涨潮流的流速和历时皆大于落潮流。
Both the velocity and duration of the flood are larger than those of the ebb.
涨潮流、向陆的密度流和混合是产生盐水入侵的动力因子。
The dynamic factors of saltwater intrusion are the tidal flood current, land - ward density current and mixing.
沉积环境可划分为河口主槽沉积环境、涨潮流沉积环境、浅滩沉积环境、拦门沙坝沉积环境及河口前缘沉积环境。
The dynamic sediment environment is divided into different areas that consist of estuarine deep trough, flood current, Jiaobeisha shoal, estuarine sandbar and seashore outside estuary.
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