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Integrating deep learning and groundwater dynamics for drought vulnerability assessment under climate scenarios 基于深度学习和地下水动力学的气候情景下干旱脆弱性评估
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2026-05-01 Epub Date: 2026-02-05 DOI: 10.1016/j.gsd.2026.101591
Wei Sun , Li-Chiu Chang , Jun Jie Lin , Fi-John Chang
Drought increasingly threatens agricultural sustainability, particularly in groundwater-dependent regions where irrigation and aquifer recharge are closely linked. Taiwan's Zhuoshui River alluvial fan exemplifies this risk: long-term intensive pumping and rising climate extremes have amplified drought vulnerability. Yet most existing drought indices treat groundwater implicitly, and many AI studies focus on groundwater prediction without translating results into integrated vulnerability metrics. This study develops an AI-driven framework to assess future drought risk from climate, groundwater, and socio-environmental drivers. Groundwater level was predicted using a hybrid Convolutional Neural Network–Backpropagation model (CNN-BP) calibrated with 22 years of basin-wide gridded precipitation, temperature, and SPI data, together with groundwater levels from 18 monitoring wells. CNN-BP outperforms a BPNN benchmark, improving the correlation coefficient by 35.85% and reducing MAE by 19.51%, enabling robust projections for 2021–2100. These groundwater forecasts are then integrated with climatic (SPI), physiographic (soil, land use, elevation, slope, distance to river) and socio-economic (population) drivers to construct the Deep Learning-based Comprehensive Drought Vulnerability Indicator (DCDVI) under SSP1-2.6 and SSP5-8.5. Scenario results indicate consistent intensification of drought vulnerability relative to the historical baseline. SSP1-2.6 yields milder drought conditions and slower groundwater decline, while SSP5-8.5 leads to stronger drying and higher vulnerability. Under SSP5-8.5, highly vulnerable areas increase from 27.31% to 41.26% by 2081–2100. Overall, DCDVI provides a scalable, climate-responsive indicator that converts AI-based groundwater forecasts into actionable vulnerability maps. The framework provides a transferable decision-support tool for drought-prone, groundwater-reliant farming systems under climate change.
干旱日益威胁到农业的可持续性,特别是在灌溉和含水层补给密切相关的依赖地下水的地区。台湾的涿水河冲积扇就是这种风险的例证:长期的密集抽水和日益加剧的极端气候加剧了干旱的脆弱性。然而,大多数现有的干旱指数都隐含地处理地下水,许多人工智能研究侧重于地下水预测,而没有将结果转化为综合脆弱性指标。本研究开发了一个人工智能驱动的框架,以评估气候、地下水和社会环境驱动因素带来的未来干旱风险。地下水水位预测使用卷积神经网络-反向传播混合模型(CNN-BP),该模型使用22年全流域网格降水、温度和SPI数据以及18口监测井的地下水水位进行校准。CNN-BP优于BPNN基准,相关系数提高了35.85%,MAE降低了19.51%,实现了2021-2100年的鲁棒预测。然后将这些地下水预测与气候(SPI)、地理(土壤、土地利用、高程、坡度、到河流的距离)和社会经济(人口)驱动因素相结合,构建SSP1-2.6和SSP5-8.5下基于深度学习的综合干旱脆弱性指数(DCDVI)。情景结果表明,相对于历史基线,干旱脆弱性持续增强。SSP1-2.6的干旱程度较轻,地下水下降速度较慢,而SSP5-8.5的干旱程度较强,脆弱性较高。在SSP5-8.5条件下,2081-2100年高度脆弱区面积由27.31%增加到41.26%。总体而言,DCDVI提供了一个可扩展的气候响应指标,将基于人工智能的地下水预测转化为可操作的脆弱性图。该框架为气候变化下易干旱、依赖地下水的农业系统提供了一个可转移的决策支持工具。
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引用次数: 0
Groundwater salinization and anthropogenic pollution imprints revealed by unsupervised learning in Ho Chi Minh city 胡志明市地下水盐渍化与人为污染的无监督学习研究
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2026-05-01 Epub Date: 2026-01-30 DOI: 10.1016/j.gsd.2026.101589
Quang Khai Ha , Ba Loc Tran , Van Qui Lai
Groundwater resources in urban coastal regions are increasingly threatened by the interacting pressures of aquifer salinization and anthropogenic pollution, undermining freshwater security and long-term urban resilience. This study applies an integrated framework of unsupervised learning techniques including Principal Component Analysis (PCA), Self-Organizing Maps (SOM), K-means clustering, and Hierarchical Cluster Analysis (HCA) to evaluate the hydrogeochemical characteristics of 441 groundwater samples collected across Ho Chi Minh City (HCMC), Vietnam's largest coastal megacity. Analytical results reveal that 72 % of groundwater samples exhibit a pH below 6.5, while concentrations of Fe, Cl, and NH4 exceed national drinking water standards in 32 %, 9 %, and 8 % of samples, respectively. The study found that land use, geology and elevation are important factor controlling groundwater quality. Multivariate analysis indicates that groundwater chemistry is primarily influenced by salinization, weathering, nitrification-induced acidification, organic matter decomposition, and sulfide mineral oxidation. Clustering analysis identified five groundwater groups. Groups 1 (fresh to brackish water), 2 (acidic saline water), and 3 (fresh groundwater) are concentrated in lowland areas. Group 4 (elevated NO3 and low pH) heavily affected by anthropogenic contamination sources, is in densely developed zones, whereas Group 5 (dilute, high-quality water) is found in high permeable and less developed highland areas. The results demonstrate that the SOM–HCA approach provides added value by producing more spatially coherent and hydrogeochemically realistic groundwater groupings. These findings underscore the value of unsupervised learning for groundwater assessment and call for local specific strategy for groundwater management: conservation for Groups 3 and 5, pollution control for Group 4, and salinity mitigation for Groups 1 and 2. This study provides a data-driven basis for sustainable groundwater resource management in vulnerable coastal cities.
城市沿海地区地下水资源日益受到含水层盐渍化和人为污染相互作用的威胁,破坏了淡水安全和城市的长期复原力。本研究采用主成分分析(PCA)、自组织图(SOM)、k均值聚类和层次聚类分析(HCA)等无监督学习技术的综合框架,对越南最大的沿海大城市胡志明市(HCMC)的441个地下水样本的水文地球化学特征进行了评估。分析结果显示,72%的地下水样品pH值低于6.5,而铁、氯和氨的浓度分别在32%、9%和8%的样品中超过国家饮用水标准。研究发现,土地利用、地质和高程是控制地下水水质的重要因素。多变量分析表明,地下水化学主要受盐渍化、风化、硝化酸化、有机质分解和硫化物矿物氧化等因素的影响。聚类分析确定了5个地下水类群。第1组(淡水至微咸水)、第2组(酸性盐水)和第3组(淡水地下水)集中在低地地区。受人为污染源严重影响的第4组(NO3升高和低pH值)位于人口密集的地区,而第5组(稀释的高质量水)位于高渗透性和欠发达的高原地区。结果表明,SOM-HCA方法通过产生更多空间相干性和水文地球化学真实的地下水分组提供了附加价值。这些发现强调了无监督学习对地下水评估的价值,并呼吁制定当地具体的地下水管理战略:保护第3和第5组,控制第4组的污染,减少第1和第2组的盐度。本研究为沿海脆弱城市地下水资源可持续管理提供了数据驱动依据。
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引用次数: 0
Long-term flood control in central Japan: A half-century groundwater monitoring and evaluating adaptation measures for sustainable use 日本中部的长期洪水控制:半个世纪的地下水监测和评估可持续利用的适应措施
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2026-05-01 Epub Date: 2026-01-31 DOI: 10.1016/j.gsd.2026.101585
Saki Nishizawa Katazakai , Jing Zhang
Groundwater depletion and quality degradation are accelerating worldwide under pressures from groundwater abstraction, land-use transitions, and climate-driven shifts in recharge. Monsoon Asia, responsible for nearly two-thirds of global freshwater withdrawals, is particularly vulnerable. At the eastern frontier of the Asian Monsoon, Japan has historically experienced groundwater crises, making it a valuable reference for anticipatory groundwater governance. This study identifies groundwater origins, quantifies recharge sources, and provides the first empirical estimate of how long-term flood-control strategies, including riverbed excavation and subsequent regulation, have influenced groundwater. Analysis combined half a century of literature with 20 years of shallow groundwater monitoring data, revealing a long-term shift in recharge pathways from river infiltration toward surface-derived inputs following riverbed excavation, with approximately 80 % of monitoring sites now exhibiting significant surface-derived recharge. A groundwater recharge project (GRP) utilizing fallow paddy fields is predicted to secure future groundwater supplies locally, and scaling seasonal GRPs nationally could potentially satisfy a fraction of Japan's freshwater demand. These findings highlight the critical role of sustained monitoring in detecting human-driven shifts in recharge dynamics and demonstrate that strategically managed agricultural land offers a flexible, transferable measure for groundwater security. Japan's experience provides actionable insight into emerging groundwater challenges across monsoon Asia and other groundwater-dependent regions, offering evidence-based guidance for integrating flood-control policies with long-term water resource management.
在地下水开采、土地利用转变和气候驱动的补给变化的压力下,世界范围内的地下水枯竭和质量退化正在加速。季风亚洲占全球淡水提取量的近三分之二,尤其脆弱。在亚洲季风的东部边界,日本历史上经历过地下水危机,这使其成为预期地下水治理的有价值的参考。本研究确定了地下水的来源,量化了补给来源,并首次提供了长期洪水控制策略(包括河床开挖和随后的调节)对地下水的影响的经验估计。分析结合了半个世纪的文献和20年的浅层地下水监测数据,揭示了河床开挖后补给途径从河流入渗向地表补给的长期转变,目前约80%的监测点显示出显著的地表补给。一个利用休耕水田的地下水补给项目(GRP)预计将确保当地未来的地下水供应,而在全国范围内扩大季节性GRP可能会满足日本淡水需求的一小部分。这些发现强调了持续监测在发现人类驱动的补给动态变化方面的关键作用,并表明战略性管理的农业用地为地下水安全提供了一种灵活、可转移的措施。日本的经验为亚洲季风地区和其他地下水依赖地区正在出现的地下水挑战提供了可行的见解,为将防洪政策与长期水资源管理相结合提供了基于证据的指导。
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引用次数: 0
Mapping uncertainty in managed aquifer recharge potential across unconfined and confined aquifers of the Murray-Darling Basin Murray-Darling盆地非承压和承压含水层管理含水层补给潜力的测绘不确定性
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2026-05-01 Epub Date: 2026-01-18 DOI: 10.1016/j.gsd.2026.101579
Dennis Gonzalez , Joseph H.A. Guillaume , Luk Peeters
The global decline in groundwater levels, particularly in agricultural regions, underscores the imperative for sustainable management practices augmented through managed aquifer recharge (MAR). This study evaluated the potential for MAR in Australia's Murray-Darling Basin (MDB), identifying substantial areas conducive to recharge across regions experiencing long-term groundwater decline. Novel methods were developed to quantitatively assess potential recharge in unconfined and confined aquifers based on aquifer properties and account for uncertainty presenting a contrast to deterministic, weight-based spatial multi-criteria analyses. This investigation revealed that specific areas, including the Lower Namoi Alluvium and Goulburn-Murray Sedimentary Plain, exhibit higher recharge potential with 5–20 ML/ha feasible in unconfined aquifer systems at high confidence. Furthermore, this study found extensive areas at high confidence where the injection potential in confined aquifers ranged from 2.5–20 ML/d. The findings suggest that resource units characterized by high potential recharge areas and elevated resource stress values may benefit from MAR implementation, thereby mitigating stress and supporting more sustainable groundwater use. The economic viability of MAR is contingent upon various factors highlighting the need for tailored project design and site-specific assessments to ensure successful implementation. These results have significant implications for informing MAR implementation and future management strategies in the MDB.
全球地下水位下降,特别是在农业地区,凸显了通过管理含水层补给(MAR)加强可持续管理做法的必要性。本研究评估了澳大利亚墨累-达令盆地(MDB)的MAR潜力,确定了有利于在地下水长期下降的地区进行补给的实质性区域。开发了基于含水层性质定量评估无承压和承压含水层潜在补给的新方法,并考虑了与确定性、基于权重的空间多准则分析不同的不确定性。该研究表明,包括Lower Namoi冲积层和Goulburn-Murray沉积平原在内的特定区域,在无承压含水层系统中具有较高的回灌潜力,高置信度可达5-20 ML/ha。此外,该研究还发现,承压含水层的注入潜力范围在2.5-20 ML/d之间,具有高置信度。研究结果表明,具有高潜在补给区和高资源压力值特征的资源单元可能受益于MAR的实施,从而减轻压力并支持更可持续的地下水利用。海洋资源评估的经济可行性取决于各种因素,这些因素强调需要有针对性的项目设计和具体地点评估,以确保成功实施。这些结果对多边开发计划署的实施和未来管理战略具有重要意义。
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引用次数: 0
Groundwater depletion and sustainability of water-intensive agriculture in the Cuatro Ciénegas region, Coahuila, Mexico 墨西哥科阿韦拉Cuatro cisamnegas地区的地下水枯竭和水密集型农业的可持续性
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2026-05-01 Epub Date: 2026-01-20 DOI: 10.1016/j.gsd.2026.101583
Adrián Pedrozo-Acuña , Marco Rodrigo López-López , José Agustín Breña-Naranjo , Edgar Yuri Mendoza-Cázares
This study aims to investigate the relationship between groundwater depletion and intensive agricultural practices in the Cuatro Ciénegas region, a water-scarce area in Mexico. Data from an extensive field campaign along with remotely sensed data is utilised. Focus is given on regional groundwater flow and the hydrogeological interconnectivity of aquifers in and around Cuatro Ciénegas, alongside the temporal variations in water levels, agricultural frontiers, and projected water consumption for the main crops in the region. Isotope analysis of water samples reveals hydrological connectivity between the Cuatro Ciénegas-Ocampo and Cuatro Ciénegas aquifers, suggesting that agricultural activities above these aquifers threaten aquatic ecosystems. Temporal variations in water levels, obtained from in-situ measurements and the Gravity Recovery and Climate Experiment (GRACE) mission, indicate a decline in groundwater across all aquifers: Cuatro Ciénegas-Ocampo (−37.45 m from 2001 to 2023), Cuatro Ciénegas (−24.23 m from 2005 to 2023), and El Hundido (−20.17 m from 2005 to 2023). The agricultural frontier in the Cuatro Ciénegas-Ocampo and El Hundido aquifers increased by 63 % and 68 %, respectively, from 2003 to 2023. Agricultural activity in the Cuatro Ciénegas aquifer, which contains the nature reserve, decreased by 7.6 %. Groundwater depletion is associated with water-intensive agriculture in the area. Since 2011, the relationship between cropland expansion and groundwater use has exacerbated water stress. Groundwater withdrawals from the three aquifers for primary crop production have surpassed their recharge capacity, leading to groundwater depletion. An urgent need exists for sustainable groundwater extraction and aquifer restoration.
本研究旨在调查墨西哥缺水地区Cuatro ci内加斯地区地下水枯竭与集约化农业实践之间的关系。从广泛的实地活动中获得的数据以及遥感数据被利用。重点是区域地下水流动和Cuatro cisamnegas及其周围含水层的水文地质相互联系,以及水位、农业边界和该地区主要作物的预计用水量的时间变化。水样的同位素分析揭示了Cuatro cisamenas - ocampo和Cuatro cisamengas含水层之间的水文连通性,表明这些含水层上方的农业活动威胁着水生生态系统。从原位测量和重力恢复和气候实验(GRACE)任务中获得的水位时间变化表明,所有含水层的地下水都在下降:2001年至2023年,Cuatro ci内加斯-奥坎波(- 37.45 m), 2005年至2023年,Cuatro ci内加斯(- 24.23 m), 2005年至2023年,El Hundido (- 20.17 m)。从2003年到2023年,Cuatro ci内加斯-奥坎波和El Hundido含水层的农业边界分别增加了63%和68%。包含自然保护区的Cuatro cisamnegas含水层的农业活动减少了7.6%。地下水枯竭与该地区的用水密集型农业有关。自2011年以来,耕地扩张与地下水利用之间的关系加剧了水资源压力。用于初级作物生产的地下水从三个含水层中抽取的水量已超过其补给能力,导致地下水枯竭。迫切需要可持续的地下水开采和含水层恢复。
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引用次数: 0
Nitrate pollution in the shallow groundwater of a rapidly urbanizing coastal area: Insight from spatial-seasonal distribution and source identification in Xiamen, China 沿海快速城市化地区浅层地下水硝酸盐污染:来自空间-季节分布和来源识别的启示
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2026-05-01 Epub Date: 2026-01-21 DOI: 10.1016/j.gsd.2026.101582
Xiang Li , Xiangke Kong , Xiongguang Li , Ximing Luo , Shengwei Cao , Xiujian Hu , Yasong Li , Yinglan Cao
Nitrate (NO3) pollution in groundwater has become an increasingly serious problem in rapidly urbanized coastal areas. However, the complex hydrogeology and intensive human activities complicate the identification of NO3 sources and pollution characteristics, constraining the groundwater resources protection. This study investigated the spatial-seasonal distribution and origin of NO3 in 39 shallow groundwater wells across diverse land-use types during both wet and dry seasons in Xiamen, a typical coastal city in China. Results showed 48.7 % of groundwater samples exceeded the WHO guideline of 11.3 mg/L NO3-N. High NO3 concentration greatly affected the hydrochemical types, with 32 % of samples classified as NO3-N (meq % ≥ 25) dominant groundwater. Significant spatiotemporal variations in NO3 concentrations were observed across various land-use types. Notably, all samples exceeding the 11.3 mg/L NO3-N threshold clustered within a 10 km coastal zone of high population density. Spearman's rank correlation analysis revealed positive correlations (p < 0.05) among NO3, Cl, and SO42−, suggesting a clear anthropogenic impact on groundwater quality. Nitrate and sulfate stable isotope analysis indicated sewage and manure (MS) as the primary NO3 sources. The Bayesian mixing model further quantified the MS contributions (69.7 % ± 11.7 % in wet season, 90.9 % ± 11.5 % in dry season), followed by soil nitrogen and chemical fertilizers. Nitrification was the predominant microbial process responsible for NO3 accumulation in groundwater. This study demonstrates that integrating land-use patterns with hydrochemical and isotopic data provides an effective strategy for identifying the origins of NO3 pollution in urbanized coastal aquifers.
在快速城市化的沿海地区,地下水中硝酸盐(NO3−)污染问题日益严重。然而,复杂的水文地质和密集的人类活动使NO3−来源和污染特征的识别复杂化,制约了地下水资源的保护。以厦门为研究对象,研究了不同土地利用类型下39口浅层地下水井干湿季节NO3−的时空分布特征及来源。结果显示,48.7%的地下水样本NO3−-N超标11.3 mg/L。高NO3−浓度对水化学类型影响较大,32%的样品属于NO3−-N (meq %≥25)为主的地下水。不同土地利用类型NO3−浓度存在显著的时空差异。值得注意的是,所有超过11.3 mg/L NO3−-N阈值的样本都集中在人口密度高的沿海10公里区域内。Spearman秩相关分析显示NO3−、Cl−和SO42−之间呈正相关(p < 0.05),表明人类活动对地下水质量有明显影响。硝酸盐和硫酸盐稳定同位素分析表明,污水和粪肥是NO3−的主要来源。贝叶斯混合模型进一步量化了MS的贡献(雨季为69.7%±11.7%,旱季为90.9%±11.5%),其次是土壤氮和化肥。硝化作用是地下水NO3−积累的主要微生物过程。该研究表明,将土地利用模式与水化学和同位素数据相结合,为确定城市化沿海含水层NO3−污染的来源提供了一种有效的策略。
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引用次数: 0
Groundwater transit time distributions in the Pampean loess of Argentina: Insights from a multi-tracer approach (85Kr, CFCs, SF6, 3H/3He and 39Ar) 阿根廷潘潘黄土地下水运移时间分布:基于多示踪剂(85Kr、CFCs、SF6、3H/3He和39Ar)的研究
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2026-05-01 Epub Date: 2026-02-10 DOI: 10.1016/j.gsd.2026.101593
Alejandro Basaldúa , Daniel Martínez , Douglas Kip Solomon , Takuya Matsumoto , Zheng-Tian Lu , Mauricio Quiroz-Londoño , Emiliano Alcaraz , Guo-Min Yang , Wei Jiang
Groundwater transit times in the unconfined to semi-confined Pampeano aquifer were assessed using eight environmental tracers (85Kr, 39Ar, CFC-11, CFC-12, CFC-113, SF6, 3H and tritiogenic 3He) measured in 17 piezometers at different depths in southeastern Buenos Aires Province, Argentina. Age distributions were derived by inverse modeling with lumped parameter models (LPMs) and the tracers’ historical input functions. Results indicate slow and complex groundwater flow, with a wide range of ages and older water than expected for a simple unconfined aquifer conceptual model. Between 0 and 10 m below the water table, 35% of groundwater lacks young groundwater tracers (ages > ∼60 years); between 10 and 20 m, over 60%; and below 30 m, more than 99%. A single 39Ar measurement at 22–48 m depth indicates a mean age of 170 years, though this is likely an underestimate. Inverse modeling of 3H, 3He and 3H/3H0 ratios suggests unsaturated zone transit times ranging from 3 to 37 years, exceeding estimates based on simple advective calculations and pointing to retarding layers and preferential winter recharge. These findings highlight the role of dispersion, sedimentological heterogeneity and low-permeability horizons in controlling groundwater age and recharge, with implications for contaminant vulnerability and resource sustainability.
利用阿根廷布宜诺斯艾利斯东南部不同深度的17个气压计测得的8种环境示踪剂(85Kr、39Ar、CFC-11、CFC-12、CFC-113、SF6、3H和三生3He),对无承压-半承压Pampeano含水层的地下水运移时间进行了评价。利用集总参数模型(lpm)和示踪剂的历史输入函数进行逆建模,得到年龄分布。结果表明,地下水流动缓慢而复杂,年龄范围广,水的年龄比简单的无承压含水层概念模型所期望的要大。在地下水位0至10米之间,35%的地下水缺乏年轻的地下水示踪剂(年龄>; ~ 60年);10 ~ 20米,60%以上;在30米以下,超过99%。在22-48米深度进行的一次39Ar测量表明,平均年龄为170岁,尽管这可能被低估了。3H、3He和3H/3H0比值的反演模型表明,不饱和带过境时间在3 ~ 37年之间,超出了基于简单平流计算的估计,表明存在延迟层和优先冬季补给。这些发现强调了分散、沉积非均质性和低渗透层在控制地下水年龄和补给方面的作用,并对污染物脆弱性和资源可持续性产生影响。
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引用次数: 0
Global distribution, synergistic interactions, and advances in in-situ remediation of prevalent heavy metal(loid)s in groundwater systems 地下水系统中重金属的全球分布、协同作用及原位修复研究进展
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2026-02-01 Epub Date: 2025-12-06 DOI: 10.1016/j.gsd.2025.101559
Diksha Dangwal , Rahul Silori , Balendu Shekher Giri
Groundwater contamination by heavy metals (HMs) is a critical environmental and public health challenge, threatening a critical source of drinking water. This review synthesizes research from the past 1.5 decades on the global occurrence, spread, mobility, interaction mechanisms and in-situ remediation of four prevalent HMs: Arsenic (As), Lead (Pb), Cadmium (Cd), and Chromium (Cr), highlighting their widespread distribution and underlying causes of contamination across groundwater systems. HMs bio-mimic vital elements and disrupt biological functions. HMs may form reactive oxygen species (ROS) and destabilize DNA, RNA and protein. Findings reveal contamination is pervasive; particularly affecting South Asian and developed nations such as Italy, Canada, Spain, Australia and USA. The maximum concentration of As, which has geogenic causes as origin, was recorded at Nigeria (3.06 mg/L), followed by USA (3 mg/L). Pb contamination by anthropogenic intervention is humungous in Kenya, attaining 121.40 mg/L. The chief sources of Cr in Tamil Nadu, India, are the mining and tannery industries, with concentration peaking to 40.52 mg/L. Cd contamination, caused by anthropogenic activities, reached 8 mg/L (Kenya), establishing Kenya as the hotspot of contamination. Microplastics increase metal bioaccumulation, PPCPs modify metal toxicity, HMs cause antimicrobial gene transfer, which causes greater mobility and persistence of HMs. Emerging PRB setups and novel media like sulfidated nZVI, goethite promises solutions of 90 % HM removal, electrocoagulation brought 80 % As removal in most field trials. By consolidating recent findings, this review equips researchers and policymakers with a comprehensive understanding of groundwater contamination scenario, associated implications and protection strategies.
地下水重金属污染是一项重大的环境和公共卫生挑战,威胁着饮用水的重要来源。本文综述了近15年来关于砷(As)、铅(Pb)、镉(Cd)和铬(Cr)四种主要有害物质的全球发生、扩散、迁移、相互作用机制和原位修复的研究,重点介绍了它们在地下水系统中的广泛分布和污染的潜在原因。HMs生物模拟重要元素,破坏生物功能。HMs可以形成活性氧(ROS),破坏DNA、RNA和蛋白质的稳定。调查结果显示,污染无处不在;尤其是影响南亚和发达国家,如意大利、加拿大、西班牙、澳大利亚和美国。砷含量最高的国家是尼日利亚(3.06 mg/L),其次是美国(3 mg/L)。肯尼亚人为干预造成的铅污染巨大,达到121.40 mg/L。在印度泰米尔纳德邦,铬的主要来源是采矿和制革工业,其浓度最高达到40.52毫克/升。人为活动造成的Cd污染达到8 mg/L(肯尼亚),肯尼亚成为污染热点。微塑料增加金属的生物积累,PPCPs改变金属毒性,HMs引起抗菌基因转移,这导致HMs更大的流动性和持久性。在大多数现场试验中,新兴的PRB装置和新型介质,如硫化nZVI、针铁矿,有望实现90%的HM去除率,电凝法可以去除80%的As。通过整合最近的研究结果,本综述使研究人员和决策者能够全面了解地下水污染情况、相关影响和保护策略。
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引用次数: 0
A comparative study of key factors influencing groundwater in a temperate and a semi-arid regions 温带与半干旱区地下水影响因素的比较研究
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2026-02-01 Epub Date: 2025-12-12 DOI: 10.1016/j.gsd.2025.101562
Mahdi Miri , Mehdi Zarei , Diana M. Allen
Groundwater depletion is a critical issue with significant impacts on water availability in diverse climatic settings. This study uses a range of statistical methods and remote-sensing techniques to investigate the factors, specifically, climatic, hydrological, and human-driven changes, that influence groundwater levels (GWLs) in aquifers in a temperate region (three aquifers in southwestern Canada) and a semi-arid region (four aquifers in southern Iran). Change point and trend analyses reveal significant declines in GWL (groundwater depletion) in one aquifer in the temperate region and in all aquifers in the semi-arid region, despite climate variables such as precipitation, temperature, and potential evapotranspiration showing minimal changes over the study period. In contrast, human-induced factors, including agricultural expansion, deforestation, and increases in the number of pumping wells, have occurred in the aquifers of both regions. The comparative design highlights contrasting resilience: Canadian aquifers exhibit partial recovery under management interventions, whereas Iranian aquifers demonstrate persistent over-extraction with limited recharge. These findings emphasize that human pressure, rather than climate, is the primary driver of depletion and that adaptive, region-specific groundwater governance is critical for sustainable management under future climate and land-use change.
地下水枯竭是一个关键问题,对不同气候条件下的水资源供应有重大影响。本研究使用一系列统计方法和遥感技术来调查影响温带地区(加拿大西南部的三个含水层)和半干旱地区(伊朗南部的四个含水层)含水层地下水位(gwl)的因素,特别是气候、水文和人为驱动的变化。变化点和趋势分析显示,尽管降水、温度和潜在蒸散发等气候变量在研究期间变化很小,但温带地区的一个含水层和半干旱区的所有含水层的GWL(地下水枯竭)都显著下降。相比之下,这两个地区的含水层都出现了人为因素,包括农业扩张、森林砍伐和抽水井数量的增加。对比设计突出了对比的恢复能力:加拿大含水层在管理干预下表现出部分恢复,而伊朗含水层则表现出持续的过度开采和有限的补给。这些发现强调,人类的压力,而不是气候,是枯竭的主要驱动因素,适应性的、特定区域的地下水治理对于未来气候和土地利用变化下的可持续管理至关重要。
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引用次数: 0
Groundwater vulnerability assessment of the Djibouti aquifer system (East Africa Rift System): A comparative study of DRASTIC, Hybrid-DRASTICs, and DRASTIC-based multi-objective evolutionary algorithm 东非裂谷系吉布提含水层系统地下水脆弱性评价:DRASTIC、hybrid -DRASTIC和基于DRASTIC的多目标进化算法的比较研究
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2026-02-01 Epub Date: 2025-12-13 DOI: 10.1016/j.gsd.2025.101564
Mohamed Osman Awaleh , Golab Moussa Omar , Abdi-Basid Ibrahim Adan , Mohammad Najafzadeh , Christelle Marlin , Magued Al-Aghbary , Mohamed Abdillahi Robleh , Awaleh Djama Iltireh , Jafar Al-Jawad , Moussa Mohamed Waberi , Rachid Robleh Ragueh , Bahdon Elmi Ragueh , Omar Assowe Dabar , Moussa Mahdi Ahmed , Mahamoud Ali Chirdon , Abdillahi Elmi Adaneh , Nasri Hassan Ibrahim , Nima Moussa Egueh , Ismail Abdillahi Guireh , Omar Ibrahim Elmi
The comprehensive mapping of groundwater contamination zones is vital for sustainable water resource management, especially in underdeveloped countries facing urban and industrial pressures. This study investigates, for the first time, the groundwater vulnerability of the Djibouti aquifer system located in the north of the East Africa Rift System (EARS). This area, which is home to 72.8 % of the country's inhabitants, has been impacted by rapid urbanization including industrial activities and the discharge of untreated wastewater. This study compares multiple groundwater vulnerability modeling frameworks, including DRASTIC (Depth to groundwater, net Recharge, Aquifer media, Soil media, Topography, Impact of the vadose zone, and hydraulic Conductivity), DRASTIC–LULC (Land Use Land Cover), DRASTIC–AHP (Analytic Hierarchy Process), AHP–DRASTIC–LULC, DRASTIC–NSGA-II (Non-dominated Sorting Genetic Algorithm-II), and NSGA-II–DRASTIC–LULC. Spatial autocorrelation analysis (Moran's I > 0.95) has been used to improve the reliability and interpretability of the vulnerability maps. Groundwater vulnerability maps indicate that high and very high vulnerability zones (13.59–47.47 % and 1.02–21.70 %, respectively) are primarily located in the eastern and northern sectors. Moderate to low vulnerability zones (30.81–56.45 %) are prevalent in the central part of the study area. Sensitivity analysis identified key parameters such as aquifer depth, vadose zone impact, and aquifer medium. The LULC factors significantly improved model sensitivity and enabled better identification of at risk zones. The NSGA-II–DRASTIC–LULC model outperformed other modified DRASTIC methods, achieving a correlation of 0.58, an AUC of 0.84, and an RMSE of 1.13. These findings may provide a critical scientific basis for Djibouti's policymakers to prioritize land-use zoning and implement targeted protection measures in the identified high-risk zones, thereby securing a sustainable water future for the region's growing population.
地下水污染区的全面测绘对于可持续水资源管理至关重要,特别是在面临城市和工业压力的不发达国家。本文首次对位于东非裂谷系北部的吉布提含水层系统的地下水脆弱性进行了研究。该地区居住着全国72.8%的居民,受到快速城市化的影响,包括工业活动和未经处理的废水排放。本研究比较了DRASTIC(地下水深度、净补给、含水层介质、土壤介质、地形、渗透带影响和水力导电性)、DRASTIC - lulc(土地利用-土地覆盖)、DRASTIC - ahp(层次分析法)、AHP-DRASTIC-LULC、DRASTIC - nsga - ii(非支配排序遗传算法- ii)和NSGA-II-DRASTIC-LULC等多个地下水脆弱性建模框架。利用空间自相关分析(Moran's I > 0.95)提高脆弱性图的可靠性和可解释性。地下水脆弱性图显示,高、高脆弱性区(13.59 ~ 47.47%)和极高脆弱性区(1.02 ~ 21.70%)主要位于东部和北部。研究区中部普遍存在中、低易损区(30.81 ~ 56.45%)。敏感性分析确定了含水层深度、渗透带影响和含水层介质等关键参数。LULC因子显著提高了模型的敏感性,并能更好地识别风险区域。NSGA-II-DRASTIC-LULC模型优于其他改进的DRASTIC方法,相关系数为0.58,AUC为0.84,RMSE为1.13。这些发现可以为吉布提的政策制定者提供重要的科学依据,以确定土地利用分区的优先顺序,并在确定的高风险区域实施有针对性的保护措施,从而为该地区不断增长的人口确保可持续的水资源未来。
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Groundwater for Sustainable Development
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