M. S. McBride, H. O. Pfannkuch

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193 Scopus citations


The mutual exchange of water between lakes and contiguous permeable ground-water bodies, which are thin relative to the diameter of the lakes, was modeled digitally. A significant rate of seepage was found to extend only a relatively short distance from shore, thus forming a narrow band around the lake's perimeter. Field measurements of seepage rates through the bottom of Lake Sallie, west-central Minnesota, confirm the model results by demonstrating that both the near-shore seepage band and the exponential decrease in seepage velocity actually exist. Equations, diagrams, tables, and curves illustrate model.

Original languageEnglish (US)
Pages (from-to)505-512
Number of pages8
JournalJ Res US Geol Surv
Issue number5
StatePublished - Jan 1 1975

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