4.5 Article

Alleviating drought and water scarcity in the Mediterranean region through managed aquifer recharge

Journal

HYDROGEOLOGY JOURNAL
Volume 30, Issue 6, Pages 1685-1699

Publisher

SPRINGER
DOI: 10.1007/s10040-022-02513-5

Keywords

Artificial recharge; Groundwater statistics; Trend analysis; Standardised precipitation index; Standardised groundwater level index

Funding

  1. European Union [814066]
  2. CRUE-CSIC
  3. Springer Nature
  4. Marie Curie Actions (MSCA) [814066] Funding Source: Marie Curie Actions (MSCA)

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This study evaluates the potential of managed aquifer recharge (MAR) to offset the adverse effects of drought and water scarcity on groundwater storage. The results show that MAR can effectively alleviate the impacts of water scarcity and drought, providing an adaptation solution to climate change worldwide.
Drought and water scarcity can significantly impair the sustainable development of groundwater resources, a scenario commonly found in aquifers in the Mediterranean region. Water management measures to address these drivers of groundwater depletion are highly relevant, especially considering the increasing severity of droughts under climate change. This study evaluates the potential of managed aquifer recharge (MAR) to offset the adverse effects of drought and water scarcity on groundwater storage. Los Arenales aquifer (central Spain), which was unsustainably exploited for irrigation in the second half of the twentieth century, is employed as a case study. Two neighbouring zones within this aquifer are contrasted, namely, Los Arenales (LA) and Medina del Campo (MC). The primary difference between them in terms of water resources management is the wide-scale implementation of MAR systems in LA since the early 2000s. Several groundwater statistical methods are used. Groundwater-level trend analysis and average piezometric levels show in LA a faster recovery of aquifer storage and less susceptibility to drought compared to MC. On the other hand, standardised precipitation indexes and standardised groundwater level indexes of detrended groundwater-level time series, which do not include the effects of MAR, show that LA can be more negatively affected by drought and groundwater abstraction. The sharper recovery of piezometric levels in LA when considering MAR, and bigger drought impacts observed when the effects of this measure are removed, demonstrate that MAR can effectively alleviate the impacts of water scarcity and drought, providing an adaptation solution to climate change worldwide.

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