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岩溶形态系统的分形特征及其机理探讨
引用本文:胡章喜,沈继方.岩溶形态系统的分形特征及其机理探讨[J].地球科学,1994,19(1):102-108.
作者姓名:胡章喜  沈继方
作者单位:上海市隧道工程设计院浦东分院 上海200127(胡章喜),中国地质大学水文系 武汉430074(沈继方)
基金项目:地质行业科学技术发展基金资助项目
摘    要:运用分形理论,系统研究了构成岩溶形态系统的岩溶地貌、水文网和洞穴系统的分形特征,并计算了分维值,以鄂西岩溶区的地貌小区为例,建立了地表峰体的分维与控制岩溶系统发育的岩性,外源水等因素的联系,揭示了分维的岩溶学含义,进而从岩溶系统介质场结构及岩溶作用过程的非线性动力特征分析探讨了岩溶形态系统的分形机理。

关 键 词:岩溶  形态系统  分维  分形机理

Study on Fractal Characteristics of Karst Morphology System and Its Mechanism
Hu Zhangxi.Study on Fractal Characteristics of Karst Morphology System and Its Mechanism[J].Earth Science-Journal of China University of Geosciences,1994,19(1):102-108.
Authors:Hu Zhangxi
Abstract:The fractal characteristics of the karst geomorphology, river networks and cave systems are sys-tematically studied for karst morphology system by using fractal geometry, and their fractal dimen-sions are calculated. With examples from several small areas in Western Hubei karst region, a connec-tion between the fractal dimensions of peak features and the control factors (lithology and allogenic water) is established, which discloses the karstological meaning of fractal dimensions. Furthermore, the fractal mechanism of karst system is discussed from the perspectives of medium field structure of karst system and nonlinear kinetic behaviour of harst process.
Keywords:karst morphology  fractal dimension  fractal mechanism    
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