geometric figure with four equal sites and four right angles”
Squares • Units within a flow net are curvilinear figures… • In certain cases, squares will be formed • Constant head boundary…
Flownet • No flow crosses the boundary of a flowline ! • If interval between equipotential lines and interval between flowlines is constant, then volume of water within each curvilinear unit is the same…
Flow nets (rules) • Flowlines are perpendicular to equipotential lines • One way to assume that Q’s are equal is to construct the flownet with curvilinear squares • Streamlines are perpendicular to constant head boundaries • Equipotential lines are perpendicular to no-flow boundaries
Flow nets (rules 2) • In heterogeneous soil, the tangent law is satisfied at the boundary • If flow net is drawn such that squares exist in one part of the formation, squares also exist in areas with the same K a1 K1 K2 a2
How to determine the spacing of wells? • Determine feasible flow rates • Determine range of influence • Determine required decrease of water table • Calculate well spacings
Confined Aquifer • Well discharge under steady state can be determined using
Unconfined Aquifer • Well discharge under steady state can be determined using
Unconfined Aquifer • Well discharge under steady state WITH surface recharge can be determined using
What is optimal well design ? • In homogeneous soil:
In heterogeneous situation: • Wells have flow rate between 1 and 100 gpm • Some wells are in clay, others in sand
Finite Difference method • Change the derivative into a finite difference D
Approach to numerical solutions • 1) Subdivide the flow region into finite blocks or subregions (discretization) such that different K values can be assigned to each block and the differentials can be converted to finite differences
Approach to numerical solutions • 2) Write the flow equation in algebraic form (using finite difference or finite elements) for each node or block
Approach to numerical solutions • 3) Use “numerical methods” to solve the resulting ‘n’ equations in ‘n’ unknowns for h subject to boundary and initial conditions
1-D example • Boundaries: h left = 10, h right = 3 • Initial conditions h = 0 • K is homogeneous = 3 • Delta x = 2