Groundwater-surface water interactions and resilience to hydrological extremes in a data-sparse arid transboundary river basin: Insights from collaborative groundwater modelling.

IF 2.8 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Hydrogeology Journal Pub Date : 2026-01-01 Epub Date: 2026-08-14 DOI:10.1007/s10040-026-03143-x
Syed Md Touhidul Mustafa, Jean-Christophe Comte, Fulvio Franchi, Alessia Matano, Anne F Van Loon, Sithabile Tirivarombo, Luis Artur, Zareen Bharucha, Annatoria Chinyama, Farisse Chirindja, Rosie Day, Joyce Dube, Stephen Hussey, Edward Nesamvuni, Wandile Nomquphu, Oluwaseun Olabode, Melanie Rohse, Simon Taylor, Jarmo de Vries
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引用次数: 0

Abstract

Sustainable groundwater management is key to building resilience to hydrological extremes but remains challenging in data-scarce transboundary river basins. In this study, a transboundary, collaborative, physically based groundwater modelling approach has been developed for the Limpopo River Basin (LRB), which is highly vulnerable to floods and droughts. Monitoring data and model results consistently suggest that prolonged wet periods and floods significantly raised groundwater levels, whereas prolonged droughts decreased them, particularly in the upstream and central regions of the basin characterized by low-storage fractured bedrock aquifers. Groundwater-surface water interactions are greater downstream, where water tables are shallower in unconsolidated superficial materials, and intensify during floods, especially in the central region. Modelling results also suggest that baseflow is less responsive to extremes than groundwater recharge across the LRB, highlighting the groundwater system's attenuation capacity. The model was subsequently used to assess and discuss a series of co-created management scenarios focused specifically on improving groundwater storage during wet periods for use during dry periods. They included: (1) managed aquifer recharge (MAR), using (1a) injection well(s) next to large dams, (1b) rainwater and runoff harvesting (RRH) and infiltration through local wells, (1c) RRH through local ponds and (1d) small reservoirs (e.g. sand dams); (2) deforestation; (3) afforestation; and (4) increased groundwater abstraction. Scenarios suggest that strategy (1b), when widely applied across the basin, may be the most effective to reduce the risk and impact of floods, droughts, and groundwater depletion by supporting the maintenance of groundwater levels and baseflow, while reducing storm runoff.

Supplementary information: The online version contains supplementary material available at https://doi.org/10.1007/s10040-026-03143-x.

在数据稀疏的干旱跨界河流流域,地下水-地表水相互作用和对极端水文的恢复力:来自协作地下水模型的见解。
可持续地下水管理是建立应对水文极端情况能力的关键,但在数据匮乏的跨界河流流域仍然具有挑战性。在这项研究中,针对林波波河流域(LRB)开发了一种跨界、协作、基于物理的地下水建模方法,该流域极易受到洪水和干旱的影响。监测数据和模型结果一致表明,长时间的湿润期和洪水显著提高了地下水位,而长时间的干旱则降低了地下水位,特别是在以低蓄水裂隙基岩含水层为特征的流域上游和中部地区。地下水-地表水的相互作用在下游更大,在松散的表层物质中地下水位较浅,并且在洪水期间加剧,特别是在中部地区。模拟结果还表明,与地下水补给相比,基底流对极端条件的响应较小,这突出了地下水系统的衰减能力。该模型随后被用于评估和讨论一系列共同创建的管理方案,这些方案的重点是改善湿润期的地下水储存,以便在干旱期使用。它们包括:(1)管理含水层补给(MAR),在大型水坝旁边使用(1a)注入井(s), (1b)雨水和径流收集(RRH)和通过当地井渗透,(1c)通过当地池塘的RRH和(1d)小型水库(例如沙坝);(2)森林砍伐;(3)绿化;(4)增加地下水采掘。情景表明,当策略(1b)在整个流域广泛应用时,通过支持维持地下水位和基流,同时减少暴雨径流,可能最有效地减少洪水、干旱和地下水枯竭的风险和影响。补充信息:在线版本包含补充资料,可在https://doi.org/10.1007/s10040-026-03143-x上获得。
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
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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