Hydrogeochemistry and pollution effects of an aquifer in Quaternary loess like sediments in the landflling area of Mar del Plata, Argentina

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Autor principal: Daniel E. Martínez
Formato: Artículo científico
Lenguaje:en
Publicado: Universidad de Antioquia 2013
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author Daniel E. Martínez
author_facet Daniel E. Martínez
contents Hydrogeochemistry and pollution effects of an aquifer in Quaternary loess like sediments in the landflling area of Mar del Plata, Argentina Daniel E. Martínez Margarita Osterrieth Ingeniería Argentina Hydrochemistry Loess sediments silica contents mineral saturation Loess like sediments cover an area of about 1.800.000 km2 in the Pampa plain of Argentina, forming an aquifer system which is used for water supply for most of the cities an rural population in the region. This aquifer supplies water to agricultural productive activities that contribute to about a 60% of the national gross produce of the country. In this paper, detailed studies in a local sector of the aquifer near to Mar del Plata, in the landfilling area of the city, are performed. The main goal is to characterise the hydrogeochemical processes giving the chemical groundwater composition, and to analyze the impact of the infiltration of the leachate from a neighbouring landfill on some samples. Five wells were drilled to take sediments and water samples. The textural and mineralogical composition of the aquifer sediments was analysed and the chemical composition of groundwater was determined. The equilibrium relationship between the solid phase and groundwater was considered using specific computer codes. The achieved conclusions were that the chemical composition of groundwater is mainly due to calcite equilibrium and cationic exchange with calcium uptake and sodium release. The dissolution of amorphous silica minerals, and subordinate silicate hydrolysis, are responsible of the characteristic high dissolved silica concentrations. High chloride and nitrate contents result from leachate infiltration, but the main geochemical processes in the mix are the same. 2013 artículo científico 0120-6230 https://www.redalyc.org/articulo.oa?id=43027041001 en http://www.redalyc.org/revista.oa?id=430 Revista Facultad de Ingeniería Universidad de Antioquia application/pdf Universidad de Antioquia Revista Facultad de Ingeniería Universidad de Antioquia (Colombia) Num.66
format Artículo científico
id redalyc_43027041001
institution Redalyc
language en
publishDate 2013
publisher Universidad de Antioquia
spellingShingle Hydrogeochemistry and pollution effects of an aquifer in Quaternary loess like sediments in the landflling area of Mar del Plata, Argentina
Daniel E. Martínez
Ingeniería
Argentina
Hydrochemistry
Loess sediments
silica contents
mineral saturation
Hydrogeochemistry and pollution effects of an aquifer in Quaternary loess like sediments in the landflling area of Mar del Plata, Argentina Daniel E. Martínez Margarita Osterrieth Ingeniería Argentina Hydrochemistry Loess sediments silica contents mineral saturation Loess like sediments cover an area of about 1.800.000 km2 in the Pampa plain of Argentina, forming an aquifer system which is used for water supply for most of the cities an rural population in the region. This aquifer supplies water to agricultural productive activities that contribute to about a 60% of the national gross produce of the country. In this paper, detailed studies in a local sector of the aquifer near to Mar del Plata, in the landfilling area of the city, are performed. The main goal is to characterise the hydrogeochemical processes giving the chemical groundwater composition, and to analyze the impact of the infiltration of the leachate from a neighbouring landfill on some samples. Five wells were drilled to take sediments and water samples. The textural and mineralogical composition of the aquifer sediments was analysed and the chemical composition of groundwater was determined. The equilibrium relationship between the solid phase and groundwater was considered using specific computer codes. The achieved conclusions were that the chemical composition of groundwater is mainly due to calcite equilibrium and cationic exchange with calcium uptake and sodium release. The dissolution of amorphous silica minerals, and subordinate silicate hydrolysis, are responsible of the characteristic high dissolved silica concentrations. High chloride and nitrate contents result from leachate infiltration, but the main geochemical processes in the mix are the same. 2013 artículo científico 0120-6230 https://www.redalyc.org/articulo.oa?id=43027041001 en http://www.redalyc.org/revista.oa?id=430 Revista Facultad de Ingeniería Universidad de Antioquia application/pdf Universidad de Antioquia Revista Facultad de Ingeniería Universidad de Antioquia (Colombia) Num.66
title Hydrogeochemistry and pollution effects of an aquifer in Quaternary loess like sediments in the landflling area of Mar del Plata, Argentina
topic Ingeniería
Argentina
Hydrochemistry
Loess sediments
silica contents
mineral saturation
url https://www.redalyc.org/articulo.oa?id=43027041001