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受火山喷发影响的安第斯流域沉积物连通性变化。

Sediment connectivity changes in an Andean catchment affected by volcanic eruption.

机构信息

University of Padova, Department of Land, Environment, Agriculture and Forestry, Padova, Italy.

University of Padova, Department of Land, Environment, Agriculture and Forestry, Padova, Italy; Universidad Austral de Chile, Faculty of Engineering, Valdivia, Chile; Universidad Austral de Chile, RINA - Natural and Anthropogenic Risks Research Center, Valdivia, Chile.

出版信息

Sci Total Environ. 2019 Nov 20;692:1209-1222. doi: 10.1016/j.scitotenv.2019.07.303. Epub 2019 Jul 21.

Abstract

River systems are continuously affected by multiple natural and anthropogenic phenomena. Among major natural disturbances, volcanic eruptions have the capability to overthrow the forms and to modify dramatically the morphological setting and sediment connectivity of the system. Moreover, the input of sediments in the channel network can lead to active channel widening, bed aggradation and river scouring, which in turn may affect downstream human settlements. In this context, the present research aims to investigate sediment connectivity by means of a geomorphometric index in a catchment affected by an explosive volcanic eruption in order to assess its variation before and after the disturbance. We developed a workflow exploiting the use of open source data (i.e., Global Digital Elevation Models, satellite imagery) to represent the impedance to the sediment fluxes and to apply the Index of Connectivity (IC) in this context characterized by the lack of high-resolution topographic data. The study area is the Blanco River basin, southern Chile, which was heavily affected by the eruption of Chaitén volcano (2008-2009) that caused the partial destruction of the forest and the profound alteration of Blanco River's morphology. The application of the IC on different land cover scenarios, derived by combining field observations and satellite image classification techniques, showed an increase in sediment connectivity after the volcanic eruption. In addition, the results highlighted different patterns of connectivity according to the expansion of the active channel induced by the massive input of pyroclastic material. The approach proposed in this study case offers a methodology to investigate sediment connectivity in a river catchment affected by natural disturbance where high-resolution data are not available. The results of the study help to improve knowledge on the effect of volcanic eruptions in the hydrologic catchment and to improve watershed management strategies in such kind of environment.

摘要

河流系统不断受到多种自然和人为现象的影响。在主要的自然干扰中,火山爆发有能力推翻地貌形态,并极大地改变系统的形态和沉积物连通性。此外,沉积物输入到河道网络中会导致活跃的河道拓宽、河床淤积和河道冲刷,这反过来又可能影响下游的人类住区。在这种情况下,本研究旨在通过地貌形态指数调查一个受爆发性火山喷发影响的流域的沉积物连通性,以评估其在干扰前后的变化。我们开发了一个工作流程,利用开源数据(即全球数字高程模型、卫星图像)来表示沉积物通量的阻力,并在缺乏高分辨率地形数据的情况下在这种情况下应用连通性指数(IC)。研究区域是智利南部的布兰科河盆地,该盆地受到柴坦火山喷发(2008-2009 年)的严重影响,导致森林部分被毁,布兰科河的形态发生了深刻变化。在不同的土地覆盖情景下应用 IC,这些情景是通过结合实地观测和卫星图像分类技术得出的,结果表明火山喷发后沉积物的连通性增加。此外,结果还根据火山灰物质大量输入引起的活跃河道的扩张,突出了不同的连通模式。本研究案例中提出的方法提供了一种在没有高分辨率数据的情况下研究受自然干扰影响的河流流域沉积物连通性的方法。研究结果有助于提高对火山喷发对水文流域的影响的认识,并改善此类环境中的流域管理策略。

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