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作 者:翟兴涛[1] 张庆华[1] 张瑞她[1] 蒋磊[1]
机构地区:[1]山东农业大学水利土木工程学院,山东泰安271018
出 处:《武汉大学学报(工学版)》2013年第6期716-719,共4页Engineering Journal of Wuhan University
基 金:水利部公益性行业专项项目(编号:201201115);山东省重大水利科研与推广项目(2012)
摘 要:溢洪道水面线推求的起始断面一般选择在闸室末端,为此,需要确定该断面的水深,目前常用的做法是假定该断面的水深为临界水深.进行了宽顶堰与下游连接坡为垂直、1:1、1:5、1:10四种情况的水力学实验,实验结果表明宽顶堰与下游坡连接处的水深h均小于临界水深h。,h/h-值在0.7~0.95之间,其中0.76~0.90之间占76.18%,其规律为:下游坡相同情况下,单宽流量越大,h/ht越大;单宽流量相同情况下,下游坡越缓,h/hk越大.实验结果为溢洪道水面线推求确定起始断面水深提供了参考.The initial section that the water line of the spillway required is usually at the end of the cham- ber; hence we need to confirm the water depth of the section. Up to now, the most common way is to as- sume this depth as the critical depth. The research mainly carried out the broad-crest weir and down stream connection slope hydraulic experiment in four conditions: vertical, 1 : 1,1 : 5 ,1 : 10. The results indicate that the depth at the conjunction of the broad-crest weir and downstream connection slope are all less than the critical water depth hk; the values of h/hk are in 0. 7 to 0. 95; and 0.76 to 0.9 occupies 76.18~//00. Therefore, the conclusion is drawn as follows. If the downstream connection is same, the grea- ter the single-width flow is, the greater the h/hk is; if the single-width flow is same, the lower the down- stream connection slope is, the greater the h/hk is. The experimental results provide the deriving of the water line of the spillway with consultation.
分 类 号:TV132.22[水利工程—水力学及河流动力学]
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