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作 者:李兆喜 周丰[2] 缪驰远[3] 施坤[4] 高扬[1] LI Zhaoxi;ZHOU Feng;MIAO Chiyuan;SHI Kun;GAO Yang(Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences,Beijing 100101,China;Sino-French Institute for Earth System Science,College of Urban and Environmental Sciences,Peking University,Beijing 100871,China;State Key Laboratory of Earth Surface Processes and Resource Ecology,Beijing Normal University,Beijing 100875,China;State Key Laboratory of Lake Science and Environment,Nanjing Institute of Geography and Limnology,Chinese Academy of Sciences,Nanjing 210008,China)
机构地区:[1]中国科学院地理科学与资源研究所,北京100101 [2]北京大学城市与环境学院,北京100871 [3]北京师范大学地表过程与资源生态国家重点实验室,北京100875 [4]中国科学院南京地理与湖泊研究所,南京210008
出 处:《Journal of Resources and Ecology》2023年第3期675-680,共6页资源与生态学报(英文版)
基 金:The National Natural Science Foundation of China(41922003,41871080)。
摘 要:全球大气氮沉降急剧增加对内陆水生态系统产生不良影响。中国是全球三大氮沉降热点地区之一,为了充分了解氮沉降对中国内陆水体的影响,制定合理的水污染治理方案,需要清楚地量化内陆水体的氮沉降通量。为此,本文利用LMDZ-OR-INCA模型结合内陆水体面积数据,获得了近三十年中国内陆水体氮沉降数据集,为进一步了解中国内陆水体氮沉降的时空格局及其影响机制奠定了基础。同时,我们公开共享该数据集(https://ecodb.scidb.cn/detail?dataSetId=892431070195089408),并提供在线访问和下载服务。Dramatic increases in global atmospheric N deposition have had adverse effects on inland water ecosystems.China is one of the three hot spots of N deposition in the world.In order to fully understand the impact of N deposition on inland waters in China and formulate a reasonable water pollution treatment plan,we need to clearly quantify the N deposition flux in inland water.Therefore,using the LMDZ-OR-INCA model combined with inland water area data,we obtained the dataset of inland water N deposition in China from the 1990s to the 2010s,which lays a foundation for further understanding the spatial-temporal pattern of inland water N deposition and its impact mechanisms.At the same time,we publicly share this dataset and provide online access and download services at https://ecodb.scidb.cn/detail?dataSetId=892431070195089408.
关 键 词:氮沉降 内陆水体 水面积变化 全球气溶胶化学气候模型 中国
分 类 号:X52[环境科学与工程—环境工程]
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