摘要
为深化洼地空间分布及其影响因素的认识,以云南石林县为例,在ArcGIS中基于DEM提取洼地分布及相关数据,并运用K函数(Ripley’s K)、核密度函数、缓冲区、空间叠加等分析方法,探讨了该区洼地密度分布特征及地理环境对其的影响。结果表明:研究区洼地在8 km尺度上为聚集分布模式,可划分为高密度(>6个·km^-2 )、中密度(5~6个·km^-2 )和低密度(<5个·km^-2 )三个区域。受多种地理环境因素影响,研究区洼地密度在不同海拔段、坡度、起伏度、地层岩石和断层缓冲区上均有差异性表现;同时,岩层节理、断层方向在一定程度上控制了洼地长轴的发育。研究区潜在水文连通性、面积—高程积分值两个指标与洼地密度呈现良好的一致性,但两个指标所反映的喀斯特洼地的地貌学意义还需进一步研究。
It is of significance to study the distribution and the factors of karst impact on the development of karst depression in the fields of geomorphology and environmental science. This paper takes Shilin county with abundant karst depressions as the study area, which is in subtropical monsoon climate zone, the south of the karst plateau in eastern Yunnan Province. The area is sandwiched between the Shizong-Mile fault and the west branch of Xiaojiang fault, and at the transition zone between the southeastern margin of Qinghai-Tibet plateau and the Beibuwan hilly plain.Based on digital elevation model(DEM), the methods of Ripley’s K function, nuclear density, buffer analysis, and spatial superposition in ArcGIS are used to analyze the distribution characteristics of the depressions and the influence of geographical environment on them. The results show that,(1) The distribution of karst depression in study area presents an aggregate pattern on a scale of 8 km, and the area can be divided into three sub-areas, namely high-density(>6·km-2), medium-density(5~6·km-2) and low-density(<5·km-2) areas. The high-density area has a total area of 308 km2, which is concentrated in two areas, namely Weihei, Muzhujing, Yusheng, Nuoyi in the east, and Hemo station and Shilin town in the northwest, with an average depression density of 7.20·km-2. The medium-density area is in the surroundings of the high-density area, including Yinai, Douhei, Southern Haiyi, and Northern Weize, with an average density of 5.74·km-2;and the low-density area is mainly at the edge of county, with an average density of 4.16·km-2. From the aspect of morphological parameters of the depression individuals, perimeter and area of them are high-density area < medium-density area < low-density area;depth and side slope are high-density area ≈ medium-density area > low-density area.(2) The spatial distribution of the depressions is controlled by the factors such as topography, geomorphology and geology. They have different quantity and density at differ
作者
丁智强
俞筱押
高璇
李玉辉
DING Zhiqiang;YU Xiaoya;GAO Xuan;LI Yuhui(School of Tourism and Geographical Sciences, Yunnan Normal University, Kunming, Yunnan 650500,China;School of Tourism and Resource Environment, Qiannan Normal University for Nationalities, Duyun, Guizhou 558000, China)
出处
《中国岩溶》
CAS
CSCD
北大核心
2019年第3期325-335,共11页
Carsologica Sinica
基金
国家自然科学基金项目(41262013,41371514)
关键词
喀斯特洼地
连通性
面积-高程积分值
地理信息系统
石林
karst depression
connectivity
hypsometric integral
geographic information system
Shilin country
