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:邓斅学 叶爱中[1] 童洪福 徐静[1] 毛玉娜[1] 马凤[1]
机构地区:[1]北京师范大学全球变化与地球系统科学研究院全球变化协同创新中心,北京100875 [2]广东省水文局清远水文测报中心,广东清远511510
出 处:《中国农村水利水电》2015年第6期70-74,共5页China Rural Water and Hydropower
基 金:国家自然科学基金项目(41475093);中央高校基本科研业务费专项资金(2013YB32)
摘 要:获得河道流量常用的方法是实测流速乘以面积法和实测水位转换法。测流速精度高但成本高,而直接由水位估算流量经济但精度不够高。采用飞来峡水文站实测的流速与流量,对中泓一点法、水位流量法和水位-流速-流量拟合法3种方法进行了对比研究。发现在传统的水位流量关系中加入了一个点的流速后能够显著的提高流量的计算精度。基于现在流速仪技术的发展,可以在河道断面长期布置一单点流速仪,实时观测一点流速,所以采用水位-流速-流量法是未来获得高精度河道流量的可行方案。There are two methods that we used to obtain the river flow ,one is the flow velocity multiplied by the area ,the other one is getting river discharge by water level .If we want to get high precision flow velocity ,we must have high costs ,and estimating by water level is economical but the accuracy is not high enough .In this paper ,we compare three methods We have found that after the flow velocity is added into stage-discharge relation ,the accuracy of results is significantly improved .Now based on technology devel‐opment of current meter ,we can arrange a single-point current meter in river section for a long time to observe flow velocity in real-time .Therefore ,the water level-flow velocity-flow method is a feasible solution to get highly accurate river flows in the future .
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:3.138.189.0