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DEPOSITIONAL FEATURE AND PATTERN OF RIVER NETWORK IN THE PEARL RIVER DELTA

机译:珠江三角洲河北河网的沉积特征与模式

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This paper studies the hydraulic and depositional characteristics of the Pearl River delta and its channel patterns by using laws and methods of subjects such as estuaries , river dynamics, channel evolution, sedimentary dynamics, dynamical morphology, and so on. There are three dynamic area, flood area, flood-tidal area and tidal area. Sediment of the Pearl River delta comes from sea and fluvial. There are two kinds of river network patterns, tidal pattern and fluvial pattern in the delta of the Pearl River. These fluvial channels could be divided into three grades, and the tidal channels could be divided into two grades, every channels has different evolutional rules and exploitation values, but with the delta protruding seaward, the fluvial dynamic area moves to downstream, these channels suffer from the dynamical effects of tidal area flood-tidal area and flood area, and its developmental history is from formation to development, then die out.
机译:本文研究了珠江三角洲的液压和沉积特征及其通道模式,通过使用河口,河流动力学,渠道演化,沉积动力学,动态形态等主体的法律和方法。 有三个动感的区域,洪水区,洪水区和潮汐区。 珠江三角洲的沉积物来自海和河流。 珠江三角洲有两种河网模式,潮汐模式和河流模式。 这些河流通道可分为三个等级,并且潮汐通道可以分为两种等级,每个渠道都有不同的进化规则和开发价值,但随着潮汐突出的海,河流动态区域移动到下游,这些渠道遭受了 潮汐区洪水区和洪水区的动力学效应,其发展史从地层发展到发展,然后灭了出来。

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