测绘通报 ›› 2025, Vol. 0 ›› Issue (5): 34-39.doi: 10.13474/j.cnki.11-2246.2025.0506

• 生态全要素监测与分析 • 上一篇    

东洞庭湖藕池河东支三角洲冲淤时空分析

罗建强1,2,3, 贺秋华1,2,3, 夏乐1,2,3, 梅金华1,2,3, 黄杰1, 余姝辰1,2,3   

  1. 1. 湖南省自然资源事务中心, 湖南 长沙 410004;
    2. 洞庭湖区生态环境遥感监测湖南省重点实验室, 湖南 长沙 410004;
    3. 自然资源部洞庭湖流域生态保护修复工程技术创新中心, 湖南 长沙 410004
  • 收稿日期:2024-09-26 发布日期:2025-06-05
  • 通讯作者: 贺秋华。E-mail:hn23559@126.com
  • 作者简介:罗建强(1982—),男,工程师,主要研究方向为生态环境遥感、自然资源与国土空间生态监测。E-mail:154019343@qq.com
  • 基金资助:
    自然资源部、湖南省自然资源厅专题性地理国情监测项目(测国土函〔2017〕37号;自然资办发〔2018〕12号;HNGQJC2017-13;HNJCCH-2018-13);湖南省自然科学基金联合基金(2024JJ8320);湖南省自然资源厅科技计划(2022-19;湘自资科20230142ST)

Temporal and spatial analysis of erosion and deposition in the Ouchi River Delta of East Dongting Lake

LUO Jianqiang1,2,3, HE Qiuhua1,2,3, XIA Le1,2,3, MEI Jinhua1,2,3, HUANG Jie1, YU Shuchen1,2,3   

  1. 1. Hunan Center of Natural Resources Affairs, Changsha 410004, China;
    2. Hunan Provincial Key Laboratory of Remote sensing Monitoring of Ecological Environment in Dongting Lake Area, Changsha 410004, China;
    3. Dongting Lake Basin Ecological Protection and Restoration Engineering Technology Innovation Center, Ministry of Natural Resources, Changsha 410004, China
  • Received:2024-09-26 Published:2025-06-05

摘要: 东洞庭湖藕池河东支三角洲是近100年以来洞庭湖发育最快的洲滩,为了分析藕池河东支三角洲冲淤过程,预测其未来发展趋势,为东洞庭湖洲滩利用与水沙治理提供数据支撑,本文基于遥感技术,结合多年水沙数据,从洲滩面积、河道变化、植被变化3个方面开展1967—2023年近55年间藕池河东支三角洲冲淤时空分析。研究表明,20世纪60年代至80年代是藕池河东支三角洲面积的快速扩张期,年均增长6.48 km2;90年代增速放缓,年均增加0.94 km2;2003年三峡水库运行后年均增加面积降低至0.13 km2。受湖泊内部水文环境影响,三角洲内部河道先向东北延伸后转向西南形成“倒U”形反向冲淤,泥沙沿河道两侧淤积,形成近河道高远河道低的坡形洲滩。从2003年起,洲滩上的芦苇面积增加而湖草面积减少,表明洲滩面积扩张趋于停止,但淤高仍在持续。

关键词: 东洞庭湖, 洲滩扩张, 遥感技术, 藕池河三角洲

Abstract: The Dongdongting Lake Ouchi River East Branch Delta is the fastest developed beach in Dongting Lake in past 100 years. In order to analyze the erosion and deposition process of the Ouchi River East Branch Delta, predict its future development trend, and provide data support for the utilization of the East Dongting Lake beach and water and sediment management, this article uses remote sensing technology and combines years of water and sediment data to conduct a spatiotemporal analysis of the erosion and deposition of the Ouchi River East Branch Delta from 1967 to 2023 in past 55 years from three aspects: beach area, river channel changes, and vegetation changes. Research has shown that the 1960s to 1980s were a period of rapid expansion in the area of the eastern branch of the Ouchi River delta, with an average annual growth rate of 6.48 km2. In the 1990s, the growth rate slowed down, with an average annual increase of 0.94 km2. After the operation of the Three Gorges Reservoir in 2003, the average annual increase in area decreased to 0.13 km2. Due to the influence of the hydrological environment inside the lake, the river channels in the delta first extend northeast and then turn southwest to form an “inverted U”-shaped reverse erosion and deposition. Sediments accumulate along both sides of the river channel, forming a slope shaped sandbar with high near the river channel and low far from it. Since 2003, the area of reeds on the sandbar has increased while the area of lake grass has decreased, indicating that the expansion of the sandbar area is tending to stop, but siltation is still continuing.

Key words: Dongting Lake, beach expansion, remote sensing technology, Ouchi River Delta

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