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黄骅地区潮间带滩涂沉积特征及其影响因素的初步分析
引用本文:孙廷智,武心尧.黄骅地区潮间带滩涂沉积特征及其影响因素的初步分析[J].海洋湖沼通报,1992(1):58-62.
作者姓名:孙廷智  武心尧
作者单位:国家海洋局北海分局,青岛海洋大学
摘    要:本文分析了黄骅潮间带的两次水准测量和地貌调查资料,结合样品作了粒度分析,得出本区潮滩的四个特征如下: 1.沉积类型简单,主要为粘土和粉砂,其含量为90%以上。 2.滩涂宽阔平坦,坡度极小,是典型的平原淤泥质海滩; 3.根据地貌和水动力特征,滩涂分为三部分:A.高潮滩的龟裂带;B.中潮滩的侵蚀滩面带;C.低潮滩的平整滩面带。 4.形成本区以上特征的控制因素有两个:一是黄河携带大量物质的影响;二是气候和潮汐波浪的作用。

关 键 词:潮间带  滩涂  沉积  黄骅地区

A PRELIMINARY ANALYSIS OF THE SEDIMENTARY CHARACTERISTICS AND THEIR INFLUENTIAL FACTORS IN THE TIDAL FLAT IN HUANGHUA COUNTY, HEBEI PROV.
Sun Tingzhi.A PRELIMINARY ANALYSIS OF THE SEDIMENTARY CHARACTERISTICS AND THEIR INFLUENTIAL FACTORS IN THE TIDAL FLAT IN HUANGHUA COUNTY, HEBEI PROV.[J].Transaction of Oceanology and Limnology,1992(1):58-62.
Authors:Sun Tingzhi
Abstract:The data, including two levelings and a geomorphic survey and sample sizing of the tidal flat in Huanghua County, was analysed in this paper. Four characteristics of the tidal flat in this area are found as follows: 1. Its sedimentary type is simple, mainly clay and silt, whose content is over 90%. 2. The flat is both broad and plain; its slope is very small, and the shore is a typically plain muddy coast. 3. According to its geomorphic and water dynamic characteristics, this flat is divided into three sections: A. the mud crack zone of high tidal flat; B. the washout zone of middle tidal flat; and C. the plain zone of low tidal flat. 4. The formation of these characteristics is controlled by two factors: the action by the Huanghe River and the action by climate, waves and tides.
Keywords:Huanghua area  tidal flat  flat sedimentation
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