阿根廷萨拉多-朱拉门托巨型河漫滩远端平原的含水层系统:地质、水文地质和数值模型的综合方法

IF 2.4 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Maria Belen Thalmeier, Leticia Rodríguez, Javier Heredia, Daniela Kröhling, Ernesto Brunetto
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引用次数: 0

摘要

对阿根廷大平原 Bajos Submeridionales(BBSS)的水文地质系统仍然了解不足。Bajos Submeridionales 位于南美洲大查科平原(Gran Chaco Plain)最大的巨型河床之一的远端。BBSS 人口稀少,经常受到极端干旱和洪水事件的影响,给社区和经济生产造成严重问题。这项研究旨在通过为该地区开发首个综合水文地质模型,提高目前对该系统的水文地质认识。BBSS 水文地质系统在区域范围内表现出相对简单的水力行为。四个水文地质单元(HU)的定义基于对该地区沉积柱的简化,代表了地下水流动态的基本特征、它们之间的相互联系以及通过直接补给与地表水体和大气之间的相互作用。由于缺乏可用的瞬态数据,水文地质概念模型在稳态流动状态下进行了数值测试。数值模型有助于检验拟议概念模型的合理性,并评估整个含水层系统的水平衡组成部分。数值模型强调了溪流与含水层相互作用作为主要排泄机制的作用,以及 HU 之间发生的水流交换。新安装的地下水监控网络将支持未来的瞬态模拟,以研究系统的时间演变,并探索管理干预措施,以实现环境可持续性标准。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

The aquifer system of the Salado-Juramento fluvial megafan distal plain, Argentina: an integrated approach of geological, hydrogeological and numerical models

The aquifer system of the Salado-Juramento fluvial megafan distal plain, Argentina: an integrated approach of geological, hydrogeological and numerical models

The hydrogeological system of the Bajos Submeridionales (BBSS), a large plain in Argentina, remains insufficiently understood. The BBSS is located in the distal part of one of the largest fluvial megafans in the Gran Chaco Plain, South America. The BBSS is sparsely populated and frequently affected by extreme drought and flood events that cause severe problems to communities and economic production. This research aims to improve the current hydrogeologic understanding of the system through the development of the first integrated hydrogeological model for the region. The BBSS hydrogeological system exhibits a relatively simple hydraulic behavior at a regional scale. The definitions of four hydrogeological units (HU) were based on the simplification of the sedimentary column for the area, representing the fundamental characteristics of the dynamics of groundwater flows, their interconnections and the interactions with surface-water bodies and the atmosphere through direct recharge. Due to the lack of available transient data, the hydrogeological conceptual model was numerically tested under a steady-state flow regime. The numerical model was instrumental to test the plausibility of the proposed conceptual model and evaluate the water balance components for the entire aquifer system. The numerical model highlighted the role of stream/aquifer interaction as a primary discharge mechanism and the occurrence of flow exchanges between HUs. A newly installed groundwater monitolring network will support future transient simulations to investigate the temporal evolution of the system and explore management interventions to achieve environmental sustainability criteria.

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来源期刊
Hydrogeology Journal
Hydrogeology Journal 地学-地球科学综合
CiteScore
5.40
自引率
7.10%
发文量
128
审稿时长
6 months
期刊介绍: Hydrogeology Journal was founded in 1992 to foster understanding of hydrogeology; to describe worldwide progress in hydrogeology; and to provide an accessible forum for scientists, researchers, engineers, and practitioners in developing and industrialized countries. Since then, the journal has earned a large worldwide readership. Its peer-reviewed research articles integrate subsurface hydrology and geology with supporting disciplines: geochemistry, geophysics, geomorphology, geobiology, surface-water hydrology, tectonics, numerical modeling, economics, and sociology.
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