[1]刘春香,黄紫乐,谭博文,等.湖南东江湖水库消落带地形因子与水文要素时空格局变化[J].山地学报,2023,(5):676-688.[doi:10.16089/j.cnki.1008-2786.000779]
　LIU Chunxiang,HUANG Ziyue,TAN Bowen,et al.Spatiotemporal Changes in Topographic and Hydrological Factors in Hydro-Fluctuation Belt in the Dongjiang Lake of Hunan Province, China[J].Mountain Research,2023,(5):676-688.[doi:10.16089/j.cnki.1008-2786.000779]
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湖南东江湖水库消落带地形因子与水文要素时空格局变化
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2023年第5期
页码:
676-688
栏目:
山地环境
出版日期:
2023-09-25

文章信息/Info

Title:
Spatiotemporal Changes in Topographic and Hydrological Factors in Hydro-Fluctuation Belt in the Dongjiang Lake of Hunan Province, China
文章编号:
1008-2786-(2023)5-676-13
作者:
刘春香;  黄紫乐;  谭博文;  李有志*
(湖南农业大学 环境与生态学院,长沙 410128)
Author(s):
LIU Chunxiang;  HUANG Ziyue;  TAN Bowen;  LI Youzhi*
(College of Environment and Ecology, Hunan Agricultural University, Changsha 410128)
关键词:
DEM;  坡度;  淹水深度;  淹水天数;  植被修复
Keywords:
DEM;  slope;  flooding depth;  flooding days;  vegetation restoration
分类号:
Q149
DOI:
10.16089/j.cnki.1008-2786.000779
文献标志码:
A1
摘要:
东江湖消落带岸坡侵蚀、水土流失严重,生态风险堪忧,生态修复刻不容缓。地形因子和水文要素作为湖库消落带修复最为关键的约束性条件,反映了库岸生态系统的基本状态。本研究基于东江湖流域DEM(Digital Elevation Model)数据和水文站2017—2021年的日水位数据,利用ArcGIS提取消落带范围,分析地形因子和水文要素时空格局变化。结果表明:(1)东江湖消落带位于263～278 m高程区间,垂直落差15 m,总面积25.16 km2。消落带高程和坡度均呈现南北高、中间低的特点,即高高程和陡坡区段主要位于滁口镇和黄草镇等地区,而低高程和缓坡主要位于白廊镇和小东江等地区; 消落带无坡向分布广泛,呈现出阴坡面积多于阳坡的特点,而长坡主要位于北部,短坡主要位于南部; 消落带剖面曲率和平面曲率在空间上呈现相同的变化趋势,即在南北两端较低,在中部较高。(2)东江湖消落带地形因子和水文要素呈现出明显的空间异质性。东江湖消落带全年淹水天数、最低持续淹水天数、平均持续淹水天数、最大淹水深度、平均淹水深度等水文要素均随高程的增加而下降,呈现出显著负相关关系。(3)白廊镇、坪石乡、兴宁镇和小东江应为消落带综合治理的重点区域,滁口镇和黄草镇等为综合治理的难点区域。消落带263～266 m高程段属于常年淹水区域,不适宜植被存活; 266～278 m高程段属于偶然淹水区,适宜开展一定植被修复。研究结果可为东江湖消落带的植物群落构建、生态修复与综合治理供科学依据。
Abstract:
Ecological restoration of the hydro-fluctuation belt in the Dongjiang Lake is important because of the increasing risk of riverbank erosion and water-soil loss. As the most critical factors for the restoration of the hydro-fluctuation belt of lakes and reservoirs, topographic and hydrological factors best describe the basic state of such an ecosystem.
In this study, digital elevation model(DEM)data of the Dongjiang Lake Basin and daily water level data(2017-2022)from hydrological stations were collected. The range of the hydro-fluctuation belt was extracted using ArcGIS, and then the changes in spatiotemporal pattern of the topographic and hydrological factors in the hydro-fluctuation belt were analyzed.
The study produced the following findings.(1)The hydro-fluctuation belt in the Dongjiang Lake was located at an elevation of 263-278 m, a vertical elevation difference of 15 m, and had a total area of 25.16 km2. The elevations and slopes in the belt had the highest values in the northern and southern areas(e.g., Chukou Town, Huangcao Town)and the lowest in the middle area(e.g., Bailang Town, Xiaodongjiang). The non-slope aspect in the belt was widely distributed, and the area of shady slope exceeded that of sunny slope. Long and short slopes were mainly located in the northern and southern areas of the belt, respectively. The profile curvature and plane curvature in the belt showed the same change trend in spatial distribution, exhibiting low values in the northern and southern belts and high values in the middle belt.(2)The topographic and hydrological factors in the hydro-fluctuation belt in the Dongjiang Lake were spatially heterogeneous. The annual, minimum continuous, and average continuous flooding days as well as the maximum and average flooding depths in the hydro-fluctuation belt showed significant negative correlations with elevation.(3)It should be considered for comprehensive control of the hydro-fluctuation belt at Bailang Town, Xingning Town, Pingshi Town, and Xiaodongjiang. Comprehensive control will be difficult in Chukou Town and Huangcao Town. The section Lof the belt at elevation ranging from 263 to 266 m was a perennial flooding area and was not suitable for habitat of vegetation, and that ranging from 266 to 278 m was an accidental flooding area that was suitable for some vegetation restoration.
This study provides a scientific basis for plant community establishment, ecological restoration, and comprehensive management of the hydro-fluctuation belt in the Dongjiang Lake.

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备注/Memo

备注/Memo:
收稿日期(Received date): 2023-04-11; 改回日期(Accepted date):2023-10-14
基金项目(Foundation item): 湖南重点研发项目(2019SK2336); 湖南省水利科技项目(XSKJ2022068-31); 郴州国家可持续发展议程创新示范区建设专项(2019sfq21)。[Key Program of Research and Development of Hunan Province(2019SK2336); Water Resources Science and Technology Program of Hunan Province(XSKJ2022068-31); Chenzhou National Sustainable Development Agenda Innovation Demonstration Zone Construction Project(2019sfq21)]
作者简介(Biography): 刘春香(2000-),女,湖南邵阳人,硕士研究生,主要研究方向:湿地生态。[LIU Chunxiang(2000-), female, born in Shaoyang, Hunan province, M.Sc. candidate, research on wetland ecology] E-mail: 2228036598@qq.com
*通讯作者(Corresponding author): 李有志(1981-),男,博士,教授,主要研究方向:湿地生态与环境。[LI Youzhi(1981-), male, Ph.D., professor, research on wetland ecology and environment] E-mail:liyouzhi2004@163.com
更新日期/Last Update: 2023-09-30