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
机构地区:[1]清华大学
出 处:《水力发电学报》1997年第2期41-49,共9页Journal of Hydroelectric Engineering
基 金:国家自然科学基金
摘 要:一般在水流试验槽的末端设置量水堰,在河流中则设置水文站,用以率定恒定流的水位H和流量Q0之间的关系。但在非恒流下,这种关系形成绳套,必须另加变量起涨水位H′0,和水位H随时程t和流程x的偏导数Ht和Hx,即Q=Q(H′0,H,Ht,Hx),才能得出合理的关系。当今对非恒流挪用恒定流Q0=Q(H)的关系是不合理的。本项研究对非恒流通过矩形薄壁堰三种堰高P分别实验,各得出满意的拟合结果。并制定出了非恒流矩形簿壁堰的流量公式,用数值计算成果和实验资料校核验证了公式的正确性,以补充当今水力学手册之不足。本试验设备获清华大学实验技术成果三等奖。In order to find the relation between discharge Q and stage H of steady flow, it is necessary to establish a weir at end of the testing flume or hydrologic station in a section of the river. For unsteady flow, however, the steady H-Q curve is changed to the form of a rope sheath around it, in which discharge depends upon the starting raising stage H 0 and the partial differentials Ht,Hx, in addition to the recorded stage H, i.e., Q=Q(H 0,H,Ht, Hx). At present, employing the steady flow relation Q=Q(H) for unsteady condition is, of coures, fallacious. In the present research for unsteady flow, a rectangular sharp crested weir is used with three weir heights P separately, all with satisfactory results.
分 类 号:TV131.4[水利工程—水力学及河流动力学] TV133.2
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:216.73.216.28