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Published in Soil Sci Soc Am J 28:156-160 (1964)
© 1964 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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The Streamline Function for Axially Symmetric Groundwater Movement1

Dan Zaslavsky and Don Kirkham2

ABSTRACT

The equation for the stream function for axially symmetric potential flow of groundwater is derived. The equation is illustrated by obtaining the streamlines for flow into an auger hole as used for hydraulic conductivity determination of soil.


NOTES

1 Journal Paper No. J-4293 of the Iowa Agr. and Home Econ. Exp. Sta., Ames. Project No. 998. Contribution from the Department of Agronomy. This paper was presented before Div. I, Soil Science Society of America, at Cincinnati, Ohio, Nov. 19, 1959.

2 Research Assistant and Professor of Agronomy (Soils) and Physics, respectively. The senior author is now on the Faculty of Civil Engineering, Israel Institute of Technology, Haifa, Israel.

Received for publication May 3, 1963. Accepted for publication September 5, 1963.







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