Hydro-morphological reconstruction of the Blanco River in the eruptive event 2008: Variables that influenced the change of the channel course in Chaitén, Chile

IF 1.7 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Ivan Javier Rojas-Castillo , Bruno Mazzorana , Pablo Iribarren-Anacona , Duilio Fonseca-Gallardo , Jorge Berkhoff , Gonzalo Durán , Andrés Iroume
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Abstract

Chaitén, a city in Chilean Patagonia, was hit by lahar flows from the Blanco River in May 2008 following a massive volcanic eruption. This cascade process resulted in the avulsion of the active channel of the Blanco River, dividing the city into two sectors, destroying built environments, and causing displacement of the local population. Hydrodynamic studies in the area have generally been based on post-event environmental conditions. However, an exhaustive reconstruction of the hydrodynamic behavior and associated river dynamics has not been performed. More fundamentally, no clear methodological approach has been proposed to accomplish this task. The present study addresses these challenges by applying non-conventional methods to reconstruct the initial and boundary conditions of the event and to trace the intervening factors that decisively influenced the hydrogeomorphic adjustments in the distal river segments. The reconstruction of the initial and boundary conditions of the event was performed by collecting primary and secondary information (using mixed methods and applying information triangulation). A conceptual model of the hydro-geomorphic evolution of the Blanco River in May 2008 was generated, elucidating the role of rainfall and morphodynamical responses and effects in the Blanco River and emphasizing the hydraulic behavior of the Blanco River bridge. Through the detailed reconstruction of the hydro-geomorphic processes, it could be corroborated that the channel responses were not exclusively due to the volcanic eruption but instead to a combination of massive sediment injections into the fluvial system, the intensity and spatiality of the precipitation pulses (associated with the presence of a frontal system and an atmospheric river), the mobilization of inorganic and organic sediments and the interaction of the flow with the Blanco River bridge.

Abstract Image

Chaitén 是智利巴塔哥尼亚的一座城市,2008 年 5 月,在一次大规模火山爆发后,该市遭到布兰科河泻流的袭击。这一级联过程导致布兰科河活动河道被冲毁,城市被分成两部分,建筑环境遭到破坏,当地居民流离失所。该地区的水动力研究一般都是基于洪灾后的环境条件。但是,还没有对水动力行为和相关河流动力学进行详尽的重建。更重要的是,还没有提出明确的方法来完成这项任务。本研究针对这些挑战,采用非常规方法重建事件的初始条件和边界条件,并追溯对远端河段水文地质调整产生决定性影响的干扰因素。通过收集第一手资料和第二手资料(采用混合方法和信息三角测量法),重建了事件的初始条件和边界条件。生成了 2008 年 5 月布兰科河水文地貌演变的概念模型,阐明了降雨和形态动力学反应在布兰科河中的作用和影响,并强调了布兰科河大桥的水力行为。通过对水文地质过程的详细重建,可以证实河道反应并不完全是火山爆发造成的,而是大量泥沙注入河道系统、降水脉冲的强度和空间性(与锋面系统和大气河流的存在有关)、无机和有机沉积物的移动以及水流与布兰科河桥的相互作用共同作用的结果。
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来源期刊
Journal of South American Earth Sciences
Journal of South American Earth Sciences 地学-地球科学综合
CiteScore
3.70
自引率
22.20%
发文量
364
审稿时长
6-12 weeks
期刊介绍: Papers must have a regional appeal and should present work of more than local significance. Research papers dealing with the regional geology of South American cratons and mobile belts, within the following research fields: -Economic geology, metallogenesis and hydrocarbon genesis and reservoirs. -Geophysics, geochemistry, volcanology, igneous and metamorphic petrology. -Tectonics, neo- and seismotectonics and geodynamic modeling. -Geomorphology, geological hazards, environmental geology, climate change in America and Antarctica, and soil research. -Stratigraphy, sedimentology, structure and basin evolution. -Paleontology, paleoecology, paleoclimatology and Quaternary geology. New developments in already established regional projects and new initiatives dealing with the geology of the continent will be summarized and presented on a regular basis. Short notes, discussions, book reviews and conference and workshop reports will also be included when relevant.
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