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Jia H, Fei X, Zhu J, Chen W, Chen R, Liao Z, Zhou B, Huang Y, Du H, Xu P, Zhang X, Li W. Soil respiration and its response to climate change and anthropogenic factors in a karst plateau wetland, southwest China. Sci Rep 2024; 14:8653. [PMID: 38622331 PMCID: PMC11018823 DOI: 10.1038/s41598-024-59495-5] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/09/2024] [Accepted: 04/11/2024] [Indexed: 04/17/2024] Open
Abstract
It is important to investigate the responses of greenhouse gases to climate change (temperature, precipitation) and anthropogenic factors in plateau wetland. Based on the DNDC model, we used meteorological, soil, and land cover data to simulate the soil CO2 emission pattern and its responses to climate change and anthropogenic factors in Guizhou, China. The results showed that the mean soil CO2 emission flux in the Caohai Karst Plateau Wetland was 5.89 ± 0.17 t·C·ha-1·yr-1 from 2000 to 2019, and the annual variation showed an increasing trend with the rate of 23.02 kg·C·ha-1·yr-1. The soil total annual mean CO2 emissions were 70.62 ± 2.04 Gg·C·yr-1 (annual growth rate was 0.28 Gg·C·yr-1). Caohai wetland has great spatial heterogeneity. The emissions around Caohai Lake were high (the areas with high, middle, and low values accounted for 3.07%, 70.96%, and 25.97%, respectively), and the emission pattern was characterized by a decrease in radiation from Caohai Lake to the periphery. In addition, the cropland and forest areas exhibited high intensities (7.21 ± 0.15 t·C·ha-1·yr-1 and 6.73 ± 0.58 t·C·ha-1·yr-1, respectively) and high total emissions (54.97 ± 1.16 Gg·C·yr-1 and 10.24 ± 0.88 Gg·C·yr-1, respectively). Croplands and forests were the major land cover types controlling soil CO2 emissions in the Caohai wetland, while anthropogenic factors (cultivation) significantly increased soil CO2 emissions. Results showed that the soil CO2 emissions were positively correlated with temperature and precipitation; and the temperature change had a greater impact on soil respiration than the change in precipitation. Our results indicated that future climate change (increased temperature and precipitation) may promote an increase in soil CO2 emissions in karst plateau wetlands, and reasonable control measures (e.g. returning cropland to lakes and reducing anthropogenic factors) are the keys to controlling CO2 emissions.
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Affiliation(s)
- Hongyu Jia
- College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, Guizhou University, 2708 Huaxi Avenue, Guiyang, 550025, Guizhou, China
- Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, Guizhou, China
- Guizhou Provincial Double Carbon and Renewable Energy Technology Innovation Research Institute, Guiyang, 550025, Guizhou, China
| | - Xuehai Fei
- College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, Guizhou University, 2708 Huaxi Avenue, Guiyang, 550025, Guizhou, China.
- Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, Guizhou, China.
- Guizhou Provincial Double Carbon and Renewable Energy Technology Innovation Research Institute, Guiyang, 550025, Guizhou, China.
- Guizhou Caohai Observation and Research Station for Wet Ecosystem, National Forestry and Grassland Administration, Weining, 553100, Guizhou, China.
| | - Jingyu Zhu
- College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, Guizhou University, 2708 Huaxi Avenue, Guiyang, 550025, Guizhou, China
- Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, Guizhou, China
- Guizhou Provincial Double Carbon and Renewable Energy Technology Innovation Research Institute, Guiyang, 550025, Guizhou, China
| | - Weiduo Chen
- College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, Guizhou University, 2708 Huaxi Avenue, Guiyang, 550025, Guizhou, China
- Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, Guizhou, China
- Guizhou Provincial Double Carbon and Renewable Energy Technology Innovation Research Institute, Guiyang, 550025, Guizhou, China
| | - Rui Chen
- College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, Guizhou University, 2708 Huaxi Avenue, Guiyang, 550025, Guizhou, China
- Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, Guizhou, China
- Guizhou Provincial Double Carbon and Renewable Energy Technology Innovation Research Institute, Guiyang, 550025, Guizhou, China
| | - Zhangze Liao
- College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, Guizhou University, 2708 Huaxi Avenue, Guiyang, 550025, Guizhou, China
- Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, Guizhou, China
- Guizhou Provincial Double Carbon and Renewable Energy Technology Innovation Research Institute, Guiyang, 550025, Guizhou, China
| | - Binghuang Zhou
- College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, Guizhou University, 2708 Huaxi Avenue, Guiyang, 550025, Guizhou, China
- Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, Guizhou, China
- Guizhou Provincial Double Carbon and Renewable Energy Technology Innovation Research Institute, Guiyang, 550025, Guizhou, China
| | - Yingqian Huang
- College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, Guizhou University, 2708 Huaxi Avenue, Guiyang, 550025, Guizhou, China
- Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, Guizhou, China
- Guizhou Provincial Double Carbon and Renewable Energy Technology Innovation Research Institute, Guiyang, 550025, Guizhou, China
| | - Haiqiang Du
- College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, Guizhou University, 2708 Huaxi Avenue, Guiyang, 550025, Guizhou, China
- Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, Guizhou, China
- Guizhou Provincial Double Carbon and Renewable Energy Technology Innovation Research Institute, Guiyang, 550025, Guizhou, China
| | - Peng Xu
- College of Resources and Environmental Engineering, Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, Guizhou University, 2708 Huaxi Avenue, Guiyang, 550025, Guizhou, China
- Guizhou Karst Environmental Ecosystems Observation and Research Station, Ministry of Education, Guiyang, 550025, Guizhou, China
- Guizhou Provincial Double Carbon and Renewable Energy Technology Innovation Research Institute, Guiyang, 550025, Guizhou, China
| | - Xu Zhang
- Guizhou Caohai Observation and Research Station for Wet Ecosystem, National Forestry and Grassland Administration, Weining, 553100, Guizhou, China
| | - Wangjun Li
- Guizhou Province Key Laboratory of Ecological Protection and Restoration of Typical Plateau Wetlands (Guizhou University of Engineering Science), Bijie, 55170, Guizhou, China
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Ma Y, Li C, Guo L, Lu W, Cheng Y, Han X, Li J, Crawshaw D, He M, Shan L, Lee D, da Silva I, Manuel P, Ramirez-Cuesta AJ, Schröder M, Yang S. Exceptional capture of methane at low pressure by an iron-based metal-organic framework. Chemistry 2024; 30:e202303934. [PMID: 38102961 DOI: 10.1002/chem.202303934] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/13/2023] [Accepted: 12/14/2023] [Indexed: 12/17/2023]
Abstract
The selective capture of methane (CH4) at low concentrations and its separation from N2 are extremely challenging owing to the weak host-guest interactions between CH4 molecules and any sorbent material. Here, we report the exceptional adsorption of CH4 at low pressure and the efficient separation of CH4/N2 by MFM-300(Fe). MFM-300(Fe) shows a very high uptake for CH4 of 0.85 mmol g-1 at 1 mbar and 298 K and a record CH4/N2 selectivity of 45 for porous solids, representing a new benchmark for CH4 capture and CH4/N2 separation. The excellent separation of CH4/N2 by MFM-300(Fe) has been confirmed by dynamic breakthrough experiments. In situ neutron powder diffraction, and solid-state nuclear magnetic resonance and diffuse reflectance infrared Fourier transform spectroscopies, coupled with modelling, reveal a unique and strong binding of CH4 molecules involving Fe-OH⋯CH4 and C⋯phenyl ring interactions within the pores of MFM-300(Fe), thus promoting the exceptional adsorption of CH4 at low pressure.
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Affiliation(s)
- Yujie Ma
- Department of Chemistry, University of Manchester, Manchester, M13 9PL, UK
| | - Cheng Li
- Neutron Scattering Division, Oak Ridge National Laboratory, Oak Ridge, TN, 37831, USA
| | - Lixia Guo
- Department of Chemistry, University of Manchester, Manchester, M13 9PL, UK
| | - Wanpeng Lu
- Department of Chemistry, University of Manchester, Manchester, M13 9PL, UK
| | - Yongqiang Cheng
- Neutron Scattering Division, Oak Ridge National Laboratory, Oak Ridge, TN, 37831, USA
| | - Xue Han
- College of Chemistry, Beijing Normal University, Beijing, 100875, China
| | - Jiangnan Li
- Department of Chemistry, University of Manchester, Manchester, M13 9PL, UK
| | - Danielle Crawshaw
- Department of Chemistry, University of Manchester, Manchester, M13 9PL, UK
| | - Meng He
- Department of Chemistry, University of Manchester, Manchester, M13 9PL, UK
| | - Lutong Shan
- Department of Chemistry, University of Manchester, Manchester, M13 9PL, UK
| | - Daniel Lee
- Department of Chemical Engineering, University of Manchester, Manchester, M13 9PL, UK
| | - Ivan da Silva
- ISIS Facility, Science and Technology Facilities Council, Rutherford Appleton Laboratory, Chilton, OX11 0QX, UK
| | - Pascal Manuel
- ISIS Facility, Science and Technology Facilities Council, Rutherford Appleton Laboratory, Chilton, OX11 0QX, UK
| | | | - Martin Schröder
- Department of Chemistry, University of Manchester, Manchester, M13 9PL, UK
| | - Sihai Yang
- Department of Chemistry, University of Manchester, Manchester, M13 9PL, UK
- Beijing National Laboratory for Molecular Sciences, College of Chemistry and Molecular Engineering, Peking University, Beijing, 100871, China
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Sobanaa M, Prathiviraj R, Selvin J, Prathaban M. A comprehensive review on methane's dual role: effects in climate change and potential as a carbon-neutral energy source. ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH INTERNATIONAL 2024; 31:10379-10394. [PMID: 37884720 DOI: 10.1007/s11356-023-30601-w] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/03/2022] [Accepted: 10/18/2023] [Indexed: 10/28/2023]
Abstract
The unprecedented population and anthropogenic activity rise have challenged the future look up for shifts in global temperature and climate patterns. Anthropogenic activities such as land fillings, building dams, wetlands converting to lands, combustion of biomass, deforestation, mining, and the gas and coal industries have directly or indirectly increased catastrophic methane (CH4) emissions at an alarming rate. Methane is 25 times more potent trapping heat when compared to carbon dioxide (CO2) in the atmosphere. A rise in atmospheric methane, on a 20-year time scale, has an impact of 80 times greater than that of CO2. With increased population growth, waste generation is rising and is predicted to reach 6 Mt by 2025. CH4 emitted from landfills is a significant source that accounts for 40% of overall global methane emissions. Various mitigation and emissions reduction strategies could significantly reduce the global CH4 burden at a cost comparable to the parallel and necessary CO2 reduction measures, reversing the CH4 burden to pathways that achieve the goals of the Paris Agreement. CH4 mitigation directly benefits climate change, has collateral impacts on the economy, human health, and agriculture, and considerably supports CO2 mitigation. Utilizing the CO2 from the environment, methanogens produce methane and lower their carbon footprint. NGOs and the general public should act on time to overcome atmospheric methane emissions by utilizing the raw source for producing carbon-neutral fuel. However, more research potential is required for green energy production and to consider investigating the untapped potential of methanogens for dependable energy generation.
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Affiliation(s)
- Murugesan Sobanaa
- Department of Microbiology, Pondicherry University, Puducherry, 605014, India
| | | | - Joseph Selvin
- Department of Microbiology, Pondicherry University, Puducherry, 605014, India
| | - Munisamy Prathaban
- Department of Microbiology, Pondicherry University, Puducherry, 605014, India.
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Feron S, Malhotra A, Bansal S, Fluet-Chouinard E, McNicol G, Knox SH, Delwiche KB, Cordero RR, Ouyang Z, Zhang Z, Poulter B, Jackson RB. Recent increases in annual, seasonal, and extreme methane fluxes driven by changes in climate and vegetation in boreal and temperate wetland ecosystems. GLOBAL CHANGE BIOLOGY 2024; 30:e17131. [PMID: 38273508 DOI: 10.1111/gcb.17131] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/23/2023] [Revised: 11/15/2023] [Accepted: 12/15/2023] [Indexed: 01/27/2024]
Abstract
Climate warming is expected to increase global methane (CH4 ) emissions from wetland ecosystems. Although in situ eddy covariance (EC) measurements at ecosystem scales can potentially detect CH4 flux changes, most EC systems have only a few years of data collected, so temporal trends in CH4 remain uncertain. Here, we use established drivers to hindcast changes in CH4 fluxes (FCH4 ) since the early 1980s. We trained a machine learning (ML) model on CH4 flux measurements from 22 [methane-producing sites] in wetland, upland, and lake sites of the FLUXNET-CH4 database with at least two full years of measurements across temperate and boreal biomes. The gradient boosting decision tree ML model then hindcasted daily FCH4 over 1981-2018 using meteorological reanalysis data. We found that, mainly driven by rising temperature, half of the sites (n = 11) showed significant increases in annual, seasonal, and extreme FCH4 , with increases in FCH4 of ca. 10% or higher found in the fall from 1981-1989 to 2010-2018. The annual trends were driven by increases during summer and fall, particularly at high-CH4 -emitting fen sites dominated by aerenchymatous plants. We also found that the distribution of days of extremely high FCH4 (defined according to the 95th percentile of the daily FCH4 values over a reference period) have become more frequent during the last four decades and currently account for 10-40% of the total seasonal fluxes. The share of extreme FCH4 days in the total seasonal fluxes was greatest in winter for boreal/taiga sites and in spring for temperate sites, which highlights the increasing importance of the non-growing seasons in annual budgets. Our results shed light on the effects of climate warming on wetlands, which appears to be extending the CH4 emission seasons and boosting extreme emissions.
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Affiliation(s)
- Sarah Feron
- Knowledge Infrastructures, Campus Fryslân, University of Groningen, Groningen, The Netherlands
- Department of Earth System Science, Stanford University, Stanford, California, USA
- Department of Physics, Universidad de Santiago, Santiago, Chile
| | - Avni Malhotra
- Biological Sciences Division, Pacific Northwest National Laboratory, Richland, Washington, USA
| | - Sheel Bansal
- U.S. Geological Survey, Northern Prairie Wildlife Research Center, Jamestown, North Dakota, USA
| | - Etienne Fluet-Chouinard
- Earth Systems Science Division, Pacific Northwest National Laboratory, Richland, Washington, USA
| | - Gavin McNicol
- Department of Earth System Science, Stanford University, Stanford, California, USA
- Department of Earth and Environmental Sciences, University of Illinois Chicago, Chicago, Illinois, USA
| | - Sara H Knox
- Department of Geography, The University of British Columbia, Vancouver, British Columbia, Canada
- Department of Geography, McGill University, Montreal, Quebec, Canada
| | - Kyle B Delwiche
- Department of Earth System Science, Stanford University, Stanford, California, USA
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, California, USA
| | - Raul R Cordero
- Department of Physics, Universidad de Santiago, Santiago, Chile
| | - Zutao Ouyang
- Department of Earth System Science, Stanford University, Stanford, California, USA
| | - Zhen Zhang
- Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
| | - Benjamin Poulter
- Biospheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
| | - Robert B Jackson
- Department of Earth System Science, Stanford University, Stanford, California, USA
- Woods Institute for the Environment, Stanford University, Stanford, California, USA
- Precourt Institute for Energy, Stanford, California, USA
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Nisbet EG. Slaying the methane minotaur. Proc Natl Acad Sci U S A 2023; 120:e2318019120. [PMID: 38011579 PMCID: PMC10710036 DOI: 10.1073/pnas.2318019120] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2023] Open
Affiliation(s)
- Euan G. Nisbet
- Department of Earth Sciences, Royal Holloway, University of London, EghamTW20 0EX, United Kingdom
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Haghnegahdar MA, Sun J, Hultquist N, Hamovit ND, Kitchen N, Eiler J, Ono S, Yarwood SA, Kaufman AJ, Dickerson RR, Bouyon A, Magen C, Farquhar J. Tracing sources of atmospheric methane using clumped isotopes. Proc Natl Acad Sci U S A 2023; 120:e2305574120. [PMID: 37956282 PMCID: PMC10666091 DOI: 10.1073/pnas.2305574120] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/06/2023] [Accepted: 10/05/2023] [Indexed: 11/15/2023] Open
Abstract
We apply a recently developed measurement technique for methane (CH4) isotopologues* (isotopic variants of CH4-13CH4, 12CH3D, 13CH3D, and 12CH2D2) to identify contributions to the atmospheric burden from fossil fuel and microbial sources. The aim of this study is to constrain factors that ultimately control the concentration of this potent greenhouse gas on global, regional, and local levels. While predictions of atmospheric methane isotopologues have been modeled, we present direct measurements that point to a different atmospheric methane composition and to a microbial flux with less clumping (greater deficits relative to stochastic) in both 13CH3D and 12CH2D2 than had been previously assigned. These differences make atmospheric isotopologue data sufficiently sensitive to variations in microbial to fossil fuel fluxes to distinguish between emissions scenarios such as those generated by different versions of EDGAR (the Emissions Database for Global Atmospheric Research), even when existing constraints on the atmospheric CH4 concentration profile as well as traditional isotopes are kept constant.
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Affiliation(s)
- Mojhgan A. Haghnegahdar
- Department of Geology, University of Maryland, College Park, MD20742
- Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD20742
- Smithsonian Environmental Research Center, Edgewater, MD21037
| | - Jiayang Sun
- Department of Geology, University of Maryland, College Park, MD20742
| | - Nicole Hultquist
- Department of Geology, University of Maryland, College Park, MD20742
| | - Nora D. Hamovit
- Department of Environmental Science and Technology, University of Maryland, College Park, MD20742
| | - Nami Kitchen
- Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA91125
| | - John Eiler
- Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA91125
| | - Shuhei Ono
- Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA02139
| | - Stephanie A. Yarwood
- Department of Environmental Science and Technology, University of Maryland, College Park, MD20742
| | - Alan J. Kaufman
- Department of Geology, University of Maryland, College Park, MD20742
- Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD20742
| | - Russell R. Dickerson
- Department of Oceanic and Atmospheric Science, University of Maryland, College Park, MD20742
| | - Amaury Bouyon
- Department of Geology, University of Maryland, College Park, MD20742
| | - Cédric Magen
- Department of Geology, University of Maryland, College Park, MD20742
| | - James Farquhar
- Department of Geology, University of Maryland, College Park, MD20742
- Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD20742
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Wang J, Ciais P, Smith P, Yan X, Kuzyakov Y, Liu S, Li T, Zou J. The role of rice cultivation in changes in atmospheric methane concentration and the Global Methane Pledge. GLOBAL CHANGE BIOLOGY 2023; 29:2776-2789. [PMID: 36752684 DOI: 10.1111/gcb.16631] [Citation(s) in RCA: 5] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/12/2022] [Accepted: 02/03/2023] [Indexed: 05/31/2023]
Abstract
Resumption of the increase in atmospheric methane (CH4 ) concentrations since 2007 is of global concern and may partly have resulted from emissions from rice cultivation. Estimates of CH4 emissions from rice fields and abatement potential are essential to assess the contribution of improved rice management in achieving the targets of the Global Methane Pledge agreed upon by over 100 countries at COP26. However, the contribution of CH4 emissions from rice fields to the resumed CH4 growth and the global abatement potential remains unclear. In this study, we estimated the global CH4 emissions from rice fields to be 27 ± 6 Tg CH4 year-1 in the recent decade (2008-2017) based on the 2019 Refinement to the 2006 IPCC Guidelines for National Greenhouse Gas Inventories. The trend of CH4 emissions from rice cultivation showed an increase followed by no significant change and then, a stabilization over 1990-2020. Consequently, the contribution of CH4 emissions from rice fields to the renewed increase in atmospheric CH4 concentrations since 2007 was minor. We summarized the existing low-cost measures and showed that improved water and straw management could reduce one-third of global CH4 emissions from rice fields. Straw returned as biochar could reduce CH4 emissions by 12 Tg CH4 year-1 , equivalent to 10% of the total reduction of all anthropogenic emissions. We conclude that other sectors than rice cultivation must have contributed to the renewed increase in atmospheric CH4 concentrations, and that optimizing multiple mitigation measures in rice fields could contribute significantly to the abatement goal outlined in the Global Methane Pledge.
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Affiliation(s)
- Jinyang Wang
- Key Laboratory of Green and Low-carbon Agriculture in Southeastern China, Ministry of Agriculture and Rural Affairs, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing, China
- Jiangsu Key Laboratory of Low Carbon Agriculture and GHGs Mitigation, Jiangsu Collaborative Innovation Center for Solid Organic Waste Resource Utilization, Nanjing, China
| | - Philippe Ciais
- Laboratoire des Sciences du Climat et de l'Environnement (LSCE), Institut Pierre Simon Laplace, CEA/CNRS/Université de Versailles Saint-Quentin-en-Yvelines/Université de Paris Saclay, Gif-sur-Yvette, France
| | - Pete Smith
- Institute of Biological and Environmental Sciences, University of Aberdeen, Aberdeen, UK
| | - Xiaoyuan Yan
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China
| | - Yakov Kuzyakov
- Department of Soil Science of Temperate Ecosystems, University of Gottingen, Gottingen, Germany
- Peoples Friendship University of Russia (RUDN University), Moscow, Russia
| | - Shuwei Liu
- Key Laboratory of Green and Low-carbon Agriculture in Southeastern China, Ministry of Agriculture and Rural Affairs, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing, China
- Jiangsu Key Laboratory of Low Carbon Agriculture and GHGs Mitigation, Jiangsu Collaborative Innovation Center for Solid Organic Waste Resource Utilization, Nanjing, China
| | - Tingting Li
- LAPC, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
| | - Jianwen Zou
- Key Laboratory of Green and Low-carbon Agriculture in Southeastern China, Ministry of Agriculture and Rural Affairs, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing, China
- Jiangsu Key Laboratory of Low Carbon Agriculture and GHGs Mitigation, Jiangsu Collaborative Innovation Center for Solid Organic Waste Resource Utilization, Nanjing, China
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8
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Nisbet EG. The urgent need to cut methane emissions. Natl Sci Rev 2021; 9:nwab221. [PMID: 35547956 PMCID: PMC9084352 DOI: 10.1093/nsr/nwab221] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/30/2021] [Accepted: 12/02/2021] [Indexed: 11/29/2022] Open
Affiliation(s)
- Euan G Nisbet
- Department of Earth Sciences, Royal Holloway University of London, UK
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