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长江下荆江段分形学特征与河道演化
引用本文:罗郧,黄长生.长江下荆江段分形学特征与河道演化[J].现代地质,2011,25(4):808-812.
作者姓名:罗郧  黄长生
作者单位:1. 中国地质环境监测院,北京,100081
2. 中国地质调查局武汉地质调查中心,湖北武汉,443003
摘    要:采用盒数维法对长江下荆江各不同时期河道岸线的分形学特征进行探讨。研究表明,下荆江河道岸线的盒数维介于1.078~1.23之间,较黄河、海河、滦河等河流的维数要小,相当于黄河下游和长江下游平原区的维数,反映出下荆江河段是高成熟度的河段。这与长江中游地区的其他河段不相称,可能是由江汉—洞庭湖平原长期沉降所造成。河道裁弯之后,河道岸线由复杂变简单,分维数显著减少。裁弯取直事件发生在分维数值为1.19~1.23之间,即分维数可作为河道突变事件发生的一个预警参数。

关 键 词:河道  地貌演化  分形特征  早期预警  长江  下荆江段

Fractal Characteristics and Watercourse Evolution of the Lower Jingjiang Segment in Middle Yangtze River
LUO Yun,HUANG Chang-sheng.Fractal Characteristics and Watercourse Evolution of the Lower Jingjiang Segment in Middle Yangtze River[J].Geoscience——Journal of Graduate School,China University of Geosciences,2011,25(4):808-812.
Authors:LUO Yun  HUANG Chang-sheng
Institution:LUO Yun1,HUANG Chang-sheng2 (1.China Institute for Geo-Environmental Monitoring,Beijing 100081,China,2.Wuhan Center of Geological Survey,China Geological Survey,Wuhan,Hubei 443003,China)
Abstract:The fractal characteristics were discussed according to the fractal analysis of segments in lower Jingjiang River in this paper.The parameter of dimensions are changing between 1.078 to 1.23 and are lower than those of Yellow River,Haihe River and Luanhe River and close to those of plain areas in lower Yellow reaches and upper Yangtze reaches.The result indicates the evolution of segment is mature period,which is disproportional to other segments of this catchment.This is maybe controlled by its geological ...
Keywords:watercourse  geomorphologic evolution  fractal characteristic  early warning parameter  Yangtze River  lower Jingjiang segment  
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