Management Alternatives of Aquifer Storage, Distribution, and Simulation in Conjunctive Use

• Published in: Water (Basel) 2022-08, Vol.14 (15), p.2332
• Main Authors: Sahuquillo, Andrés, Cassiraga, Eduardo, Gómez-Hernández, J. Jaime, Andreu, Joaquín, Pulido-Velazquez, Manuel, Pulido-Velazquez, David, Álvarez-Villa, Oscar D., Estrela, Teodoro
• Format: Article
• Language: English
• Subjects: Aquifers; Artificial recharge; Base flow; Canals; Climate change; Coastal aquifers; Developing countries; Environmental conditions; Global warming; Groundwater; Hydrology; Irrigation; LDCs; Overexploitation; Reservoirs; Return flow; Rivers; Saline water intrusion; Salinization; Salt water intrusion; Seawater; Soil salinity; Stream flow; Surface water; Water availability; Water levels; Water resources; Water supply; Waterlogged ground; Waterlogging
• ISSN: 2073-4441; 2073-4441
• DOI: 10.3390/w14152332

Aquifers are ubiquitous, and their water is easy to obtain with low extraction costs. On many occasions, these characteristics lead to overexploitation due to important water level declines, reduction of river base flows, enhanced seawater intrusion, and wetland affection. The forecasted increase in water demands and global warming will impact the future availability of water resources. Conjunctive use of surface and subsurface waters can help in mitigating these impacts. There are two main conjunctive use strategies: artificial recharge (AR) and alternate conjunctive use (ACU). AR stores waters that are not to be used directly in aquifers. ACU utilizes groundwater in dry periods, while surface waters are preferred in wet ones; this allows the increase of water supply with lower dam storage, economic gains, and environmental advantages. Efficient conjunctive use can prevent soil salinization and waterlogging problems in semiarid countries due to excessive recharge from irrigation return flows or other origins. Groundwater is a neglected and generally misused resource to maintain environmental conditions. When considering the solution to a water resources problem, groundwater should always be part of the design as an alternative or a complementary resource. Aquifers have large inertia, and changes in their volumes are only noticeable after years of observations. Unfortunately, groundwater observation networks are much poorer than surface ones, something that should be changed if groundwater is to come to the rescue in these times of climate change. Human and material resources should be made available to monitor, control, analyze, and forecast groundwater.