Water Quality and Soil Natural Salinity in the Southern Imera Basin (Sicily, Italy)

The Southern Imera river crosses one of the most arid part of Sicily. The geochemical composition of the river water is due to the solubilization processes of gypsum rocks, which accounts for the particularly low quality of resources in the areas in which the presence of evaporitics deposits is high...

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Main Authors: Roberta Selvaggi, Nicola Colonna, Flavio Lupia, Maria S. Murgia, Antonio Poletti
Format: Article
Language:English
Published: PAGEPress Publications 2010-10-01
Series:Italian Journal of Agronomy
Subjects:
Online Access:https://www.agronomy.it/index.php/agro/article/view/71
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spelling doaj-487da9b695104c8db871ad7b7e691a052020-11-25T00:32:43ZengPAGEPress PublicationsItalian Journal of Agronomy1125-47182039-68052010-10-0153S10.4081/ija.2010.s3.8159Water Quality and Soil Natural Salinity in the Southern Imera Basin (Sicily, Italy)Roberta SelvaggiNicola ColonnaFlavio LupiaMaria S. MurgiaAntonio PolettiThe Southern Imera river crosses one of the most arid part of Sicily. The geochemical composition of the river water is due to the solubilization processes of gypsum rocks, which accounts for the particularly low quality of resources in the areas in which the presence of evaporitics deposits is highest. The geochemical composition and hydraulic parameters of river was monitored with the aim of reaching a better understanding of the relationships between litology and water quality. The Imera river is a potential local hydric resource, but seasonal variability of salinity does not allow farmers to use its water. A geochemical monitoring of the Imera river water has been carried out in selected localities integrating a GIS analysis of the river hydrography basin and of the distribution of the evaporitic formation. During 2003 and 2005 we performed four monitoring surveys of water chemicophysical parameters (temperature, pH and electrical conductivity) and of the main ionic concentrations (Ca2+, Mg2+, K+, Na+, Cl-, SO4 2- ). We also installed a multiparameter probe next to the hydrometrical station of Drasi, about 15 km from the river mouth. Such multiparameter probe was used to determine, continuously and simultaneously, temperature, electrical conductivity, pH, dissolved oxygen, redox potenzial, water level. The geochemical composition of the water allowed to confirm the results of Roda (1971) and Favara (2000), who pointed out that the main cause of degrade of the Southern Imera river are the salt-rich waters of some tributaries flowing over gypsum rocks and halite deposits. We have been able to identify which specific areas are the main contributors to the degradation of the Imera river.https://www.agronomy.it/index.php/agro/article/view/71hydrochemistrysalinisationwater qualityImera RiverGIS.
collection DOAJ
language English
format Article
sources DOAJ
author Roberta Selvaggi
Nicola Colonna
Flavio Lupia
Maria S. Murgia
Antonio Poletti
spellingShingle Roberta Selvaggi
Nicola Colonna
Flavio Lupia
Maria S. Murgia
Antonio Poletti
Water Quality and Soil Natural Salinity in the Southern Imera Basin (Sicily, Italy)
Italian Journal of Agronomy
hydrochemistry
salinisation
water quality
Imera River
GIS.
author_facet Roberta Selvaggi
Nicola Colonna
Flavio Lupia
Maria S. Murgia
Antonio Poletti
author_sort Roberta Selvaggi
title Water Quality and Soil Natural Salinity in the Southern Imera Basin (Sicily, Italy)
title_short Water Quality and Soil Natural Salinity in the Southern Imera Basin (Sicily, Italy)
title_full Water Quality and Soil Natural Salinity in the Southern Imera Basin (Sicily, Italy)
title_fullStr Water Quality and Soil Natural Salinity in the Southern Imera Basin (Sicily, Italy)
title_full_unstemmed Water Quality and Soil Natural Salinity in the Southern Imera Basin (Sicily, Italy)
title_sort water quality and soil natural salinity in the southern imera basin (sicily, italy)
publisher PAGEPress Publications
series Italian Journal of Agronomy
issn 1125-4718
2039-6805
publishDate 2010-10-01
description The Southern Imera river crosses one of the most arid part of Sicily. The geochemical composition of the river water is due to the solubilization processes of gypsum rocks, which accounts for the particularly low quality of resources in the areas in which the presence of evaporitics deposits is highest. The geochemical composition and hydraulic parameters of river was monitored with the aim of reaching a better understanding of the relationships between litology and water quality. The Imera river is a potential local hydric resource, but seasonal variability of salinity does not allow farmers to use its water. A geochemical monitoring of the Imera river water has been carried out in selected localities integrating a GIS analysis of the river hydrography basin and of the distribution of the evaporitic formation. During 2003 and 2005 we performed four monitoring surveys of water chemicophysical parameters (temperature, pH and electrical conductivity) and of the main ionic concentrations (Ca2+, Mg2+, K+, Na+, Cl-, SO4 2- ). We also installed a multiparameter probe next to the hydrometrical station of Drasi, about 15 km from the river mouth. Such multiparameter probe was used to determine, continuously and simultaneously, temperature, electrical conductivity, pH, dissolved oxygen, redox potenzial, water level. The geochemical composition of the water allowed to confirm the results of Roda (1971) and Favara (2000), who pointed out that the main cause of degrade of the Southern Imera river are the salt-rich waters of some tributaries flowing over gypsum rocks and halite deposits. We have been able to identify which specific areas are the main contributors to the degradation of the Imera river.
topic hydrochemistry
salinisation
water quality
Imera River
GIS.
url https://www.agronomy.it/index.php/agro/article/view/71
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