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Advisor(s)
Abstract(s)
The Pinhal do Souto mine exploited a quartz vein containing uranium minerals, mainly autunite and
torbernite. This vein intersects a two-mica granite containing 10 ppm U and uraninite. The mine was
exploited underground and produced 93091 kg U3O8 between 1978 and 1989 and was then closed down.
Two dumps were left in the mine area and these are partially covered by natural vegetation. Groundwater
and surface water have a similar slightly acid-to-alkaline pH. The 2
2
UO is abundant and complexed
with 2
3 CO , under neutral to alkaline pH. Metals and arsenic concentrations in the water increase during the
dry season due to the evaporation. Uranium concentration in the water increases (up to 104.42 g/l) in the
wet season, because secondary uranium minerals are dissolved and uranium is released into the water. Soils
tend to retain a higher concentration of several metals, including U (up to 336.79 mg/kg) than stream
sediments (up to 35.68 mg/kg), because vermiculite from the former could adsorb it more easily than could
kaolinite from the latter. The Fe-oxides precipitate retains the highest concentrations of several metals,
including U and Th (up to 485.20 and 1053.12 mg/kg, respectively) and the metalloid As, because it is richer in oxyhydroxides and organic matter than stream sediments and soils. The median concentrations of Fe, As,
Cd, Pb, Sb, Th, U, W and Zn in soils from this area are higher than in European soils of the FOREGS data.
Waters from dry and wet seasons, stream sediments and soils are contaminated and must not be used. This
area was compared with another Portuguese abandoned uranium mine area. The former mine caused a lower
environmental impact attributable to it having lower sulfide concentration and mineral alteration than in the
latter.
Description
Keywords
Abandoned uranium mine Water Stream sediments Soils Contamination
Pedagogical Context
Citation
NEIVA, A. M. R. [et al.] (2014) - Contaminated water, stream sediments and soils close to the abandoned Pinhal do Souto uranium mine, central Portugal. Journal of Geochemical Exploration. ISSN 0375-6742. Vol. 136 p. 102-117
Publisher
Elsevier