检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:刘章君[1] 郭生练[1] 钟逸轩 郭海晋 李妍清 LIU Zhang-jun GUO Sheng-lian ZHONG Yi-xuan GUO Hai-jin LI Yan-qing(State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan 430072, China Bureau of Hydrology, Changjiang Water Resources Commission, Wuhan 430010, China)
机构地区:[1]武汉大学水资源与水电工程科学国家重点实验室,武汉430072 [2]长江水利委员会水文局,武汉430010
出 处:《中国农村水利水电》2016年第11期1-6,11,共7页China Rural Water and Hydropower
基 金:国家自然科学基金重点项目(51539009);国家重点研发技划重点专项(2016YFC0402206)
摘 要:水库建成以后,流域产汇流条件发生改变,采用入库洪水系列作为设计和调度依据更符合实际情况。介绍了入库洪水的概念及特点,综述了国内外入库设计洪水计算方法的研究进展,分析比较了各类方法的适用范围和适用条件。最后讨论了存在的主要问题,并展望了入库洪水研究的发展方向。The runoff generation and confluence conditions at intervener basin have been altered after the completion of reservoir. Consequently, it's more rational to take the inflow flood series as scientific base for reservoir design and operation. In this paper, the concept and characteristic of inflow flood are introduced firstly, and then the research advances of inflow flood estimation methods are reviewed. Scope and condition of application for different methods are also analyzed and compared. Finally, main problems existing in the present study are dis- cussed and research directions of inflow flood are suggested.
关 键 词:入库洪水 坝址洪水 流量叠加法 马斯京根法 槽蓄曲线法 水量平衡法
分 类 号:TV122[水利工程—水文学及水资源]
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:3.148.192.125