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Assessment of the recurrence intervals of rockfall through dendrogeomorphology and counting scar approach: A comparative study in a mixed forest stand from the Vercors massif (French Alps)

机译:通过树状地貌和计数疤痕法评估落石的复发间隔:来自韦科尔地块(法国阿尔卑斯山)的混交林林分的比较研究

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摘要

As direct observations of rockfalls are rare and difficult to obtain over long timescales, stem injuries and their dating with dendrogeomorphic techniques have been applied frequently in the past to reconstruct process activity. However, the analysis of tree-ring samples requires considerable temporal efforts, which can be detrimental in applied research and expert opinions. To compensate for this shortcoming, several studies have lately explored the potential of the counting of visible scars as an alternative method to dendrogeomorphology as it requires much less time and human efforts to reconstruct spatial patterns of rockfall activity. Yet, to date, both approaches have not been compared at the same site. In this paper, based on the extensive analysis of 278 conifer and broadleaved trees (from which 1097 tree-ring cores were extracted) from a mixed forest plot of the Vercors Massif (French Alps), we demonstrate that both methods provide similar spatial patterns of rockfall activity with a strong increase of recurrence intervals down the talus slope and a clear lateral zonation of activity. Despite this apparent convergence between both approaches, our study also evidences that rockfall frequencies strongly differ with tree species and diameter: the visual inspection of conifer stems and the analysis of tree-ring signals in large-diameter broadleaved trees typically lead to an overestimation of recurrence intervals. Based on these findings, we recommend giving priority to the scar-counting approach on small diameter (15 cm) broadleaved stems and to restrict tree-ring analysis to old conifers that are more susceptible - through the identification of tangential rows of traumatic resin ducts - to provide reliable estimations of long recurrence intervals (as generally observed in the lower portions of the slope). These guidelines should help to improve the reliability of recurrence interval maps of rockfall process activity in forests further, but also to improve cost-benefit ratios of future studies. (C) 2019 Elsevier B.V. All rights reserved.
机译:由于对落石的直接观测非常少见,而且很难在长时间范围内获得,因此过去人们经常将茎损伤及其与树状地貌技术的年代结合起来,以重建过程活动。但是,对树轮样本的分析需要大量时间上的努力,这可能对应用研究和专家意见不利。为了弥补这一缺点,最近有几项研究探索了计数可见疤痕作为树突状地貌学替代方法的潜力,因为它需要更少的时间和人力来重建落石活动的空间格局。但是,迄今为止,尚未在同一站点上比较这两种方法。在本文中,基于对Vercors Massif(法国阿尔卑斯山)混交林地中的278针叶树和阔叶树(从中提取了1097个年轮核心)的广泛分析,我们证明了这两种方法都提供了相似的空间格局落石活动,沿距骨斜坡向下的复发间隔大大增加,且活动的横向区域清晰。尽管这两种方法之间存在明显的收敛性,但我们的研究还证明,落石频率随树木种类和直径的不同而存在很大差异:针叶树茎的目视检查以及大直径阔叶树中树环信号的分析通常会导致高估复发率间隔。基于这些发现,我们建议优先采用小直径(<15 cm)阔叶茎上的疤痕计数方法,并通过更容易受到伤害的树脂导管切向行的识别,将树环分析的范围限制在更易感的旧针叶树上-提供长重复间隔的可靠估计(通常在斜面的下部观察到)。这些指导方针应有助于进一步提高森林中崩塌过程活动的重复间隔图的可靠性,而且还可以提高未来研究的成本效益比。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Geomorphology》 |2019年第1期|160-171|共12页
  • 作者单位

    Univ Grenoble Alpes, Irstea, UR LESSEM, 2 Rue Papeterie BP 76, F-38402 St Martin Dheres, France|Univ Grenoble Alpes, Irstea, UR ETGR, 2 Rue Papeterie BP 76, F-38402 St Martin Dheres, France;

    Univ Geneva, Inst Sci Environm, 66 Bd Carl Vogt, CH-1205 Geneva, Switzerland;

    Univ Blaise Pascal, GEOLAB, UMR6042, CNRS, Maison Sci Homme, F-63057 Clermont Ferrand 2, France;

    Univ Geneva, Inst Sci Environm, 66 Bd Carl Vogt, CH-1205 Geneva, Switzerland|Univ Geneva, Dept Earth Sci, Dendrolab Ch, 13 Rue Maraichers, CH-1205 Geneva, Switzerland|Univ Geneva, Dept FA Forel Environm & Aquat Sci, 66 Blvd Carl Vogt, CH-1205 Geneva, Switzerland;

    Univ Grenoble Alpes, Irstea, UR LESSEM, 2 Rue Papeterie BP 76, F-38402 St Martin Dheres, France;

    Univ Grenoble Alpes, Irstea, UR ETGR, 2 Rue Papeterie BP 76, F-38402 St Martin Dheres, France;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Rockfalls; Recurrence interval; Tree-ring analyses; French Alps;

    机译:落石;复发间隔;树轮分析;法国阿尔卑斯山;

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