Stable isotopes and chloride ion of precipitation events in the northeastern Tibetan Plateau, China  

作　　者：CUI Bu-li LI Dong-sheng JIANG Bao-fu WANG Ying WANG Ya-xuan WANG Long-sheng LI Xiao-yan 

机构地区：[1]State Key Laboratory of Earth Surface Processes and Resource Ecology,Beijing Normal University,Beijing 100875,China [2]School of Resources and Environmental Engineering,Ludong University,Yantai 264025,China [3]State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences,Xi’an 710061,China

出　　处：《Journal of Mountain Science》2021年第4期834-846,共13页山地科学学报（英文）

基　　金：supported by the National Natural Science Foundation of China (Grant Nos.41877157, 41730854);the State Key Laboratory of Loess and Quaternary Geology (SKLLQG1904);the Science and Technology Support Plan for Youth Innovation of Colleges and Universities of Shandong (2019KJH009);the Natural Science Foundation of Shandong Province (ZR2019MD040);the State Key Laboratory of Earth Surface Processes and Resource Ecology (2017-KF-15)。

摘　　要：Stable isotopes and chloride ion of precipitation are ideal environmental tracers to explain and reveal the formation and evolution mechanisms of water bodies. It is crucial to investigate the stable isotopes and chloride in precipitation events in the northeastern part of the Tibetan Plateau(NETP) due to the limitation of available data. This study sampled each event of precipitation during the period from July 2018 to June 2019 and the monthly dustfall in the NETP to investigate the temporal changes of stable isotopes and chloride in precipitation, and to reveal the moisture source of precipitation over the NETP using a back trajectory model. Results showed that the δ^(2)H values of precipitation ranged from-183.51‰ to 17.75‰, and the δ^(18)O values ranged from-25.18‰ to 0.48‰. The slope of the Local Meteoric Water Line was slightly lower than 8 due to the effect of belowcloud secondary evaporation on the precipitation process. Most d-excess values were higher than 10‰ because moisture recycled from the continent and Qinghai Lake surface mixed with precipitation. The chloride in precipitation accounted for 86.5% of the annual total deposition mass of chloride(1329.64 mg/m2), indicating that precipitation was the main source of chloride in the NETP. The temperature and amount effects of stable isotope in the precipitation were obvious in the NETP. The precipitation was predominantly derived from the Westerly Circulation from September through May and the East Asian Monsoon from June to August, with precipitation amounts of 246.5 mm and 178.0 mm, respectively, indicating that the precipitation over the NETP brought by the Westerly Circulation was more than that brought by the East Asian Monsoon. The air mass over the NETP transited in late May and early September, and a slight change in transition period would mainly be related to the intensity of the East Asian Monsoon, which is strongly influenced by El Ni?o-Southern Oscillation. These results provide not only baseline data for hydrological and clim

关 键 词：Stable isotope Chloride ion PRECIPITATION Moisture source Northeastern Tibetan Plateau 

分 类 号：P426.6[天文地球—大气科学及气象学]