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This is a Quantitative Study study.

Hydrogeochemical Runoff in the Central Kazakhstan and Its Role in the Development of Exogenous Processes

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This analysis reveals groundwater flow patterns and chemical flux in surface waters, highlighting its role in lithospheric processes.

Groundwater acts as the primary mechanism for matter redistribution in the Earth's crust, influencing geological processes.
The study quantifies chemical flux from groundwater and surface water, measuring the impact of atmospheric precipitation.
Four major inland water bodies were identified to assess hydrogeochemical runoff across 14 distinct areas.
In limited surface runoff regions, groundwater facilitates significant physicochemical interactions within the rock-water system.

Absametov et al. (2025) studied this question.

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