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Mechanisms Associated with Lower Methane Emissions from Paddy Soil by Aged Polylactic Acid Microplastics
Lili Wang1, Xiaonan Lu1, Yao Yao1
1Agro-Environmental Protection Institute, Ministry of Agriculture and Rural Affairs, Tianjin 300191, China.
Environmental Science & Technology
|December 12, 2025
Summary
Microplastics (MPs) in paddy soils affect methane emissions. Aging of polyethylene (PE) MPs mitigates methane, while aged polylactic acid (PLA) MPs enhance emissions, impacting greenhouse gas inventories.
Area of Science:
- Environmental Science
- Soil Science
- Biogeochemistry
Background:
- Microplastic (MP) contamination in paddy soils is a growing concern.
- MPs can influence methane (CH4) emissions, a potent greenhouse gas.
- Mechanisms underlying MP effects on CH4, especially aged MPs, are poorly understood.
Purpose of the Study:
- To investigate the impact of pristine and aged microplastics (polyethylene and polylactic acid) on CH4 emissions from paddy soils.
- To elucidate the mechanisms by which aged MPs influence CH4 production and oxidation.
- To quantify the role of MPs in the global carbon cycle and greenhouse gas emissions.
Main Methods:
- Microcosm experiment using paddy soil incubated with pristine and aged polyethylene (PE) and polylactic acid (PLA) MPs.
- Measurement of cumulative CH4 emissions over a 50-day incubation period.
- Analysis of microbial gene abundance related to methanogenesis and CH4 oxidation.
Main Results:
- Both pristine PE and PLA MPs inhibited CH4 emissions, with PLA being more effective.
- Aging increased the CH4 mitigation efficacy of PE but decreased that of PLA.
- Aged PE altered microbial gene abundance, reducing the methanogenesis to CH4 oxidation ratio.
- Aged PLA acted as an electron shuttle, competing for electrons and inhibiting methanogenesis.
Conclusions:
- Microplastic aging significantly influences CH4 emissions from paddy soils.
- Understanding these mechanisms is crucial for accurate greenhouse gas inventories and mitigation strategies.
- The study highlights the complex interactions between aged MPs, soil microbes, and carbon cycling.
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