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0. Introduction
Contents
1. Steady one-dimensional flow with constant transmissivity
1.1. Flow between two rivers
1.2. Areal recharge between two rivers
1.3. Areal recharge between an impermeable boundary and a river
1.4. Flow through two zones of different transmissivities
2. Steady one-dimensional semi-confined flow
2.1. Flow from a canal to a drained area
2.2. Flow between a lake and a drained area
2.3. Flow to a river of finite width
2.4. Flow to a river in a two-aquifer system
2.5. Areal recharge between two rivers in a two-aquifer system
3. Steady one-dimensional unconfined flow with variable saturated thickness
3.1. Areal recharge between an impermeable boundary and a river
3.2. Flow over a step in the aquifer base
3.3. Combined confined/unconfined flow with areal recharge
4. Steady one-dimensional flow in coastal aquifers
4.1. Confined interface flow
4.2. Unconfined interface flow
4.3. Combined confined/semi-confined interface flow
5. Transient one-dimensional flow
5.1. Step changes in surface water level
5.2. Periodic changes in surface water level
5.3. Areal recharge between two rivers
5.4. Solutions with Laplace transforms
5.5. Unconfined flow with variable transmissivity
6. Steady two-dimensional flow to wells
6.1. Radially symmetric flow on a circular island
6.2. Wells near rivers and impermeable boundaries
6.3. Wells near an inhomogeneity boundary
6.4. Wells in a semi-confined aquifer
6.5. Wells in a two-aquifer system
7. Steady two-dimensional flow to wells in uniform background flow
7.1. A single well in uniform background flow
7.2. Well capture zones
7.3. A well in uniform background flow near a river
7.4. A well in uniform background flow near the coast
7.5. Two wells in uniform background flow
7.6. A well in uniform background flow near a river with a leaky stream bed
8. Analytic element modeling of steady two-dimensional flow
8.1. Uniform flow and wells
8.2. Line-sinks for modeling rivers and streams
8.3. Area-sinks for modeling areal recharge
9. Transient two-dimensional flow
9.1. Wells in confined and unconfined aquifers
9.2. A well with a periodic discharge
9.3. Wells in a semi-confined aquifer
9.4. Wells with wellbore storage and skin effect
9.5. Wells in a two-aquifer system
10. Steady two-dimensional flow in the vertical plane
10.1. Vertical anisotropy
10.2. Flow to a partially penetrating stream
10.3. Flow over a step in the base
10.4. Spatially varying head at the top of the aquifer
10.5. Interface flow towards the coast
10.6. Interface flow below a strip island
Appendices
A. Python primer
A.1 Basics
A.2 Loops and if statements
A.3 The
numpy
package and arrays
A.4 The
matplotlib
package for visualization
A.5 Functions
A.6 The
scipy
package for scientific computing
B. Acknowledgement
Bibliography
Repository
Open issue
Index
