Magnesium as Environmental Tracer for Karst Spring Baseflow/Overflow Assessment—A Case Study of the Pertuso Karst Spring (Latium Region, Italy)

Following a previous research carried out on the same site, this paper presents the update of the Mg<sup>2+</sup> based method for the estimation of Pertuso Spring discharge, located in Central Italy. New collected data confirmed the validity of the proposed model and the conservative be...

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Main Authors: Francesco Maria De Filippi, Silvia Iacurto, Gerardo Grelle, Giuseppe Sappa
Format: Article
Language:English
Published: MDPI AG 2021-01-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/1/93
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spelling doaj-18e00dea1a50434ea81efd62c50114192021-01-05T00:01:38ZengMDPI AGWater2073-44412021-01-0113939310.3390/w13010093Magnesium as Environmental Tracer for Karst Spring Baseflow/Overflow Assessment—A Case Study of the Pertuso Karst Spring (Latium Region, Italy)Francesco Maria De Filippi0Silvia Iacurto1Gerardo Grelle2Giuseppe Sappa3Department of Civil, Building and Environmental Engineering (DICEA), Sapienza University of Rome, 00184 Rome, ItalyDepartment of Civil, Building and Environmental Engineering (DICEA), Sapienza University of Rome, 00184 Rome, ItalyDepartment of Civil, Building and Environmental Engineering (DICEA), Sapienza University of Rome, 00184 Rome, ItalyDepartment of Civil, Building and Environmental Engineering (DICEA), Sapienza University of Rome, 00184 Rome, ItalyFollowing a previous research carried out on the same site, this paper presents the update of the Mg<sup>2+</sup> based method for the estimation of Pertuso Spring discharge, located in Central Italy. New collected data confirmed the validity of the proposed model and the conservative behaviour of Mg<sup>2+</sup> for groundwater related to the Pertuso Spring aquifer. Further analysis allowed to obtain a local linear relationship between magnesium concentration and total spring discharge (including exploitation rate), regardless of the mixing model proposed with the Aniene River. As regards two samples which fall out of the linear relationship and could have been detected as “outliers”, more in-depth data processing and sensitivity analyses revealed that the lowering in magnesium, at equal discharges, is determined by the appearance of the quick-flow component, less mineralized and related to storm events. Results showed that under specific conditions, related to the absence or presence of previous intense rainfall events, Mg<sup>2+</sup> could be effectively a useful tracer for separating spring conduit flow (overflow) from diffuse flow (baseflow) within the karst aquifer.https://www.mdpi.com/2073-4441/13/1/93karst springaquifermagnesiumenvironmental tracerdischargebaseflow
collection DOAJ
language English
format Article
sources DOAJ
author Francesco Maria De Filippi
Silvia Iacurto
Gerardo Grelle
Giuseppe Sappa
spellingShingle Francesco Maria De Filippi
Silvia Iacurto
Gerardo Grelle
Giuseppe Sappa
Magnesium as Environmental Tracer for Karst Spring Baseflow/Overflow Assessment—A Case Study of the Pertuso Karst Spring (Latium Region, Italy)
Water
karst spring
aquifer
magnesium
environmental tracer
discharge
baseflow
author_facet Francesco Maria De Filippi
Silvia Iacurto
Gerardo Grelle
Giuseppe Sappa
author_sort Francesco Maria De Filippi
title Magnesium as Environmental Tracer for Karst Spring Baseflow/Overflow Assessment—A Case Study of the Pertuso Karst Spring (Latium Region, Italy)
title_short Magnesium as Environmental Tracer for Karst Spring Baseflow/Overflow Assessment—A Case Study of the Pertuso Karst Spring (Latium Region, Italy)
title_full Magnesium as Environmental Tracer for Karst Spring Baseflow/Overflow Assessment—A Case Study of the Pertuso Karst Spring (Latium Region, Italy)
title_fullStr Magnesium as Environmental Tracer for Karst Spring Baseflow/Overflow Assessment—A Case Study of the Pertuso Karst Spring (Latium Region, Italy)
title_full_unstemmed Magnesium as Environmental Tracer for Karst Spring Baseflow/Overflow Assessment—A Case Study of the Pertuso Karst Spring (Latium Region, Italy)
title_sort magnesium as environmental tracer for karst spring baseflow/overflow assessment—a case study of the pertuso karst spring (latium region, italy)
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2021-01-01
description Following a previous research carried out on the same site, this paper presents the update of the Mg<sup>2+</sup> based method for the estimation of Pertuso Spring discharge, located in Central Italy. New collected data confirmed the validity of the proposed model and the conservative behaviour of Mg<sup>2+</sup> for groundwater related to the Pertuso Spring aquifer. Further analysis allowed to obtain a local linear relationship between magnesium concentration and total spring discharge (including exploitation rate), regardless of the mixing model proposed with the Aniene River. As regards two samples which fall out of the linear relationship and could have been detected as “outliers”, more in-depth data processing and sensitivity analyses revealed that the lowering in magnesium, at equal discharges, is determined by the appearance of the quick-flow component, less mineralized and related to storm events. Results showed that under specific conditions, related to the absence or presence of previous intense rainfall events, Mg<sup>2+</sup> could be effectively a useful tracer for separating spring conduit flow (overflow) from diffuse flow (baseflow) within the karst aquifer.
topic karst spring
aquifer
magnesium
environmental tracer
discharge
baseflow
url https://www.mdpi.com/2073-4441/13/1/93
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