By H. M. Haitjema

ISBN-10: 0123165504

ISBN-13: 9780123165503

Modeling has turn into a necessary device for the groundwater hydrologist. the place box info is proscribed, the analytic aspect approach (AEM) is quickly changing into the modeling approach to selection, specially given the provision of cheap modeling software program. Analytic point Modeling of Groundwater movement presents the entire fundamentals essential to procedure AEM effectively, together with a presentation of basic strategies and a radical advent to Dupuit-Forchheimerflow. This publication is exclusive in its emphasis at the genuine use of analytic point versions. Real-world examples supplement fabric awarded within the text.An academic model of the analytic aspect application GFLOW is incorporated to permit the reader to breed a number of the recommendations to groundwater stream difficulties mentioned within the textual content. Researchers and graduate scholars in groundwater hydrology, geology, andengineering will locate this ebook an crucial resource.** offers a primary creation to using the analytic point method.* deals a step by step method of groundwater circulate modeling.* contains an instructional model of the GFLOW modeling software program.

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**Example text**

DUPUIT-FORCHHEIMER FLOW P . . . . . . . . . . . . . ....................... . . . . . 9 I Q1 Q2 reference point , , xO ~ . 15: Locations of two nearby wells in an aquifer. 96) Tile integration constants C1 and C2 are not yet defined at this point.

If we follow a (fictitious) water particle through the aquifer, its path will cross equipotentials under 900 angles, by virtue of our preceding analysis. Under steady-state flow conditions, the pathlines of water particles are called streamlines. 8, a few streamlines and equipotentials are sketched. 64). Note that the total amount of water AQ [L3/T] that moves between two streamlines does not change, regardless of whether the streamlines converge or diverge. By definition of a streamline, there is no water that can cross a streamline, and hence no water can be added to or escape from the domain bounded by two streamlines.

The origin of a radial (r, 0) coordinate system is chosen at the center of the well. Because of radial symmetry, there is only flow parallel to the direction r. 1. 12: Radial flow toward a well. 82) where Q [ L 3 / T ] is the discharge (pumping rate) of the well, and where ( - Q r ) is the discharge vector component across the circle per unit length of the circle. 12. 85) 48 C H A P T E R 3. D U P U I T - F O R C H H E I M E R F L O W where Cw is a constant of integration which may be chosen to satisfy some boundary condition.

### Analytic Element Modeling of Groundwater Flow by H. M. Haitjema

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