首页> 外文期刊>The Science of the Total Environment >Plant reestablishment 15 years after the debris avalanche at Mount St. Helens, Washington
【24h】

Plant reestablishment 15 years after the debris avalanche at Mount St. Helens, Washington

机译:华盛顿圣海伦斯山的雪崩后15年的工厂重建

获取原文
获取原文并翻译 | 示例
       

摘要

Vegetation has slowly reestablished on the debris avalanche deposit in the 15 years after the 1980 eruption of Mount St. Helens that created a 60-km~2 debris avalanche, the largest landslide in recorded history. There has been a gradual increase in species richness and cover, but only 61% of the species present on the mountain before the eruption have established on the debris avalanche deposit. Plant cover averages 38% and is extremely patchy. Life form composition changed over successional time, because part of the avalanche deposit was invaded by introduced plant species aerially seeded to reduce erosion, the site offers the opportunity to compare successional processes occurring with and without introduced species. Long-term recovery trends and effects of nonnative species on succession are important to understand since plant reestablishment practices often rely on nonnative species for enhancing vegetation recovery of denuded sites along road sides, strip mines, or other human-generated clearing. Fifteen years after the eruption and 10 years since the invasion by introduced species, plots invaded by nonnative species had greater vegetation cover and more native plant richness than plots that were not inundated. Significantly greater mortality of conifers occurred in the plots dominated by introduced species shortly after the invasion of those species, but no difference in conifer mortality occurred in the last 5 years. Even so, the plots dominated by introduced species still have fewer conifer trees. Thus, the short-term pulse of conifer mortality after the invasion of introduced species may have long-term effects on the recovery of the dominant vegetation. It will likely be decades before there is 100% plant cover on the debris avalanche deposit and a century or more before full recovery of the vegetation system.
机译:1980年圣海伦斯火山喷发后,在15年内,植被在雪崩沉积上的植被逐渐恢复,形成了60 km〜2的碎片雪崩,这是有史以来最大的滑坡。物种丰富度和覆盖度逐渐增加,但是在喷发之前山上存在的物种中只有61%建立在碎片雪崩沉积上。植物覆盖率平均为38%,并且非常零散。生命形式的组成在连续时间内发生了变化,因为部分雪崩矿床被空中播种的引入植物入侵,以减少侵蚀,该地点为比较有无引入物种发生的演替过程提供了机会。理解长期恢复趋势和非本地物种对演替的影响很重要,因为植物重建实践通常依靠非本地物种来增强路旁,露天矿或其他人为清除的裸露地点的植被恢复。喷发后十五年和外来物种入侵后十年,与未淹没的土地相比,外来物种入侵的土地具有更大的植被覆盖度和更多的原生植物丰富度。入侵物种后不久,在以引进种为主的地块中,针叶树的死亡率显着增加,但在最近5年中没有发生针叶树死亡率的差异。即使这样,以引进物种为主的地块的针叶树仍然较少。因此,入侵物种入侵后针叶树死亡率的短期脉动可能会对优势植被的恢复产生长期影响。可能需要数十年的时间才能在雪崩沉积物上实现100%的植物覆盖,而在完全恢复植被系统之前可能需要一个世纪或更长时间。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号