首页> 外文会议>International conference on ocean, offshore and arctic engineering;OMAE2009 >EFFECT OF SPATIAL VARIATION OF A WAVE FIELD ON THE RESULTING RIPPLE CHARACTERISTICS AND COMPARISON TO PRESENT RIPPLE PREDICTORS
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EFFECT OF SPATIAL VARIATION OF A WAVE FIELD ON THE RESULTING RIPPLE CHARACTERISTICS AND COMPARISON TO PRESENT RIPPLE PREDICTORS

机译:波场的空间变化对产生的纹波特性的影响以及与当前纹波预测器的比较

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Laboratory experiments analyzed herein focus on the validity of ripple predictors under spatially variable wave envelopes. Present-day ripple predictors commonly derived from laboratory data (for smaller wave periods of about 1 to 4 s) within which only small regions of the facilities were used to observe and measure the sand ripple geometric characteristics of the nearly progressive waves measured overhead. When extended to large sediment test sections, our results show that the predictors are still valid along the tank under wave conditions which have significant wave envelope spatial variation (e.g., standing waves), provided that ripple predictors use the wave measurements directly above the respective locations within the computations. Results indicate that even under the case of mild reflection, noticeable variation in ripple characteristics can be seen along the sediment test section; thus, compels the necessity of measuring the wave field along the entire sediment section to achieve accurate results.
机译:本文分析的实验室实验侧重于在空间可变波包络下的波动预测器的有效性。当前的波纹预测因子通常是从实验室数据中得出的(对于大约1-4 s的较小波浪周期),在该数据中,仅使用设施的一小部分区域来观察和测量在顶部测量的近乎渐进的波浪的砂波纹几何特性。当扩展到较大的沉积物测试段时,我们的结果表明,在波纹状况具有明显的波包空间变化(例如驻波)的波浪条件下,预测器仍然有效,前提是波纹预测器直接在相应位置上方使用波浪测量值在计算中。结果表明,即使在轻微反射的情况下,在沉积物测试区也可以看到波纹特征的明显变化;因此,必须测量整个沉积物剖面的波场,以获得准确的结果。

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