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四川大学水力学及山区河流开发保护国家重点实验室、水利水电学院
纸质出版日期:2015,
网络出版日期:2014-11-30,
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夏叶.光滑陡坡泄槽上大颗粒泥沙运动特性试验研究[J].工程科学与技术,2015,47(Z2):.
xiaye. Experimental study on the movement characteristics of large particle sediment[J]. Advanced Engineering Sciences, 2015,47(Z2).
中文摘要: 基于室内不同粒径的大颗粒泥沙概化模型,通过不同影响因素的对比试验,采用摄像技术对大颗粒泥沙的跳跃轨迹进行记录,观察了大颗粒泥沙在陡槽上的运动情况。试验结果表明:当水深h超过临界水深hc时,大颗粒泥沙将不再跳跃,且随着粒径d的增加,临界水深hc逐渐变大,hc约等于d;通过分析卵石跳跃的特性,可知当粒径d与坡度J一定时,水深h与卵石的跃高Lh、跃长Ll呈负相关;当h
J一定时,d与Lh
Ll呈正相关;当h
d一定时, 随着J的增加,Lh变小,Ll增加;Lh
Ll与粒径的倍数关系k
m与h
d呈负相关。本试验结论将对泄水建筑物的防护设计提供一定的参考依据。
Abstract: The comparing experiment of different influence factors were conducted on the basis of the conceptual model test of various large particle sediment . Thus the movement of large particle sediment were investigated by using photography technology to record the skip trajectory. The results indicated that when the water depth exceeded the critical condition
the sediment will no longer jumping. What’ more
the critical depth increased with the increase of grain diameter
the critical depth approximately equal to the grain diameter. Meanwhile
according to the characteristics of jumping pebble
under a certain grain diameter and gradient
the depth had a negative power function relationship with the saltation height and length. Whereas
under the same depth and gradient
there was a positive power function relationship between jumping height
length and particle size. Besides
when the water depth and particle size are certain
with the increase of gradient
the jumping height decreased
and the jumping length increased. In addition
the jumping length and height had a multiple relations with the particle size and all showed a negative correlations with the water depth and the grain diameter. The experimental conclusions will provide certain reference frame to the design of outlet structures.
光滑陡坡卵石跳跃特性临界条件
smooth and steep slopepebblesaltation characteristicscritical condition
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