Conversion of winter flooded rice paddy planting to rice-wheat rotation decreased methane emissions during the rice-growing seasons

被引:18
|
作者
Xu, Peng [1 ,2 ]
Zhou, Wei [1 ,2 ]
Jiang, Mengdie [1 ,2 ]
Shaaban, Muhammad [3 ]
Zhou, Minghua [4 ]
Zhu, Bo [4 ]
Ren, Xiaojing [1 ]
Jiang, Yanbin [1 ,2 ]
Hu, Ronggui [1 ,2 ]
机构
[1] Huazhong Agr Univ, Minist Agr, Coll Resources & Environm, Key Lab Arable Land Conservat Middle & Lower Reac, Wuhan 430070, Peoples R China
[2] Huazhong Agr Univ, Ecol Environm Ctr, Wuhan 430070, Peoples R China
[3] Bahauddin Zakariya Univ, Fac Agr Sci & Technol, Dept Soil Sci, Multan, Pakistan
[4] Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China
来源
SOIL & TILLAGE RESEARCH | 2020年 / 198卷
关键词
Winter-flooded rice paddy; Rice-wheat rotation; CH4; emission; Soil temperature; Floodwater depth; Soil carbon and nitrogen; NITROUS-OXIDE EMISSIONS; GREENHOUSE-GAS EMISSIONS; CROPPING SYSTEM; ORGANIC-CARBON; WATER REGIME; N2O FLUXES; SOIL; TEMPERATURE; CH4; FIELDS;
D O I
10.1016/j.still.2019.104490
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
To our knowledge, the conversion of winter flooded rice paddy (RF) to rice-wheat rotation (RW) has markedly decreased methane (CH4) emissions during the wheat-growing seasons. However, the effects of this conversion on CH4 emissions during the rice-growing seasons are unclear. To determine CH4 emissions during the rice-growing season and associated environmental factors under RF and RW systems, a split-plot design experiment was conducted in three RF fields in hilly areas of Sichuan province, China. One-half of each field was converted to RW, and the other half remained RF. Each plot of RW and RF was further divided into four subplots: three subplots for conventional nitrogen fertilization treatment (RW-CN and RF-CN) and one for unfertilized treatment (RW-NN and RF-NN). The study showed that the cumulative CH4 emissions from RW-CN during the rice-growing seasons were 192.77 +/- 11.36 and 302.07 +/- 28.34 kg C ha(-1) in 2013 and 2014, respectively, which were decreased by 26.8% and 24.3% as compared to that from RF-CN. While for RW-NN, the cumulative CH4 emissions decreased by 54.1% and 24.0% as compared to that from RF-NN (372.49 +/- 67.05 and 300.53 +/- 13.49 kg C ha(-1) in 2013 and 2014, respectively, P < 0.05). A higher Q(10) (soil temperature sensitivity coefficient) of CH4 emissions during the whole experiment period was observed for RW-CN (6.69) than that for RF-CN (4.48). With rising soil temperature during the rice-growing seasons, the CH4 emissions for RW-CN escalated more rapidly than that for RF-CN. As expected, a positive correlation between CH4 fluxes and soil dissolved organic carbon (DOC) for both RF-CN and RW-CN was observed and DOC in RF-CN during the rice-growing seasons were higher than RW-CN. The soil dissolved inorganic nitrogen (DIN) was negatively correlated to CH4 emissions as the soil temperature ranged 22 degrees C-28 degrees C. Moreover, rice yields in the RF-CN and RW-CN treatments were similar in both years of 2013 and 2014. These findings suggested that CH4 emissions were primarily controlled by soil environment, which was affected by water and fertilizer managements. The implication of this study is that the decreased CH4 emissions and increased crop yields could be achieved by conversion management from RF to RW.
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页数:8
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