Morfometría de una cuenca de los Andes Centrales, San Juan, Argentina: evaluación de los factores condicionantes del terreno a la ocurrencia de aluviones

IF 0.9 4区 地球科学 Q3 GEOLOGY
Natalia Noemí Rios, Carla Ginesta Torcivia, M. R. Onorato, Valeria Sofia Cortez Taillant, María Yanina Esper Angillieri
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引用次数: 0

Abstract

The present work aims to determine flash flood occurrence prone areas, in the Jáchal river basin, San Juan Province, Argentina. The Jáchal river basin covers ~29,000 km2 and has a perimeter of ~2,400 km, while the eponymous river extends for nearly 570 km. It is a 7th order basin according to Strahler’s classification, subdivided into four 6th order sub-basins. Various morphometric basin characteristics are analysed and some basic and derived parameters are calculated. These calculations allow predicting the basin behaviour due to heavy rainfall, which translates into large volumes of water with peak flows capable of generating significant flash floods. The basin has a torrential character, so in case of intense rainfall the terrain conditions would contribute to increasing the flow of the main rivers. An inventory of alluvial deposits was carried out and their relationship with the conditioning variables of the terrain was evaluated. At the confluence zones, the river tributaries show more intense overflows than the main collector. This promotes the generation of flash floods. The areas most likely to be affected by flash flood events correspond to low-humidity, east-facing slightly rough terrains, with slopes of up to 15° as well as low-lying flood plain sectors, and at the confluence of tributaries with the main rivers. Populated centres and provincial and national routes are prone to be affected by alluvial events in the study area.
阿根廷圣胡安中安第斯山脉盆地的形态测量:评估冲积层出现的地形条件因素。
本研究旨在确定阿根廷圣胡安省 Jáchal 河流域的山洪易发区。贾查尔河流域面积约为 29,000 平方公里,周长约为 2,400 公里,同名河流绵延近 570 公里。根据 Strahler 的分类,该流域属于七级流域,又细分为四个六级子流域。分析了流域的各种形态特征,并计算了一些基本参数和衍生参数。通过这些计算结果,可以预测流域在暴雨情况下的表现,暴雨会产生大量的水,其峰值流量能够引发严重的山洪暴发。该流域具有暴雨特征,因此在强降雨情况下,地形条件将有助于增加主要河流的流量。对冲积层进行了清查,并评估了它们与地形条件变量之间的关系。在汇流区,河流支流的溢流比主要集水区更为剧烈。这促进了山洪的产生。最有可能受到山洪暴发影响的地区是湿度低、地势略微崎岖、坡度达 15° 的东向地区,以及低洼的洪泛平原区和支流与主要河流的汇合处。研究区域内的人口中心、省道和国道容易受到冲积事件的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Andean Geology
Andean Geology 地学-地质学
CiteScore
3.90
自引率
0.00%
发文量
17
审稿时长
>12 weeks
期刊介绍: This journal publishes original and review articles on geology and related sciences, in Spanish or English, in three issues a year (January, May and September). Articles or notes on major topics of broad interest in Earth Sciences dealing with the geology of South and Central America and Antarctica, and particularly of the Andes, are welcomed. The journal is interested in publishing thematic sets of papers and accepts articles dealing with systematic Paleontology only if their main focus is the chronostratigraphical, paleoecological and/or paleogeographical importance of the taxa described therein.
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