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自然资源遥感  2025, Vol. 37 Issue (5): 24-31    DOI: 10.6046/zrzyyg.2024317
  湖泊生态环境遥感监测专栏 本期目录 | 过刊浏览 | 高级检索 |
1933—2024年洞庭湖注滋口三角洲时空演变特征
邹娟1,2(), 余姝辰1,2(), 贺秋华1,2, 徐质彬3, 尹向红1, 邹聪1
1.湖南省自然资源事务中心,长沙 410004
2.洞庭湖区生态环境遥感监测湖南省重点实验室,长沙 410004
3.湖南省遥感地质调查监测所,长沙 410015
Spatiotemporal evolution of the Zhuzikou delta in Dongting Lake from 1933 to 2024
ZOU Juan1,2(), YU Shuchen1,2(), HE Qiuhua1,2, XU Zhibin3, YIN Xianghong1, ZOU Cong1
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. Remote Sensing Geological Survey and Monitor Institute of Hunan Province,Changsha 410015,China
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摘要 藕池河东支注滋口三角洲是近百年来洞庭湖区发育最快、面积最大的洲滩之一。该文基于1933年以来20个时段的历史地图和航天航空遥感数据,采用遥感解译与历史对比分析方法,剖析1933年以来该三角洲时空演变特征。结果表明:1933—2024年间,空间上注滋口三角洲表现为不断向湖域推进,淤积的高位洲滩被围垦形成堤垸,老的河道废弃为垸内“哑河型内湖”,新的河道不断向湖域延伸并多次改道;注滋口下游河道向湖域延伸38.99 km,年均推进速度为428.46 m/a;注滋口三角洲淤积面积340.19 km2,年均淤积3.74 km2;该三角洲边淤积边围垦,累计围垦面积230.42 km2,占总淤积面积近50%;不同时段扩张速率不同,分为1933—1954年的缓慢扩张期、1954—1998年的快速扩张期、1998—2010年的基本稳定期和2010—2024年的微略萎缩期等,2010年之后该三角洲开始萎缩,结束了1933年以来的扩张历史。研究成果为科学保护修复洞庭湖洲滩湿地资源提供了原创性资料。
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邹聪
关键词 历史地图遥感技术洞庭湖区注滋口三角洲时空演变    
Abstract

The Zhuzikou delta,located on the east branch of the Ouchi River,has been one of the fastest-growing and largest marshlands in the Dongting Lake area over the past century. Based on the historical maps and aerospace remote sensing data from 20 periods since 1933,this paper analyzed the spatiotemporal evolution of the delta through remote sensing interpretation and historical comparative analysis. The results showed that over the past 90 years,the Zhuzikou delta had been persistently advancing towards the lake area,with the deposited high-level bottomland being reclaimed into embankments. The old river channels had been abandoned and evolved into inner lakes of a blocked river type within the embankments,while the new river channels had been continuously extended towards the lake area along changing paths caused by multiple course changes. The channels of the lower reaches in the Zhuzikou delta have extended 38.99 km towards the lake area at an average annual rate of 428.46 m/a. The sedimentation area in the delta has expanded to 340.19 km2 at an average annual rate of 3.74 km2/a. Reclamation of the delta has been carried out in parallel with sedimentation,with a cumulatively reclaimed area of 230.42 km2,accounting for nearly 50% of the total sedimentation area. The expansion rate has been varying across periods,including a slow expansion period from 1933 to 1954,a rapid expansion period from 1954 to 1998,a period of relative stability from 1998 to 2010,and a slight shrinkage period from 2010 to 2024. The delta has started to shrink since 2010,marking an end of its expansion history since 1933. The research findings provide original data for the scientific protection and restoration of wetland resources in the Dongting Lake.

Key wordshistorical map    remote sensing technology    Dongting Lake area    Zhuzikou delta    spatiotemporal evolution
收稿日期: 2024-10-08      出版日期: 2025-10-28
ZTFLH:  TP79  
基金资助:湖南省自然科学基金项目“近百年来洞庭湖洲滩湿地时空演替及其与水文环境耦合机理研究”(2024JJ8320);湖南省科技人才托举工程“年轻优秀科技人才培养计划”(2023TJ-N16);湖南省自然资源科技计划项目“洞庭湖区水生态安全及解决方案研究”(湘自资科20230151ST);“‘洞庭湖区山水林田湖草沙一体化保护修复工程’监测评估关键技术研究”(湘自资科20230142ST)
通讯作者: 余姝辰(1990-),女,高级工程师,主要从事生态环境遥感监测与研究。Email:22581400@qq.com
作者简介: 邹 娟(1989-),女,高级工程师,主要从事资源环境遥感监测与科研工作。Email:339818271@qq.com
引用本文:   
邹娟, 余姝辰, 贺秋华, 徐质彬, 尹向红, 邹聪. 1933—2024年洞庭湖注滋口三角洲时空演变特征[J]. 自然资源遥感, 2025, 37(5): 24-31.
ZOU Juan, YU Shuchen, HE Qiuhua, XU Zhibin, YIN Xianghong, ZOU Cong. Spatiotemporal evolution of the Zhuzikou delta in Dongting Lake from 1933 to 2024. Remote Sensing for Natural Resources, 2025, 37(5): 24-31.
链接本文:  
https://www.gtzyyg.com/CN/10.6046/zrzyyg.2024317      或      https://www.gtzyyg.com/CN/Y2025/V37/I5/24
Fig.1  研究区及外围水系
Fig.2  1933年以来注滋口三角洲空间扩展典型信息源
Fig.3  1933年以来注滋口三角洲洲滩发育与围垦变化系列图
Fig.4  1933年以来注滋口三角洲面积时序变化曲线
[1] 陈宜瑜, 吕宪国. 湿地功能与湿地科学的研究方向[J]. 湿地科学, 2003, 1(1):7-11.
Chen Y Y, Lyu X G. The wetland function and research tendency of wetland science[J]. Wetland Science, 2003, 1(1):7-11.
[2] Zedler J B, Kercher S. Wetland resources:Status,trends,ecosystem services,and restorability[J]. Annual Review of Environment and Resources, 2005, 30:39-74.
[3] van Asselen S, Verburg P H, Vermaat J E, et al. Drivers of wetland conversion:A global meta-analysis[J]. PLoS One, 2013, 8(11):e81292.
[4] Long X R, Lin H, An X X, et al. Evaluation and analysis of ecosystem service value based on land use/cover change in Dongting Lake wetland[J]. Ecological Indicators, 2022, 136:108619.
[5] 陈宝顺. 洞庭湖区整治开发综合考察研究报告[R]. 长沙: 湖南省国土委员会办公室, 1986.
Chen B S. Comprehensive investigation and research report on the improvement and development of Dongting Lake area[R]. Changsha: Office of Hunan Provincial Land and Resources Commission, 1986.
[6] 周松鹤, 黄万士. 洞庭湖区泥沙淤积分析[J]. 泥沙研究, 1985, 10(2):62-67.
Zhou S H, Huang W S. Analysis of sediment deposition in Dongting Lake area[J]. Journal of Sediment Research, 1985, 10(2):62-67.
[7] 张琳, 马敬旭, 张倩, 等. 近60多年洞庭湖水沙演变特征及其与人类活动的关系[J]. 长江科学院院报, 2021, 38(9):14-20.
doi: 10.11988/ckyyb.20200708
Zhang L, Ma J X, Zhang Q, et al. Characteristics of runoff-sediment variation of Dongting Lake in recent six decades and its relationship with human activities[J]. Journal of Yangtze River Scientific Research Institute, 2021, 38(9):14-20.
doi: 10.11988/ckyyb.20200708
[8] 高耶. 三峡工程运行后荆江三口与洞庭湖的水沙变化[D]. 长沙: 湖南农业大学, 2019.
Gao Y. Changes of water and sediment in Jingjiang Sankou and Dongting Lake after the operation of Three Gorges Project[D]. Changsha: Hunan Agricultural University, 2019.
[9] 李正最, 谢悦波, 徐冬梅. 洞庭湖水沙变化分析及影响初探[J]. 水文, 2011, 31(1):45-53,40.
Li Z Z, Xie Y B, Xu D M. Runoff-sediment variation and its effect on the Dongting Lake[J]. Journal of China Hydrology, 2011, 31(1):45-53,40.
[10] 刘晓群, 易放辉, 栾震宇, 等. 东洞庭湖近期冲淤演变分析[J]. 泥沙研究, 2019, 44(4):25-32.
Liu X Q, Yi F H, Luan Z Y, et al. Processes of east Dongting Lake in recent period[J]. Journal of Sediment Research, 2019, 44(4):25-32.
[11] 袁穗波, 谢振华. 洞庭湖洲滩湿地形成规律研究[J]. 湖南林业科技, 2005, 32(5):12-15.
Yuan S B, Xie Z H. The formation law of the wetland of beach of the Dongting Lake[J]. Hunan Forestry Science and Technology, 2005, 32(5):12-15.
[12] 姜加虎, 黄群, 孙占东. 洞庭湖泥沙淤积与洲滩变化研究[J]. 人民长江, 2009, 40(14):74-75.
Jiang J H, Huang Q, Sun Z D. Study on sediment deposition and beach change in Dongting Lake[J]. Yangtze River, 2009, 40(14):74-75.
[13] 梁婕, 蔡青, 郭生练, 等. 基于MODIS的洞庭湖湿地面积对水文的响应[J]. 生态学报, 2012, 32(21):6628-6635.
Liang J, Cai Q, Guo S L, et al. MODIS-based analysis of wetland area responses to hydrological processes in the Dongting Lake[J]. Acta Ecologica Sinica, 2012, 32(21):6628-6635.
[14] 周柏林, 谢石, 肖义, 等. 三峡工程运行初期洞庭湖洲滩变化及成因分析[J]. 水资源研究, 2015(1):81-87.
Zhou B L, Xie S, Xiao Y, et al. Analysis of the changes and causes of Dongting Lake Shoal during the initial operation of the Three Gorges Project[J]. Journal of Water Resources Research, 2015(1):81-87.
[15] 杜耘, 蔡述明. 近代洞庭湖三角洲发育特征[J]. 世界科技研究与发展, 2000, 22(s1):5-8.
Du Y, Cai S M. The development character of Dongting Lake’ deltas in neoteric time[J]. World Sci-Tech Research & Development, 2000, 22(s1):5-8.
[16] 余姝辰, 李长安, 余德清, 等. 洞庭湖区湖泊洲滩地表覆盖变化[J]. 地球科学, 2020, 45(6):1918-1927.
Yu S C, Li C A, Yu D Q, et al. Land cover change on beach of Dongting Lake’s beach[J]. Earth Science, 2020, 45(6):1918-1927.
[17] 余姝辰, 余德清, 王伦澈, 等. 三峡水库运行前后洞庭湖洲滩面积变化遥感认识[J]. 地球科学, 2019, 44(12):4275-4283.
Yu S C, Yu D Q, Wang L C, et al. Remote sensing study of Dongting Lake beach changes before and after operation of Three Gorges Reservoir[J]. Earth Science, 2019, 44(12):4275-4283.
[18] 余姝辰. 基于历史地图和多源遥感数据的近百年来洞庭湖区江湖格局演化[D]. 武汉: 中国地质大学, 2021.
Yu S C. Evolution of the river-lake pattern in the Dongting lake region in the past 100 years based on historical maps and multi-source remote sensing data[D]. Wuhan: China University of Geosciences, 2021.
[19] 余姝辰, 邱罗, 贺秋华, 等. 基于多源遥感的洞庭湖洲滩时空演变研究[J]. 自然资源遥感, 2025, 37(2):228-234.doi:10.6046/zrzyyg.2023298.
Yu S C, Qiu L, He Q H, et al. Exploring the spatiotemporal evolution of bottomland in Dongting Lake based on multisource remote sensing[J]. Remote Sensing for Natural Resources, 2025, 37(2):228-234.doi:10.6046/zrzyyg.2023298.
[20] Yu S C, Zhang Y Z, He Q H. Spatiotemporal evolution of the Dongting Lake Beach in recent 90 years[J]. Journal of Earth Science, 2024, 35(6):2081.
[21] 郭小虎, 刘亚, 陈栋. 2022特枯年洞庭湖区洲滩面积变化特性分析[J]. 人民长江, 2023, 54(2):43-48.
Guo X H, Liu Y, Chen D. Analysis on beach and flat area change characteristics in Dongting Lake area in 2022 extreme dry year[J]. Yangtze River, 2023, 54(2):43-48.
[22] 余德清, 皮建高. 洞庭湖区洲土变化特征与地壳沉降遥感研究[J]. 湖南地质, 2002, 21(1):46-50,76.
Yu D Q, Pi J G. The characteristic of continent soil change in Dongting lake district and remote sencing research on crust subsidence[J]. Hunan Geology, 2002, 21(1):46-50,76.
[23] 李丛蕾, 田书荣, 宋玉成, 等. 湖南洞庭湖麋鹿种群生存力分析[J]. 兽类学报, 2023, 43(3):280-292.
doi: 10.16829/j.slxb.150710
Li C L, Tian S R, Song Y C, et al. Population viability analysis of Père David's deer(Elaphurus davidianus) in Dongting Lake,Hunan Province[J]. Acta Theriologica Sinica, 2023, 43(3):280-292.
[24] 中华人民共和国水利部. 中国河流泥沙公报-2022[M]. 北京: 中国水利水电出版社, 2023.
Ministry of Water Resources of the People’s Republic of China. China river sediment bulletin-2022[M]. Beijing: China Water and Power Press, 2023.
[25] 余姝辰, 李长安, 张永忠, 等. 近百年来洞庭湖区垸内湖泊时空演变分析[J]. 遥感学报, 2021, 25(9):1989-2003.
Yu S C, Li C A, Zhang Y Z, et al. Analysis of the temporal and spatial evolution of lakes in the Dongting Lake Area in the past 100 years[J]. National Remote Sensing Bulletin, 2021, 25(9):1989-2003.
[26] 湖南省政府编. 湖南省滨湖洲土视察报告书[R]. 1947.
Compiled by the Hunan Provincial Government. Hunan Province Binhu Zhou Soil inspection report[R]. 1947.
[27] 贺建林. 近50年来湖南省旱洪灾害及其时空分布[J]. 灾害学, 2000, 15(1):62-66.
He J L. Flood and drought disasters and their spatial temoral distribution in Hunan Province in the recent 50 years[J]. Journal of Catastrophology, 2000, 15(1):62-66.
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