Stand age amplifies greenhouse gas and NO releases following conversion of rice paddy to tea plantations in subtropical China

被引:38
作者
Yao, Zhisheng [1 ,2 ]
Zheng, Xunhua [1 ,3 ]
Liu, Chunyan [1 ]
Wang, Rui [1 ]
Xie, Baohua [4 ]
Butterbach-Bahl, Klaus [2 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing 100029, Peoples R China
[2] Karlsruhe Inst Technol, Atmospher Environm Res, Inst Meteorol & Climate Res, D-82467 Garmisch Partenkirchen, Germany
[3] Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China
[4] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Key Lab Coastal Zone Environm Proc & Ecol Remedia, Yantai 264003, Peoples R China
关键词
Tea plantation; Land-use conversion; Greenhouse gas emissions; Nitric oxide; Emission factor; NITROUS-OXIDE EMISSIONS; DIRECT N2O EMISSIONS; LAND-USE CHANGE; NITRIC-OXIDE; FERTILIZER NITROGEN; MICROBIAL BIOMASS; SPLIT APPLICATION; GROWING-SEASON; SOIL; FIELDS;
D O I
10.1016/j.agrformet.2017.10.020
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Increasing demand of commercial markets for tea products is driving the conversion from rice paddies to tea plantations in subtropical China. So far, however, little is known on how this land-use change, along with the age of plantation establishment, will affect the fluxes of greenhouse gases (GHG) methane (CH4) and nitrous oxide (N2O) and the air-pollutant nitric oxide (NO). Thus, we measured CH4, N2O and NO fluxes over an entire year from two tea plantations (one- and five-year-old plantations) and a native rice-fallow system under two system specific nitrogen fertilizer options. On an annual scale, comparable or higher GHG emissions were measured for tea plantations as compared to the rice-fallow system. Besides the pollution swapping from CH4 being the dominating GHG in rice paddies to N2O in tea plantations, annual NO emissions increased significantly. Annual direct emission factors of N2O and NO in tea plantations were 2.47-5.80% and 2.00-3.99%, respectively, significantly higher than in the rice-fallow system (N2O: 1.05-2.05%; NO: 0.033-0.051%). Differences in N fertilizer inputs and soil environmental conditions (e.g., soil water regime, pH and organic carbon) due to contrasting managements of these systems and their interactions are clearly driving the stimulation of N2O and NO emissions and contributing to the significant CH4 reductions. Furthermore, we observed that increasing tea stand age, particularly under organic fertilization, further stimulated N2O and NO emissions that varied significantly intraannually. Nevertheless, the higher N2O and NO emissions of tea plantations and the increasing emission strength with stand age deserve further research attention and consideration for future land-use conversions.
引用
收藏
页码:386 / 396
页数:11
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