Groundwater Temperature as an Indicator of the Vulnerability of Karst Coastal Aquifers

Coastal karst aquifers show a three-dimensional vulnerability, which consists of the whole of the “intrinsic vulnerability” and the “groundwater vulnerability to seawater intrusion”. The results of a study carried out in the Salento karst coastal aquifer (southern Italy) show that temperature, as we...

Full description

Bibliographic Details
Main Authors: Fidelibus, Maria Dolores, Pulido Bosch, Antonio
Format: info:eu-repo/semantics/article
Language:English
Published: MDPI 2020
Subjects:
Online Access:http://hdl.handle.net/10835/7619
_version_ 1789406605534560256
author Fidelibus, Maria Dolores
Pulido Bosch, Antonio
author_facet Fidelibus, Maria Dolores
Pulido Bosch, Antonio
author_sort Fidelibus, Maria Dolores
collection DSpace
description Coastal karst aquifers show a three-dimensional vulnerability, which consists of the whole of the “intrinsic vulnerability” and the “groundwater vulnerability to seawater intrusion”. The results of a study carried out in the Salento karst coastal aquifer (southern Italy) show that temperature, as well as being a reliable tracer of groundwater flow, is also an effective indicator of vulnerability in anisotropic media. The trend of isotherms related to a cross-section of the aquifer thermal field, combined with geological, geomorphological, and hydrogeological information, allows the role of faults and dolines in the mass transport from ground surface to be inferred. Isotherm trends may also give information on the permeability distribution along faults. A specific temperature value evidence the saltwater top, thus indicating the groundwater vulnerability to salinization.
format info:eu-repo/semantics/article
id oai:repositorio.ual.es:10835-7619
institution Universidad de Cuenca
language English
publishDate 2020
publisher MDPI
record_format dspace
spelling oai:repositorio.ual.es:10835-76192023-04-12T18:59:38Z Groundwater Temperature as an Indicator of the Vulnerability of Karst Coastal Aquifers Fidelibus, Maria Dolores Pulido Bosch, Antonio karst karst coastal aquifer vulnerability seawater intrusion temperature doline fault water level monitoring Salento Coastal karst aquifers show a three-dimensional vulnerability, which consists of the whole of the “intrinsic vulnerability” and the “groundwater vulnerability to seawater intrusion”. The results of a study carried out in the Salento karst coastal aquifer (southern Italy) show that temperature, as well as being a reliable tracer of groundwater flow, is also an effective indicator of vulnerability in anisotropic media. The trend of isotherms related to a cross-section of the aquifer thermal field, combined with geological, geomorphological, and hydrogeological information, allows the role of faults and dolines in the mass transport from ground surface to be inferred. Isotherm trends may also give information on the permeability distribution along faults. A specific temperature value evidence the saltwater top, thus indicating the groundwater vulnerability to salinization. 2020-01-20T09:24:46Z 2020-01-20T09:24:46Z 2018-12-30 info:eu-repo/semantics/article 2076-3263 http://hdl.handle.net/10835/7619 en https://www.mdpi.com/2076-3263/9/1/23 Attribution-NonCommercial-NoDerivatives 4.0 Internacional http://creativecommons.org/licenses/by-nc-nd/4.0/ info:eu-repo/semantics/openAccess MDPI
spellingShingle karst
karst coastal aquifer
vulnerability
seawater intrusion
temperature
doline
fault
water level
monitoring Salento
Fidelibus, Maria Dolores
Pulido Bosch, Antonio
Groundwater Temperature as an Indicator of the Vulnerability of Karst Coastal Aquifers
title Groundwater Temperature as an Indicator of the Vulnerability of Karst Coastal Aquifers
title_full Groundwater Temperature as an Indicator of the Vulnerability of Karst Coastal Aquifers
title_fullStr Groundwater Temperature as an Indicator of the Vulnerability of Karst Coastal Aquifers
title_full_unstemmed Groundwater Temperature as an Indicator of the Vulnerability of Karst Coastal Aquifers
title_short Groundwater Temperature as an Indicator of the Vulnerability of Karst Coastal Aquifers
title_sort groundwater temperature as an indicator of the vulnerability of karst coastal aquifers
topic karst
karst coastal aquifer
vulnerability
seawater intrusion
temperature
doline
fault
water level
monitoring Salento
url http://hdl.handle.net/10835/7619
work_keys_str_mv AT fidelibusmariadolores groundwatertemperatureasanindicatorofthevulnerabilityofkarstcoastalaquifers
AT pulidoboschantonio groundwatertemperatureasanindicatorofthevulnerabilityofkarstcoastalaquifers