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Legacy of Insect Defoliators: Increased Wind-Related Mortality Two Decades After a Spruce Budworm Outbreak

机译:昆虫落叶者的遗产:云杉芽虫爆发后的两个世纪,与风相关的死亡率增加

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摘要

Effects of spruce budworm (Choristoneura fumiferana Clem.) outbreaks on growth and survival of balsam fir (Abies balsamea [L.] Mill.) and spruce (Picea spp.) are well documented, but few studies extend beyond 10 years after defoliation ceased. We used inventory data from 106 permanent sample plots in >50-year-old balsam fir stands in northern New Brunswick, Canada, to determine legacy effects of the 1969-1993 budworm outbreak on stand development up to 29 years after defoliation ceased. Defoliation data were from annual aerial surveys from 1945 to 1993 and plot ground sampling from 1985 to 1993. Plots were stratified into net stand volume development categories (decreasing, stable, and increasing 1985-2005 stemwood volume) and related to outbreak phases (outbreak, direct 1-10 years after defoliation ceased, and legacy >10 years), outbreak severity (1-4 [low], 5-8 [medium], and 9-12 [high] years of defoliation), and stand age (mature and overmature). Stand age was an important factor influencing outbreak severity (e.g., r^sup 2^ = 0.383, P < 0.01). Trend and rate of volume development over time were related to past outbreak severity and increased rate of postoutbreak wind-related mortality, which peaked at 11 m^sup 3^/ha/yr 11-15 years after defoliation ceased. Results indicate that aging postoutbreak stands are more vulnerable to wind disturbance events, effecting rapid stand decline. [PUBLICATION ABSTRACT]
机译:云杉芽虫(Choristoneura fumiferana Clem。)的爆发对香脂冷杉(Abies balsamea [L.] Mill。)和云杉(Picea spp。)的生长和存活的影响已有充分文献记载,但是在脱叶停止后超过10年的研究很少。我们使用来自加拿大新不伦瑞克省北部具有50年历史的苦香冷杉林地的106个永久性样地的清单数据,来确定1969-1993年bud虫暴发对脱叶停止后长达29年的林分发育的传统影响。落叶数据来自1945年至1993年的年度航空调查和1985年至1993年的地块采样。地块分为净林分蓄积量发展类别(1985-2005年枯木量减少,稳定和增加),并与爆发阶段(爆发,脱叶停止后1-10年(且传统> 10年),暴发严重程度(1-4 [低],5-8 [中]和9-12 [高]年),以及树龄(成熟)和过早的)。林分年龄是影响暴发严重程度的重要因素(例如r ^ sup 2 ^ = 0.383,P <0.01)。随着时间的流逝,体积发展趋势和速率与过去暴发的严重程度和暴发后与风有关的死亡率的增加速率有关,在落叶停止后的11-15年达到峰值,最高为3 m / s / ha / 11 m / s。结果表明,暴发后老化的林分更易受到风灾事件的影响,导致林分迅速下降。 [出版物摘要]

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  • 来源
    《Forest Science》 |2009年第3期|p.256-267|共12页
  • 作者单位

    Sarah L. Taylor, University of Keele, UK, School of Life Sciences, Keele University, Keele, Staffordshire ST5 5BG, UK-Phone 011-44-1782-733025, Fax: 011-44-1782-733516, s.l.taylor@biol.keele.ac.uk. David A. MacLean, University of New Brunswick, NB, Canada - macleand@unb.ca.Acknowledgments: Thanks to Dale Wilson for New Brunswick Department of Natural Resources permanent sample plot data. Funding for this project was provided by a Natural Sciences and Engineering Research Council Discovery Grant to DAM, and a Canadian Commonwealth Scholarship and Magee-Third Century Postgraduate Merit Award to SLTManuscript received August 5, 2008, accepted March 18, 2009 Copyright © 2009 by the Society of American Foresters,;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
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