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as mountainous terraines, and under different scales. This may be a reason why flownet<br />
analysis is not used much in practice.<br />
Flownets can be generated very easily by means of the dual theory of analysis. This<br />
method, which comes from fluid dynamics, was first introduced in Canada in the<br />
early 1980s by the first author, and it has since been enhanced by the second author.<br />
The dual method consists of two governing equations: the standard equation for potentials,<br />
and a complementary equation, based on the Cauchy-Riemann relationship,<br />
for streamfunctions. The boundary conditions are also complementary. Because both<br />
equations have the same form, they can be solved together using the same numerical<br />
techniques. The plots of these two independent solutions give an accurate flownet<br />
for any type of flow system, even under highly complex conditions or extreme scale<br />
distortions. With some enhancements, it can also inform about groundwater age. The<br />
only limitations are that flow is within the cross-sectional plane, of uniform density,<br />
and at steady state, and the system has no internal sources or sinks. Incorporated into<br />
the model FLONET, the dual solution can be used to verify 3D solutions for more<br />
complex situations. A key feature is that the method can easily be used to test the<br />
effect of many different configurations and boundary conditions for a given system –<br />
giving answers to the ubiquitous “what if ” question – without running an expensive<br />
3D model. Above all, it is a valuable teaching tool in both the classroom and the computer<br />
lab, and as the above-mentioned former student aptly recognized, it gives a clear<br />
understanding of how a groundwater system works.<br />
311 - Unstated assumptions – a challenge for students and<br />
hidden traps for the unwary<br />
Garth van der Kamp<br />
Water Science and Technology, Environment Canada, Saskatoon, Saskatchewan, Canada<br />
In hydrogeology, as in all of human thought, there are always unstated assumptions.<br />
Often it is precisely these invisible statements that turn out to cause the failure of the<br />
bridge, or the unintended consequences of a government policy, or to be the critical<br />
flaw in a paper in Water Resources Research. But it is also these assumptions that are<br />
hardest to detect – they are smoothed over beautifully because usually the authors<br />
are not even aware of them. Hydrogeology science and its publications contain many<br />
examples of invalid unstated assumptions, as hidden traps for the unwary. Unstated<br />
assumptions which are shared by a whole community of researchers are hardest to<br />
detect – such paradigms are very interesting when they are identified, because that can<br />
lead to major advances in the science!<br />
We published a minor paper in Water Resources Research in 1969 (Carr and van der<br />
Kamp, Vol. 5, 1023-1031) which contains a fatal flaw. The source of the error was an<br />
unstated and invalid assumption in a 1950 publication by C.E. Jacob, a recognized<br />
“authority” in hydrogeology, so we could be excused. It was three years later before<br />
the error was identified by a graduate student (myself ) in an “aha!” moment while<br />
puzzling over some strange observations that could not be explained by the theory in<br />
192 IAH-CNC 2015 WATERLOO CONFERENCE