Affiliation:
1. United Nations University Institute for the Advanced Study of Sustainability Shibuya‐ku Tokyo 150‐8925 Japan
2. Centre for Hydrogeology and Geothermics University of Neuchâtel Rue Emile Argand 11 2000 Neuchâtel Switzerland
3. Department of Environment Systems, Graduate School of Frontier Sciences The University of Tokyo, Kashiwa Chiba 277‐8563 Japan
Abstract
AbstractSubsurface dam is a promising engineering technology for groundwater resources development. However, the possible impacts of these dams on the groundwater environment have been a major concern. Here, we used a three‐dimensional (3D), variable‐density, unsaturated‐saturated groundwater flow model to explore how a groundwater‐storage‐type subsurface dam, built in the freshwater domain of an unconfined coastal aquifer, affected groundwater levels and salinity in the downstream area. Model results suggested that, after subsurface dam construction, groundwater levels in the downstream area showed intensified fluctuations in terms of phase advances, greater amplitudes, and higher frequencies following heavy rainfall events. Numerical simulations with variable subsurface dam scenarios indicated that the groundwater level fluctuations were further intensified with a higher crest elevation or a shorter distance from the coast. Moreover, during the recharging period of the subsurface reservoir, sea water in the downstream area intruded landward from its initial location, which can at least temporarily threaten water quality near the coast. A higher dam crest elevation prolonged the duration of sea water intrusion, while a dam positioned closer to the coast induced sea water intrusion with a greater horizontal extent. General implications are discussed with respect to improving assessment methodologies and engineering designs of subsurface dams.
Funder
Japan Society for the Promotion of Science
Kurita Water and Environment Foundation
Subject
Computers in Earth Sciences,Water Science and Technology
Cited by
3 articles.
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