广西师范大学学报(自然科学版) ›› 2012, Vol. 30 ›› Issue (4): 166-171.

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基于GIS的漓江流域水文特征空间分析

苏文静1, 卢远2, 蔡德所3,4,5   

  1. 1.广西林业科学研究院,广西南宁 530001;
    2.广西师范学院资源与环境科学学院,广西南宁 530023;
    3.三峡大学水利与环境学院,湖北宜昌 443002;
    4.广西水利电力勘测设计研究院,广西南宁 530023;
    5.广西大学土木建筑工程学院,广西南宁 530004
  • 收稿日期:2012-08-01 发布日期:2018-11-27
  • 通讯作者: 通信联系人:卢远(1971—),男,广西横县人,广西师范学院教授,博士。E-mail:luyuangx@yahoo.com.cn
  • 基金资助:
    国家自然科学基金资助项目(40971280,30870345);中央分成水资源费资助项目(2010-2011);广西水利电力勘测设计研究院重点科技项目基金资助项目(20100013)

Spatial Analysis of Hydrological Characteristics for Lijiang River Basin Based on GIS

SU Wen-jing1, LU Yuan2, CAI De-suo3,4,5   

  1. 1.Guangxi Forestry Research Institute,Nanning Guangxi 530001,China;
    2.School of Resources and Environmental Science,Guangxi Teachers Education University,Nanning Guangxi 530023,China;
    3.College of Hydraulic and Environment Engineering,China Three Gorges University,Yichang Hubei 443002,China;
    4.Guangxi Water and Power Design Institute,Nanning Guangxi 530023,China;
    5.College of Civil Engineering and Architecture,Guangxi University,Nanning Guangxi 530004,China
  • Received:2012-08-01 Published:2018-11-27

摘要: 流域水文特征的提取与分析不仅为水文过程模拟提供重要参数,而且是流域水生态系统健康监测与评价的基础依据。本文基于30 m空间分辨率DEM提取漓江流域水系、确定流域范围、划分子流域,并计算流域内河流长度、河网密度、水系分维等水系形态特征;根据流域内多年平均降雨量与径流资料,对流域及其子流域的径流系数进行计算。结果表明:①根据集水区面积域值与河网密度关系曲线,最终确定以网密度为0.53 km·km-2提取水系;②根据流域内各主河道特征,以及流域水生态系统健康监测与评价尺度,最终将流域划分为15个子流域;③降雨量与径流深度空间分布趋势基本一致,但降雨量与径流系数趋势有差异,各子流域的径流系数为0.637~0.800,引起径流系数差异的主要原因有植被覆盖、地层岩性、人类活动等。

关键词: 漓江流域, 水文特征, 空间分析

Abstract: Extraction and analysis of hydrological characteristics not only provide important parameters for the hydrological processes simulation,but also offer beneficial support to health monitoring and evaluation of aquatic ecosystem.Based on DEM with 30 m resolution of Lijiang river basin,river network is extracted;the watershed is determined;the sub catchments are divided;and the river length,river density,and fractal dimension are calculated,etc.According to the average rainfall and runoff data of many years,the runoff coefficient of drainage basin is calculated.The results indicate that:1)By using the catchment threshold value and drainage density curve,the network density of0.53 km·km-2 is ultimately determined to extract the network.2)With the main drainage line characteristics,and health monitoring and evaluation scale,the river is at last divided into 15 sub-watershed.3)The spatial distribution trend of rainfall and runoff depth isbasically the same,with slight difference between rainfall and runoff coefficient.The runoff coefficient of each sub-watershed ranges from 0.637 to 0.800.Differences in runoff coefficient is mainly affected by vegetation cover,stratum lithology and human activities.

Key words: Lijiang river basin, hydrological characteristic, spatial analysis

中图分类号: 

  • X8
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[1] 何东艳, 华璀, 卢远. 漓江流域土地利用生态风险评价[J]. 广西师范大学学报(自然科学版), 2012, 30(4): 172-178.
[2] 王晓超, 蔡德所, 祝铁钢, 张永祥, 林红军, 武大勇. 农田引水拦河坝对漓江流域河流生态系统的影响[J]. 广西师范大学学报(自然科学版), 2012, 30(4): 179-183.
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