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The effects of sediment characteristics and wave height on shape-parameter for representing equilibrium beach profiles

机译:沉积物特征和波高对代表平衡海滩剖面的形状参数的影响

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摘要

The shape parameter helps determining the shape of equilibrium beach profile in terms of offshore distance and water depth. The shape parameter therefore, should represent the effect of all the environmental factors involved in beach profile formation, such as wave climate and sediment properties. However, all the previous studies carried out to define shape parameter only consider the effects of sediment characteristics in their definitions. The aim of this study is to add the effect of wave climate also in the definition of shape parameter. This is achieved by integrating wave energy dissipation rate per unit volume at the surf zone. The result yields equilibrium wave energy dissipation rate that leads to theoretical definition of equilibrium beach profiles involving the effects of both the grain size and the wave climate parameters. It is found that the sediment grain size and the incoming wave height affect the value of shape parameter; whereas, the effects of wave period can be neglected. By means of energy equation, it is also possible to observe in macro scale the strength of wave energy on beach profile for different grain sizes. The findings also bring about the possibility of defining shape parameter such that any two arbitrary beach profiles owning the same sediment grain sizes can have the opportunity to have different beach profile formations. Finally, by adding the effect of wave height in the definition of shape parameter the graphical representation of the parameter, previously given by Moore (1982) is improved herein.
机译:形状参数有助于根据离岸距离和水深确定平衡海滩轮廓的形状。因此,形状参数应代表海滩轮廓形成所涉及的所有环境因素的影响,例如波浪气候和沉积物特性。但是,所有先前进行的定义形状参数的研究都只在定义中考虑了沉积物特征的影响。这项研究的目的是在形状参数的定义中增加波浪气候的影响。这是通过对冲浪区域每单位体积的波能量耗散率进行积分来实现的。结果产生了平衡波能量耗散率,从而导致了平衡滩形剖面的理论定义,其中包括了晶粒尺寸和波浪气候参数的影响。研究发现,沉积物粒径和入射波高会影响形状参数的值。而波浪周期的影响可以忽略不计。通过能量方程,还可以在宏观尺度上观察不同粒度的海滩剖面上波能的强度。这些发现还带来了定义形状参数的可能性,使得拥有相同沉积物粒径的任意两个任意海滩剖面都可以有不同的海滩剖面形成的机会。最后,通过在形状参数的定义中增加波高的影响,此处改进了由Moore(1982)先前给出的参数的图形表示。

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