International Institute for Earth System Sciences, Nanjing University, Nanjing 210023, China; Institute of Scientific and Technical Information, Chinese Academy of Tropical Agricultural Sciences, Haikou 571101, China.
International Institute for Earth System Sciences, Nanjing University, Nanjing 210023, China.
Sci Total Environ. 2019 Nov 10;690:973-990. doi: 10.1016/j.scitotenv.2019.07.012. Epub 2019 Jul 4.
The paddy rice fields act as an important anthropogenic source of methane (CH) to the atmosphere. The study of pattern, magnitude, and environmental controls of CH emissions are still insufficient due to limited measurements and understand of underlying drivers for variations of CH fluxes at different temporal scales. In this study, CH fluxes from a rice-wheat rotation agroecosystem in eastern China were continuously measured using the eddy covariance technique. The diurnal and seasonal variations of CH flux and potential controlling factors in 2016 were analyzed using wavelet coherence, conditional Granger causality, correlation analysis and path analysis methods. CH fluxes showed distinguishable diurnal variations with single peaks during 13: 00-16: 00 local time. At the diurnal timescale, gross primary productivity (GPP) regulates CH fluxes after accounting for the effects of latent heat flux (LE), air temperature (TA), and soil temperature (TS) on CH fluxes. LE mirrored the diurnal pattern of CH fluxes when the effects of TA and TS on CH fluxes were considered. Daily CH fluxes exhibited large seasonal variations, with the largest daily CH flux of 1191.78 mg C-CH m d on 29 July 2016. The daily CH fluxes were continuously low in the growing season of wheat, and sharply increased from very low values in late June to peaks in late July and early August, and then gradually decreased to low values at the end of the rice growing season in late November and early December. Correlation analysis and path analysis showed that seasonal variations of soil temperature, air temperature, and GPP had strong effects on daily CH fluxes during pre-panicle initiation of the rice growing season, while soil temperature and leaf area index (LAI) had very strong effects on daily CH fluxes during the post-panicle initiation stage. The total of CH fluxes from the rice-wheat rotation agroecosystem into the atmosphere amounted to 58.08 ± 9.87 g C m in 2016, and the annual net carbon (C) budget and greenhouse gas (GHG) budget were 163.50 ± 9.87 g C m and 2322.53 ± 329.00 g COeq m, respectively. This study represents a comprehensive assessment of fluxes and drivers of CH from a rice-wheat rotation agroecosystem at different timescales. Additionally, the consecutive data of CH emission in this region will also useful for model calibration and validation.
稻田是大气中甲烷(CH)的一个重要人为排放源。由于在不同时间尺度上对 CH 通量变化的潜在驱动因素的了解有限,限制了对 CH 排放的模式、幅度和环境控制的研究。本研究采用涡度相关技术连续测量了中国东部稻麦轮作农业生态系统的 CH 通量。利用小波相干、条件格兰杰因果关系、相关分析和路径分析方法,分析了 2016 年 CH 通量的日变化和季节变化及其潜在控制因素。CH 通量具有明显的日变化特征,在当地时间 13:00-16:00 出现单峰。在日时间尺度上,总初级生产力(GPP)在考虑潜热通量(LE)、空气温度(TA)和土壤温度(TS)对 CH 通量的影响后,调节 CH 通量。当考虑 TA 和 TS 对 CH 通量的影响时,LE 反映了 CH 通量的日变化模式。日 CH 通量表现出较大的季节变化,2016 年 7 月 29 日最大日 CH 通量为 1191.78mgC-CH-m-d。小麦生长季,日 CH 通量持续较低,6 月下旬至 7 月下旬、8 月上旬急剧增加,11 月下旬至 12 月初水稻生长季末期逐渐降低至低值。相关分析和路径分析表明,在水稻生长前期,土壤温度、空气温度和 GPP 的季节变化对每日 CH 通量有较强的影响,而在后期,土壤温度和叶面积指数(LAI)对每日 CH 通量有很强的影响。2016 年,稻麦轮作农业生态系统向大气中排放的 CH 总量为 58.08±9.87gC-m,其中年净碳(C)收支和温室气体(GHG)收支分别为 163.50±9.87gC-m和 2322.53±329.00gCOeq-m。本研究综合评估了不同时间尺度上稻麦轮作农业生态系统 CH 的通量和驱动因素。此外,该地区连续的 CH 排放数据也将有助于模型校准和验证。