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Utilizing Soil Density Fractionation to Separate Distinct Soil Carbon Pools
Published on: December 16, 2022
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Persistent organic pollutants in global surface soils: Distributions and fractionations
Yi-Fan Li1,2,3,4, Shuai Hao1,2,3, Wan-Li Ma1,2,3
1International Joint Research Center for Persistent Toxic Substances (IJRC-PTS), State Key Laboratory of Urban Water Resource and Environment, Harbin Institute of Technology, Harbin, 150090, China.
Environmental Science and Ecotechnology
|September 15, 2023
Summary
Persistent organic pollutants (POPs) fractionate differently based on molecular weight, influencing their transport and accumulation in remote regions. Low molecular weight POPs travel farther, while high molecular weight POPs remain near their sources.
Area of Science:
- Environmental Chemistry
- Atmospheric Science
- Ecotoxicology
Background:
- Persistent organic pollutants (POPs) are chemicals that remain intact in the environment for long periods.
- Understanding POPs distribution and fractionation is crucial for assessing their transport to remote areas like the Arctic.
Purpose of the Study:
- To review progress in understanding POPs distribution and fractionation.
- To analyze intermedia processes governing POPs transfer between air and soil.
- To develop quantitative methods for studying POPs distribution and fractionation.
Main Methods:
- Review of existing literature on POPs distribution and fractionation.
- Analysis of four intermedia processes: dry and wet deposition of gaseous and particulate POPs.
- Development of equations for quantitative analysis of primary and secondary POPs distribution and fractionation.
- Use of a one-dimensional transport model to simulate POPs transport.
Main Results:
- POPs transfer from air to soil depends on molecular weight: low molecular weight (LMW) POPs via gas diffusion and particle deposition, high molecular weight (HMW) POPs mainly via particle deposition.
- HMW-POPs are typically trapped near the source, while LMW-POPs undergo long-range atmospheric transport.
- Primary fractionation is temperature-independent, while secondary fractionation occurs along temperature gradients.
Conclusions:
- Temperature gradients drive secondary POPs distribution and fractionation, not primary fractionation.
- Decreasing temperatures with latitude do not primarily cause POPs fractionation into polar ecosystems.
- Cold climates and polar regions facilitate longer-term POPs accumulation through processes like polar cold trapping.
Keywords:
POPsPrimary and secondary distribution patternsPrimary and secondary emissionsPrimary and secondary fractionationsPrimary and secondary sources
