Groundwater Decline and Depletion

A special issue of Hydrology (ISSN 2306-5338). This special issue belongs to the section "Surface Waters and Groundwaters".

Deadline for manuscript submissions: closed (30 May 2023) | Viewed by 16819

Special Issue Editors


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Guest Editor
School of Environmental Sciences, Jawaharlal Nehru University, New Delhi, India
Interests: hydrochemistry; groundwater

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Guest Editor
Department of Applied Sciences, Faculty of Engineering and Science, Curtin University Malaysia, CDT 250, Miri 98009, Sarawak, Malaysia
Interests: environmental hydrogeochemistry

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Guest Editor
Research Scientist, Water Research Centre, Kuwait Institute for Scientific Research, Safat, Kuwait
Interests: geochemistry; hydrogeology; aquatic ecosystems; hydrology; groundwater; water chemistry; hydrogeochemistry; groundwater quality; environmental chemistry; water quality

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Guest Editor
Department of Geology, Ravenshaw University, Cuttack, Odisha, India
Interests: hydrochemistry; hydrology; hydrochemical modeling; isotopes

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Guest Editor
Department of Hydrology, University of Zululand, Richards Bay, South Africa
Interests: groundwater quality; groundwater management; groundwater modeling; hydrogeochemistry; hydrogeology
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Special Issue Information

Dear Colleagues,

Rapid urbanization and climate change have continued to affect both the quality and quantity of groundwater. The increase in population and climate change has led to the mismanagement and high abstraction of groundwater to fulfil the needs, resulting in the decline and depletion of the water level. This has led to an increase in the aquifer stress index in many cities across the world. This important resource, groundwater, is vulnerable to contamination by chemicals resulting from human activities such as the population density increasing. While discussing groundwater quality, groundwater chemistry should be considered as it is the deciding factor for utility. On the other hand, groundwater is intimately connected with the landscape and land use that it underlies and most of the landscape and is vulnerable to the anthropogenic activities on the land surface above. In this scenario, the United Nations has declared in the Sustainable Development Goals (SDG-6, Clean Water, Sanitation and Hygiene) to achieve the target “universal and equitable access to safe and affordable drinking water for all” by 2030. In order to achieve this, the problem should be addressed in a multi-dimensional approach considering the end users, stakeholders, policymakers, researchers, agriculturalists, and politicians. In recent years, artificial intelligence methods have been widely used to predict water-system variables due to their high ability to learn complex mathematical relationships between output and prediction variables. One of the most common machine-learning algorithms used to predict the groundwater level is the artificial neural network (ANN). A large portion of the world’s groundwater is stored in the aquifers shared by several counties known as trans-boundary aquifers (TBA). So far, 592 identified trans-boundary aquifers were identified as defined in the European Union Water Framework Directive, EU WFD, underlying almost every nation. There is an urgent need for improved governance to address the over-exploitation and degradation of this vital ‘shared and hidden' groundwater aquifer, to preserve and optimize this decline and depletion. Groundwater depletion can pose other serious threats to the environment apart from the depletion of resources, such as saltwater intrusion, submarine groundwater discharge, limited biodiversity, and the development of dangerous sinkholes. Reports also indicate that more comprehensive research and data sharing is essential to replenish the resource and conserve it for sustainable use in the future.

Themes:

  • Traditional methods to enhance the aquifer potential.
  • Impact of land-use/land-cover changes on groundwater.
  • Influence of surface water and extreme events on groundwater resources.
  • Modern approaches (machine learning, IoT, AI, GIS, RS, big-data analysis, groundwater modeling) for groundwater management.
  • Geochemical approaches (soil and water chemistry) to assess the aquifer vulnerability through natural and anthropogenic processes.
  • The impact of population and climate change on groundwater resources.
  • SDGs—capacity building and community-level participation for groundwater management.

Prof. Dr. AL. Ramanathan
Dr. Prasanna Mohan Viswanathan
Dr. Chidambaram Sabarathinam
Dr. Banajarani Panda
Dr. Elumalai Vetrimurugan
Guest Editors

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Keywords

  • aquifer
  • SDG
  • TBA
  • pollution
  • groundwater chemistry
  • land use/landcover
  • artificial intelligence

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Published Papers (5 papers)

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Research

20 pages, 8049 KiB  
Article
Hydrogeochemistry, Geothermometry, and Sourcing of High Dissolved Boron, Tungsten, and Chlorine Concentrations in the Trans-Himalayan Hotsprings of Ladakh, India
by Arif H. Ansari, Veeru Kant Singh, Pankaj Kumar, Mukund Sharma, Anupam Sharma, Satyakam Patnaik, Gurumurthy P. Gundiga, Ishwar Chandra Rahi, Mohammad Arif Ansari and AL Ramanathan
Hydrology 2023, 10(6), 118; https://doi.org/10.3390/hydrology10060118 - 24 May 2023
Cited by 3 | Viewed by 3316
Abstract
Boron (B) and Tungsten (W) are often found enriched in high-temperature geothermal waters associated with the development of subduction-related mafic to felsic arc magma. However, knowledge about the sourcing and transportation of these elements from such hydrothermal systems is sparse and ambiguous. Being [...] Read more.
Boron (B) and Tungsten (W) are often found enriched in high-temperature geothermal waters associated with the development of subduction-related mafic to felsic arc magma. However, knowledge about the sourcing and transportation of these elements from such hydrothermal systems is sparse and ambiguous. Being the only active continental collision site in the world, the Trans-Himalaya offers a unique chance to study how continental collision sources the high boron and tungsten concentrations in geothermal fluids. This study investigated the distribution of trace elements, major cations, and anions in three physicochemically distinct hotspring sites in the Ladakh region. The results were integrated with the existing geochemical and isotopic data to address the research problem more effectively. This study exhibits that the extreme concentrations of boron, sodium, chlorine, potassium, and tungsten in the hotspring waters were primarily governed by magmatic fluid inputs. In addition, this study recorded the highest-ever chlorine and boron concentrations for the Trans-Himalayan hotspring waters. The highest-ever boron and chlorine concentrations in the hotspring waters probably represented an increase in magmatic activity in the deeper source zone. Full article
(This article belongs to the Special Issue Groundwater Decline and Depletion)
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22 pages, 6378 KiB  
Article
Determining the Optimal Aquifer Exploitation under Artificial Recharge using the Combination of Numerical Models and Particle Swarm Optimization
by Rahimeh Maghsoudi, Saman Javadi, Mojtaba Shourian and Golmar Golmohammadi
Hydrology 2023, 10(5), 100; https://doi.org/10.3390/hydrology10050100 - 25 Apr 2023
Cited by 2 | Viewed by 2372
Abstract
Determining optimal exploitation from aquifers is always a major challenge, especially for aquifers facing a drop in their groundwater level. In aquifers with artificial recharge, more complex algorithms are required to determine the optimal exploitation amount. Therefore, in this study, the optimal amount [...] Read more.
Determining optimal exploitation from aquifers is always a major challenge, especially for aquifers facing a drop in their groundwater level. In aquifers with artificial recharge, more complex algorithms are required to determine the optimal exploitation amount. Therefore, in this study, the optimal amount of harvest from the exploitation wells has been determined using a combined simulation–optimization model considering the artificial recharge in Yasouj aquifer in Iran. The model is based on a combination of MODFLOW code and gene expression programming (GEP) simulator tool to simulate the aquifer and particle swarm optimization (PSO) to maximize the total exploitation from the aquifer. The simulation results showed that the artificial recharge was ineffective in maximum exploitation from the aquifer. As a result, considering several constraints, including the maximum pumping rate from the aquifer and the permissible drop in the groundwater level, the maximum exploitation from the aquifer was defined as the objective function. The optimization results showed that the optimal exploitation rate is equal to 8.84 million cubic meters (MCM) per year, and only 74% of the water from artificial recharge can be used based on this amount. Additionally, the most appropriate locations to exploit this amount of water are the northwest and east of the aquifer. According to the findings, it is suggested to ban exploitation from the central and southern parts of the aquifer due to the low groundwater level. The results of the sensitivity analysis show that the reduction in the maximum exploitation rate along with a 50% drop in the groundwater level play an effective role in decreasing the optimal exploitation amount. Full article
(This article belongs to the Special Issue Groundwater Decline and Depletion)
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17 pages, 4953 KiB  
Article
Influence of Dissolved Oxygen, Water Level and Temperature on Dissolved Organic Carbon in Coastal Groundwater
by Thilagavathi Rajendiran, Chidambaram Sabarathinam, Banajarani Panda and Vetrimurugan Elumalai
Hydrology 2023, 10(4), 85; https://doi.org/10.3390/hydrology10040085 - 6 Apr 2023
Cited by 12 | Viewed by 3711
Abstract
The quality of groundwater has been severely impacted by urbanization around coasts. The change in climate and land use patterns has deteriorated the quality and availability of groundwater. One of the main issues in contemporary groundwater quality research is dissolved organic carbon (DOC) [...] Read more.
The quality of groundwater has been severely impacted by urbanization around coasts. The change in climate and land use patterns has deteriorated the quality and availability of groundwater. One of the main issues in contemporary groundwater quality research is dissolved organic carbon (DOC) in the water. The influence of DO, water level and water temperature on DOC in groundwater was identified in the current study by sampling 68 groundwater samples. The analytical results revealed that ~18% of total samples have DOC > 5 mg/L. The groundwater samples represented in the urban regions show high DOC. The samples with higher DOC correlated positively with dissolved inorganic ions, such as Ca, K, NO3, Fe and DO. Domestic wastewater, agricultural runoff and local geology all have an impact on the DOC of groundwater. Groundwater chemistry is shown to be controlled by both aerobic and anaerobic conditions based on the DOC’s interactions with other ions. The study interrelates various sources, such as land use, geology, water level and temperature, to the DOC in groundwater and infers that the levels are higher in shallow groundwater, predominantly around the built-up region followed by the agricultural region. The temperature changes enhance the DOC in groundwater due to the variation in microbial activity. The shallow water level with a lower temperature shows the maximum DOC. Apart from the sediment organic matter and microbes, the study also attributes land use pattern to the source of DOC in groundwater. Full article
(This article belongs to the Special Issue Groundwater Decline and Depletion)
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27 pages, 76507 KiB  
Article
Simulating Groundwater Potential Zones in Mountainous Indian Himalayas—A Case Study of Himachal Pradesh
by Anshul Sud, Rahul Kanga, Suraj Kumar Singh, Gowhar Meraj, Shruti Kanga, Pankaj Kumar, AL. Ramanathan, Sudhanshu and Vinay Bhardwaj
Hydrology 2023, 10(3), 65; https://doi.org/10.3390/hydrology10030065 - 10 Mar 2023
Cited by 27 | Viewed by 3867
Abstract
Groundwater resources are increasingly important as the main supply of fresh water for household, industrial, and agricultural activities. However, overuse and depletion of these resources can lead to water scarcity and resource deterioration. Therefore, assessing groundwater availability is essential for sustainable water management. [...] Read more.
Groundwater resources are increasingly important as the main supply of fresh water for household, industrial, and agricultural activities. However, overuse and depletion of these resources can lead to water scarcity and resource deterioration. Therefore, assessing groundwater availability is essential for sustainable water management. This study aims to identify potential groundwater zones in the Bilaspur district of Himachal Pradesh using the Multi Influencing Factor (MIF) technique, a modern decision-making method widely used in various sectors. Geospatial models were integrated with the MIF technique to evaluate prospective groundwater areas. Grid layouts of all underground water influencing variables were given a predetermined score and weight in this decision-making strategy. The potential groundwater areas were then statistically assessed using graded data maps of slope, lithology, land-use, lineament, aspect, elevation, soil, drainage, geomorphology, and rainfall. These maps were converted into raster data using the raster converter tool in ArcGIS software, utilizing Survey of India toposheets, SRTM DEM data, and Resourcesat-2A satellite imageries. The prospective groundwater zones obtained were classified into five categories: nil–very low, covering 0.34% of the total area; very low–low (51.64%); low–moderate (4.92%); moderate–high (18%) and high–very high (25%). Scholars and policymakers can collaborate to develop systematic exploration plans for future developments and implement preservative and protective strategies by identifying groundwater recharge zones to reduce groundwater levels. This study provides valuable insights for long-term planning and management of water resources in the region. Full article
(This article belongs to the Special Issue Groundwater Decline and Depletion)
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22 pages, 10892 KiB  
Article
Methods for Characterizing Groundwater Resources with Sparse In Situ Data
by Ren Nishimura, Norman L. Jones, Gustavious P. Williams, Daniel P. Ames, Bako Mamane and Jamila Begou
Hydrology 2022, 9(8), 134; https://doi.org/10.3390/hydrology9080134 - 27 Jul 2022
Cited by 4 | Viewed by 2673
Abstract
Accurate characterization of groundwater resources is required for sustainable management. Due to the cost of installing monitoring wells and challenges in collecting and managing in situ data, groundwater data are sparse—especially in developing countries. In this study, we demonstrate an analysis of long-term [...] Read more.
Accurate characterization of groundwater resources is required for sustainable management. Due to the cost of installing monitoring wells and challenges in collecting and managing in situ data, groundwater data are sparse—especially in developing countries. In this study, we demonstrate an analysis of long-term groundwater storage changes using temporally sparse but spatially dense well data, where each well had as few as one historical groundwater measurement. We developed methods to synthetically estimate groundwater table elevation (WTE) times series by clustering wells using two different methods; a uniform grid and k-means-constrained clustering to create pseudo-wells. These pseudo-wells had a more complete groundwater level time history, which we then temporally and spatially interpolated to analyze groundwater storage changes in an aquifer. We demonstrated these methods on the Beryl-Enterprise aquifer in Utah, USA, where other researchers quantified the groundwater storage depletion rate, and the wells had a large number of historical measurements. We randomly used one measurement per well and showed that our methods yielded storage depletion rates similar to published values. We applied the method to a region in southern Niger where wells had only one measurement per well, and showed that our estimated groundwater storage change trend reasonably matched that which was calculated using GRACE satellite data. Full article
(This article belongs to the Special Issue Groundwater Decline and Depletion)
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