重度火灾对缙云山林地持水力的影响研究
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1.重庆师范大学地理与旅游学院;2.西南大学地理科学学院

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基金项目:

国家自然科学基金项目(面上项目,重点项目,重大项目),其他:重庆市自然科学基金面上项目;重庆市技术创新与应用发展专项面上项目


Research on the influence of severe fire on the water-holding capacity of forest land in Jinyun Mountain
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1.College of Geography and Tourism, Chongqing Normal University;2.College of Geographical Science, Southwest University

Fund Project:

The National Natural Science Foundation of China (General Program, Key Program, Major Research Plan); Chongqing Natural Science Foundation Project; Chongqing technical innovation and application development special surface project

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    摘要:

    为阐明重度火灾对林地持水力的影响,揭示森林持水性能对林火的响应机制。以缙云山火烧迹地为研究对象,测定土壤理化性质和枯落物持水力等指标,量化各因素对林地持水力的重要性。研究结果表明:(1)缙云山重度火灾区林地有效持水量减少44.3 %,林地最大持水量提高14.6 %。枯落物蓄积量下降36.9 %,而枯落物有效拦蓄率提高13.6 %;土壤平均自然含水率、饱和含水率分别提高68.0 %、15.9 %。(2)随土层深度的增加,土壤理化性质变化明显。重度火烧后土壤容重下降15.3 %,毛管孔隙度下降44.3 %,总孔隙度提高14.7 %,土壤有机质增加48.2 %。(3)冗余分析结果表明,土壤容重、土壤毛管孔隙度、非毛管孔隙度是影响土壤持水力的关键因子,三项所占解释量之和达83.1 %。火烧干扰、土壤有机质和土层深度对林地持水力也具有重要影响。土壤持水力在林地持水力中贡献最大,土壤容重、土壤毛管孔隙度是影响重度火烧后林地持水力的关键因素。研究结果量化了重度火灾对林地持水力的影响,可为后续制定林地恢复与管理策略提供科学依据,促进生态系统的可持续发展。

    Abstract:

    In Jinyun Mountain of Chongqing, a comprehensive study was conducted on burned areas to analyze the water-holding capacity of forest land with measuring soil physicochemical properties and the water-holding capacity of litter. The research aimed to elucidate the effects of severe forest fire on the water-holding capacity of forest land and reveal the response mechanism of forest water-holding performance to forest fire. The findings revealed that: (1) In the severely burned area of Jinyun Mountain, the effective water holding capacity of the forest land decreased by 44.3%, while the maximum water holding rate of the forest land increased by 14.6%. The litter accumulation declined by 36.9%, yet the effective interception rate of litter rose by 13.6%. The average natural water content and saturated water content of the soil increased by 68.0 % and 15.9% respectively. (2) The physical and chemical properties of soil exhibited pronounced changes with increasing soil depth. After severe burning, the soil bulk density decreased by 15.3%, capillary porosity declined by 44.3%, total porosity increased by 14.7%, and soil organic matter rose by 48.2%. (3) The results of redundancy analysis indicated that soil bulk density, capillary porosity, and non-capillary porosity were the key factors affecting soil water-holding capacity, and the sum of the explanatory amounts accounted for by the three amounts to 83.1%. Fire disturbance, soil organic matter, and soil layer depth also exerted significant influences on the water-holding capacity of forest land. Soil water-holding capacity made the greatest contribution to the water-holding capacity of forest land. Soil bulk density and soil capillary porosity were the key factors affecting the water-holding capacity of forest land after severe fire. The research findings quantified the effects of severe fire on the water-holding capacity of forest land, which would offer a scientific basis for the subsequent formulation of forest land restoration and management strategies, and promote the sustainable development of the ecosystem.

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冷佳欣,刘春红,王轶浩,薄纯悦,张凤,杨喻涵,张雉昀.重度火灾对缙云山林地持水力的影响研究.生态学报,,(). http://dx. doi. org/[doi]

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