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分别于1986年12月和1985年3月1日—1987年3月1日在海州湾进行了波浪和含沙量观测，运用所获资料以及本区长期水文、地形资料，采用流体力学、沉积学和泥沙运动力学相结合的研究方法，建立了海州湾淤泥质海滩剖面堆积过程的二维计算模式。结果表明，在堆积型淤泥质海滩，由于浮泥的经常性存在，使波浪急剧衰减，其对岸滩的作用甚为微弱，潮流成为塑造淤泥质海滩的主要动力，岸滩在淤涨过程中，在平均高潮位厂沿和平均低潮位附近出现两个凸点，上一个凸点外推速率大于下一个凸点，潮下带变化缓慢。
Waves and sediment concentrations were observed in Haizhou Bay in December 1986 and March 1, 1985 - March 1, 1987 respectively. Using the data obtained and long-term hydrological and topographical data of the area, hydrodynamics, Sedimentology and sediment transport mechanics, a two-dimensional calculation model of the deposition process of the silt beach in Haizhou Bay was established. The results show that on the accumulation type of silt beach, the wave declines sharply due to the regularity of the floating mud, its effect on the shore beach is very weak, and the tidal current becomes the main driving force for shaping the muddy beach. During the silting up of the beach, Two bumps appear along the average orgasm and the average low tide, and the extrapolation rate of the previous bump is greater than that of the next bump. The subtidal band changes slowly.