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淹水增加对闽江河口淡水潮汐湿地孔隙水地球化学特征及CO2和CH4排放通量的影响 被引量:8
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作者 李敬 黄佳芳 +5 位作者 罗敏 刘育秀 谭季 朱爱菊 王声钰 仝川 《环境科学》 EI CAS CSCD 北大核心 2019年第12期5493-5502,共10页
海平面上升使得河口潮汐湿地淹水高度增加,对CO2和CH4的排放通量产生重要影响,但目前绝大多数研究集中在淹水增加对河口盐沼湿地的影响,淹水增加对于河口淡水潮汐湿地的影响缺乏数据.鉴于此,本研究利用模拟潮汐池和中型生态系,研究淹水... 海平面上升使得河口潮汐湿地淹水高度增加,对CO2和CH4的排放通量产生重要影响,但目前绝大多数研究集中在淹水增加对河口盐沼湿地的影响,淹水增加对于河口淡水潮汐湿地的影响缺乏数据.鉴于此,本研究利用模拟潮汐池和中型生态系,研究淹水增加15 cm和30 cm后对闽江河口淡水潮汐湿地孔隙水(NH4+、NO3-、DOC、溶解性CH4和DIC)浓度及CO2和CH4排放通量的影响.结果表明,淹水高度增加15 cm和30 cm后,CO2的排放通量分别下降28. 53%和36. 56%;淹水增加15 cm时,CH4的排放通量没有显著变化,增加至30 cm后,CH4的排放通量显著增加29. 27%;淹水高度增加15 cm和30 cm,孔隙水CH4的浓度分别增加47. 83%和73. 91%.淹水增加对孔隙水DOC浓度变化影响不显著.淹水增加促进孔隙水NH4+浓度,并降低孔隙水DIC和NO3-的浓度.淹水增加降低CO2和CH4排放通量的温度敏感性.根据研究结果,未来海平面上升50 a和100 a后,闽江河口淡水潮汐湿地的综合增温潜势将分别降低28%和35%. 展开更多
关键词 淹水增加 CO2排放通量 ch4排放通量 海平面上升 淡水潮汐湿地 闽江河口
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Effects of elevated atmospheric CO_2 concentration and temperature on the soil profile methane distribution and diffusion in rice–wheat rotation system 被引量:5
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作者 Bo Yang Zhaozhi Chen +5 位作者 Man Zhang Heng Zhang Xuhui Zhang Genxing Pan Jianwen Zou Zhengqin Xiong 《Journal of Environmental Sciences》 SCIE EI CAS CSCD 2015年第6期62-71,共10页
The aim of this experiment was to determine the impacts of climate change on soil profile concentrations and diffusion effluxes of methane in a rice-wheat annual rotation ecosystem in Southeastern China. We initiated ... The aim of this experiment was to determine the impacts of climate change on soil profile concentrations and diffusion effluxes of methane in a rice-wheat annual rotation ecosystem in Southeastern China. We initiated a field experiment with four treatments:ambient conditions(CKs), CO2 concentration elevated to - 500 μmol/mol(FACE),temperature elevated by ca. 2°C(T) and combined elevation of CO2 concentration and temperature(FACE + T). A multilevel sampling probe was designed to collect the soil gas at four different depths, namely, 7 cm, 15 cm, 30 cm and 50 cm. Methane concentrations were higher during the rice season and decreased with depth, while lower during the wheat season and increased with depth. Compared to CK, mean methane concentration was increased by 42%, 57% and 71% under the FACE, FACE + T and T treatments, respectively, at the 7 cm depth during the rice season(p 〈 0.05). Mean methane diffusion effluxes to the 7 cm depth were positive in the rice season and negative in the wheat season, resulting in the paddy field being a source and weak sink, respectively. Moreover, mean methane diffusion effluxes in the rice season were 0.94, 1.19 and 1.42 mg C/(m^2·hr) in the FACE,FACE + T and T treatments, respectively, being clearly higher than that in the CK. The results indicated that elevated atmospheric CO2 concentration and temperature could significantly increase soil profile methane concentrations and their effluxes from a rice-wheat field annual rotation ecosystem(p 〈 0.05). 展开更多
关键词 Paddy field T-FACE Climate change ch4 concentration Soil profile Diffusion efflux
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