Identification of the hydrogeochemical processes in groundwater using classic integrated geochemical methods and geostatistical techniques, in Amol-Babol Plain, Iran.

ScientificWorldJournal · 2014 · PMC3913491 · PMID 24523640

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a decreasing trendno p-value reported

In the plot of Na + /Cl − versus EC, the Na + /Cl − showed a decreasing trend with increasing EC along with a higher a Na + /Cl − ratio in class 1, which indicated that the Na + originated from the silicate weathering process ( Figure 5(d) ).

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