湿地植被对干湿状态的响应特征研究——以挠力河湿地群为例
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1:大连理工大学建设工程学院水环境研究所,大连 116024 ,2:黑龙江省水利水电勘测设计研究院,哈尔滨 150080

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国家自然科学项目(52309079,42077348,42377412)资助


Response of wetland vegetation to dry and wet condition—A case study of the Naoli River Wetland Group
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1:Institute of Water and Environmental Research, Faculty of Infrastructure Engineering, Dalian University of Technology, Dalian 116024 , P.R.China,2:Heilongjiang Provincial Water Conservancy and Hydroelectric Power Investigation,Design and Research Institute, Harbin 150080 , P.R.China

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    摘要:

    气候是湿地形成和发展的主要驱动力,气候变化造成的水分盈亏会对湿地植被产生严重威胁。量化湿地植被对干湿状态的响应特征,对湿地生态恢复具有重要意义。挠力河湿地群是中国重要的淡水沼泽湿地集中区,在全球温带湿地生态系统中具有代表性。因此,本文以挠力河湿地群保护区内的湿地植被为研究对象,基于归一化植被指数(normalized difference vegetation index,NDVI)和标准化降水蒸散发指数(standardized precipitation evapotranspiration index,SPEI),分析2003—2023年挠力河湿地群保护区内NDVI及SPEI的演变情况。根据干湿状态将研究期划分为干旱、湿润及洪涝期,在此基础上,揭示了湿地NDVI对SPEI累积效应和滞后效应的响应特征。结果显示:2003—2023年挠力河湿地群保护区内湿地NDVI整体呈波动增长趋势,增长速率为0.003/10 a,气象条件呈现由干旱向湿润的变化趋势。在干旱时期,挠力河、东升自然保护区湿地NDVI受SPEI累积效应和滞后效应的响应时间较短(2个月),七星河、三环泡自然保护区湿地NDVI受SPEI累积效应(9个月)和滞后效应(4~6个月)的响应时间较长。在湿润时期和洪涝时期,各湿地保护区内湿地NDVI受SPEI累积效应(9个月)和滞后效应(9~10个月、9~11个月)的响应较长。气象条件在轻度干旱和湿润(-1.15<SPEI<1.20)以及由湿润向干旱转变时,湿地NDVI与SPEI呈正相关,而当干旱和湿润强度较大(SPEI≤-1.15 ,SPEI≥1.20)以及由干旱向湿润转变时,湿地NDVI与SPEI呈负相关。研究结果为湿地植被对气象条件响应特征的深入研究提供参考价值,也为湿地生态保护和修复工作提供科学依据。

    Abstract:

    Climate is the main driver of wetland formation and development, and water gains or losses caused by climate change can pose a serious threat to wetland vegetation. Quantifying the response characteristics of wetland vegetation to wet and dry states is important for wetland ecological restoration. The Naoli River wetland complex is an important freshwater marsh concentration area in China, which is representative of temperate wetlands in the world. This paper analyzed the evolution of normalized difference vegetation index (NDVI) and standardized precipitation evapotranspiration index (SPEI) in the Naoli River Wetland Group Reserve from 2003 to 2023, taking the wetland vegetation in the reserve as the study object. The study period was divided into drought, wet and flood periods according to the dry and wet status, based on which the response characteristics of NDVI to the cumulative and lagged effects of SPEI were revealed. The results showed that from 2003 to 2023, the NDVI of the wetland in the Naoli River Wetland Reserve showed a fluctuating growth trend, with a growth rate of 0.003/10 a, and the meteorological conditions showed a trend from drought to wet. During the drought period, the response time of wetland NDVI in Naoli River and Dongsheng Nature Reserves to SPEI cumulative effect and lag effect was shorter (2 months), and the response time of wetland NDVI in Qixing River and Sanhuanpao Nature Reserves to SPEI cumulative effect (9 months) and lag effect (4-6 months) was longer. During the wet period and the flood period, the wetland NDVI in each wetland reserve was subject to the cumulative effect of SPEI (9 months) and the lag effect (9-10 months, 9-11 months).When the meteorological conditions were mildly dry and wet (-1.15<SPEI<1.20 ) and changed from wet to dry, wetland NDVI was positively correlated with SPEI. When the drought and wet intensity were large (SPEI≤ -1.15, SPEI≥1.20 ) and changed from dry to wet, wetland NDVI was negatively correlated with SPEI. This study provide reference value for the in-depth study of the response characteristics of wetland vegetation to meteorological conditions, and provide scientific basis for wetland ecological protection and restoration work.

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王振山,王天亮,景海华,刘建卫,逄晓腾.湿地植被对干湿状态的响应特征研究——以挠力河湿地群为例.湖泊科学,2025,37(4):1445-1456. DOI:10.18307/2025.0442

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  • 收稿日期:2024-09-12
  • 最后修改日期:2024-10-22
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  • 在线发布日期: 2025-07-04
  • 出版日期: 2025-07-06
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