Integrating current and historical water chemistry data with long-term piezometric records to develop a regional-scale conceptual flow model: Las Salinas spring, Medina del Campo, Spain

Study region: Old Las Salinas spring in Medina del Campo, Duero river basin, central Spain. Study focus: Medina del Campo groundwater body (MCGWB) is a multilayer semiconfined aquifer subject to intensive pumping since the 1970’s, where the current existence of spas where there used to be traditiona...

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Main Authors: A. De la Hera-Portillo, J. López-Gutiérrez, C. Marín-Lechado, P. Martínez-Santos, A. Ruíz-Constán, M.M. Corral-Lledó, E. Galindo-Rodríguez, R. Mediavilla, J.I. Santisteban, E. Rodríguez-Jiménez, M.F. Callaú-Lópes
Format: Article
Language:English
Published: Elsevier 2021-04-01
Series:Journal of Hydrology: Regional Studies
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2214581821000100
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author A. De la Hera-Portillo
J. López-Gutiérrez
C. Marín-Lechado
P. Martínez-Santos
A. Ruíz-Constán
M.M. Corral-Lledó
E. Galindo-Rodríguez
R. Mediavilla
J.I. Santisteban
E. Rodríguez-Jiménez
M.F. Callaú-Lópes
author_facet A. De la Hera-Portillo
J. López-Gutiérrez
C. Marín-Lechado
P. Martínez-Santos
A. Ruíz-Constán
M.M. Corral-Lledó
E. Galindo-Rodríguez
R. Mediavilla
J.I. Santisteban
E. Rodríguez-Jiménez
M.F. Callaú-Lópes
author_sort A. De la Hera-Portillo
collection DOAJ
description Study region: Old Las Salinas spring in Medina del Campo, Duero river basin, central Spain. Study focus: Medina del Campo groundwater body (MCGWB) is a multilayer semiconfined aquifer subject to intensive pumping since the 1970’s, where the current existence of spas where there used to be traditional baths could confirm the existence of deep groundwater flow paths. The old spring of Las Salinas (OSLS) is a saline anomaly in an aquifer with predominance of CaCO3H waters whose occurrence has not yet been formally explained. Long-term geological, geophysical, hydrogeological and hydrochemical records were integrated and complemented with field work to clarify its existence. New hydrological insights for the region: Outcomes led to the conclusion that the hydrochemistry of the Olmedo and Palacio de las Salinas salt baths is associated with the existence of a major threshold in the impervious basement of the aquifer, which intercepted deep regional groundwater flow and caused upwelling to the surface under unperturbed conditions. These results allow for the development of a conceptual flow model at the regional scale that explains the changes in natural water chemistry that have been identified in recent decades.
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spelling doaj.art-f16ac3d298ba43e09d8fad56c2b7546d2022-12-21T22:27:57ZengElsevierJournal of Hydrology: Regional Studies2214-58182021-04-0134100781Integrating current and historical water chemistry data with long-term piezometric records to develop a regional-scale conceptual flow model: Las Salinas spring, Medina del Campo, SpainA. De la Hera-Portillo0J. López-Gutiérrez1C. Marín-Lechado2P. Martínez-Santos3A. Ruíz-Constán4M.M. Corral-Lledó5E. Galindo-Rodríguez6R. Mediavilla7J.I. Santisteban8E. Rodríguez-Jiménez9M.F. Callaú-Lópes10Instituto Geológico y Minero de España (IGME), Geological Survey of Spain, Ríos Rosas 23, 28003, Madrid, Spain; Corresponding author.Instituto Geológico y Minero de España (IGME), Geological Survey of Spain, Ríos Rosas 23, 28003, Madrid, SpainInstituto Geológico y Minero de España (IGME), Geological Survey of Spain, Alcázar del Genil, 4. Edificio Zulema bajo, 18006, Granada, SpainDepartment of Geodynamics, Stratigraphy and Paleontology, Faculty of Geological Sciences, Complutense University of Madrid, C/José Antonio Novais, 12, 28040, Madrid, SpainInstituto Geológico y Minero de España (IGME), Geological Survey of Spain, Alcázar del Genil, 4. Edificio Zulema bajo, 18006, Granada, SpainInstituto Geológico y Minero de España (IGME), Geological Survey of Spain, Ríos Rosas 23, 28003, Madrid, SpainInstituto Geológico y Minero de España (IGME), Geological Survey of Spain, Ríos Rosas 23, 28003, Madrid, SpainInstituto Geológico y Minero de España (IGME), Geological Survey of Spain, Ríos Rosas 23, 28003, Madrid, SpainDepartment of Geodynamics, Stratigraphy and Paleontology, Faculty of Geological Sciences, Complutense University of Madrid, C/José Antonio Novais, 12, 28040, Madrid, SpainConfederación Hidrográfica del Duero (CHD), SpainDepartment of Geodynamics, Stratigraphy and Paleontology, Faculty of Geological Sciences, Complutense University of Madrid, C/José Antonio Novais, 12, 28040, Madrid, SpainStudy region: Old Las Salinas spring in Medina del Campo, Duero river basin, central Spain. Study focus: Medina del Campo groundwater body (MCGWB) is a multilayer semiconfined aquifer subject to intensive pumping since the 1970’s, where the current existence of spas where there used to be traditional baths could confirm the existence of deep groundwater flow paths. The old spring of Las Salinas (OSLS) is a saline anomaly in an aquifer with predominance of CaCO3H waters whose occurrence has not yet been formally explained. Long-term geological, geophysical, hydrogeological and hydrochemical records were integrated and complemented with field work to clarify its existence. New hydrological insights for the region: Outcomes led to the conclusion that the hydrochemistry of the Olmedo and Palacio de las Salinas salt baths is associated with the existence of a major threshold in the impervious basement of the aquifer, which intercepted deep regional groundwater flow and caused upwelling to the surface under unperturbed conditions. These results allow for the development of a conceptual flow model at the regional scale that explains the changes in natural water chemistry that have been identified in recent decades.http://www.sciencedirect.com/science/article/pii/S2214581821000100SpaDeep groundwater flowsSustainable groundwater abstractionWater securityIntensive groundwater exploitation assessmentMedina del Campo
spellingShingle A. De la Hera-Portillo
J. López-Gutiérrez
C. Marín-Lechado
P. Martínez-Santos
A. Ruíz-Constán
M.M. Corral-Lledó
E. Galindo-Rodríguez
R. Mediavilla
J.I. Santisteban
E. Rodríguez-Jiménez
M.F. Callaú-Lópes
Integrating current and historical water chemistry data with long-term piezometric records to develop a regional-scale conceptual flow model: Las Salinas spring, Medina del Campo, Spain
Journal of Hydrology: Regional Studies
Spa
Deep groundwater flows
Sustainable groundwater abstraction
Water security
Intensive groundwater exploitation assessment
Medina del Campo
title Integrating current and historical water chemistry data with long-term piezometric records to develop a regional-scale conceptual flow model: Las Salinas spring, Medina del Campo, Spain
title_full Integrating current and historical water chemistry data with long-term piezometric records to develop a regional-scale conceptual flow model: Las Salinas spring, Medina del Campo, Spain
title_fullStr Integrating current and historical water chemistry data with long-term piezometric records to develop a regional-scale conceptual flow model: Las Salinas spring, Medina del Campo, Spain
title_full_unstemmed Integrating current and historical water chemistry data with long-term piezometric records to develop a regional-scale conceptual flow model: Las Salinas spring, Medina del Campo, Spain
title_short Integrating current and historical water chemistry data with long-term piezometric records to develop a regional-scale conceptual flow model: Las Salinas spring, Medina del Campo, Spain
title_sort integrating current and historical water chemistry data with long term piezometric records to develop a regional scale conceptual flow model las salinas spring medina del campo spain
topic Spa
Deep groundwater flows
Sustainable groundwater abstraction
Water security
Intensive groundwater exploitation assessment
Medina del Campo
url http://www.sciencedirect.com/science/article/pii/S2214581821000100
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