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Boundaries and Superposition Groundwater Hydraulics Daene C. McKinney

Boundaries and Superposition Groundwater Hydraulics Daene C. McKinney

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Boundaries and Superposition

Groundwater Hydraulics

Daene C. McKinney

Introduction

• Review– Continuity in Aquifers– Steady flow to a well in confined aquifer

• Superposition• Two Wells in an Aquifer• Image Well

– for an Impermeable Boundary– for a Constant Head Boundary

• Multiple Wells in an Aquifer

Continuity in Aquifers

• Confined aquifer

• Unconfined aquifer

• Linear equations– If h1 and h2 both satisfy a linear equation– Then another solution is

h3 = Ah1 + Bh2

– where A and B are constants(For unconfined aquifer, everything is in terms of h2)

Steady Flow to a Well in a Confined Aquifer

2rw

Ground surface

Bedrock

Confined aquifer

Q

h0

Pre-pumping head

Confining Layer

br1

r2

h2h1

hw

Observation wells

Drawdown curve

Q

Pumping well

Point of interest (x,y) Well at = (xw,yw)

Superposition (2 wells pumping)

Superposition (n Wells pumping)

1r2r

3r

1Q

2Q

3Q

),(11yx

),(33yx

),(22yx

),( yx

Steady Flow to a Well in an Unconfined Aquifer

2rw

Ground surface

Bedrock

Unconfined aquifer

Q

h0

Pre-pumping Water level

r1

r2

h

2h1

hw

Observation wells

Water Table

Q

Pumping well

Example

x

y

1r 2rQ Q

),( yx

oH

ExampleQ = 2x10-2 m3/s, T = 5x10-3 m2/s, Ho = 25 m, rw = 0.25 m

x

y

600 m

1r 2rQ Q

)0,25(

),( yx

)0,25(o

H

mC 9.201

mC 9.202

Example• How much does the pumping in

well 2 affect the head in well 1?

• With both wells pumping

• With only Well 1 pumping

• Difference = 1.54 m

x

Q Q

)0,25(

),( yx

)0,25(

Superposition (n Wells pumping)

1r2r

3r

1Q

2Q

3Q

),(11yx

),(33yx

),(22yx

),( yx

Image Well to Simulate Impermeable Boundary

x

Q

wellImage

)0,(wx

),( yx

)0,(wx

Q

wellReal

1r 2

r

region Real region Image

y

Boundary

Drawdown Near Impermeable Boundary

Todd, 1980.

Image Well to Simulate Constant Head Boundary

x

Q

wellImage

)0,(wx

),( yx

)0,(wx

Q

wellReal

1r 2

r

region Real region Image

y

Stream

Example - Constant Head Boundary

Example – Impermeable Boundary

Multiple Well Systems

Summary

• Review– Continuity in Aquifers– Steady flow to a well in confined aquifer

• Superposition• Two Wells in an Aquifer• Image Well

– for an Impermeable Boundary– for a Constant Head Boundary

• Multiple Wells in an Aquifer

Well 1 pumping alone

Well 2 pumping alone

Both wells pumping together