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Hydrochemistry and isotopic characterization of water resources in Santa Rosa mining area, Ecuador 厄瓜多尔圣罗莎矿区水资源的水化学和同位素表征
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2025-11-01 DOI: 10.1016/j.gsd.2025.101556
Karla Villamar-Marazita , Cindy Goyburo-Chávez , Priscila E. Valverde-Armas , Tomas Vitvar , Peter Čech , Juraj Michalko , Samantha Jiménez-Oyola
This study analyzed the hydrochemical and isotopic characteristics of water resources in the Santa Rosa mining region, southern Ecuador, with the aim of understanding the processes that influence the chemical composition of water, its origin, and sources of contamination. The research focused on assessing the impact of anthropogenic activities on water quality, providing an integrated perspective of the region. Between 2022 and 2024, water samples were collected during both dry and rainy seasons. Surface water samples were taken from the Santa Rosa River and its tributaries, while groundwater samples were obtained from commercial wells within the watershed. Major ions (Ca2+, Mg2+, K+, Na+, HCO3, SO42−, Cl, NO3) and isotopic content (δ18O, δ2H, δ3H, δ34S-SO42-, and δ18O-SO42-) were analyzed. The data were analyzed using hydrochemical diagrams, multivariate statistical analysis, and geospatial analysis. The findings revealed that surface waters are characterized by Ca2+ - SO42-- and Ca2+- HCO3 compositions, while groundwater was identified as Na+ - Cl type. The chemistry of surface water is mainly regulated by rock-water interactions, while marine evaporites dominate groundwater chemistry. Isotopes 18O and 2H suggest that the water primarily originates from meteoric sources. The source of SO42− in surface water is attributed to atmospheric deposition and the oxidation of sulfur compounds, whereas the dissolution of evaporites is the key factor driving groundwater SO42− concentrations. This study represents the first comprehensive hydrochemical and isotopic analysis of water resources in a mining region in Ecuador, providing crucial data for the sustainable management of water resources in areas affected by mining. The results offer a scientific basis for developing water protection and conservation strategies essential for mitigating the impacts of mining on local water quality.
本研究分析了厄瓜多尔南部圣罗莎矿区水资源的水化学和同位素特征,目的是了解影响水的化学成分、来源和污染源的过程。研究的重点是评估人类活动对水质的影响,为该地区提供一个综合的视角。在2022年至2024年期间,在旱季和雨季都收集了水样。地表水样本取自圣罗莎河及其支流,地下水样本取自流域内的商业水井。主要离子(Ca2+、Mg2+、K+、Na+、HCO3−、SO42−、Cl−、NO3−)和同位素含量(δ18O、δ2H、δ3H、δ34S-SO42-和δ18O-SO42-)进行了分析。数据分析采用水化学图、多元统计分析和地理空间分析。结果表明,地表水以Ca2+- SO42-和Ca2+- HCO3 -组成为主,地下水以Na+ - Cl为主。地表水的化学成分主要受岩石-水相互作用的调节,而海洋蒸发岩主导地下水化学成分。同位素18O和2H表明水主要来源于大气。地表水中SO42−的来源主要是大气沉降和硫化物氧化,而地下水中SO42−的主要来源是蒸发岩的溶解。这项研究首次对厄瓜多尔矿区的水资源进行了全面的水化学和同位素分析,为受采矿影响地区的水资源可持续管理提供了重要数据。研究结果为制定水资源保护和节约战略提供了科学依据,这些战略对于减轻采矿对当地水质的影响至关重要。
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引用次数: 0
Navigating an impending crisis: Groundwater governance in Konya Closed Basin, Türkiye 应对迫在眉睫的危机:科尼亚封闭盆地的地下水治理,<s:1> rkiye
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2025-11-01 DOI: 10.1016/j.gsd.2025.101540
Irem Daloğlu Çetinkaya , İzel Uygur , Ali Kerem Saysel
Groundwater, a critical resource for agriculture, faces severe overexploitation globally, resulting in sustainability challenges and ecological consequences. This study examines the groundwater governance dynamics in the Konya Closed Basin (KCB), Türkiye's agricultural hub often referred to as the country's “granary.” Overexploitation in the region has led to a rapid decline in groundwater levels, nearly 30 m since the 1980s, exacerbating water scarcity, land subsidence, and environmental degradation. Combining fieldwork, stakeholder interviews, secondary data analysis, and an examination of crop pattern changes, we investigate the interplay between climate change, shifting agricultural practices, and inadequate governance structures. Our findings highlight significant shortcomings in the current governance framework, including weak enforcement, fragmented coordination, inadequate monitoring, and eroding roles of cooperatives and unions. The study underscores the urgent need for integrated governance frameworks that enhance stakeholder collaboration, prioritize demand management, and promote adaptive policies. Insights from the KCB are broadly applicable to other arid regions heavily reliant on agriculture and groundwater, providing critical lessons for mitigating overexploitation and promoting long-term sustainability.
地下水是农业的重要资源,在全球范围内面临严重的过度开采,造成了可持续性挑战和生态后果。本研究考察了Konya封闭盆地(KCB)的地下水治理动态,KCB是 rkiye的农业中心,通常被称为该国的“粮仓”。该地区的过度开采导致地下水位迅速下降,自20世纪80年代以来下降了近30米,加剧了水资源短缺、地面沉降和环境退化。结合实地调查、利益相关者访谈、二手数据分析和作物模式变化的研究,我们研究了气候变化、农业实践转变和治理结构不足之间的相互作用。我们的研究结果突出了当前治理框架的重大缺陷,包括执行不力、协调分散、监督不足以及合作社和工会的作用受到侵蚀。该研究强调了对集成治理框架的迫切需要,这些框架可以加强利益相关者的协作,优先考虑需求管理,并促进适应性政策。KCB的见解广泛适用于其他严重依赖农业和地下水的干旱地区,为减轻过度开采和促进长期可持续性提供了重要的经验教训。
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引用次数: 0
Nitrate dynamics in coastal groundwater and rivers: Insights into oligotrophication management 沿海地下水和河流中的硝酸盐动态:对少营养化管理的见解
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2025-11-01 DOI: 10.1016/j.gsd.2025.101536
Therese Line Laure Jokam Nenkam , Jing Zhang , Daisuke Komatsu , Keiji Horikawa , Ade S. Oktaviani
Coastal ecosystems rely significantly on terrestrial-derived essential nutrients for primary productivity. However, efforts to reduce anthropogenic nutrient inputs to mitigate eutrophication led to coastal oligotrophication when tipping points were exceeded. In Toyama Bay, land-derived nutrients significantly enrich the euphotic zone. However, nutrient reduction policies since the 1990s have raised concerns about declining marine productivity. To investigate these trends, we studied the Kurobe River Alluvial Fan (KRAF), Japan's largest fan, focusing on nitrate (NO3) dynamics. The KRAF was selected due to its multi-water system and diverse land use influenced by the Asian Monsoon Climate, which controls its hydrological and nutrient dynamics, serving as a model for the broader Asian region. Using isotopic analyses (δ15N-NO3-, δ18O-NO3-, δ2H-H2O, δ18O-H2O), hydrochemical parameters, and mixing models, we examined hydrological dynamics, NO3 sources, transformation processes, and temporary storage from 35 seasonally collected water samples.
Results showed low NO3-N concentrations (0.05–1.89 mg/L), over 80 % below environmental standards, influenced by hydrological dynamics, land-use changes, and management policies. Soil and fertilisers were primary NO3 sources, highlighting the impact of water management strategies on nutrient reduction. Nitrification was dominant in lowland and riverine areas, while denitrification was primarily limited to highland paddy fields. Fresh submarine groundwater discharge (FSGD) contributed 52 %–70 % of the total NO3 flux to the sea, surpassing river contributions. Total flux of terrestrial NO3 was estimated at 347.4 ± 121.1 kg/year, a 31 % decrease compared to the 2005 estimate.
Promoting coastal agriculture can mitigate oligotrophication by slowing water flow and enhancing nutrient supply through the use of FGSD. This research employs a science-based approach to recommend sustainable nutrient management strategies. More broadly, the method can be adapted for use in other water bodies to identify NO3 sources and dynamics, thereby promoting comprehensive nutrient management and supporting the health and productivity of coastal ecosystems.
沿海生态系统的初级生产力在很大程度上依赖陆源必需营养素。然而,为减轻富营养化而减少人为营养投入的努力,在超过临界点时导致沿海少营养化。富山湾的陆源营养物显著地丰富了绿化带。然而,自20世纪90年代以来的营养减少政策引起了人们对海洋生产力下降的担忧。为了研究这些趋势,我们研究了日本最大的冲积扇黑部河冲积扇(KRAF),重点研究了硝酸盐(NO3−)的动态。KRAF之所以被选中,是因为它的多水系统和受亚洲季风气候影响的多样化土地利用,控制着其水文和营养动态,可作为更广泛的亚洲地区的模式。利用同位素分析(δ15N-NO3-、δ18O-NO3-、δ2H-H2O、δ18O-H2O)、水化学参数和混合模型,研究了35个季节采集的水样的水文动力学、NO3-来源、转化过程和临时储存。结果表明:受水文动态、土地利用变化和管理政策的影响,NO3−-N浓度较低(0.05 ~ 1.89 mg/L),低于环境标准80%以上;土壤和肥料是NO3−的主要来源,这突出了水管理策略对养分减少的影响。硝化作用主要发生在低地和河流地区,反硝化作用主要发生在高原水田。新鲜海底地下水排放(FSGD)贡献了总NO3−通量的52% - 70%,超过了河流的贡献。陆地NO3−的总通量估计为347.4±121.1 kg/年,与2005年的估计相比减少了31%。促进沿海农业可以减缓水流,并通过使用FGSD增加营养供应,从而缓解少营养化。本研究采用基于科学的方法推荐可持续的营养管理策略。更广泛地说,该方法可适用于其他水体,以确定NO3−的来源和动态,从而促进综合营养管理,支持沿海生态系统的健康和生产力。
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引用次数: 0
A multiscale soil water balance for sustainable groundwater management of a local transboundary karst aquifer 跨界喀斯特含水层可持续地下水管理的多尺度土壤水分平衡
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2025-11-01 DOI: 10.1016/j.gsd.2025.101551
Paola Petrone , Pantaleone De Vita , Pasquale Allocca , Silvio Coda , Delia Cusano , Radka Kodešová , Daniele Lepore , Vincenzo Allocca
Sustainable groundwater management of transboundary aquifers (TBAs) remains a major global and regional challenge that requires necessitating enhanced, coordination and cooperation among neighboring countries and institutions. The Avella Mts. are a major karst TBA of the Campania region (Italy), providing vital groundwater resources, whose water balance equilibrium is increasingly threatened by uncontrolled growth in groundwater extraction, especially during prolonged drought periods. A multiscale soil water balance was performed for the period 2010–2021 to assess the sustainability of current groundwater withdrawals. The findings reveal a high spatio-temporal variability of groundwater recharge (GR). At the aquifer scale, average GR equals to 244.40 Mm3/y, with interannual variability of about −45 % and +73 %. At the basin scale, recharge on average varies between 29.64 Mm3/y and 100.28 Mm3/y. The springs inventory map and the register of authorized wells highlight an outgoing groundwater volume of 252.30 Mm3/y, at the aquifer scale, while at the basin scale, it varies between 6.30 Mm3/y and 97.76 Mm3/y, exceeding the recharge in certain groundwater basins. Consequently, there is a budgetary disequilibrium within the aquifer, which is particularly pronounced during drought years, as evidenced by the drying of springs and streams. These results highlight significant aquifer stress, which is projected to worsen in the future due to climate change. They demonstrate the urgent need to adopt sustainable groundwater management strategies and reform existing water governance model in the Campania region, as well as in other parts of Italy and Europe.
跨界含水层的可持续地下水管理仍然是一项重大的全球和区域挑战,需要加强邻国和机构之间的协调与合作。阿维拉山脉是坎帕尼亚地区(意大利)的主要喀斯特TBA,提供重要的地下水资源,其水平衡日益受到地下水开采不受控制的增长的威胁,特别是在长期干旱时期。在2010-2021年期间进行了多尺度土壤水分平衡,以评估当前地下水提取的可持续性。研究结果表明,地下水补给具有高度的时空变异性。在含水层尺度上,平均GR为244.40 Mm3/y,年际变化约为- 45%和+ 73%。在流域尺度上,补给量平均在29.64 Mm3/y ~ 100.28 Mm3/y之间。泉水库存图和授权井记录显示,在含水层尺度上,地下水出水量为252.30 Mm3/年,而在流域尺度上,地下水出水量在6.30 Mm3/年至97.76 Mm3/年之间变化,超过了某些地下水盆地的补给量。因此,在含水层内部存在预算不平衡,这在干旱年份尤为明显,泉水和溪流的干涸就是明证。这些结果突出了严重的含水层压力,预计由于气候变化,这种压力将在未来恶化。它们表明,迫切需要在坎帕尼亚地区以及意大利和欧洲其他地区采用可持续的地下水管理战略并改革现有的水治理模式。
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引用次数: 0
Mapping contamination and health risks posed by heavy metals in groundwater from industrial and landfill-affected localities in central India 绘制印度中部受工业和垃圾填埋场影响地区地下水重金属污染和健康风险的地图
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2025-11-01 DOI: 10.1016/j.gsd.2025.101554
Rajesh Ahirwar , Kamini Arya , Dharma Raj
Groundwater contamination by trace metals poses a serious environmental and public health concern in rapidly urbanizing regions of India. This study evaluated the seasonal and spatial variability of groundwater quality, metal contamination, and associated health risks across three environmentally distinct sites in central India – Adampur Chawni (new landfill), Bhanpur (legacy landfill), and Mandideep (industrial hub). A total of 205 groundwater samples were collected during pre-monsoon, monsoon, and post-monsoon seasons and analyzed for physicochemical parameters, trace metals, and pollution indices. Health risk assessment, following the USEPA framework, estimated chronic daily intake, hazard indices, and carcinogenic risks for adults and children. A community morbidity survey was also undertaken to supplement exposure evaluation. Groundwater pH remained within permissible limits (7.20 ± 0.3 to 7.81 ± 0.4), while total dissolved solids exceeded acceptable levels at Adampur Chawni (up to 712 mg/L). Elevated chloride (up to 505 mg/L), sulphate (up to 265 mg/L), and hardness (up to 278 mg/L) were recorded near landfill sites. Although most metal concentrations were within limits, Pb, Mn, and Zn occasionally exceeded national standards. Heavy metal pollution index (3.43–7.85) and water quality index (15.69–49.21) indicated excellent to good water quality across all locations, while metal index (0.25–1.39) showed moderate pollution levels. Health risk assessment revealed higher chronic exposure in children, with manganese intake up to 4.18 × 10−2 mg/kg/day, and non-carcinogenic hazard indices (HI) exceeding 1.5 in Mandideep. Carcinogenic risks exceeded USEPA limits for children at all sites, particularly in Mandideep (TCR = 3.73 × 10−4). Morbidity survey data revealed fatigue, joint pain, and neurological symptoms consistent with metal exposure. These findings indicate localized contamination of groundwater and emphasize for groundwater monitoring, improved waste management, and interventions, as health risk assessment revealed hazards despite generally good water quality indices.
在印度快速城市化的地区,地下水受到微量金属污染已成为一个严重的环境和公共健康问题。本研究评估了印度中部三个环境不同的地点——Adampur Chawni(新垃圾填埋场)、Bhanpur(遗留垃圾填埋场)和Mandideep(工业中心)——地下水质量、金属污染和相关健康风险的季节和空间变化。在季风前、季风期和季风后3个季节共采集205份地下水样本,分析其理化参数、痕量金属和污染指数。健康风险评估,根据美国环保署的框架,估计慢性每日摄入量,危害指数,以及成人和儿童的致癌风险。还进行了社区发病率调查,以补充接触评价。地下水pH值保持在允许范围内(7.20±0.3至7.81±0.4),而总溶解固体超过了Adampur Chawni的可接受水平(高达712 mg/L)。在垃圾填埋场附近,氯化物(高达505毫克/升)、硫酸盐(高达265毫克/升)和硬度(高达278毫克/升)均有所升高。虽然大多数金属浓度在限定范围内,但铅、锰和锌偶尔超过国家标准。重金属污染指数(3.43 ~ 7.85)和水质指数(15.69 ~ 49.21)表明水质优良至良好,金属污染指数(0.25 ~ 1.39)表明水质中等。健康风险评估显示,儿童的慢性接触量较高,锰摄入量高达4.18 × 10−2 mg/kg/天,下颌深地区的非致癌危害指数(HI)超过1.5。所有地点的儿童致癌风险均超过USEPA限值,特别是在Mandideep (TCR = 3.73 × 10−4)。发病率调查数据显示疲劳、关节疼痛和与金属接触一致的神经系统症状。这些发现表明地下水受到局部污染,并强调地下水监测、改进废物管理和干预措施,因为健康风险评估揭示了尽管水质指数总体良好的危害。
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引用次数: 0
Arsenic mobilization and recirculation dynamics: Groundwater circulation wells for enhanced decontamination in complex coastal aquifer environments 砷的动员和再循环动力学:地下水循环井在复杂的沿海含水层环境中加强去污染
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2025-11-01 DOI: 10.1016/j.gsd.2025.101538
Paolo Ciampi , Damiano Feriaud , Daniele D’Emilio , Felice Tatangelo , Lorenzo Lanzafame , Monica Pasini , Marco Petrangeli Papini
Arsenic (As) contamination poses serious risks to groundwater quality and human health, with millions globally exposed to unsafe levels, making remediation a critical challenge. Coastal aquifers are especially vulnerable due to heterogeneous lithology, saline intrusion, and complex hydrogeochemical dynamics, which limit the effectiveness of conventional pump-and-treat (P&T) systems and call for innovative remediation solutions. This study evaluates groundwater circulation wells (GCWs) as a technology to mobilize and remove As, focusing on the development of the GCW-induced recirculation cell. The research was conducted at a coastal industrial site with longstanding As pollution, representative of complex hydrogeology. A relational geodatabase integrated data from 76 boreholes, 41 piezometers, 2 multi-level sampling wells (MLSWs), and 1 GCW. A 3D stratigraphic model supported the design of a 23 m GCW with screened sections at 6 ÷ 8, 12 ÷ 15, and 19 ÷ 22 m. Groundwater was extracted, treated above ground, and reinjected to establish a recirculation cell. Hydrochemical and electrical conductivity (EC) monitoring over 550 days captured the spatial and temporal dynamics of As mobilization, removal, and salinity mixing. The GCW-induced recirculation cell mobilized As up to ∼9000 μg/L—around 900 times the World Health Organization (WHO) guideline of 10 μg/L—before stabilizing at ∼6500 μg/L. The system achieved 66 % removal efficiency, extracting ∼80 kg of As while promoting groundwater mixing. EC data from MLSWs provided unprecedented insights into the spatio-temporal evolution of the recirculation process. These findings demonstrate that GCWs provide a viable and sustainable alternative to conventional remediation strategies for addressing persistent As contamination in complex coastal aquifers.
砷污染对地下水质量和人类健康构成严重风险,全球数百万人暴露在不安全的水平,使补救措施成为一项重大挑战。由于非均质岩性、盐水侵入和复杂的水文地球化学动力学,沿海含水层尤其脆弱,这限制了常规泵送处理(P&;T)系统的有效性,需要创新的修复解决方案。本研究对地下水循环井(GCWs)作为一种调动和去除砷的技术进行了评价,重点研究了地下水循环井诱导循环池的开发。本研究选取了一个长期受砷污染的沿海工业基地,具有复杂的水文地质特征。一个关系型地质数据库整合了76口井、41口压力表、2口多级采样井(MLSWs)和1口GCW的数据。三维地层模型支持了23 m GCW的设计,该GCW在6 ÷ 8、12 ÷ 15和19 ÷ 22 m处进行了筛选。地下水被提取出来,在地面上处理,并重新注入,以建立一个再循环池。550多天的水化学和电导率(EC)监测捕捉到了砷的移动、去除和盐度混合的时空动态。gcw诱导的再循环细胞在稳定在~ 6500 μg/L之前,动员了高达~ 9000 μg/L的砷,这是世界卫生组织(WHO)标准10 μg/L的900倍左右。该系统达到66%的去除效率,在促进地下水混合的同时提取约80 kg的砷。来自MLSWs的EC数据为再循环过程的时空演变提供了前所未有的见解。这些发现表明,gcw为解决复杂沿海含水层中持续存在的砷污染问题提供了一种可行和可持续的替代方法,可替代传统的修复策略。
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引用次数: 0
Bridging the resolution gap: Machine learning for local-scale groundwater drought monitoring in Punjab, Pakistan 弥合分辨率差距:机器学习用于巴基斯坦旁遮普邦的局部地下水干旱监测
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2025-11-01 DOI: 10.1016/j.gsd.2025.101545
Fahimeh Youssefi , Shoaib Ali , Behnam Khorrami , Mohammad Mohsin Khan , Muhammad Jehanzaib , Talha Mahmood , Zhiming Han , Wu Haotian , Muhammad Faisal
The drought, resulting from insufficient precipitation, significantly impacts groundwater resources, thereby threatening water availability and human livelihood. Conventional approaches to evaluating groundwater shortages are influenced by limited observations across spatial and temporal dimensions. Previous studies on groundwater drought occurrences in the Punjab Doabs of Pakistan were explored at limited resolution (0.25°). Therefore, the Extreme Gradient Boosting (XGBoost) machine learning model was employed to downscale the Terrestrial Water Storage Anomaly (TWSA) data (0.25°) obtained from Gravity Recovery and Climate Experiment (GRACE) to 0.1° resolution and derived high-resolution Groundwater Storage Anomaly (GWSA) data (0.1°) to assess the Groundwater Drought Index (GGDI) at higher resolution. The XGBoost model had a Pearson correlation (R) of 0.99, an NSE of 0.99, an RMSE of 5.22 mm, and an MAE of 2.75 mm. The groundwater dynamics can be accurately simulated by the XGBoost model, which has demonstrated a validation with in situ groundwater level data showing an R of 0.77. The characteristics of the GGDI trend, along with its spatio-temporal variations, were analyzed in the Punjab Doabs from 2003 to 2020. Findings indicated severe drought events in 2010 and from 2018 to 2020 in the study area. Additionally, results indicated that GGDI exhibited similar drought patterns to the model-generated Groundwater Storage Percentile (GWSP) with a correlation coefficient of 0.66. This framework serves as an effective tool for monitoring drought in the Punjab Doabs and similar climatic zones.
由于降水不足造成的干旱严重影响地下水资源,从而威胁到水的供应和人类的生计。评价地下水短缺的传统方法受到有限的时空观测的影响。以前对巴基斯坦旁遮普省多布斯地下水干旱事件的研究是在有限分辨率(0.25°)下进行的。为此,采用极端梯度增强(XGBoost)机器学习模型,将重力恢复与气候实验(GRACE)获得的陆地蓄水异常(TWSA)数据(0.25°)缩小到0.1°分辨率,并导出高分辨率地下水蓄水异常(GWSA)数据(0.1°),在更高分辨率下评估地下水干旱指数(GGDI)。XGBoost模型的Pearson相关(R)为0.99,NSE为0.99,RMSE为5.22 mm, MAE为2.75 mm。XGBoost模型可以准确地模拟地下水动态,并与现场地下水位数据进行了验证,R值为0.77。分析了2003 - 2020年旁遮普省GGDI变化趋势特征及其时空变化特征。研究结果表明,研究区域在2010年和2018年至2020年发生了严重干旱事件。此外,GGDI与模型生成的地下水储存百分位数(GWSP)表现出相似的干旱模式,相关系数为0.66。该框架是监测旁遮普邦和类似气候带干旱的有效工具。
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引用次数: 0
Groundwater level forecasting in response to climate change scenarios in southwestern Saskatchewan using wavelet decomposition and artificial neural networks 基于小波分解和人工神经网络的萨斯喀彻温省西南部地下水位预测对气候变化的响应
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2025-11-01 DOI: 10.1016/j.gsd.2025.101550
Ahmed Shawky Okasha , Mohamed Khafagy , Corinne Schuster-Wallace , Sarah Dickson-Anderson
Global warming has intensified extreme climate events, including prolonged droughts, altering precipitation patterns and threatening groundwater resources. Additional stresses from economic development, population growth, and land use changes exacerbate groundwater depletion, often exceeding recharge rates. This study develops a hybrid artificial neural networks (ANN) and wavelet decomposition (WA) model to forecast long-term groundwater levels (GWLs) until 2100 under future climate scenarios in southwestern Saskatchewan to inform sustainable groundwater management strategies in a data-scarce region with a complex disconnected aquifer system. Monthly gridded precipitation and temperature data were combined with monthly GWLs from three wells in two aquifers. Three machine learning ANN models were applied and evaluated to forecast GWLs: i) nonlinear autoregressive network with exogenous input (NARX), ii) nonlinear autoregressive network (NAR), and iii) nonlinear input-output network (NIO). WA was integrated with NIO and NAR for signal denoising. Moreover, two base models were applied to each well: i) linear regression (LR), and ii) autoregressive integrated moving average (ARIMA) to quantify WA-ANN added value. Three learning algorithms, Levenberg-Marquardt (LM), Bayesian Regularization (BR), and scaled conjugate gradient (SCG), trained the models with varying neurons and delay times. Results show that NARX trained with BR produce the most accurate predictions for all wells. The applicability of WA-NIO and WA-NAR trained with LM in data-sparse settings remains largely exploratory with potential for improvement. GWLs are least impacted under SSP1-2.6, moderately affected under SSP2-4.5, and severely impacted under SSP5-8.5. These findings support decision-making through informing aquifer sustainability management plans under changing climate conditions.
全球变暖加剧了极端气候事件,包括长期干旱、改变降水模式和威胁地下水资源。经济发展、人口增长和土地利用变化带来的额外压力加剧了地下水的枯竭,常常超过补给速率。本研究开发了一种混合人工神经网络(ANN)和小波分解(WA)模型,用于预测萨斯喀彻温省西南部未来气候情景下至2100年的长期地下水位(gwl),为具有复杂断续含水层系统的数据稀缺地区的可持续地下水管理策略提供信息。每月的网格化降水和温度数据与来自两个含水层的三口井的月gwl数据相结合。应用并评估了三种机器学习人工神经网络模型来预测gwl: i)外生输入非线性自回归网络(NARX), ii)非线性自回归网络(NAR)和iii)非线性输入输出网络(NIO)。将WA与NIO和NAR相结合进行信号去噪。此外,每口井应用了两个基本模型:i)线性回归(LR)和ii)自回归综合移动平均(ARIMA),以量化WA-ANN的附加值。Levenberg-Marquardt (LM)、贝叶斯正则化(BR)和缩放共轭梯度(SCG)三种学习算法对具有不同神经元和延迟时间的模型进行了训练。结果表明,经过BR训练的NARX可以对所有井进行最准确的预测。用LM训练的WA-NIO和WA-NAR在数据稀疏设置中的适用性在很大程度上仍处于探索阶段,有改进的潜力。gwl在SSP1-2.6下受影响最小,在SSP2-4.5下受影响中等,在SSP5-8.5下受影响严重。这些发现通过为气候变化条件下的含水层可持续性管理计划提供信息来支持决策。
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引用次数: 0
Groundwater quality and risk assessment in urban areas of arid regions on the western Qinghai-Tibet Plateau
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2025-11-01 DOI: 10.1016/j.gsd.2025.101547
Qingshan Li , Xiaobing Kang , Mo Xu , Dan Wang , Ke Li
The western region of the Qinghai-Tibet Plateau is characterized by an arid climate with minimal rainfall, making groundwater the primary water source for local towns. In recent years, levated concentrations of arsenic(As), fluoride(F) and nitrate(NO3) in groundwater have raised concerns about drinking water safety. This study, collected 52 groundwater samples from wells in seven towns across six basins in the Ali region. By employing methods such as mathematical statistics, major ion ratio analysis, the Entropy-Weighted Water Quality Index (EWQI), and Monte Carlo simulation, the characteristics of hydrogeochemical components, controlling factors, and potential risks of groundwater in this region were clarified. The groundwater chemistry type is dominated by HCO3–Ca, and its ion concentration from high to low is Ca2+ > Na+ > Mg2+ > K+ and HCO3 > SO42− > Cl > NO3 >F. The most severe As pollution (0–0.09 mg/L) occurred in Gaer(GR)and Geji(GJ) towns within the Shiquan River Basin in the western part of the study area, This is primarily attributed to high As hot spring discharge, ion exchange, and the weathering and dissolution of As-containing minerals in silicate rocks Elevated F concentrations (0.01–1.41 mg/L) were observed in Gaize(GZ) of the Luoren River Basin and Ritu(RT) of the Maka River Basin, driven by evaporation and the dissolution of F-containing minerals in evaporitic salt rocks and silicate rocks. NO3 concentrations ranged from 1.44-30.2 mg/L, and were mainly influenced by human activities. Groundwater quality was evaluated using the EWQI method. Groundwater samples from Gaer(GR)and Geji(GJ) in the Shiquan River Basin exhibited poor to very poor quality, while samples from the other five towns ranged from excellent to good. Health risks were simulated using the Monte Carlo method, revealing that both carcinogenic and non-carcinogenic risks require attention, particularly in the Shiquan River Basin, where As pollution is significant. The effective exposure factor (EF) was the most critical parameter influencing health risks, followed by As concentration and body weight (BW), with BW showing a negative correlation and other parameters showing positive correlations with risk. This study offers new insights into groundwater pollution control mechanisms and associated health risks in the western urban area of the Qinghai-Tibet Plateau. It also provides valuable references for groundwater resource management and pollution prevention in the region and downstream South Asian countries.
近年来,地下水中砷(As)、氟化物(F -)和硝酸盐(NO3 -)浓度的升高引起了人们对饮用水安全的担忧。本研究从阿里地区6个盆地的7个城镇的水井中收集了52个地下水样本。通过数理统计、主离子比分析、熵权加权水质指数(EWQI)、蒙特卡罗模拟等方法,阐明了该地区地下水的水文地球化学成分特征、控制因素及潜在风险。地下水化学类型以HCO3 - ca为主,其离子浓度由高到低依次为Ca2+ >; Na+ > Mg2+ >; K+和HCO3−>; SO42−> Cl−> NO3−>F−。研究区西部石泉河流域的尕尔镇和格集镇砷污染最严重(0 ~ 0.09 mg/L),其主要原因是高砷温泉排放、离子交换、含砷矿物在硅酸盐岩中的风化和溶蚀作用等。罗仁河流域的改泽镇和玛卡河流域的日都镇的砷浓度升高(0.01 ~ 1.41 mg/L)。由蒸发作用和含氟矿物在蒸发盐岩和硅酸盐岩中的溶解作用驱动。NO3−浓度范围为1.44 ~ 30.2 mg/L,主要受人类活动影响。采用EWQI法对地下水水质进行评价。石泉河流域的葛尔镇和葛集镇的地下水水质为差到极差,其他5个镇的地下水水质为优到良。使用蒙特卡罗方法模拟了健康风险,揭示了致癌和非致癌风险都需要关注,特别是在砷污染严重的石泉河流域。影响健康风险的最关键参数是有效暴露因子(EF),其次是砷浓度和体重(BW),其中体重与健康风险呈负相关,其他参数与健康风险呈正相关。为本地区及下游南亚国家地下水资源管理和污染防治提供了有价值的参考。
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引用次数: 0
Misiones lateritic soil as a safely disposable, single-use adsorbent for arsenate removal 将红土作为一种安全的一次性吸附剂,用于去除砷酸盐
IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Pub Date : 2025-10-13 DOI: 10.1016/j.gsd.2025.101535
R. Boglione , M.C. Panigatti , C. Griffa , S. Keller , M.C. Schierano , M. Asforno , M. Farías , F.D. Reina , E.B. Halac , A.L. Marzocca , P.N. Alderete , P.C.V. Sánchez , E.G. De Seta , J.M. Meichtry
Lateritic soil (LS) from Misiones province, Argentina, was evaluated as a single-use, safely disposable adsorbent for pentavalent arsenic (As(V)) removal on three different systems:1) synthetic solutions at [As(V)]0 ≤ 10 mg L−1 and pH 6.5 (LSL); 2) synthetic solutions at [As(V)]0 ≤ 50 mg L−1 and pH 2 (LSH); and 3) three different groundwaters obtained nearby Rafaela city (Santa Fe, Argentina), with [As(V)]0 ≤ 0.165 mg L−1 and 7 < pH < 8 (LSR). Adsorption equilibrium followed the Langmuir isotherm, with qmax = 0.44 mg As g−1 and KL = 51 mg−1 L for LSL, and qmax = 2.1 mg As g−1 and KL = 0.6 mg−1 L mg for LSH. In LSR, an up to 47 times decrease in adsorbed As(V) (qe) was observed, attributable to the presence of interfering ions. Desorption with 0.10 M hydrochloric acid (HCl), acetic acid (HAc) and sodium hydroxide (NaOH) showed that NaOH achieved over 72 % As(V) release, while with HAc and HCl was <10 %, indicating near irreversible adsorption. As(V) concentrations in HCl and HAc leachates from LSL and LSR remained below the 1 mg L−1 limit for hazardous waste; for LSH, this limit was surpassed. Kinetic experiments with LSL showed that, after 1 h, desorbed As(V) peaked to 0.2 and 0.07 mg L−1 for HCl and HAc, respectively, followed by gradual re-adsorption onto precipitated iron oxy-hydroxides until [As(V)] ≤ 0.06 mg L−1 after 24 h. These results support the suitability of LS as a single-use, safely disposable adsorbent for treating waters with low As(V) concentrations.
来自阿根廷米西奥内斯省的红土(LS)作为一种一次性、安全的五价砷(as (V))吸附剂,在三种不同的系统上进行了评估:1)[as (V)]0≤10 mg L - 1和pH 6.5 (LSL)的合成溶液;2) [As(V)]0≤50 mg L−1,pH 2 (LSH)的合成溶液;3)在Rafaela市(Santa Fe, Argentina)附近获得的3种不同地下水,[As(V)]0≤0.165 mg L−1,pH < 8 (LSR)。吸附平衡遵循Langmuir等温线,LSL的qmax = 0.44 mg As g−1,KL = 51 mg−1,LSH的qmax = 2.1 mg As g−1,KL = 0.6 mg−1。在LSR中,由于干扰离子的存在,观察到吸附的As(V) (qe)减少了47倍。用0.10 M盐酸(HCl)、乙酸(HAc)和氢氧化钠(NaOH)解吸,NaOH的As(V)释放率达到72%以上,而用HAc和HCl解吸的As(V)释放率为10%,表明吸附接近不可逆。LSL和LSR的HCl和HAc渗滤液中的As(V)浓度仍低于危险废物1 mg L−1的限值;对于LSH来说,已经超过了这个限制。LSL的动力学实验表明,1 h后,HCl和HAc解吸的As(V)分别达到0.2和0.07 mg L−1,随后在24 h后逐渐重新吸附到沉淀的铁氧羟基上,直到[As(V)]≤0.06 mg L−1。这些结果支持了LS作为一次性安全吸附剂处理低As(V)浓度水的适宜性。
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Groundwater for Sustainable Development
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