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
Included in: Professional Book Archive
Activate our intelligent search to find suitable subject content or patents.
Select sections of text to find matching patents with Artificial Intelligence. powered by
Select sections of text to find additional relevant content using AI-assisted search. powered by
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.