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Ecotoxicology and Environmental Safety | 2016

Potential risk assessment in stream sediments, soils and waters after remediation in an abandoned W>Sn mine (NE Portugal)

I.M.H.R. Antunes; M.E.P. Gomes; A.M.R. Neiva; Patrícia Catarina Sanches de Carvalho; A.C.T. Santos

The mining complex of Murçós belongs to the Terras de Cavaleiros Geopark, located in Trás-os-Montes region, northeast Portugal. A stockwork of NW-SE-trending W>Sn quartz veins intruded Silurian metamorphic rocks and a Variscan biotite granite. The mineralized veins contain mainly quartz, cassiterite, wolframite, scheelite, arsenopyrite, pyrite, sphalerite, chalcopyrite, galena, rare pyrrhotite, stannite, native bismuth and also later bismuthinite, matildite, joseite, roosveltite, anglesite, scorodite, zavaritskite and covellite. The exploitation produced 335t of a concentrate with 70% of W and 150t of another concentrate with 70% of Sn between 1948 and 1976. The exploitation took place mainly in four open pit mines as well as underground. Three lakes were left in the area. Remediation processes of confination and control of tailings and rejected materials and phytoremediation with macrophytes from three lakes were carried out between 2005 and 2007. Stream sediments, soils and water samples were collected in 2008 and 2009, after the remediation process. Most stream sediments showed deficiency or minimum enrichment for metals. The sequential enrichment factor in stream sediments W>Bi>As>U>Cd>Sn=Ag>Cu>Sb>Pb>Be>Zn is mainly associated with the W>Sn mineralizations. Stream sediments receiving drainage of a mine dump were found to be significantly to extremely enriched with W, while stream sediments and soils were found to be contaminated with As. Two soil samples collected around mine dumps and an open pit lake were also found to be contaminated with U. The waters from the Murçós W>Sn mine area were acidic to neutral. After the remediation, the surface waters were contaminated with F(-), Al, As, Mn and Ni and must not be used for human consumption, while open pit lake waters must also not be used for agriculture because of contamination with F(-), Al, Mn and Ni. In most waters, the As occurred as As (III), which is toxic and is easily mobilized in the drainage system. The remediation promoted a decrease in metals and As concentrations of soils and waters, however the applied processes were not enough to rehabilitate the area.


Advances In Solar Energy Technology#R##N#Proceedings of the Biennial Congress of the International Solar Energy Society, Hamburg, Federal Republic Of Germany, 13–18 September 1987 | 1988

COMBINING SOLAR HEAT WITH HEAT RECOVERED FROM FIREPLACES

Albino Reis; Vasconcelos Carvalho; A.C.T. Santos

ABSTRACT The annual solar fraction given by conventional solar water heating systems in a country like Portugal varies between 50 and 70 %. On a monthly basis one could expect values as low as 20 % in winter and as high as 100 % in summer. A common source of “free energy” in a number of dwellings is the fireplace which, we all know, is not very efficient. However, heat recovery from these fireplaces is possible, simple and cheap. Depending on the type of the heat exchanger, usually integrated within the structure of the fireplace itself, something between 4 and 12 KW can be recovered not only for water heating but also for space heating, with efficiencies of between 50 and 80 %, say. Thus, the idea of combining the fireplace with solar radiation springs to mind. In this paper one starts by presenting a number of recuperators which are made and used in Portugal. Then, typical water and space heating systems designed by the authors and already installed are introduced. Finally, an experimental rig is described and the results discussed for three types of utilization profiles. It is concluded that the combination of a conventional solar water heating system with a fireplace recuperator leads to an annual “solar fraction” which approaches 100 %.


Journal of Geochemical Exploration | 2014

Contaminated water, stream sediments and soils close to the abandoned Pinhal do Souto uranium mine, central Portugal

A.M.R. Neiva; Patrícia Catarina Sanches de Carvalho; I.M.H.R. Antunes; M.M.V.G. Silva; A.C.T. Santos; M.M.S. Cabral Pinto; Pedro P. Cunha


Journal of Geochemical Exploration | 2016

Uranium and arsenic contamination in the former Mondego Sul uranium mine area, Central Portugal

A.M.R. Neiva; I.M.H.R. Antunes; Patrícia Catarina Sanches de Carvalho; A.C.T. Santos


Chemie Der Erde-geochemistry | 2015

Spatial and temporal variability of surface water and groundwater before and after the remediation of a Portuguese uranium mine area

A.M.R. Neiva; Paula Carvalho; I.M.H.R. Antunes; A.C.T. Santos; Marina Marques da Silva Cabral-Pinto


Chemie Der Erde-geochemistry | 2016

Spatial variability of soils and stream sediments and the remediation effects in a Portuguese uranium mine area

A.M.R. Neiva; Paula Carvalho; I.M.H.R. Antunes; Marina M.S. Cabral Pinto; A.C.T. Santos; Pedro P. Cunha; Maria Mafalda Costa


Environmental Geochemistry and Health | 2018

Potential toxic elements in stream sediments, soils and waters in an abandoned radium mine (central Portugal)

I.M.H.R. Antunes; A.M.R. Neiva; M.T.D. Albuquerque; Patrícia Catarina Sanches de Carvalho; A.C.T. Santos; Pedro P. Cunha


Environmental Geochemistry and Health | 2017

Human health risks in an old gold mining area with circum-neutral drainage, central Portugal.

Patrícia Catarina Sanches de Carvalho; A.M.R. Neiva; M.M.V.G. Silva; A.C.T. Santos


Archive | 2018

Zonas sensíveis na influência da drenagem de minas de rádio/urânio – caso da mina de Picoto, centro de Portugal

Isabel Margarida Horta Ribeiro Antunes; R. J. S. Teixeira; A.M.R. Neiva; A.C.T. Santos


Archive | 2018

Geoquímica de minerais portadores de urânio da mina de Picoto, Centro de Portugal

R. J. S. Teixeira; Isabel Margarida Horta Ribeiro Antunes; A.M.R. Neiva; A.C.T. Santos

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I.M.H.R. Antunes

Polytechnic Institute of Castelo Branco

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M.T.D. Albuquerque

Polytechnic Institute of Castelo Branco

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M.E.P. Gomes

University of Trás-os-Montes and Alto Douro

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