大兴安岭雷击火烧迹地地表可燃物燃烧性变化及其影响因素
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1.东北林业大学;2.中国林业科学研究院森林生态环境与自然保护研究所 国家林业草原火灾监测预警与防控工程技术研究中心;3.黑龙江省自然资源权益调查监测院

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中图分类号:

S762????????????

基金项目:

国家自然科学基金(32371881);国家林草局“揭榜挂帅”项目(2023132032) 


Change of combustibility of forest surface fuel and their influencing factors in lightning fire burned area in the Daxing’an Mountains
Author:
Affiliation:

1.Northeast Forestry University;2.National Forestry and Grasland Fire Monitoring Early Waring and Prevention Engineering Technology Research Center Ecology and Nature Conservation Institute Chinese Academy of Forestry;3.The Natural Resources Rights and Interests Survey and Monitoring Institute of Heilongjiang Province

Fund Project:

The National Natural Science Foundation of China (32371881);State Forestry and Grassland Administration "unveiled the leader" project(2023132032).

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    摘要:

    【目的】揭示雷击火烧迹地地表死可燃物燃烧性的变化趋势及其影响因素,为我国大兴安岭地区雷击火烧迹地火灾风险评估提供理论支撑。【方法】以大兴安岭塔河地区兴安落叶松林雷击火烧迹地为研究对象,以火烧迹地内地表可燃物为实验材料,测定其理化性质,并通过主成分分析计算其燃烧性,基于聚类分析对其燃烧性进分级,利用随机森林法明确地表可燃物燃烧性的影响因素。【结果】地表可燃物的未分解层在火后17 -23较易燃,杂木生物量、过火年限和坡向显著影响综合燃烧性(P< 0.05);半分解层的地表可燃物中木质素对半分解层可燃物燃烧性的影响显著;地形因素对半分解层可燃物燃烧性影响均不显著(P > 0.05)。灰分,热值和粗脂肪均显著影响地表可燃物燃烧性(P < 0.01)。灰分和热值分别是未分解层和半分解层地表可燃物燃烧性的最重要影响因素。【结论】过火11年后的雷击火烧迹地地表可燃物较易燃。森林地表可燃物燃烧性不受单一因素控制,而受多因素共同影响。过火年限、杂木生物量和坡向、坡位显著影响未分解层地表可燃物燃烧性。过火年限、样地生物量和地形因子对半分解层的燃烧性影响均不显著。因此,应对过火11-23年的雷击火烧迹地进行重点管控。

    Abstract:

    【Objective】To reveal the change trend of combustibility of burned area combustibility and its influencing factors in lightning burned areas, so as to provide theoretical support for fire risk assessment of lightning burned areas in the Daxing’an Mountains in China.【Method】Using the method of "space-time displacement", the combustibilities on the forest surface fuel of Larix gmelinii with different times after fire in the Tahe area of the Daxing’an Mountains were taken as the research object to determine their physical and chemical properties.【Result】The litter layer of the forest surface fuel was more flammable at 17-23 after fire, and the ash content had the greatest impact on its flammability. The biomass of other tree species, time after fire and slope aspect significantly affected the comprehensive flammability (P< 0.05). The calorific value of surface fuel in the fermentative layer has the greatest influence on its flammability. Terrain factors had no significant effect on the flammability of forest surface fuel in the fermentative layer (P > 0.05). Ash content, calorific value and fat significantly affected the combustibility of forest surface fuel (P < 0.01). Ash content and high calorific value are the most important factors affecting the combustibility of forest surface fuel in litter layer and fermentative layer, respectively.【Conclusion】The forest surface fuel in the litter layer 17-23 years after the fire and the fermentative layer 11-23 years after the fire are more flammable. Ash content, calorific value, fat and hemicellulose are significant factors affecting the combustibility of forest surface fuel. The time after fire, biomass of other tree species, slope aspect and slope position significantly affected the flammability of forest surface fuel in the litter layer. The effects of time after fire, biomass and terrain factors on the flammability of the fermentative layer were not significant. Therefore, we should focus on the control of lightning fires that have been burned for 11-23 years.

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杨光,张瑞杰,王立轩,宁吉彬,郑鑫,王明玉,孙建.大兴安岭雷击火烧迹地地表可燃物燃烧性变化及其影响因素.生态学报,,(). http://dx. doi. org/[doi]

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