Occurrence and Removal of Copper and Aluminum in a Stream Confluence Affected by Acid Mine Drainage

Acid mine drainage (AMD) is an environmental concern characterized by low pH and high concentrations of dissolved metals and sulfate. Yerba Loca Creek in Santiago, Chile, is an AMD-affected water stream that originates in a glacier and, therefore, has a season-dependent flow. This water course is ch...

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Main Authors: Carolina Rodríguez, Enzo Leiva-Aravena, Jennyfer Serrano, Eduardo Leiva
Format: Article
Language:English
Published: MDPI AG 2018-04-01
Series:Water
Subjects:
Online Access:http://www.mdpi.com/2073-4441/10/4/516
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spelling doaj-759adcbaf57d4619b2b073426b7f62cb2020-11-25T00:04:03ZengMDPI AGWater2073-44412018-04-0110451610.3390/w10040516w10040516Occurrence and Removal of Copper and Aluminum in a Stream Confluence Affected by Acid Mine DrainageCarolina Rodríguez0Enzo Leiva-Aravena1Jennyfer Serrano2Eduardo Leiva3Departamento de Ingeniería Hidráulica y Ambiental, Pontificia Universidad Católica de Chile, Avenida Vicuña Mackenna 4860, Macul, Santiago 7820436, ChileDepartamento de Ingeniería Hidráulica y Ambiental, Pontificia Universidad Católica de Chile, Avenida Vicuña Mackenna 4860, Macul, Santiago 7820436, ChileEscuela de Biotecnología, Universidad Mayor, Camino La Pirámide 5750, Huechuraba, Santiago 8580745, ChileDepartamento de Ingeniería Hidráulica y Ambiental, Pontificia Universidad Católica de Chile, Avenida Vicuña Mackenna 4860, Macul, Santiago 7820436, ChileAcid mine drainage (AMD) is an environmental concern characterized by low pH and high concentrations of dissolved metals and sulfate. Yerba Loca Creek in Santiago, Chile, is an AMD-affected water stream that originates in a glacier and, therefore, has a season-dependent flow. This water course is characterized by low pH (3.75 ± 0.13) and high concentrations of aluminum (2.2–2.6 mg/L) and copper (4.8–6.5 mg/L). A field campaign was carried out to study the geochemical behavior around the confluence of the Yerba Loca Creek with the San Francisco River, which has a neutral pH and low concentration of dissolved metals. The results show that the geochemical parameters after the confluence are very similar to those registered for the Yerba Loca Creek, due to its great flow in relation to the San Francisco River. The pH after the mixing zone was controlled by the geochemical conditions and flow of the Yerba Loca Creek; however, the turbidity decreases and stabilizes downstream. We found that, despite the low impact of pH on the precipitation of aluminum and copper phases due to poor neutralization, the dissolved aluminum and copper concentrations are slightly decreased after the mixing zone by natural microscale removal processes or suspended solids formation. Scanning electron microscopy–energy-dispersive X-ray spectroscopy (SEM–EDX) analysis of suspended solids indicates the presence of various oxides, hydroxy-sulfates and aluminosilicates, which have a great affinity for adsorption and co-precipitation with dissolved metals (i.e., Al and Cu). A pH-neutralization would favor the formation of more minerals and, therefore, the immobilization of the heavy metals found in these waters. These results contribute to a better understanding of the effect of the confluence of water courses related to pollution by AMD. It is possible that the seasonal variation of the flows has an impact on the composition of water and minerals formed.http://www.mdpi.com/2073-4441/10/4/516acid mine drainagelow pHmetals solubilityconfluence
collection DOAJ
language English
format Article
sources DOAJ
author Carolina Rodríguez
Enzo Leiva-Aravena
Jennyfer Serrano
Eduardo Leiva
spellingShingle Carolina Rodríguez
Enzo Leiva-Aravena
Jennyfer Serrano
Eduardo Leiva
Occurrence and Removal of Copper and Aluminum in a Stream Confluence Affected by Acid Mine Drainage
Water
acid mine drainage
low pH
metals solubility
confluence
author_facet Carolina Rodríguez
Enzo Leiva-Aravena
Jennyfer Serrano
Eduardo Leiva
author_sort Carolina Rodríguez
title Occurrence and Removal of Copper and Aluminum in a Stream Confluence Affected by Acid Mine Drainage
title_short Occurrence and Removal of Copper and Aluminum in a Stream Confluence Affected by Acid Mine Drainage
title_full Occurrence and Removal of Copper and Aluminum in a Stream Confluence Affected by Acid Mine Drainage
title_fullStr Occurrence and Removal of Copper and Aluminum in a Stream Confluence Affected by Acid Mine Drainage
title_full_unstemmed Occurrence and Removal of Copper and Aluminum in a Stream Confluence Affected by Acid Mine Drainage
title_sort occurrence and removal of copper and aluminum in a stream confluence affected by acid mine drainage
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2018-04-01
description Acid mine drainage (AMD) is an environmental concern characterized by low pH and high concentrations of dissolved metals and sulfate. Yerba Loca Creek in Santiago, Chile, is an AMD-affected water stream that originates in a glacier and, therefore, has a season-dependent flow. This water course is characterized by low pH (3.75 ± 0.13) and high concentrations of aluminum (2.2–2.6 mg/L) and copper (4.8–6.5 mg/L). A field campaign was carried out to study the geochemical behavior around the confluence of the Yerba Loca Creek with the San Francisco River, which has a neutral pH and low concentration of dissolved metals. The results show that the geochemical parameters after the confluence are very similar to those registered for the Yerba Loca Creek, due to its great flow in relation to the San Francisco River. The pH after the mixing zone was controlled by the geochemical conditions and flow of the Yerba Loca Creek; however, the turbidity decreases and stabilizes downstream. We found that, despite the low impact of pH on the precipitation of aluminum and copper phases due to poor neutralization, the dissolved aluminum and copper concentrations are slightly decreased after the mixing zone by natural microscale removal processes or suspended solids formation. Scanning electron microscopy–energy-dispersive X-ray spectroscopy (SEM–EDX) analysis of suspended solids indicates the presence of various oxides, hydroxy-sulfates and aluminosilicates, which have a great affinity for adsorption and co-precipitation with dissolved metals (i.e., Al and Cu). A pH-neutralization would favor the formation of more minerals and, therefore, the immobilization of the heavy metals found in these waters. These results contribute to a better understanding of the effect of the confluence of water courses related to pollution by AMD. It is possible that the seasonal variation of the flows has an impact on the composition of water and minerals formed.
topic acid mine drainage
low pH
metals solubility
confluence
url http://www.mdpi.com/2073-4441/10/4/516
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