静止液体作用在与其接触的某个平面或曲面上的总压力。
讨论了海底沙脊和沙波发育演变问题。
The development and evolution of sea bottom sand ridges and sand ripples are discussed.
沙波的形成是典型的简单巨系统自组织现象。
The formation of sand wave is a typical self organization phenomenon of simple giant systems.
水槽实验和海岸高空照片资料上清楚的分辨出这种由反射壁效应产生的沙波的客观存在性。
From flume experiments and aeroplane photographs of the coast, one can see the existence of sand wave induced by the reflection wall.
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