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EVOLUTION PRINCIPLE OF DEBRIS FLOW CONFLUENCE WITH MAIN RIVER

机译:碎片流动汇合与主要河流的演变原理

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In this paper, relative water depth, deposit volume, deposit ratio and deposit depth of debris flow at the confluence area were experimentally studied. Relative water depth, which was caused by the confluence of debris flow, was found to increases with the increasing of the discharge ratio and the confluence angle. As deposit principle of debris flow behind the confluence port was studied, deposit volume was found to increase with the increasing of lateral discharge when the confluence angle was 30°, 60° and 120° respectively. And it decreased with the increasing of discharge of debris flow at the angle of 90°. When the confluence angle was 30° and 120°, it got an uphill-sinusoid relationship between the deposit volume and discharge ratio. And it became a liner curve at 60°. Though the reason was different, the deposit volume of 60° and 120° were almost equal. When the confluence angle was 90°, it became a downhill-sinusoid relationship between the deposit volume and discharge ratio. And the deposit volume was the smallest at the angle. Meanwhile, deposit ratio decreased with the increasing of total discharge when the confluence angle was 30°, 60° and 120°, and increased at the angle of 90°. Deposit ratio changed with the discharge ratio as a parabola relationship at the angle of 30°, 60° and 120°. And it was a contrary parabola relationship at the angle of 90°. It got the maximum value when the discharge ratio was 0.5 at the confluence angle of 30°, 60° and 120°. And it got a minor value at the same discharge ratio when the confluence angle was 90°. Both average and maximum deposit depth got the maximum value when discharge ratio was 0.5. When debris flow entered Main River along downstream direction, the larger confluence angle, the larger maximum value of the deposit depth was. The maximum value of deposit depth, however, was the same at confluence angle of 120° and 30°.
机译:本文研究了汇合面积的相对水深,存款体积,沉积物比和沉积物流量的碎片流动。发现由碎屑流动汇合引起的相对水深,随着排出比和汇合角度的增加而增加。由于研究了汇合端口背后的碎片流量的存款原理,发现沉积体积随着汇率分别为30°,60°和120°时的横向放电而增加。并且随着碎片流动的越来越大,碎屑以90°的角度而降低。当汇合角度为30°和120°时,它在沉积体积和排出比之间获得了上坡正弦关系。它变成了60°的衬垫曲线。虽然原因不同,但沉积体积为60°和120°几乎相等。当汇合角度为90°时,它成为沉积体积和排出比之间的下坡正弦关系。沉积量为角度最小。同时,当汇合角度为30°,60°和120°时,沉积物比率随着总排出的增加而降低,并且以90°的角度增加。沉积物比例随排出比改变为30°,60°和120°角度的抛物线关系。它是一个相反的抛物线关系,以90°的角度。当排出比为0.5在30°,60°和120°时,它得到最大值。当汇合角度为90°时,它以相同的放电比率得到了次要值。当放电比例为0.5时,平均和最大沉积深度都得到了最大值。当碎片流入沿着下游方向进入主河的主河,汇率较大,沉积物深度的最大值较大。然而,沉积深度的最大值与120°和30°的汇合角度相同。

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