An Assessment of Groundwater Recharge at A Regional Scale for Sustainable Resource Management: Province of Alicante (SE Spain)
Autor: | Rebeca Palencia, J. M. Andreu, Ernesto García-Sánchez, Miguel Fernández-Mejuto |
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Přispěvatelé: | Universidad de Alicante. Departamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante. Instituto Universitario del Agua y las Ciencias Ambientales, Geología Aplicada e Hidrogeología |
Jazyk: | angličtina |
Rok vydání: | 2021 |
Předmět: |
Mediterranean climate
Southeast Spain lcsh:Hydraulic engineering Groundwater flow Water table Geography Planning and Development Aquifer Aquatic Science Biochemistry Groundwater recharge lcsh:Water supply for domestic and industrial purposes lcsh:TC1-978 Spring (hydrology) Precipitation Mediterranean region Water Science and Technology Hydrology aquifer management geography lcsh:TD201-500 geography.geographical_feature_category Recharge coefficient groundwater recharge Geodinámica Externa Natural Aquifer Recharge (RENATA) Environmental science recharge coefficient Aquifer management Groundwater |
Zdroj: | Water, Vol 13, Iss 862, p 862 (2021) RUA. Repositorio Institucional de la Universidad de Alicante Universidad de Alicante (UA) Water Volume 13 Issue 6 |
ISSN: | 2073-4441 |
Popis: | For decades, the Province of Alicante, located in the Southeast of Spain, has experienced important economic development associated with groundwater exploitation. The scarcity of superficial resources and irregular distribution in the time and space of rainfall, typical of the Mediterranean environment, together with the extensive limestone outcrops, have made groundwater a key resource for the area. However, insufficient knowledge about aquifers, especially the lack of precise recharge estimates, hinders regional water management. This study establishes updated recharge estimates and water budgets for the 200 aquifers found in Alicante, using readily usable methodologies and available data. These are soil water budget models, groundwater flow models, water table fluctuation methods, and spring flow analyses. The results show low mean annual values of recharge from precipitation (69 mm/year and a coefficient of 12%) and two main differentiated domains. The first one, in the northeast of the province, under more humid climatic conditions with larger carbonate aquifer systems, has higher recharge coefficients, ranging from 14% to 24%, and greater resources. For the rest of the province, where aquifers are smaller and annual averages of rainfall range between 250 and 400 mm, average recharge rates are low (9–12%). This research was funded partially by the projects of the Spanish Ministry of Economy and Competitiveness (ALTERACLIM; CGL2015-69773-C2-1-P) and the Ministry of Science and Innovation (PID2019-111332RB-C21). In the same way, this work was partially funded by Cátedra del Agua (Water Chair) of the University of Alicante and Diputación de Alicante (https://catedradelaguaua.org/ accessed on 10 February 2021). |
Databáze: | OpenAIRE |
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