| 黄河三角洲横向水文结构连结空间尺度变异性分析 |
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| 引用本文： | 刘佳凯,崔保山,张振明,张明祥.黄河三角洲横向水文结构连结空间尺度变异性分析[J].生态学报,2021,41(10):3745-3754. |
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| 作者姓名： | 刘佳凯 崔保山 张振明 张明祥 |
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| 作者单位： | 北京师范大学环境学院, 北京 100093;国家林业和草原局黄河流域生态保护重点实验室, 北京 100083;北京林业大学生态与自然保护学院, 北京 100083;国家林业和草原局黄河流域生态保护重点实验室, 北京 100083 |
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| 基金项目： | 国家自然科学基金重点项目（51639001，U1901212）；国家自然科学基金（41771547）；中国博士后科学基金资助项目（2020M680437） |
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| 摘 要： | 水文连通是影响滨海湿地生态和水文过程的基础要素之一。引入无标度网络模型改进已有横向静态水文连通参数化方法，将其应用于较大尺度（100 hm2）量化黄河三角洲滨海湿地的水文连通，并结合已有研究结果分析3个尺度（1 m2，100 m2和100 hm2）水文连通的空间变异性。研究结果显示，潮间区和生态补水区的水文连通较强，3个尺度的空间变异性主要来自于水文连通指数较高的样点；盐沼区和河滨区相对较弱，空间变异性主要来自于水文连通指数较小的样点，且大尺度水文连通空间变异性相对中尺度和小尺度更高。小尺度和中尺度方法描述了一个样地与周边较小范围的空间区域土壤水分连通状况，在大的潮汐或补水条件下不同区域各个样地倾向于保持一致；而大尺度方法则侧重于描述区域内的水文过程，这是导致尺度差异的根本原因。
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| 关 键 词： | 水文连通 无标度网络 尺度变异性 滨海湿地 黄河三角洲 |
| 收稿时间： | 2020/7/22 0:00:00 |
| 修稿时间： | 2021/4/12 0:00:00 |
Scale effects of structural hydrological connectivity in coast wetlands in the Yellow River Delta |
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| LIU Jiakai,CUI Baoshan,ZHANG Zhenming,ZHANG Mingxiang.Scale effects of structural hydrological connectivity in coast wetlands in the Yellow River Delta[J].Acta Ecologica Sinica,2021,41(10):3745-3754. |
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| Authors: | LIU Jiakai CUI Baoshan ZHANG Zhenming ZHANG Mingxiang |
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| Institution: | School of Environment, Beijing Normal University, Beijing 100093, China;The Key Laboratory of Ecological Protection in the Yellow River Basin of National Forestry and Grassland Administration, Beijing Forestry University, Beijing 100083, China;School of Ecology and Nature Conservation, Beijing Forestry University, Beijing 100083, China;The Key Laboratory of Ecological Protection in the Yellow River Basin of National Forestry and Grassland Administration, Beijing Forestry University, Beijing 100083, China |
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| Abstract: | Hydrological connectivity is one of the driving factors influence both hydrological and ecological processes in coastal wetlands. In the current study, we used Scale-free Network Model to improve the soil water-topography based static hydrological index, developed for the point (1 m2) and plot scale (100 m2), and parameterized landscape-scale (100 hm2) hydrological connectivity in four wetland classes in the Yellow River Delta and analyzed the scale effects. Results showed, similar with point and plot scales, the inter-tidal flat wetland and artificial reed (Phragmites communis) swamp have relatively stronger hydrological connectivity than tidal marsh and river side wetlands. The hydrological connectivity variation in the landscape scale is higher than which in the other two scales and in areas with higher hydrological connectivity, the spatial variation comes from plots with higher indices and vice versa. The parametrization methods as well as hydrological process heterogeneity are the main reasons for the spatial variation:for point and plot scale, the method focused on the spatial configuration of the soil water content in the target sample and perimeter area which is merely influenced by the tides or other hydrological processes. The landscape method is targeting on the whole study area which is mainly influenced by the hydrological processes. |
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| Keywords: | hydrological connectivity scale-free network scale effects coastal wetlands Yellow River Delta |
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