<p>Soil water content (WC) and microbial soil amendments (MSA) can influence methane (CH<sub>4</sub>) and carbon dioxide (CO<sub>2</sub>) emissions from carbon cycles in paddy fields. However, their individual and interactive effects remain to be elucidated. Thus, this study aimed to explore the individual and interactive effects of WC and MSA on CO<sub>2</sub> and CH<sub>4</sub> emissions and soil chemical properties. WC exerted a more pronounced influence on CH<sub>4</sub> and CO<sub>2</sub> emissions than MSA throughout the experimental period. In the first month, CO<sub>2</sub> emissions primarily contributed to partial global warming potential (pGWP). The cumulative CO<sub>2</sub> emissions under moist and flooded soil treatments were 332.29–353.42 and 240.3–273.17&#xa0;g·m<sup>− 2</sup>, respectively. The pGWP in the moist control group significantly increased by 22.61% compared with that in the flooded control group. In the second month, CH<sub>4</sub> emissions accounted for 34.75% and 63.01% of the total pGWP under flooded MSA and control treatments, respectively. Overall, the application of MSA promoted mineralization and nitrification during the aerobic phase of moist soils by stimulating organic matter-decomposing bacteria and nitrifiers, which consequently contributed to the reduction in CH<sub>4</sub> emissions. The experimental results indicate that extending the aerobic phase after MSA application is an effective strategy for reducing pGWP by mitigating CH<sub>4</sub> emissions. Field-scale evaluations are needed to clarify the long-term impacts of MSA on the atmospheric environment in paddy systems.</p>

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Effects of microbial soil amendments on global warming potential in paddy soils under different soil water contents

  • Liyuan Chen,
  • Kimihito Nakamura,
  • Natsuki Nobe,
  • Takanori Nagano

摘要

Soil water content (WC) and microbial soil amendments (MSA) can influence methane (CH4) and carbon dioxide (CO2) emissions from carbon cycles in paddy fields. However, their individual and interactive effects remain to be elucidated. Thus, this study aimed to explore the individual and interactive effects of WC and MSA on CO2 and CH4 emissions and soil chemical properties. WC exerted a more pronounced influence on CH4 and CO2 emissions than MSA throughout the experimental period. In the first month, CO2 emissions primarily contributed to partial global warming potential (pGWP). The cumulative CO2 emissions under moist and flooded soil treatments were 332.29–353.42 and 240.3–273.17 g·m− 2, respectively. The pGWP in the moist control group significantly increased by 22.61% compared with that in the flooded control group. In the second month, CH4 emissions accounted for 34.75% and 63.01% of the total pGWP under flooded MSA and control treatments, respectively. Overall, the application of MSA promoted mineralization and nitrification during the aerobic phase of moist soils by stimulating organic matter-decomposing bacteria and nitrifiers, which consequently contributed to the reduction in CH4 emissions. The experimental results indicate that extending the aerobic phase after MSA application is an effective strategy for reducing pGWP by mitigating CH4 emissions. Field-scale evaluations are needed to clarify the long-term impacts of MSA on the atmospheric environment in paddy systems.