首页 | 本学科首页   官方微博 | 高级检索  
     

秦淮河流域水系结构及连通度变化分析
引用本文:高玉琴,刘云苹,闫光辉,何平,陆晓华. 秦淮河流域水系结构及连通度变化分析[J]. 水利水电科技进展, 2020, 40(5): 32-39
作者姓名:高玉琴  刘云苹  闫光辉  何平  陆晓华
作者单位:河海大学水利水电学院,江苏 南京 210098;江苏省泰州引江河管理处,江苏 泰州 225321;河海大学水利水电学院,江苏 南京 210098;中水北方勘察设计研究有限责任公司,天津 300222
基金项目:江苏省自然科学基金(BK20181310);中央高校基本科研业务费专项(2019B45314);国家自然科学基金(52039039)
摘    要:为定量分析城镇化所导致的河网结构及水系连通变化,通过计算1990年、2000年、2010年和2015年4个时期秦淮河流域的河网密度、水面率、河网复杂度、河网稳定度、河网连通度、水文连通度,得出秦淮河流域水系结构演变过程及连通度变化规律,并运用统计学方法得到水系结构指标与水系连通度之间的联系。结果表明:近25年来,秦淮河流域河网密度、水面率均呈不断减小趋势,河道呈现主干化特征,流域河网整体规模呈萎缩趋势,水系连通变化与河网结构变化总体趋势一致,均呈降低趋势,且其变化与水面率、河网密度和河网复杂度具有显著相关性。

关 键 词:水系结构  水系连通度  Pearson相关分析  偏相关分析  秦淮河流域

Analysis on variation of water system structure and connectivity of Qinhuai River Basin
GAO Yuqin,LIU Yunping,YAN Guanghui,HE Ping,LU Xiaohua. Analysis on variation of water system structure and connectivity of Qinhuai River Basin[J]. Advances in Science and Technology of Water Resources, 2020, 40(5): 32-39
Authors:GAO Yuqin  LIU Yunping  YAN Guanghui  HE Ping  LU Xiaohua
Affiliation:College of Water Conservancy and Hydropower Engineering, Hohai University, Nanjing 210098, China;Taizhou Yinjiang Canal Administration of Jiangsu Province, Taizhou 225321, China; College of Water Conservancy and Hydropower Engineering, Hohai University, Nanjing 210098, China; China Water Resources Beifang Investigation, Design and Research Co., Ltd., Tianjin 300222, China
Abstract:To quantitatively analyze the variation of river network structure and water system connectivity caused by urbanization, the river network density, water surface rate, river network complexity, river network structural stability, river network connectivity, and hydrological connectivity of the Qinhuai River Basin in 1990, 2000, 2010 and 2015 were calculated. The evolution process of the water system structure and connectivity in the Qinhuai River Basin were obtained. The statistical method is used to obtain the relationship between the water system structure index and the water system connectivity. The results show that the river network density and water surface rate in the Qinhuai River Basin have been decreasing continuously in the past 25 years. The river channel is characterized by main trunking. The overall scale of the river network in the basin is shrinking. The water system connectivity variation is consistent with the overall trend of river network structure variation, both showing a decreasing tendency. The change is significantly correlated with the water surface rate, river network density and river network complexity.
Keywords:water system structure   water system connectivity   Pearson correlation analysis   partial correlation analysis   Qinhuai River Basin
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《水利水电科技进展》浏览原始摘要信息
点击此处可从《水利水电科技进展》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号