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What is Brine Flow Modeling Near Konarsiah Diapir about?

The study investigates brine flow from the Konarsiah salt diapir in Iran into adjacent aquifers, revealing that halite dissolution is the primary source of salinity. Monthly measurements indicated significant salinity levels in springs and seepages, with proposed models for groundwater flow and potential remediation strategies to mitigate salinization. The findings emphasize the need for protective measures to preserve fresh groundwater resources in the region.

Author

alibivash1379

Language

EN