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| DOI | 10.1016/j.accre.2022.02.001 |
| In-situ measurement on air–water flux of CH4, CO2 and their carbon stable isotope in lakes of northeast Tibetan Plateau | |
| Wang L.; Xiao C.-D.; Du Z.-H.; Maher D.T.; Liu J.-F.; Wei Z.-Q. | |
| 发表日期 | 2022 |
| ISSN | 1674-9278 |
| 起始页码 | 279 |
| 结束页码 | 289 |
| 卷号 | 13期号:2 |
| 英文摘要 | Inland waters are important sources of greenhouse gases (GHGs) to the atmosphere that may partially offset the terrestrial carbon sink. However, GHG emissions from high altitude saline lakes on the Tibetan Plateau are currently poorly constrained. In this study, we measured methane (CH4) and carbon dioxide (CO2) concentrations and their carbon stable isotope (δ13C), and calculated diffusive water-to-air fluxes from two saline high-altitude lakes, Qinghai Lake and Hala Lake, located in northeast Tibetan Plateau in October 2020. The two lakes were mostly supersaturated in CH4 (89.8%–4623.9% sat) and acted as sources of CH4 to the atmosphere. Conversely, more than 96% investigated area of Qinghai Lake and all investigated area of Hala Lake was a sink of CO2. The average diffusive fluxes of CH4 and CO2 in the surface waters of Qinghai Lake were 34.51 μmol m−2 d−1 and −1.29 mmol m−2 d−1, while diffusive fluxes of CH4 and CO2 in Hala Lake averaged 5.48 μmol m−2 d−1 and −5.24 mmol m−2 d−1, respectively. Salinity (Sal), fluorescent dissolved organic matter (fDOM), temperature (Temp) and dissolved oxygen (DO) are key factors for diffusive CH4 and CO2 flux in Qinghai Lake and Hala Lake. CH4 diffusive fluxes across water–air interface from Qinghai Lake and Hala Lake were found to be significantly lower than other freshwater lakes, likely due to their saline nature. A simple isotope mixing model (Miller–Tans plots) revealed a distinctly different isotopic source values of CO2 and CH4 in Qinghai Lake and Hala Lake. The CH4 production pathway of Qinghai Lake was mainly by the acetate fermentation, while that of Hala Lake was mainly by the CO2 reduction. The results show that the continuous measurement can help capture the spatial variability of GHGs fluxes in saline lakes. © 2022 The Authors |
| 英文关键词 | Air–water flux; Carbon stable isotope; Greenhouse gas; Saline lakes; Tibetan Plateau |
| 语种 | 英语 |
| 来源期刊 | Advances in Climate Change Research
 |
| 来源机构 | 中国科学院西北生态环境资源研究院 |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/262081 |
| 作者单位 | State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing, 100875, China; State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China; Southern Cross Geoscience, Southern Cross University, Lismore, NSW 2480, Australia; College of Geography and Environmental Science, Northwest Normal University, Lanzhou, 730070, China; Zhuhai Branch of State Key Laboratory of Earth Surface Process and Resource Ecology, Beijing Normal University, Zhuhai, 519087, China |
| 推荐引用方式 GB/T 7714 | Wang L.； Xiao C.-D.； Du Z.-H.； Maher D.T.； Liu J.-F.； Wei Z.-Q.. In-situ measurement on air–water flux of CH4, CO2 and their carbon stable isotope in lakes of northeast Tibetan Plateau[J]. 中国科学院西北生态环境资源研究院,2022,13(2). |
| APA | Wang L.； Xiao C.-D.； Du Z.-H.； Maher D.T.； Liu J.-F.； Wei Z.-Q..(2022).In-situ measurement on air–water flux of CH4, CO2 and their carbon stable isotope in lakes of northeast Tibetan Plateau.Advances in Climate Change Research,13(2). |
| MLA | Wang L.； Xiao C.-D.； Du Z.-H.； Maher D.T.； Liu J.-F.； Wei Z.-Q.."In-situ measurement on air–water flux of CH4, CO2 and their carbon stable isotope in lakes of northeast Tibetan Plateau".Advances in Climate Change Research 13.2(2022). |
| 条目包含的文件 | 条目无相关文件。 | |||||
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