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Saturation index time series of the Barme Jamal spring water; a SIcal, SIdole and PCo2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{P}}_{{{\text{Co}}_{2} }}$$\end{document}, b Correlation between PCo2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{P}}_{{{\text{Co}}_{2} }}$$\end{document} and SIcal, c SIgyp and Q, d SIhal
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The Barme Jamal is an important karstic spring with mean discharge of 1.3 m3/s, located in the Meydavod county southwestern of Iran. Its outlet appeared in the Asmari limestone formation and drains the karstic limbs of Kuhe-Safid anticline. Naturally, the spring water salinity is more than expected for a karstic spring with EC about 2100 ms/cm. The...
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