山丘区地表基质空间异质性特征及其对植被生态影响

    Spatial heterogeneity characteristics of ground substrate in hilly area and its impact on vegetation ecology

    • 摘要: 地表基质是地球表层孕育和支撑森林、草原、水、湿地等各类自然资源的基础物质,受地球关键带空间结构、元素特征等因素的影响,山丘区地表基质呈现明显的空间异质性特征,并显著影响着所属植被的空间分布和生态演化。研究地表基质空间异质性特征及其对植被生态的影响机理,对于进一步认识地球关键带结构及地表作用规律,支撑国土空间生态环境修复具有重要意义。以宁波山丘区地表基质为研究对象,采取剖面研究和样品测试的方法,从地表基质空间结构和元素特征角度,对花岗岩、流纹岩和玄武岩3类典型地表基质空间异质性进行了分析。研究发现,花岗岩类具有土质粗、透水性强等特点,流纹岩类具有土质较粗、浅表透气好等特点,玄武岩类具有土质细、通气性差等特点。此外,花岗岩类主量和微量元素较缺乏,流纹岩类富含Mo和Zn,玄武岩类富含Fe、Mg、Co、Cu、Zn等元素,且玄武岩CIA值明显高于花岗岩和流纹岩。结果表明,山丘区地表基质空间异质性主要受基岩的结构和元素组成影响,并对植被生长产生明显的生态效应。地表基质的空间结构主要影响水分的分布与运移,元素特征影响着养分的分布状况,由此引起的水分和养分的空间分布和丰度差异直接影响着植被生长。

       

      Abstract: The ground substrate is the basic material of the Earth's surface layer that nurtures and supports various natural resources such as forests, grasslands, water and wetlands, etc. Influenced by the spatial structure of the Earth's key zones and elemental characteristics, the ground substrate of the hill area presents obvious spatial heterogeneity characteristics, and significantly influences the spatial distribution of the vegetation belonging to it and its ecological evolution.The study of the spatial heterogeneity characteristics of the ground substrate and its impact on vegetation ecology is of great significance for further understanding the structure and surface process laws of the Earth's critical zone, and supporting the restoration of the national territorial space ecological environment. Taking the ground substrate of Ningbo hill area as the research object, this paper analyzes the spatial heterogeneity of three typical surface matrices, namely granite, rhyolite and basalt, from the perspective of the spatial structure and elemental characteristics of the ground substrate by adopting the methods of sectional research and sample testing. It was found that the granite group is characterized by coarse soil and high permeability, the rhyolite group is characterized by coarser soil and good shallow−surface permeability, and the basalt group is characterized by fine soil and poor aeration. In addition, the main trace elements of granite type are deficient, rhyolite type is rich in Mo and Zn, basalt type is rich in Fe, Mg, Co, Cu and Zn, and the CIA value of basalt is significantly higher than that of granite and rhyolite. The results showed that the spatial heterogeneity of the ground substrate in the hilly area was mainly influenced by the structure and elemental composition of the bedrock, and had obvious ecological effects on the growth of vegetation. The spatial structure of the ground substrate mainly affects the distribution and transportation of water, and the elemental characteristics affect the distribution of nutrients, and the resulting differences in the spatial distribution and abundance of water and nutrients have a direct impact on the growth of vegetation.

       

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