基于景观格局与过程的地表水文联系指数构建

Construction of surface hydrological linkage index based on landscape pattern and process

  • 摘要: 在资源开发、土地利用等人类活动高强度影响下,景观格局与地形地貌将发生显著变化,进而影响各生态单元之间的地表水文联系与过程。为空间定量表达景观格局变化对其所在流域内各生态单元土壤水地表径流补给能力的影响,描述各生态单元之间的生态关系,基于景观生态学和地表径流过程原理,借鉴重力模型创新性构建了地表水文联系指数。该指数主要由反映地表径流汇集和土壤持水潜力的土壤地形指数作为联系项,以及反映不同生态单元之间地表径流路径上阻抗强度的阻力项2部分组成,联系项与阻力项呈比值关系。该指数对于景观格局改变引起的地表水文过程变化具有较好的指示意义,其与斑块密度、聚合度指数等常见景观指数相比具有明显的物理过程机制,以及空间分布式表达的优势。以某半干旱地区大型露天煤矿为例,分析了露天开采前后矿区地表水文联系指数变化的空间异质特征,结果发现开采导致矿区地表水文联系指数的空间异质性增强,排土场等区域地表水文联系明显减弱,采场区域地表水文联系显著增强。露天矿区挖损压占活动对周边区域地表水文联系的影响主要受地势径流路径主控,而并非随采坑或排土场远近呈等半径弧形均质扩散影响。该指数在用于空间分析景观格局与地形地貌变化条件下,对流域或景观尺度下地表土壤水再分布及其生态效应具有重要价值。

     

    Abstract: Under the high-intensity disturbance of human activities such as resource development and land use, landscape patterns and topography are substantially altered, thereby influencing surface hydrological connectivity and processes among ecological units. To quantitatively characterize how landscape-pattern change affects the soil-water storage and surface-runoff recharge capacity of watershed ecological units, and to describe ecological linkages among units, core concepts from hydrology and landscape ecology are integrated. Following the principles of surface-runoff processes and drawing on the gravity model, a novel surface hydrological linkage index is proposed. The index comprises two components: (1) a linkage term representing surface-runoff convergence and soil water-holding potential (captured by the soil topographic index), and (2) a resistance term describing impedance along runoff pathways between ecological units; the linkage and resistance terms are expressed as proportional components. Strong indicative capability is demonstrated for shifts in surface hydrological processes induced by landscape-pattern alteration. Relative to commonly used landscape metrics (e.g., patch density and aggregation index), a clearer physical-process basis and a spatially distributed representation are provided. Using a large open-pit coal mine in a semi-arid region as a case example, spatial heterogeneity of the index is examined before and after mining. Increased heterogeneity is revealed within the mining-affected area, with pronounced weakening over waste dumps and marked enhancement within the open pit. Effects on surrounding areas are shown to be primarily controlled by dominant topographic runoff pathways, rather than exhibiting a uniform distance-decay pattern with equal-radius diffusion from the pit or dumps. The index is therefore suited for spatial analysis of surface soil-water redistribution and associated ecological effects under landscape-pattern and topographic change at watershed and landscape scales.

     

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