Difference between revisions of "Groundwater Gourmet (TM)"

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(New page: The Groundwater Gourmet is a place for community contributions of recipes, howtos and examples for analytical and numerical modeling of ground water flow and transport. Groundwater Gourme...)
 
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Confidence in contributed code might be enhanced if principles of design by contract are agreed upon for object oriented languages (see wikipedia [http://en.wikipedia.org/wiki/Design_by_contract Design By Contract],  [http://www.nongnu.org/pydbc/ Python DBC], and [http://www.swe.uni-linz.ac.at/publications/abstract/TR-SE-97.24.html Design by Contract for Python]).
 
Confidence in contributed code might be enhanced if principles of design by contract are agreed upon for object oriented languages (see wikipedia [http://en.wikipedia.org/wiki/Design_by_contract Design By Contract],  [http://www.nongnu.org/pydbc/ Python DBC], and [http://www.swe.uni-linz.ac.at/publications/abstract/TR-SE-97.24.html Design by Contract for Python]).
  
= [[library| library of analytic solutions (proposed)]] =
+
 
 +
= analytic and analytic element solutions (Strack,1989 classification) =
 +
 
 +
== horizontal confined flow ==
 +
 
 +
=== one-dimensional flow ===
 +
 
 +
insert text description
 +
 
 +
<math> \phi = -(\phi_1 - \phi_2 )\frac{x}{L} + \frac{1}{2}(\phi_1 + \phi_2) </math>
 +
 
 +
 
 +
insert conceptual model (graphic)
 +
 
 +
insert code snippets (python, fortran)
 +
 
 +
insert solution heads (graphic)
 +
 
 +
=== radial flow ===
 +
 
 +
=== two-dimensional flow ===
 +
 
 +
== shallow unconfined flow ==
 +
 
 +
=== one-dimensional flow ===
 +
=== two-dimensional flow ===
 +
 
 +
== combined shallow confined and unconfined flow ==
 +
 
 +
=== one-dimensional flow ===
 +
=== radial flow ===
 +
 
 +
== shallow unconfined flow with rainfall ==
 +
 
 +
== shallow interface flow ==
 +
 
 +
== aquifers with vertically varying hydraulic conductivity ==
 +
 
 +
== shallow flow in aquifers with clay laminae ==
 +
 
 +
== shallow interface flow in aquifers with impermeable laminae ==
 +
 
 +
== shallow semiconfined flow ==
 +
 
 +
== shallow flow in systems of aquifers separated by leaky layers ==
 +
 
 +
== transient shallow flow ==
 +
 
 +
== two-dimensional flow in the vertical plane ==
 +
 
 +
== three-dimensional flow ==
 +
 
 +
= analytical solutions (Bruggeman,1999 classification) =
 +
 
 +
== Phreatic groundwater ==
 +
 
 +
Exact solutions
 +
 
 +
One-dimensional horizontal flow
 +
 
 +
Two-dimensional radial-symmetric horizontal flow
 +
 
 +
General two-dimensional horizontal flow
 +
 +
== Confined groundwater ==
 +
 
 +
One-dimensional flow
 +
 
 +
Two-dimensional radial-symmetric flow
 +
 
 +
General two-dimensional flow
 +
 
 +
Three-dimensional spherical flow
 +
 
 +
Three-dimensional axial-symmetric flow
 +
 
 +
General three-dimensional flow
 +
 
 +
== Multi-layer systems ==
 +
 
 +
== Dispersion ==
 +
 
 +
==  Density flow (interface)==
  
 
= recipes =
 
= recipes =

Revision as of 15:06, 6 November 2007

The Groundwater Gourmet is a place for community contributions of recipes, howtos and examples for analytical and numerical modeling of ground water flow and transport.

Groundwater Gourmet wiki uses a subset of TeX, including some extensions from LaTeX and AMSLaTeX, for mathematical formulae. Thus, only a limited part of the full TeX language is supported. Here is a guide for math syntax.

Please note that all contributions to the Groundwater Gourmet may be edited, altered, or removed by other contributors, in the spirit of collegiality and peer review. Do not submit copyrighted work with permission. You are encouraged to assign an open source license to your source code.

Confidence in contributed code might be enhanced if principles of design by contract are agreed upon for object oriented languages (see wikipedia Design By Contract, Python DBC, and Design by Contract for Python).


analytic and analytic element solutions (Strack,1989 classification)

horizontal confined flow

one-dimensional flow

insert text description

<math> \phi = -(\phi_1 - \phi_2 )\frac{x}{L} + \frac{1}{2}(\phi_1 + \phi_2) </math>


insert conceptual model (graphic)

insert code snippets (python, fortran)

insert solution heads (graphic)

radial flow

two-dimensional flow

shallow unconfined flow

one-dimensional flow

two-dimensional flow

combined shallow confined and unconfined flow

one-dimensional flow

radial flow

shallow unconfined flow with rainfall

shallow interface flow

aquifers with vertically varying hydraulic conductivity

shallow flow in aquifers with clay laminae

shallow interface flow in aquifers with impermeable laminae

shallow semiconfined flow

shallow flow in systems of aquifers separated by leaky layers

transient shallow flow

two-dimensional flow in the vertical plane

three-dimensional flow

analytical solutions (Bruggeman,1999 classification)

Phreatic groundwater

Exact solutions

One-dimensional horizontal flow

Two-dimensional radial-symmetric horizontal flow

General two-dimensional horizontal flow

Confined groundwater

One-dimensional flow

Two-dimensional radial-symmetric flow

General two-dimensional flow

Three-dimensional spherical flow

Three-dimensional axial-symmetric flow

General three-dimensional flow

Multi-layer systems

Dispersion

Density flow (interface)

recipes

I imagine placing code snippets here of solutions like in AEM Depot of James Craig.. Once a solution is accepted by the community (test of time) then it is added to the library.

flow

transport

howtos

Not sure, but perhaps tricks of the trade in solution techniques, modeling practice.

examples

laboratory experiments/physical analoges (e.g., Hele shaw)

numerical laboratories (e.g., Igor Jankovic)

benchmark and example problems (e.g., Henry Problem)

controlled field experiments (e.g., Borden site, MADE site, Cape Cod site)