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    茶园扩张对流域水文连通性的影响分析:以福建土楼区大地溪小流域为例

    Analysis of the impact of tea plantation expansion on watershed hydrological connectivity: A case study of the Dadi Creek watershed in the Fujian Tulou area

    • 摘要: 为探究梯地茶园扩张及其配套工程对流域水文连通性的影响,以福建土楼区大地溪小流域为例,基于1999年(自然状态为主)和2023年(茶园扩张强烈干预)两期数据,采用矢量-栅格离散化方法构建基于水文响应单元(HRU)的水文网络,并结合图论指标系统分析了流域结构与功能连通性的变化。结果表明:道路、沟渠等线性工程显著改变汇流网络结构,沟壑密度由1.85km/km²增至2.90 km/km²,高可达性节点比例下降5.92%,使网络结构趋于松散化;人工沟渠优化了局部径流路径,高效传输节点比例增加5.13%,提升了物质传输能力;梯地茶园通过改变微地形产生径流阻滞效果,滞留性节点比例增加2.37%;流域整体连通性下降14.9%,但人工沟渠处形成新的关键连通节点。研究表明茶园扩张对水文连通性具有“局部增强、整体减缓”双重效应,所识别的关键连通区域可为水土保持措施的精准布设与管理提供依据。

       

      Abstract: BackgroundHydrological connectivity is central to understanding watershed eco-hydrological processes and soil-water conservation functions. In the Fujian Tulou UNESCO World Heritage Site, large-scale expansion of terraced tea plantations and the construction of associated roads and ditches have substantially altered the natural morphology of the underlying surface, forming a complex composite hydrological system intertwining natural and artificial elements. Quantifying the impact of such anthropogenic activities on watershed hydrological connectivity is essential for enabling precise ecological regulation and management, as well as for promoting sustainable watershed development. Methods This study selected the Dadi Creek watershed in the Fujian Tulou area as a case study. The year 1999, prior to large-scale tea plantation development, was designated as the baseline state, while 2023, representing a period of intensive anthropogenic intervention and mature plantation expansion, was selected as the changed state. Utilizing UAV imagery and field-investigated data, landscape elements such as terraces and ditches were finely delineated as Hydrological Response Units (HRUs). A vector-raster hybrid discretization approach was then employed to construct the hydrological network. Graph theory metrics were applied to systematically evaluate changes in structural and functional connectivity: the Shimbel Index (Shi) was used to quantify the compactness of the network structure; the Potential Flow Index (Fi) served to identify potential hubs for material transport; and the Residual Flow Index (RF) was employed to distinguish between functional "transport-enhanced zones" and "runoff-retention zones." Furthermore, the Integral Index of Connectivity (IIC) and the delta IIC (dIIC) were calculated to assess the overall functional level of the watershed and the spatial contribution of individual nodes, respectively. Finally, a dual-threshold method was implemented to precisely identify the critical connectivity nodes that exert a decisive influence on the watershed's connectivity pattern.Results Linear engineering projects such as roads and ditches significantly altered the structural characteristics of the small watershed's confluence network: gully density increased from 1.85 km/km² to 2.90 km/km², and the hydrological network structure became more fragmented (with the proportion of high-reachability nodes decreasing by 5.92%); (2) Artificial ditches optimized local runoff pathways, enhancing the potential for local material transport (the proportion of high-Fi nodes increased by 5.13%). Meanwhile, terraced tea plantations, by modifying slope micro-topography, generated a significant runoff retention effect (the proportion of nodes with RF < 0, indicative of flow retardation, increased by 2.37%); (3) The overall watershed hydrological connectivity (IIC) decreased by 14.9%. However, the spatial pattern of node importance (dIIC) revealed that new critical connectivity zones formed at the confluences of artificial ditches and the natural drainage system, marking a spatial shift of hydrological control hubs from natural river channels toward composite artificial-natural nodes.ConclusionsThe research indicates that terraced tea plantation expansion exerts a dual effect of “local enhancement but overall reduction” on hydrological connectivity. The identified key connectivity zones can provide a basis for the precise layout and management of soil and water conservation measures. Moreover, the “hydrological network–graph theory” analytical framework established in this study can also serve as a model basis for analyzing hydrological processes in similar small watersheds subject to human activities.

       

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