{"id":"d576c0fa-ff3d-44bf-8102-d7eec8474000","title":"黄河源区径流分析简表（2014-2016）","title_en":"Runoff analysis of the source area of the Yellow River (2014-2016)","serial":"","user_limit":"为尊重知识产权、保障数据作者的权益、扩展数据中心的服务、评估数据的应用潜力，请数据使用者在使用数据所产生的研究成果中（包括公开发表的论文、论著、数据产品和未公开发表的研究报告、数据产品等成果），明确注明数据来源和数据作者。对于转载（二次或多次发布）的数据，作者还须注明原始数据来源。","instructions":"数据命名：黄河源区径流成分简表.xlsx。","description":"数据包含了黄河源区黄河干流和4条支流的径流成分资料。在2014-2016，春季，夏季和冬季，通过测试黄河源区几种冻土区河流水样的氡同位素和氚同位素含量，根据河道水流的质量守恒模型和同位素平衡模型，对河道流量进行径流成分解析，初步划分了地下水补给和地下冰融水在河川径流中的占比。模型计算得到的数据质量较好，相对误差在20%以内，通过了与以往实测数据的对比分析。该数据可为未来水文模型的参数率定及水文径流过程的模拟提供帮助。","doi":"10.1007/s10967-019-06720-5","projection":"","language":"zh","share_type":"online","east":99.0,"west":97.0,"south":34.0,"north":36.0,"scale":null,"crs":null,"filesize":1.0,"share_policy":"a","ts_created":"2020-06-12T07:57:12.358657+08:00","doi_type":"沿用数据已有DOI","ts_updated":"2021-04-19T10:47:31.938389+08:00","time_description":"","datas_group":3,"time_description_en":"","data_format":null,"project":[11],"specials":["f2a78cde-1c98-4241-94dc-7532eba32b80"],"cite":null,"review_status":5,"review_invite":[],"review_editor":null,"data_sources":null,"temporal_resolution":"Yearly","spatial_resolution":"-","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[],"subtopics":{"metadata":"d576c0fa-ff3d-44bf-8102-d7eec8474000","three_pole":null,"third_pole":"XDA20100103"},"username":"XDA20100103","review_time":"2020-06-14T11:55:18.739999+08:00","protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":2951}