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1988 | OriginalPaper | Chapter

Ionic Ratios as a Tool to Identify and Select Groundwater Resources

Author : B. Azmon

Published in: Contaminated Soil ’88

Publisher: Springer Netherlands

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Values or $$ r\frac{{Mg}}{{Ca}} $$ for water flowing through Dolomite and Limestone terrains are usually found in the range of 0.5–0.9. Indeed this ratio is found in the Karkara Springs, Pequi’in, Ziv, Hardalit and Na’aman.

Metadata
Title
Ionic Ratios as a Tool to Identify and Select Groundwater Resources
Author
B. Azmon
Copyright Year
1988
Publisher
Springer Netherlands
DOI
https://doi.org/10.1007/978-94-009-2807-7_43