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September 5, 2026Journal of Environmental Engineering and Science

Dissolved inorganic carbon in Chongqing urban section of Yangtze River, China

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Authors

QWQingzheng WuYQYu QinZLZhen Liu

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Overview

Observational study reveals hydrological regulation and thermal stratification drive dissolved inorganic carbon dynamics in urban river waters, highlighting reservoir impacts on inland carbon cycling.

Key Points

  • To investigate the sources, distribution, and influencing factors of dissolved inorganic carbon in an urban river reservoir during distinct hydrological periods.
  • Monitored dissolved inorganic carbon (DIC) concentrations and stable carbon isotopes (δ13C-DIC) during low-water and reservoir impoundment periods.
  • Applied carbon stable isotope tracing and a mass balance model to quantify DIC sources and evaluate the influence of thermal stratification and water chemistry.
  • Demonstrated that DIC dominates the aquatic carbon pool, primarily originating from soil carbon dioxide inputs and carbonate weathering.
  • Observed that summer δ13C-DIC correlated negatively with temperature and pCO2 (p < 0.001) and positively with pH and total particulate matter (p < 0.05), alongside a strong negative relationship between DIC concentration and δ13C-DIC in autumn.

Cite This Study

Wu et al. (2026) studied this question.

synapsesocial.com/papers/6a9bd3f16b95aff0620eb216https://doi.org/10.1680/jenes.25.00147
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