不同海岸地貌背景下的南海周边岸带35年建设用地扩张分析

doi:10.11821/dlxb201601008

Abstract

Abstract:

Data of coastal construction land around the South China Sea in 2010 and 1975 were extracted and the spatial-temporal characteristics of construction land expansion based on different geomorphologic backgrounds in this period was discussed. Results showed that: (1) In South China Mainland and Malay Peninsula, construction land in coastal zone was generally expanded rapidly; in Indochina, construction land in coastal zone was expanded moderately; in Sumatra, Kalimantan and Philippines, construction land in coastal zone was expanded slowly except Manila Bay. (2) There were significant differences in construction land expansion between different geomorphology types because of natural resources, development difficulty and hinterland area. As there were good conditions of water transport and wide hinterland, construction land in delta plain coast and estuary plain coast expanded rapidly; construction land expansion in mesa coast and barrier - lagoon coast was remarkable due to the suitability for building small or medium-sized ports; construction land expansion in gulf coast and mountain coast was relatively slow because there existed limited development potential; construction land expansion in flat dike coast was even slower because of the limited hinterland and underdeveloped water transport. (3) Development patterns varied according to coastal geomorphologic features. The spatial morphology of construction land was diverse in delta plain coast and estuary plain coast; in mountain coast, mesa coast and gulf plain coast, it presented agglomerating or zonal distribution; in barrier - lagoon coast, it presented agglomerating or star distribution; in flat dyke coast, it presented zonal, linear or point distribution.

Key words: South China Sea, coastal zone, coastal geomorphology, construction land, spatial-temporal expansion

ZHANG Junjue,SU Fenzhen,ZHOU Chenghu,ZUO Xiuling,DING Zhi,LI Haochuan. Construction land expansion in coastal zone around the South China Sea based on different geomorphologic backgrounds in the past 35 years[J].Acta Geographica Sinica, 2016, 71(1): 104-117.

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海岸类型	空间形态	空间分布	典型岸段
山地岸	团块状或条带状	山麓下的港湾或山间谷地	铁炉嶂岸段;红河北部高地岸段
台地岸	团块状或条带状	台地溺谷或岬湾	丁加奴高地东侧沿海岸段;柔佛南岸岸段
三角洲平原	空间形态多样化,核心区呈团块状,其它呈放射条带状/网状小斑块,分布密集而均匀;还有沿堤岸而建,纵横阡陌式的线状分布	广布,核心区位于河口或河曲	昭披耶河三角洲岸段;红河三角洲岸段;湄公河三角洲岸段
河口平原	与三角洲平原类似	河口/河曲或沿河流,海岸线而建	清化--河静平原岸段
海湾平原	团块状或条带状	湾头或湾口	豆蔻山脉北丘岸段
沙坝--潟湖平原	团块状;星状	潟湖口	汕头--汕尾岸段
平直沙堤平原	条带状分布;线状分布;点状分布	沿交通干线或沿海岸线	普吉山沿海岸带

Construction land expansion in coastal zone around the South China Sea based on different geomorphologic backgrounds in the past 35 years

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