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Dynamic Response of Water and Soil Resources in the Context of Climate Change and Human Activities

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

Deadline for manuscript submissions: 31 October 2025 | Viewed by 222

Special Issue Editors


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Guest Editor
School of Water and Environment, Chang’an University, Xi’an 710054, China
Interests: groundwater resource evaluation and environmental protection; ecological hydrogeology and water safety; water and soil resources security; geological hazard risk assessment
Special Issues, Collections and Topics in MDPI journals

E-Mail Website
Guest Editor
Department of Hydraulic Engineering, Hebei University of Water Resources and Electric Engineering, Cangzhou Technology Innovation Center of Remote Sensing and Smart Water, Cangzhou 061001, China
Interests: water and soil resources security; groundwater hydrology; groundwater of saline–alkali land; water resources evaluation; water resources optimization; geological hazard risk assessment; numerical simulation
Special Issues, Collections and Topics in MDPI journals

E-Mail Website
Guest Editor
School of Water and Environment, Chang’an University, Xi’an 710054, China
Interests: soil water transfer; vapor flow; hydrological cycle; freeze–thaw process; numerical simulation

Special Issue Information

Dear Colleagues,

Water and soil resources are foundational to sustaining ecosystems, agricultural productivity, and human livelihoods. However, these critical resources face unprecedented pressures from climate change and intensified human activities, including urbanization, industrialization, and land-use alterations. Rising global temperatures, shifting precipitation patterns, and extreme weather events are altering hydrological cycles and soil stability, while anthropogenic interventions such as overexploitation, pollution, and unsustainable practices further exacerbate resource degradation. Understanding the dynamic interplay between natural processes and human influences is essential to mitigate risks and ensure the sustainable management of water and soil systems. This Special Issue invites innovative research addressing the integrated responses of water and soil resources to climate variability and anthropogenic stressors. Topics of interest include, but are not limited to, the following:

  • Impacts of climate change on hydrological regimes and soil health;
  • Human-induced alterations in water availability and soil quality;
  • Modeling and prediction of water–soil interactions under changing environments;
  • Pollution mechanisms and remediation strategies for water and soil systems;
  • Socio-ecological resilience and adaptive management approaches;
  • Technological advances in monitoring and sustainable resource utilization.

By synthesizing multidisciplinary insights, this Special Issue aims to advance scientific understanding and inform policies for balancing resource conservation with developmental needs. Contributions from hydrology, soil science, remote sensing, climatology, ecology, and environmental engineering are encouraged.

Prof. Dr. Yudong Lu
Dr. Huanhuan Li
Dr. Ce Zheng
Guest Editors

Manuscript Submission Information

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Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Water is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2600 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • water and soil resources security
  • water–soil interactions
  • climate change impacts on water and soil
  • anthropogenic stressors to water and soil
  • hydrological modeling
  • soil degradation
  • pollution remediation
  • sustainable agriculture
  • ecosystem resilience
  • land-use change

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Published Papers (1 paper)

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Research

26 pages, 9639 KiB  
Article
Hydrochemical Characteristics and Evolution Laws of Groundwater in Huangshui River Basin, Qinghai
by Ziqi Wang, Ting Lu, Shengnan Li, Kexin Zhou, Yidong Gu, Bihui Wang and Yudong Lu
Water 2025, 17(9), 1349; https://doi.org/10.3390/w17091349 - 30 Apr 2025
Viewed by 107
Abstract
Groundwater plays a leading role in ecological environment protection in semi-arid regions. The Huangshui River Basin is located in the Tibetan Plateau and Loess Plateau transition zone of semi-arid areas. Its ecological environment is relatively fragile, and there is an urgent need for [...] Read more.
Groundwater plays a leading role in ecological environment protection in semi-arid regions. The Huangshui River Basin is located in the Tibetan Plateau and Loess Plateau transition zone of semi-arid areas. Its ecological environment is relatively fragile, and there is an urgent need for systematic study of the basin to develop a groundwater environment and realize the rational and efficient development of water resources. In this study, methodologically, we combined the following: 1. Field sampling (271 groundwater samples across the basin’s hydrogeological units); 2. Comprehensive laboratory analysis of major ions and physicochemical parameters; 3. Multivariate statistical analysis (Pearson correlation, descriptive statistics); 4. Geospatial techniques (ArcGIS kriging interpolation); 5. Hydrochemical modeling (Piper diagrams, Gibbs plots, PHREEQC simulations). Key findings reveal the following: 1. Groundwater is generally weakly alkaline (pH 6.94–8.91) with TDS ranging 155–10,387 mg/L; 2. Clear spatial trends: TDS and major ions (Na+, Ca2+, Mg2+, Cl, SO42−) increase along flow paths; 3. Water types evolve from Ca-HCO3-dominant (upper reaches) to complex Ca-SO4/Ca-Cl mixtures (lower reaches); 4. Water–rock interactions dominate hydrochemical evolution, with secondary cation exchange effects; 5. PHREEQC modeling identifies dominant carbonate dissolution (mean SIcalcite = −0.32) with localized evaporite influences (SIgypsum up to 0.12). By combining theoretical calculations and experimental results, this study reveals distinct hydrochemical patterns and evolution mechanisms. The groundwater transitions from Ca-HCO3-type in upstream areas to complex Ca-SO4/Cl mixtures downstream, driven primarily by dissolution of gypsum and carbonate minerals. Total dissolved solids increase dramatically along flow paths (155–10,387 mg/L), with Na+ and SO42− showing the strongest correlation to mineralization (r > 0.9). Cation exchange processes and anthropogenic inputs further modify water chemistry in midstream regions. These findings establish a baseline for sustainable groundwater management in this ecologically vulnerable basin. Full article
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