首页|期刊导航|水资源保护|鄱阳湖流域水系格局与连通性变化分析

鄱阳湖流域水系格局与连通性变化分析OA

Analysis of water system pattern and connectivity change in the Poyang Lake Basin

中文摘要英文摘要

基于高精度水面数据集,结合水系数量特征、结构特征及连通性指标,对 1995-2021 年鄱阳湖流域丰水期与枯水期的水系格局与连通性变化进行了定量分析.结果表明:鄱阳湖流域的丰水期与枯水期水系的干流总长度基本不变,支流均存在较低等级河流向较高等级河流演变的现象;2021 年不同水文时期的Ⅰ级河流长度相较于 1995 年表现出相反的变化特征,丰水期Ⅰ级河流长度整体增长率达7.81%,枯水期Ⅰ级河流长度的减小率达 5.83%;鄱阳湖流域丰水期的水系格局趋于复杂化,水系数量与结构特征指标总体呈增加趋势,水面率、河网密度、河网复杂度和河网发育系数的增长率均达到5.50%以上,枯水期水系发育程度基本不变但河湖总面积逐渐减少;鄱阳湖流域丰水期水系的节点数和河链数总体上均呈增加态势(增长率超 8.50%),枯水期水系的节点数和河链数整体保持稳定,两水文时期水系连通性基本不变,均呈现出良好的连通状态.

Based on a high-precision water surface dataset,combined with water system quantitative characteristics,structural characteristics and connectivity indicators,a quantitative analysis was conducted on the changes in water system pattern and connectivity during the flood season and dry season of the Poyang Lake Basin from 1995 to 2021.The results indicate that the total length of the main rivers in the Poyang Lake Basin remains largely unchanged during both the flood and dry seasons.However,there is a phenomenon where lower-grade rivers evolve into higher-grade rivers in the tributaries.The length of Grade I rivers in different hydrological periods in 2021 showed opposite characteristics compared to 1995.The overall increase rate of Grade I river length during the flood season reached 7.81%,while the decrease rate during the dry season reached 5.83%.The water system pattern of the Poyang Lake Basin during the flood season has become more complex,with overall increases in the number of water systems and structural characteristics.The growth rates of water surface ratio,river network density,river network complexity,and river network development coefficient all exceeded 5.5%.During the dry season,the development level of water systems remained largely unchanged,but the total area of rivers and lakes gradually decreased.During the flood season,the number of nodes and river chains in the river system generally increased(growth rate exceeded 8.5%),while during the dry season,the number of nodes and river chains remained stable overall.The water system connectivity remained basically unchanged during both hydrological periods,showing good connectivity.

李加林;杨佳铭;刘永超;曹罗丹;周驰

宁波大学浙江省陆海国土空间利用与治理协同创新中心宁波大学地理科学与遥感技术学院宁波大学东海研究院宁波大学浙江省陆海国土空间利用与治理协同创新中心宁波大学地理科学与遥感技术学院

水系格局水系连通性丰水期枯水期鄱阳湖流域

water system patternwater system connectivityflood seasondry seasonthe Poyang Lake Basin

《水资源保护》 2026 (1)

30-38,9

国家社科基金重大项目(23&ZD105)

10.3880/j.issn.1004-6933.2026.01.004

评论