首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Impacts of successive wildfire on soil hydraulic properties: Implications for debris flow hazards and system resilience
【24h】

Impacts of successive wildfire on soil hydraulic properties: Implications for debris flow hazards and system resilience

机译:连续野火对土壤液压特性的影响:对碎片流动危害的影响和系统弹性

获取原文
获取原文并翻译 | 示例
           

摘要

Climate and land use changes have led to recent increases in fire size, severity, and/or frequency in many different geographic regions and ecozones. Most post-wildfire geomorphology studies focus on the impact of a single wildfire but changing wildfire regimes underscore the need to quantify the effects of repeated disturbance by wildfire and the subsequent impacts on system resilience. Here, we examine the impact of two successive wildfires on soil hydraulic properties and debris flow hazards. The 2004 Nuttall-Gibson Complex and the 2017 Frye Fire affected large portions of the Pinaleno Mountains in southern Arizona, creating a mosaic of burn severity patterns that allowed us to quantify differences in wildfire-induced hydrologic changes as a function of burn severity and recent fire history (i.e. burned in only the Frye Fire or burned in both fires). Field observations after the 2017 Frye Fire indicated debris flow activity in areas burned predominantly at low severity. Many of these areas, however, were also affected by the 2004 Nuttall-Gibson Complex, suggesting that the relatively short recovery time between the two wildfires may have played a role in the geomorphic response to the most recent wildfire. Field measurements of soil hydraulic properties suggest that soils burned at moderate severity in 2004 and low severity in 2017 have a lower infiltration capacity relative to those that remained unburned in 2004 and burned at low severity in 2017. Simulations of runoff demonstrate that measured differences in infiltration capacity between once- and twice-burned soils are sufficient in some cases to influence the rainfall intensities needed to initiate runoff generated debris flows. Results quantify the impact of wildfire history and burn severity on runoff and debris flow activity in a landscape affected by successive wildfires and provide insight into how the resilience of geomorphic systems may be affected by successive wildfires. (c) 2019 John Wiley & Sons,
机译:气候和土地利用变化导致最近在许多不同地理区域和杂波中的火灾尺寸,严重程度和/或频率增加。大多数野外大火地貌研究侧重于单一野火的影响,但改变野火制度强调了量化野火反复扰动的影响以及随后对系统弹性的影响。在这里,我们研究了两次连续野火对土壤液压特性和碎片流动危害的影响。 2004年的2004年坚果-Gibson复合体和2017年Frye Fire在亚利桑那州南部影响了大量的Pinouteno山脉,创造了烧伤严重程度模式的马赛克,使我们能够量化野火诱导的水文变化的差异作为烧伤严重程度和最近的火灾的功能历史(即仅在Frye火灾中烧毁或在两次火灾中烧毁)。在2017年FRYE火灾之后的现场观测指示在大幅度燃烧的区域中的碎片流动活动。然而,许多这些领域也受到2004年坚果-Gibson复合体的影响,这表明两个野火之间的恢复时间相对较短,可能在对最近野火的地貌反应中发挥作用。土壤液压特性的田间测量表明,2004年的严重程度燃烧的土壤和2017年低严重程度相对于2004年仍然不燃烧的渗透能力较低,并在2017年以低严重程度烧毁。径流模拟表明渗透差异差异在某些情况下,一次和两次烧坏的土壤之间的能力就足够了,以影响启动径流所产生的碎片流动所需的降雨强度。结果量化野火历史的影响,并烧伤了连续野火影响的景观中的径流和碎片流动活动,并深入了解地貌系统的抵御如何受到连续野火的影响。 (c)2019 John Wiley&Sons,

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
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