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March 14, 2026Journal of Salt Lake Research0 citations

Characteristics of Hydrogen and Oxygen Isotope Variations in Subsurface Brine

Study on the Characteristics of Hydrogen and Oxygen Isotope Variations in Subsurface Brine along the Northern Shore of Dabson Lake during the Water-Supplement Dissolution Process

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Authors

JSJiaxing SHUWMWeiliang MiaoXZXiying ZHANG

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Overview

Examines isotope variations in brine, suggesting insights into potassium mineral extraction efficiency.

Key Points

  • The goal is to explore the dynamic changes in hydrogen and oxygen isotopes in subsurface brine during the dissolution of potassium minerals.
  • Analyzed brine samples from water-supplement channels and observational wells at different depths.
  • Conducted hydrochemical and hydrogen-oxygen isotope analysis.
  • Studied the hydrological interactions during solid-liquid transitions in the brine.
  • Brine ion concentrations are influenced primarily by the dissolution and precipitation of halite, carnallite, and kieserite.
  • Hydrogen and oxygen isotope enrichment in brine is caused by evaporation and mineral dissolution after lake water supplementation.
  • The combined effects of brine mixing and mineral leaching are key factors affecting isotope changes.
  • Isotope ratio variations can indicate the potassium extraction efficiency during liquid extraction processes.
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Cite This Study

SHU et al. (2026) studied this question.

synapsesocial.com/papers/69b4fa9ab39f7826a300b424https://doi.org/10.3724/j.yhyj.2025062
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