期刊文献+

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

Effect of Increasing Tidewater Inundation on Porewater Geochemistries and CO2 and CH4 Effluxes in the Tidal Freshwater Marshes of the Minjiang River Estuary,Southeast China
原文传递
导出
摘要 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%. While the effect of increasing tidewater inundation caused by sea-level rise on carbon cycling had been well studied in saltmarshes,little is known about the effect of increasing tidewater inundation on CO2 and CH4 effluxes in the tidal freshwater marsh soils.Herein,the effects of tide inundation on porewater geochemistries(NH+4,NO-3,DOC,dissolved CH4,and DIC)and CH4 and CO2 effluxes were examined in the soils of tidal freshwater marshes in the Minjiang River Estuary,East China Sea.By applying“mesocosm”and a simulated tide pool,the tide inundation height increased by 15 cm and 30 cm over the control(CK).The CO2 effluxes decreased by 28.53%and 36.56%,and the dissolved CH4 concentrations increased by 47.83%and 73.91%,in treatments(CK+15 cm)and(CK+30 cm),respectively.The CH4 effluxes did not change significantly in the treatment(CK+15 cm),but increased by 29.27%in treatment(CK+30 cm).The increasing tidewater inundation had no significant impact on DOC concentrations,but increased NH+4 concentrations and decreased DIC and NO-3 concentrations.Increasing tide inundation also reduced the temperature sensitivity of CH4 and CO2 effluxes.The study highlighted that the sea level rise-induced increase in tidewater inundation would decrease the annual global warming potential of tidal freshwater wetlands by 28%and 35%in the next 50 and 100 years,respectively.
作者 李敬 黄佳芳 罗敏 刘育秀 谭季 朱爱菊 王声钰 仝川 LI Jing;HUANG Jia-fang;LUO Min;LIU Yu-xiu;TAN Ji;ZHU Ai-ju;WANG Sheng-yu;TONG Chuan(Institute of Geography,Fujian Normal University,Fuzhou 350007,China;School of Geographical Sciences,Fujian Normal University,Fuzhou 350007,China;Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education,Fujian Normal University,Fuzhou 350007,China;Wetland Ecosystem Research Station of Minjiang Estuary,State Forestry and Grassland Administration,Fuzhou 350007,China)
出处 《环境科学》 EI CAS CSCD 北大核心 2019年第12期5493-5502,共10页 Environmental Science
基金 国家自然科学基金项目(41601102,41877335) 湿润亚热带生态-地理过程教育部重点实验室开放基金项目(2017KFJJ02) 中国科学院海岸带环境过程与生态修复重点实验室开放基金项目(2018KFJJ10) 福建省科技厅重点项目(2019J02008)
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 increased inundation CO2 efflux CH4 efflux sea-level rise freshwater tidal wetlands Minjiang River Estuary
  • 相关文献

参考文献11

二级参考文献189

共引文献224

同被引文献84

引证文献8

二级引证文献15

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部