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作 者:Chong Liu Liping Zhu Junbo Wang Jianting Ju Qingfeng Ma Baojin Qiao Yong Wang Teng Xu Hao Chen Qiangqiang Kou Run Zhang Jinlei Kai 刘翀;朱立平;王君波;鞠建廷;马庆峰;乔宝晋;汪勇;许腾;陈浩;寇强强;张润;开金磊(Key Laboratory of Tibetan Environment Changes and Land Surface Processes,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China;Center for Excellence in Tibetan Plateau Earth System,Chinese Academy of Sciences,Beijing 100101,China;University of Chinese Academy of Sciences,Beijing 100049,China;School of Geosciences and Technology,Zhengzhou University,Zhengzhou 450001,China;School of Geography and Tourism,Anhui Normal University,Wuhu 241000,China.)
机构地区:[1]Key Laboratory of Tibetan Environment Changes and Land Surface Processes,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China [2]Center for Excellence in Tibetan Plateau Earth System,Chinese Academy of Sciences,Beijing 100101,China [3]University of Chinese Academy of Sciences,Beijing 100049,China [4]School of Geosciences and Technology,Zhengzhou University,Zhengzhou 450001,China [5]School of Geography and Tourism,Anhui Normal University,Wuhu 241000,China.
出 处:《Science Bulletin》2021年第17期1727-1730,M0003,共5页科学通报(英文版)
基 金:This work was supported by the Strategic Priority Research Program of Chinese Academy of Sciences(XDA19020303);the National Natural Science Foundation of China(41831177);the Second Tibetan Plateau Scientific Expedition and Research(2019QZKK0202);the Alliance of Field Observation Stations of Chinese Academy of Sciences(KFJ-SW-YW038).
摘 要:The lakes on the Tibetan Plateau(TP)account for 57%of the total lake area in China[1],which is a key component of the Asia water tower[2-4].A recent study showed that there are 1424 lakes greater than 1 km^(2) on the TP,while the total lake area reached 5.0-10^(4)±791.4 km^(2) in 2018[5].Most lakes on the TP are closed and are less disturbed by human activities than the other inland water bodies in China.青藏高原广泛分布的湖泊是"亚洲水塔"的重要组成部分.对该地区湖泊水质的调查与研究,是区域水环境与水资源评估以及气候和环境变化研究的重要基础. 20世纪80年代之前的第一次青藏高原综合科学考察之后,对该地区大范围湖泊水质调查十分匮乏.本研究基于2009~2020年期间野外调查工作,共采集获取涉及124个封闭湖泊的实测水质参数.调查与研究表明,青藏高原湖泊盐度变化很大,大多数湖泊表现出碱性状态,富营养化程度低,叶绿素a和溶解有机物浓度低、浊度低、透明度高.分析显示部分湖泊水质参数随空间、季节、面积变化而发生较大变化.本研究揭示了青藏高原湖泊水质近期基本状态与规律,为区域生态、水文、资源、环境与气候变化等研究提供了基础数据.
关 键 词:水质参数 湖泊水质 区域水环境 溶解有机物 富营养化程度 综合科学考察 盐度变化 野外调查工作
分 类 号:X832[环境科学与工程—环境工程]
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