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Observation of Concurrent Latitudinal and Longitudinal Fractionations of α- and β-HCH in Chinese Rural Surface Soil: Implications for Global Lifecycle

  • Shuai Hao*
  • , Yi Fan Li*
  • , Wan Li Ma
  • , Li Yan Liu
  • , Zi Feng Zhang
  • , Wen Long Li
  • , Ning Zheng Zhu
  • , Pu Fei Yang
  • , Hong Liang Jia
  • , Min Gang Cai
  • , Roland Kallenborn
  • , Derek C.G. Muir
  • *Corresponding author for this work
  • Harbin Institute of Technology
  • HPKL-PEE)
  • Heilongjiang University of Science and Technology
  • IJRC-PTS-NA
  • Xiamen University
  • Tongji University
  • Norwegian University of Life Sciences
  • University of Guelph

Research output: Contribution to journalArticlepeer-review

Abstract

In this study, for the first time, the distribution and fractionation of persistent organic pollutants (POPs) along both latitudinal and longitudinal transects are investigated simultaneously in surface soil. Distributions and fractionations of two isomers of hexachlorocyclohexane (HCH), α- and β-HCH, were analyzed in Chinese rural surface soil using a set of soil samples collected in 2005, 2012, and 2019 to study the lifecycle of the global/latitudinal fractionation of POPs. The primary longitudinal and secondary latitudinal distributions for each of α- and β-HCH and the primary longitudinal and secondary latitudinal fractionations formed together by these two isomers were observed concurrently in these three years. Based on these observations, we identified three stages for the lifecycle of global/latitudinal fractionation for α- and β-HCH. In Stage I, the primary fractionation of the two isomers mainly due to the distance from the source regions begins and intensifies with the fractionation pattern of the enrichment of the compounds having lower KOA (octanol-air partition ratio) values and the depletion of the compounds with higher KOA values. In Stage II, the secondary fractionation caused mainly by the air temperature gradient along latitudinal directions begins and intensifies, keeping the fractionation patterns appearing in the Stage I unchanging. In Stage III, the secondary fractionation is weakened primarily caused by local factors, degradation in particular, until its disappearance. The fractionation patterns appearing in the Stages I and II may change. Although the present study on the three stages for the development of latitudinal fractionation is for α- and β-HCH in Chinese surface soil. We believe that the findings presented in this study can provide instructive implications for the lifecycle of all polar cold-trapped persistent organic pollutants (PCT‑POPs) on a global scale.

Original languageEnglish
Article number28
JournalArchives of Environmental Contamination and Toxicology
Volume90
Issue number4
DOIs
StatePublished - May 2026

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