CE 3354 Engineering Hydrology

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Presentation transcript:

CE 3354 Engineering Hydrology Lecture 23: Transient (Time-Varying) Well Hydraulics; Superposition

Outline Steady flow to well Superposition to represent Confined Unconfined Superposition to represent Multiple wells Aquifer Boundaries

Outline Unsteady flow to a well Superposition Convolution Spreadsheets Confined (Theis Solution) Superposition Multiple wells Aquifer Boundaries Convolution Time-varying pumping rates Leaky (Hantush Solution) Spreadsheets

Confined Aquifer Theim solution

Confined Aquifer Theim solution Derivation in attached reading

Unconfined Aquifer Sketch

Unconfined Aquifer Several solutions: Use this one

Superposition Linear combination of solutions to model effect of Multiple wells Boundaries

Superposition

Superposition

Superposition

Superposition

Superposition

Superposition

Superposition

Superposition

Well Interference Two (or more) wells operating near each other produce a combination drawdown that might affect operation of the wells If the pump impellers are not deep enough, the well may not produce because of drawdown caused by nearby wells

Well Interference Superposition is used to model such situations

Well Interference Superposition is used to model such situations

Well Interference

Well Interference

Confined Aquifer Transient flow to a well (sketch of derivation – more in readings)

Confined Aquifer Governing PDE and BCs Oddly enough Drawdown is lower case “s” and storativity is upper case “S”– need to be aware when reading. Storage Coefficient Drawdown

Confined Aquifer Governing PDE and BCs

Confined Aquifer Solving the PDE – apply a Boltzman Transformation

Confined Aquifer Solving the PDE – apply a Boltzman Transformation Convert PDE into an ODE

Confined Aquifer Solving the PDE – Algebra and Calculus

Confined Aquifer Apply IC and BCs

Confined Aquifer Apply IC and BCs

Confined Aquifer Now we have a solution, but how to evaluate the integral? Once upon a time you would look up values in a table (readings) Alternatively, you can apply a series expansion of the integrand and find a series solution

Confined Aquifer Now we have a solution, but how to evaluate the integral?

Confined Aquifer Now we have a solution, but how to evaluate the integral?

Confined Aquifer Now we have a solution, but how to evaluate the integral?

Confined Aquifer VBA Code (to evaluate the well function)

Confined Aquifer

Superposition

Superposition

Superposition

Superposition

Superposition

Convolution Convolution == Superposition in Time

Convolution Convolution == Superposition in Time

Leaky Aquifer Hantush Model

Leaky Aquifer Hantush Model

Leaky Aquifer Leakage prior to pumping

Leaky Aquifer Leakage after pumping begins

Leaky Aquifer Leakage – drawdown relationship

Leaky Aquifer Governing PDE and BCs

Leaky Aquifer Governing PDE and BCs

Leaky Aquifer Solution(s)

Leaky Aquifer Solution(s)

Leaky Aquifer Solution(s)

Leaky Aquifer Example

Leaky Aquifer Example

Leaky Aquifer Example

Leaky Aquifer Example

Leaky Aquifer Table-look up

Leaky Aquifer Table-look up

Leaky Aquifer More Modern Approach: VBA Script in Excel to evaluate W(u,r/B) Complex uses: ERFC (complimentary error function) BESSELI (Bessel Function Type I) BESSELJ (Bessel Function Type J) Script too complex to display – but ultimately it is just a function that can be evaluated just like SQRT(Z).

Leaky Aquifer

Next Time Contaminant Transport Concepts Aquifer Numerical Modeling Advection, Dispersion, Retardation, Decay Aquifer Numerical Modeling Flow Nets