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斯里兰卡干旱地区古代人造乡村蓄水池梯级系统(VTCSs)中地表水与地下水之间的水文相互作用。

Hydrological interactions between surface water and groundwater in ancient manmade village tank cascade systems (VTCSs) in the dry zone of Sri Lanka.

作者信息

Indika Suresh, Hu Dazhou, Wei Yuansong, Yapabandara Isuru, Athauda Samadhi, Randika Ashen, Prasad Sangeeth, Cooray Titus, Makehelwala Madhubhashini, Zhong Hui, Wang Yawei, Jinadasa K B S N, Weragoda Sujithra K, Weerasooriya Rohan

机构信息

State Key Joint Laboratory of Environmental Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; Laboratory of Water Pollution Control Technology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; University of Chinese Academy of Sciences, Beijing 100049, China; China-Sri Lanka Joint Research and Demonstration Center for Water Technology, Ministry of Water Supply, Meewathura, Peradeniya 20400, Sri Lanka; Department of Chemical and Process Engineering, University of Peradeniya, Peradeniya 20400, Sri Lanka.

State Key Joint Laboratory of Environmental Simulation and Pollution Control, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; Laboratory of Water Pollution Control Technology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; University of Chinese Academy of Sciences, Beijing 100049, China; Fujian Governmental Investment Projects Appraisal, Fuzhou 350000, China.

出版信息

Sci Total Environ. 2024 Dec 1;954:176526. doi: 10.1016/j.scitotenv.2024.176526. Epub 2024 Sep 24.

Abstract

Sri Lanka, a tropical island, confronts climate-driven water scarcity and is of great concern to building climate-resilient water management to achieve UN SDGs 6 and 13. This study explores the dynamic interaction between surface water (SW) and groundwater (GW) in the dry zone of Sri Lanka, employing a multi-tracer of dual stable isotopes (O and H) and chloride. Two basins, Mahakanadarawa (MK) basin with numerous village tanks and tank cascade systems (VTCSs/TCSs) and Kawudulla (KW) basin serving as a control with a lack of tanks, were selected in this study. Results show that the presence or absence of TCSs emerges as a pivotal factor influencing regional water dynamics. Water quality (TDS and Cl) in natural waters between the two basins was significantly different (ANOVA: p < 0.05) in both seasons. Statistically uniform dissolved mineral content in tanks and shallow groundwater in the MK basin contrasted with significant regional deviation in the KW basin. ANOVA and Tukey tests showed significant seasonal differences (p < 0.05) in mean values of ẟH and ẟO compositions of shallow groundwater and tank water within the MK basin, while non-significance in the KW basin. Isotopic mass balance calculations revealed that tank water mixing in the shallow groundwater (f: mixed Tank water mass fraction) ranged from 0.9 % to 77.8 % across the MK basin depending on the regional soil characteristics. Lack of tank-aquifer interconnection observed in the shallow soil in rock knob plain results in groundwater depletion while enhanced interconnections within alluvial sediment regions encourage stable and pollution-resistant shallow groundwater bodies. The consistency of the groundwater flow system in TCS regions throughout the year ensures a stable water supply, highlighting the vital synergy between TCSs and regional groundwaters in these arid regions. These results shed insights for policymakers and water managers to implement effective conservation strategies for rehabilitation and restoring these ancient VTCSs/TCSs.

摘要

斯里兰卡是一个热带岛屿,面临着气候驱动的水资源短缺问题,因此建立具有气候适应力的水资源管理对于实现联合国可持续发展目标6和13至关重要。本研究利用双稳定同位素(氧和氢)和氯的多示踪剂,探讨了斯里兰卡干旱地区地表水(SW)与地下水(GW)之间的动态相互作用。本研究选取了两个流域,一个是马哈卡纳达拉瓦(MK)流域,有众多乡村水罐和水罐梯级系统(VTCSs/TCSs),另一个是卡武杜拉(KW)流域作为对照,该流域没有水罐。结果表明,TCSs的存在与否是影响区域水动态的关键因素。两个流域天然水体中的水质(总溶解固体和氯)在两个季节均存在显著差异(方差分析:p < 0.05)。MK流域水罐和浅层地下水中的溶解矿物质含量在统计上较为均匀,这与KW流域明显的区域偏差形成对比。方差分析和Tukey检验表明,MK流域浅层地下水和水罐水的δH和δO组成平均值存在显著季节性差异(p < 0.05),而KW流域则不显著。同位素质量平衡计算表明,根据区域土壤特征,MK流域浅层地下水中水罐水的混合比例(f:混合水罐水质量分数)在0.9%至77.8%之间。在岩丘平原浅层土壤中观察到水罐与含水层缺乏连通性导致地下水枯竭,而冲积沉积区内部增强的连通性则促进了稳定且抗污染的浅层地下水体的形成。TCS区域全年地下水流动系统的一致性确保了稳定的供水,凸显了这些干旱地区TCSs与区域地下水之间至关重要的协同作用。这些结果为政策制定者和水资源管理者实施有效的保护策略以修复和恢复这些古老的VTCSs/TCSs提供了见解。

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