The primary source of dissolved silica in groundwater is the chemical breakdown of silicate minerals/rocks by chemical weathering process. Therefore, high silica content in groundwater implies more intense water–rock interaction that in turn is related to the residence time of contact of subsurface water with the silicate rocks, permeability and lithology.

When dissolve silica content shows a negative correlation with TDS, then what it indicates?  - The majority of solute acquisition (TDS) would not have resulted from water–rock interaction?  - Means TDS are related to anthropogenic rather than geogenic. What is your opinion?

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