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作 者:黄奕龙[1] 王仰麟[1] 刘珍环[1] 曾祥坤[1] 陈朗
机构地区:[1]北京大学深圳研究生院,深圳518055 [2]深圳市水利规划设计院,深圳518036
出 处:《地理研究》2008年第5期1212-1220,共9页Geographical Research
基 金:国家自然科学基金重点项目(40635028);中国博士后科学基金资助项目(2005037282)
摘 要:为了探讨城市化对水系结构的影响,应用深圳市1982、2002年的二期水系详查图,定量分析了水系长度、密度、分枝比、分枝能力和分维数等参数的变化特征。结果表明:快速城市化过程中,深圳市的河道总长度减少、密度减小,河道数目减少,特别是低级别的支流减少较多;河道的分枝比和分枝能力都有不同程度的弱化,单个水系片区和全市的河流分维数都下降,河流具有简单化的趋势,河流的多元化特征削弱;对于不同水系片区来说,其变化速度不同,表明城市化过程对水系结构的干扰存在空间差异性。建议强力推进河流的蓝线规划和滨水区的开发管理,将水网的保护和规划纳入到城市规划的管理范围;注重在开发利用中的保护,减少各类新建城市用地、农用地整理过程中对水系的破坏;加大水土保持力度,减少因水土流失导致河流淤塞;加强管理,严禁向河道中倾倒垃圾。Urban River is an important part of urban ecosystem. There are close relation- ship between stream construction and its ecological function. The form and evolution of stream construction is controlled by geology, topography, soil, climate, vegetation and human activity at local area. At present, human activity, especially urbanization has be- come the major factor influencing the stream structure. In order to study the effect of ur- banization on stream construction, taking Shenzhen city, a rapid urbanization area as a case, which is one of the most rapid urbanization areas in China, by using Strahler classifi- cation and Horton laws, this paper analyzed the effect of urbanization on stream length, stream density, bifurcation ratio of rivers, ability of bifurcation of rivers and fractal di- mension etc. The result exhibited that. (1) The stream length, stream density and stream number all decreased, especially for the lower order stream from 1982 to 2002. and (2) the ratio and ability of bifurcation decreased of all the watersheds. The stream construc- tion was simplified with time. The fractal dimension of stream construction also decreased with time. (3) The stream construction changing characteristic was different for different watersheds due to the effect of urbanization level. This paper suggested. (1) to improve planning and implement blue-line, strengthen the management of river net and add it to the content of urban planning and managing; (2) to protect the stream in the process of land use change; and (3) to strengthen the control of soil and water erosion, thus decrease the yield of river sediments.
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