The Cr(VI) Stability in Contaminated Coastal Groundwater: Salinity as a Driving Force

Chromium concentrations in seawater are less than 0.5 μg/L, but the Cr(VI) in contaminated coastal groundwater affected by Cr-bearing rocks/ores and/or human activities, coupled with the intrusion of seawater may reach values of hundreds of μg/L. A potential explanation for the stability of the harm...

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Main Authors: Ioannis-Porfyrios D. Eliopoulos, George D. Eliopoulos, Maria Economou-Eliopoulos
Format: Article
Language:English
Published: MDPI AG 2021-02-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/11/2/160
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spelling doaj-12a682f6197c49298098a0c91fc42bed2021-02-04T00:03:53ZengMDPI AGMinerals2075-163X2021-02-011116016010.3390/min11020160The Cr(VI) Stability in Contaminated Coastal Groundwater: Salinity as a Driving ForceIoannis-Porfyrios D. Eliopoulos0George D. Eliopoulos1Maria Economou-Eliopoulos2Department of Pharmacy, School of Health Sciences, National University of Athens, GR-15771 Zografou, GreeceDepartment of Chemistry, University of Crete, GR-70013 Heraklion, GreeceDepartment of Geology and Geoenvironment, National University of Athens, GR-15784 Athens, GreeceChromium concentrations in seawater are less than 0.5 μg/L, but the Cr(VI) in contaminated coastal groundwater affected by Cr-bearing rocks/ores and/or human activities, coupled with the intrusion of seawater may reach values of hundreds of μg/L. A potential explanation for the stability of the harmful Cr(VI) in contaminated coastal aquifers is still unexplored. The present study is an overview of new and literature data on the composition of coastal groundwater and seawater, aiming to provide potential relationships between Cr(VI) with major components in seawater and explain the elevated Cr(VI) concentrations. It is known that the oxidation of Cr(III) to Cr(VI) and the subsequent back-reduction of Cr(VI) processes, during the transport of the mobilized Cr(VI) in various aquifers, facilitate the natural attenuation process of Cr(VI). Moreover, the presented positive trend between B and Cr(VI) and negative trend between δ<sup>53</sup>Cr values and B concentration may suggest that seawater components significantly inhibit the Cr(VI) reduction into Cr(III), and provide insights on the role of the borate, [B(OH)<sub>4</sub>]<sup>−</sup> ions, a potential buffer, on the stability of Cr(VI) in coastal groundwater. Therefore, efforts are needed toward the prevention and/or minimization of the contamination by Cr(VI) of in coastal aquifers, which are influenced by the intrusion of seawater and are threatened by changes in sea level, due to climate change. The knowledge of the contamination sources, hotspots and monitoring of water salinization processes (geochemical mapping) for every coastal country may contribute to the optimization of agricultural management strategies.https://www.mdpi.com/2075-163X/11/2/160groundwatercontaminationchromium(VI)salinizationboratechromium isotopes
collection DOAJ
language English
format Article
sources DOAJ
author Ioannis-Porfyrios D. Eliopoulos
George D. Eliopoulos
Maria Economou-Eliopoulos
spellingShingle Ioannis-Porfyrios D. Eliopoulos
George D. Eliopoulos
Maria Economou-Eliopoulos
The Cr(VI) Stability in Contaminated Coastal Groundwater: Salinity as a Driving Force
Minerals
groundwater
contamination
chromium(VI)
salinization
borate
chromium isotopes
author_facet Ioannis-Porfyrios D. Eliopoulos
George D. Eliopoulos
Maria Economou-Eliopoulos
author_sort Ioannis-Porfyrios D. Eliopoulos
title The Cr(VI) Stability in Contaminated Coastal Groundwater: Salinity as a Driving Force
title_short The Cr(VI) Stability in Contaminated Coastal Groundwater: Salinity as a Driving Force
title_full The Cr(VI) Stability in Contaminated Coastal Groundwater: Salinity as a Driving Force
title_fullStr The Cr(VI) Stability in Contaminated Coastal Groundwater: Salinity as a Driving Force
title_full_unstemmed The Cr(VI) Stability in Contaminated Coastal Groundwater: Salinity as a Driving Force
title_sort cr(vi) stability in contaminated coastal groundwater: salinity as a driving force
publisher MDPI AG
series Minerals
issn 2075-163X
publishDate 2021-02-01
description Chromium concentrations in seawater are less than 0.5 μg/L, but the Cr(VI) in contaminated coastal groundwater affected by Cr-bearing rocks/ores and/or human activities, coupled with the intrusion of seawater may reach values of hundreds of μg/L. A potential explanation for the stability of the harmful Cr(VI) in contaminated coastal aquifers is still unexplored. The present study is an overview of new and literature data on the composition of coastal groundwater and seawater, aiming to provide potential relationships between Cr(VI) with major components in seawater and explain the elevated Cr(VI) concentrations. It is known that the oxidation of Cr(III) to Cr(VI) and the subsequent back-reduction of Cr(VI) processes, during the transport of the mobilized Cr(VI) in various aquifers, facilitate the natural attenuation process of Cr(VI). Moreover, the presented positive trend between B and Cr(VI) and negative trend between δ<sup>53</sup>Cr values and B concentration may suggest that seawater components significantly inhibit the Cr(VI) reduction into Cr(III), and provide insights on the role of the borate, [B(OH)<sub>4</sub>]<sup>−</sup> ions, a potential buffer, on the stability of Cr(VI) in coastal groundwater. Therefore, efforts are needed toward the prevention and/or minimization of the contamination by Cr(VI) of in coastal aquifers, which are influenced by the intrusion of seawater and are threatened by changes in sea level, due to climate change. The knowledge of the contamination sources, hotspots and monitoring of water salinization processes (geochemical mapping) for every coastal country may contribute to the optimization of agricultural management strategies.
topic groundwater
contamination
chromium(VI)
salinization
borate
chromium isotopes
url https://www.mdpi.com/2075-163X/11/2/160
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