groundwater pumping to remediate groundwater pollution

Groundwater pumping to remediate groundwater

pollutionMarch 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 formedConstant head boundary…

Flownet

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

K1K2

2

1

tantan

21

KK1

2

Second: McClellan Airbase

Piping system

Groundwater extraction wells

Waste water treatment plant

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

)ln(

2

1

2

12

rr

hhbKQ

Unconfined Aquifer Well discharge under steady state can be

determined using

)ln(

1

2

21

22

rr

hhKQ

Unconfined Aquifer Well discharge under steady state WITH surface

recharge can be determined using

21

22

)ln(

w

orr

wo hhKQ

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

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

xhK

xxhK

x xx

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