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Planar velocity distribution of viscous debris flow at Jiangjia Ravine,Yunnan, China-A field measurement with two radar velocimeters

机译:云南省江家沟壑区粘性泥石流的平面速度分布-两个雷达测速仪的现场测量

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This paper presents measured data of planar velocity distribution of viscous debris flows at Jiangjia Ravine, Yunnan, China. The velocities along the ravine width were measured by using two radar velocimeters, and the cross-sectional mean velocities were then calculated. The velocity coefficient, K, defined by the ratio of the mean velocity to the maximum velocity, ranges from 0.2 to 0.6. The Kang et al. (2004) relationship, which was established for converting the flow velocity at river centerline measured by a radar velocimeter into the meanvelocity, was found to being inapplicable to flows with K smaller than 0.44.
机译:本文介绍了云南江家沟壑区粘性泥石流平面速度分布的实测数据。使用两个雷达测速仪测量沿沟谷宽度的速度,然后计算出横截面平均速度。由平均速度与最大速度之比定义的速度系数K介于0.2到0.6之间。康等。 (2004年)发现,这种关系不适用于将雷达测速仪测得的河流中心线流速转换为平均流速,但不适用于K小于0.44的流量。

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