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Soil and Groundwater Quality and Resources Assessment, 2nd Edition

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Soil and Water".

Deadline for manuscript submissions: closed (20 October 2025) | Viewed by 5852

Special Issue Editors


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Guest Editor
1. College of Water Conservancy, North China University of Water Resources and Electric Power, Zhengzhou 450046, China
2. Henan Provincial Key Laboratory of Hydrosphere and Watershed Water Security, North China University of Water Resources and Electric Power, Zhengzhou 450046, China
Interests: groundwater pollution; Isotope hydrogeochemistry
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Special Issue Information

Dear Colleagues,

Human activities, particularly in regions experiencing the development of industry and agriculture and the exploitation of mineral resources, pose increasing threats to terrestrial ecosystems and groundwater environments. This situation is critical in areas facing water scarcity, where groundwater serves as the primary source of drinking water. Such concerns center around the type, distribution, source, migration, transformation, and ecological health risks associated with various contaminants in soil–groundwater ecosystems. The concentrations of contaminants in these ecosystems are complex due to long-term water–rock interactions, diverse groundwater recharge patterns, hydrological–biogeochemical processes, and intensive human exploitation. Notably, the threat extends to both traditional and emerging inorganic and organic pollutants, which find their way into human bodies via bioaccumulation, food chains, and drinking water, thus leading to health risks such as chemical toxicity, radiation exposure, and carcinogenic effects. In the face of escalating environmental challenges and the urgent need for sustainable land management, the assessment of soil quality and resources has never been more crucial. Given the pivotal role that soil and groundwater play in supporting agriculture, maintaining natural landscapes, extracting geothermal resources, and providing potable water, it is imperative that we deepen our understanding of these resources.

In response to these environmental challenges, we have established a Special Issue entitled “Soil and Groundwater Quality and Resources Assessment, 2nd Edition”. This collection of research articles aims to illuminate the critical processes at play and promote innovative approaches that protect our soil and groundwater ecosystems.

Dr. Wanjun Jiang
Prof. Dr. Yizhi Sheng
Dr. Hairu Mao
Guest Editors

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Keywords

  • multiple contaminants
  • source apportionment
  • migration–transformation
  • ecological health risks
  • soil–groundwater system

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Related Special Issue

Published Papers (7 papers)

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Research

18 pages, 9017 KB  
Article
Research on the Influence of Groundwater Level Dynamic Rising Process on Buildings Based on Numerical Simulation
by Hongzhao Li, Mingxu Gu, Ming Zhang, Baiheng Ma, Xiaolong Zhu, Liangyu Gu, Jiaoyang Tai and Lili Chen
Water 2025, 17(20), 3014; https://doi.org/10.3390/w17203014 - 20 Oct 2025
Viewed by 199
Abstract
In the North China region, measures such as restricting groundwater extraction and promoting cross-basin water diversion have effectively alleviated the problem of excessive groundwater exploitation. Nevertheless, the continuous rise in groundwater levels may alter the mechanical properties of foundation soil layers, potentially leading [...] Read more.
In the North China region, measures such as restricting groundwater extraction and promoting cross-basin water diversion have effectively alleviated the problem of excessive groundwater exploitation. Nevertheless, the continuous rise in groundwater levels may alter the mechanical properties of foundation soil layers, potentially leading to geotechnical hazards such as foundation instability and the uneven settlement of structures. This study employs FLAC3D software to simulate the displacement, deformation, and stress–strain behavior of buildings and their surrounding strata during the dynamic recovery of groundwater levels, aiming to assess the impact of this process on structural integrity. Research findings indicate that the maximum building settlement within the study area reaches 54.8 mm, with a maximum inter-column differential settlement of 8.9 mm and a peak settlement rate of 0.16 mm/day. In regions where differential settlement aligns with the interface between the floor slab and walls, tensile stress concentrations are observed. The maximum tensile stress in these zones increases progressively from 1.8 MPa to 2.19 MPa, suggesting a potential risk of tensile cracking in the concrete structures. The influence of groundwater level recovery on buildings exhibits distinct phase characteristics, and the response mechanisms of different lithological strata vary significantly. Therefore, particular attention should be given to the physical properties and mechanical behavior of strata that are highly sensitive to variations in moisture content. These findings hold significant reference value for the sustainable development and utilization of underground space in the North China region. Full article
(This article belongs to the Special Issue Soil and Groundwater Quality and Resources Assessment, 2nd Edition)
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23 pages, 6751 KB  
Article
Health Risk Assessment of Groundwater in Cold Regions Based on Kernel Density Estimation–Trapezoidal Fuzzy Number–Monte Carlo Simulation Model: A Case Study of the Black Soil Region in Central Songnen Plain
by Jiani Li, Yu Wang, Jianmin Bian, Xiaoqing Sun and Xingrui Feng
Water 2025, 17(20), 2984; https://doi.org/10.3390/w17202984 - 16 Oct 2025
Viewed by 407
Abstract
The quality of groundwater, a crucial freshwater resource in cold regions, directly affects human health. This study used groundwater quality monitoring data collected in the central Songnen Plain in 2014 and 2022 as a case study. The improved DRASTICL model was used to [...] Read more.
The quality of groundwater, a crucial freshwater resource in cold regions, directly affects human health. This study used groundwater quality monitoring data collected in the central Songnen Plain in 2014 and 2022 as a case study. The improved DRASTICL model was used to assess the vulnerability index, while water quality indicators were selected using a random forest algorithm and combined with the entropy-weighted groundwater quality index (E-GQI) approach to realize water quality assessment. Furthermore, self-organizing maps (SOM) were used for pollutant source analysis. Finally, the study identified the synergistic migration mechanism of NH4+ and Cl, as well as the activation trend of As in reducing environments. The uncertainty inherent to health risk assessment was considered by developing a kernel density estimation–trapezoidal fuzzy number–Monte Carlo simulation (KDE-TFN-MCSS) model that reduced the distribution mis-specification risks and high-risk misjudgment rates associated with conventional assessment methods. The results indicated that: (1) The water chemistry type in the study area was predominantly HCO3–Ca2+ with moderately to weakly alkaline water, and the primary and nitrogen pollution indicators were elevated, with the average NH4+ concentration significantly increasing from 0.06 mg/L in 2014 to 1.26 mg/L in 2022, exceeding the Class III limit of 1.0 mg/L. (2) The groundwater quality in the central Songnen Plain was poor in 2014, comprising predominantly Classes IV and V; by 2022, it comprised mostly Classes I–IV following a banded distribution, but declined in some central and northern areas. (3) The results of the SOM analysis revealed that the principal hardness component shifted from Ca2+ in 2014 to Ca2+–Mg2+ synergy in 2022. Local high values of As and NH4+ were determined to reflect geogenic origin and diffuse agricultural pollution, whereas the Cl distribution reflected the influence of de-icing agents and urbanization. (4) Through drinking water exposure, a deterministic evaluation conducted using the conventional four-step method indicated that the non-carcinogenic risk (HI) in the central and eastern areas significantly exceeded the threshold (HI > 1) in 2014, with the high-HI area expanding westward to the central and western regions in 2022; local areas in the north also exhibited carcinogenic risk (CR) values exceeding the threshold (CR > 0.0001). The results of a probabilistic evaluation conducted using the proposed simulation model indicated that, except for children’s CR in 2022, both HI and CR exceeded acceptable thresholds with 95% probability. Therefore, the proposed assessment method can provide a basis for improved groundwater pollution zoning and control decisions in cold regions. Full article
(This article belongs to the Special Issue Soil and Groundwater Quality and Resources Assessment, 2nd Edition)
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28 pages, 3006 KB  
Article
Surface Water–Groundwater Interactions in a Sahelian Catchment: Exploring Hydrochemistry and Isotopes and Implications for Water Quality Management
by Issoufou Ouedraogo, Marnik Vanclooster, Frederic Huneau, Yuliya Vystavna, Seifu Kebede and Youssouf Koussoubé
Water 2025, 17(18), 2756; https://doi.org/10.3390/w17182756 - 17 Sep 2025
Viewed by 829
Abstract
The Sahel Transboundary Taoudéni Basin, covering about 20% of Burkina Faso, hosts vital aquifers critical for water security and development. Effective groundwater monitoring is essential for sustainable resource management. In the Kou sub-basin, groundwater quality assessment is increasingly important. This study integrates hydrochemistry, [...] Read more.
The Sahel Transboundary Taoudéni Basin, covering about 20% of Burkina Faso, hosts vital aquifers critical for water security and development. Effective groundwater monitoring is essential for sustainable resource management. In the Kou sub-basin, groundwater quality assessment is increasingly important. This study integrates hydrochemistry, water stable isotopes (δ18O, δ2H), GIS, and multivariate statistics to understand subsurface geochemical processes. A total of 48 samples—43 groundwater and 5 surface water—were analyzed for 19 hydrochemical parameters and isotopes. In surface water, δ18O ranged from −5.96‰ to −5.09‰, and δ2H from −37.65‰ to −29.15‰. In groundwater, δ18O ranged from −5.93‰ to −4.39‰, and δ2H from −34.62‰ to −25.05‰. The spatial distribution of δ18O and δ2H was mapped using inverse distance weighted (IDW) interpolation in ArcGIS 10.8. A δ2H vs. δ18O plot showed groundwater values clustered near the Global Meteoric Water Line, indicating minimal evaporation during recharge. Groundwater chemistry was dominated by Ca2+ > Na+ > Mg2+ > K+ and HCO3 > NO3 > Cl > SO42−. Key hydrogeochemical processes include water–rock interaction (leaching, weathering, ion exchange) and anthropogenic pollution. Isotopic signatures reveal heterogeneous recharge sources and aquifer connectivity. These findings enhance the understanding of water sources and geochemical processes in the Kou basin, supporting informed groundwater resource management. Full article
(This article belongs to the Special Issue Soil and Groundwater Quality and Resources Assessment, 2nd Edition)
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19 pages, 8399 KB  
Article
Integrating Inverse Modeling to Investigate Hydrochemical Evolution in Arid Endorheic Watersheds: A Case Study from the Qaidam Basin, Northwestern China
by Liang Guo, Yuanyuan Ding, Haisong Fang, Chunxue An, Wanjun Jiang and Nuan Yang
Water 2025, 17(14), 2074; https://doi.org/10.3390/w17142074 - 11 Jul 2025
Viewed by 652
Abstract
The hydrochemical characteristics and evolution mechanisms of groundwater are critical for accurately understanding the input–output budget of hydrochemical constituents in pristine groundwater. However, few studies have analyzed the changes in mineral precipitation and dissolution equilibrium along the groundwater flow path, especially in arid [...] Read more.
The hydrochemical characteristics and evolution mechanisms of groundwater are critical for accurately understanding the input–output budget of hydrochemical constituents in pristine groundwater. However, few studies have analyzed the changes in mineral precipitation and dissolution equilibrium along the groundwater flow path, especially in arid regions. This study integrated hydrochemical analysis, stable isotopes, and inverse hydrochemical modeling to identify groundwater recharge sources, hydrochemical evolution, and controlling mechanisms in an arid endorheic watershed, northwestern China. A stable isotope signature indicated that groundwater is primarily recharged by high-altitude meteoric precipitation and glacial snowmelt. The regional hydrochemical type evolved from HCO3·Cl-Ca·Mg·Na types in phreatic aquifers to more complex HCO3·Cl-Ca·Mg Na and HCO3·Cl-Na Mg types in confined aquifers and a Cl-Mg·Na type in high-salinity groundwater. The dissolution of halite, gypsum, calcite, K-feldspar, and albite was identified as the primary source of dissolved substances and a key factor controlling the hydrochemical characteristics. Meanwhile, hydrochemical evolution is influenced by cation exchange, mineral dissolution–precipitation, and carbonate equilibrium mechanisms. Inverse hydrochemical modeling demonstrated that high-salinity groundwater has experienced intensive evaporation and quantified the transfer amounts of associated minerals. This study offers deeper insight into hydrochemical evolution in the Golmud River watershed and elucidates mineral transport and enrichment mechanisms, providing a theoretical basis for investigating hydrochemical metallogenic processes. Full article
(This article belongs to the Special Issue Soil and Groundwater Quality and Resources Assessment, 2nd Edition)
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21 pages, 2113 KB  
Article
Research on Ecological–Environmental Geological Survey and Evaluation Methods for the Kundulun River Basin in Baotou City
by Yi Hao, Junwei Wan, Yihui Xin, Wenhui Zhou, Yongli Li, Lei Mao, Xiaomeng Li, Limei Mo and Ruijia Li
Water 2025, 17(13), 1926; https://doi.org/10.3390/w17131926 - 27 Jun 2025
Cited by 1 | Viewed by 614
Abstract
The Kundulun River Basin is the most prominent branch of the Yellow River system within the jurisdiction of Baotou City. As an important water source and ecological barrier, its ecological quality is directly related to the ecological security and sustainable development of the [...] Read more.
The Kundulun River Basin is the most prominent branch of the Yellow River system within the jurisdiction of Baotou City. As an important water source and ecological barrier, its ecological quality is directly related to the ecological security and sustainable development of the surrounding areas. This study selected the Kundulun River Basin in Baotou City as the research area. On the basis of collecting relevant information, a field investigation was conducted on the ecological and geological conditions of the atmospheric surface subsurface Earth system, using the watershed as the survey scope and water as the carrier for the transfer and conversion of materials and energy in the watershed. This study selected the main factors that affect the ecological geological quality of the watershed and established an evaluation model using the analytic hierarchy process, the coefficient of variation method, and the comprehensive analysis method. We have established an ecological geological quality evaluation index system for the Kundulun River Basin. We conducted quantitative evaluation and comprehensive analysis of regional ecological and geological environment quality. The results indicate that ecological environment indicators contribute the most to the ecological quality of the study area, while the impact of human activities on ecological quality is relatively small. From the perspective of evaluation indicators, grassland has the highest weight, followed by precipitation, groundwater depth, forest land, and cultivated land. Approximately 30.26% of the land in the research area is in a state of high or relatively high ecological and geological–environmental quality risk. It can be seen that the overall quality of the ecological geological environment is not optimistic and needs further protection. Full article
(This article belongs to the Special Issue Soil and Groundwater Quality and Resources Assessment, 2nd Edition)
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24 pages, 4712 KB  
Article
Characterization of Groundwater Dynamics and Their Response Mechanisms to Different Types of Compound Stress in a Typical Hilly Plain Area
by Qian Zhang, Meng Zhang, Wanjun Jiang, Yang Hao, Feiwu Chen and Mucheng Zhang
Water 2025, 17(13), 1846; https://doi.org/10.3390/w17131846 - 20 Jun 2025
Cited by 1 | Viewed by 1005
Abstract
Groundwater is a crucial source of water supply and an important ecological element globally. Research on the dynamic characteristics of groundwater and their causative mechanisms is fundamental to objectively evaluating groundwater resources and their sustainable utilization. Based on the large amount of hydrogeological [...] Read more.
Groundwater is a crucial source of water supply and an important ecological element globally. Research on the dynamic characteristics of groundwater and their causative mechanisms is fundamental to objectively evaluating groundwater resources and their sustainable utilization. Based on the large amount of hydrogeological data collected and analyzed in typical hilly plain areas, a multi-factor weighted comprehensive evaluation system (MFWCES) based on GIS was used to evaluate the response of groundwater dynamics to combined stress elements in Tangshan City. The study area is located in the plains and hilly regions of Tangshan City. The evaluation system was based on seven influencing factors, including hydraulic conductivity, soil media, aquifer thickness, depth of groundwater, land use type, extraction intensity of groundwater, and groundwater evaporation. The results of groundwater dynamics in the study area were obtained by weighted comprehensive evaluation, with their score size ranging from 2.4 to 12.7. The spatial distribution of groundwater dynamics was classified into four categories: rapid response (10.3–12.7), dual response to precipitation and anthropogenic extraction (9.6–10.3), delayed response (7.6–9.6), and strong superimposed response to human activities (2.4–7.6). The related conclusions will provide key references for regional water resource planning, ecological protection, and the development of differentiated groundwater management strategies under compound stress. Full article
(This article belongs to the Special Issue Soil and Groundwater Quality and Resources Assessment, 2nd Edition)
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29 pages, 3276 KB  
Article
Study on the Factors Affecting the Drainage Efficiency of New Integrated Irrigation and Drainage Networks and Network Optimization Based on Annual Cost System
by Zhiwei Zheng, Mingrui Li, Tianzhi Wang and Hejing Ren
Water 2025, 17(8), 1201; https://doi.org/10.3390/w17081201 - 16 Apr 2025
Viewed by 1354
Abstract
With the frequent occurrence of extreme weather events worldwide, the compound frequency of drought and flood events has significantly increased, imposing multidimensional pressures on agricultural water resource management. Agricultural water consumption accounts for approximately 70%, with severe waste, as a large amount of [...] Read more.
With the frequent occurrence of extreme weather events worldwide, the compound frequency of drought and flood events has significantly increased, imposing multidimensional pressures on agricultural water resource management. Agricultural water consumption accounts for approximately 70%, with severe waste, as a large amount of water is lost during transmission and distribution. Faced with increasingly severe and frequent extreme weather, traditional drainage systems may become unsustainable. Identifying the factors influencing drainage time is crucial for efficient drainage. The MIKE URBAN model has significant potential in farmland waterlogging simulation and drainage network optimization. This study validated the model’s accuracy based on infiltration well overflow capacity experiments, with Average Relative Error (ARE) values of 2.29%, 6.52%, 4.41%, 3.17%, 4.37%, and 5.69%, demonstrating good simulation accuracy. The MIKE URBAN model was used to simulate drainage networks, explore factors affecting drainage time, establish an annual cost system for the drainage network, and optimize the network using a genetic algorithm with the objective of minimizing annual costs. Research findings: There is a clear negative correlation between the maximum inflow of infiltration wells and drainage time. As inflow increases, drainage becomes faster, but beyond 0.0075 m3/s (27 m3/h), the efficiency gains level off. This indicates that selecting infiltration wells with at least a 20% opening ratio is essential. Similarly, increasing the collector’s diameter enhances drainage efficiency significantly, though the effect follows a diminishing return pattern. While smaller lateral spacing improves local water collection, it may lead to flow congestion if the collector is undersized; conversely, larger spacing increases drainage paths and delays, even if the collector is large. An optimal spacing range of 100–150 m is suggested alongside the collector diameter. Lateral diameter also affects performance: increasing it reduces drainage time, but the benefit plateaus around 200 mm, making further enlargement cost-ineffective. The genetic algorithm helped to optimize the drainage network design. Utilizing the genetic algorithm, the drainage network was optimized in just 15 iterations. The fitness function value rapidly decreased from 351,000 CNY to 55,000 CNY and then stabilized, reducing the annual cost from 59,640.67 CNY to 45,337.86 CNY—a 24% savings—highlighting the approach’s effectiveness in designing efficient and economical farmland drainage systems. This study has shown that the simulation-based optimization of drainage networks provides a more rational and cost-effective approach to planning drainage infrastructure. Full article
(This article belongs to the Special Issue Soil and Groundwater Quality and Resources Assessment, 2nd Edition)
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