首页> 外文会议>International Symposium on River Sedimentation vol.3; 20041018-21; Yichang(CN) >SIMULATION EXPERIMENT OF ANASTOMOSING MULTIPLE CHANNEL FORMATION
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SIMULATION EXPERIMENT OF ANASTOMOSING MULTIPLE CHANNEL FORMATION

机译:多通道合成的模拟实验

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The anastomosing river is a fluvial river pattern that recently gets more and more attention from researchers. The hydrological, geomorphologic and sedimentological characteristics of some anastomosing rivers have been revealed. But the experiment simulation of anastomosing rivers is vacant hitherto. The flume simulation experiments are the reappearance of natural rivers under the condition of decreasing time and space. This work reports the formation and evolution of an anastomosing river simulated in the flume. The experimental beginning condition is: an artificial meandering channel in the assistant area of flume; a rectangle floodplain (4.5 m x 16.5 m) with concave cross sections is in the objective area and its stratum has a structure of double layers. The upper layer with a thickness of 1.5 cm consisted of Gaoling which median grain size is 0.013,2 mm; the under layer, consisted of fine sands which median grain size is 0.188 mm, has a thickness of 0.5 m. The mean longitudinal gradient of the floodplain is 0.005,8 from 5.5 m to 17 m and 0.007,7 from 17 m to 22 m along the ordinate. Adoptive constant discharge is 3 L · s~(-1). Suspended sediment discharge is 4.5 g · min~(-1) in the primary 3 h and 1.2 g · s~(-1) thereafter. The total time span of flume experiment is 50 h. In the initial stage of simulation sedimentation mainly occurred in the upper reach, random erosion occurred in the middle reach and the backward erosion mainly occurred in the lower reach of the objective area. A rudimental anastomosing river with multiple channels connected each other basically appears about 13.5 h. Hereafter, up to 25.5 h the evolution fashion of the anastomosing river changed from downcutting erosion to faint lateral erosion and the fall back of channel banks is not evident, it indicates that the anastomosing channels changes into its autumn. From 25.5 h to 50 h the abandonment or avulsion of an individual channel are the new evolution characteristics of the simulated anastomosing river. The whole flume experiment simulates successfully the formation and evolution of natural anastomosing rivers and proves that the anastomosing river is a new river pattern, which is different from anabranched river. This is a useful attempt to reveal the formation of anastomosing rivers via flume simulation and helpful to understand the characteristics of anastomosing rivers.
机译:吻合河是一条河流型河流,最近引起了研究人员的越来越多的关注。揭示了一些吻合河的水文,地貌和沉积特征。但是迄今为止,吻合河的实验模拟是空缺的。水槽模拟实验是在时间和空间减少的条件下天然河流的再现。这项工作报告了在水槽中模拟的一条吻合河的形成和演变。实验的起始条件是:在水槽的辅助区域内有一条人工曲折的通道。在目标区域中,一个矩形的洪泛区(4.5 m x 16.5 m)具有凹形横截面,其地层具有双层结构。上层厚度为1.5厘米,由高岭土组成,中位粒径为0.013,2毫米。底层由中值粒度为0.188 mm的细砂组成,厚度为0.5 m。洪泛区的平均纵向坡度沿纵坐标为5.5 m至17 m为0.005,8,17 m至22 m为0.007,7。过继恒定放电为3 L·s〜(-1)。最初3 h悬浮泥沙排放为4.5 g·min〜(-1),此后为1.2 g·s〜(-1)。水槽实验的总时间为50小时。在模拟的初期,沉积主要发生在上游,随机侵蚀发生在中游,后向腐蚀主要发生在目标区的下游。一条多通道相互连接的基本河道基本上出现了约13.5小时。此后,在长达25.5 h的时间内,吻合河的演化方式从下冲侵蚀变为微弱的侧向侵蚀,河道堤岸的回落不明显,这表明吻合河道一直向秋季过渡。从25.5小时到50小时,单个通道的放弃或破坏是模拟吻合河的新演变特征。整个水槽实验成功地模拟了自然吻合河的形成和演化,证明了吻合河是一条新的河流形态,不同于支流河。这是通过水槽模拟揭示吻合河的形成的有用尝试,有助于理解吻合河的特征。

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