Mobilisation of arsenic, selenium and uranium from Carboniferous black shales in west Ireland

Joseph G.T. Armstrong, John Parnell, Liam A Bullock, Adrian J Boyce, Magali Perez, Jörg Feldmann

Research output: Contribution to journalArticle

Abstract

The fixation and accumulation of critical elements in the near surface environment is an important factor in understanding elemental cycling through the crust, both for exploration of new resources and environmental management strategies. Carbonaceous black shales are commonly rich in trace elements relative to global crustal averages, many of which have potential environmental impacts depending on their speciation and mobility at surface. This trace element mobility can be investigated by studying the secondary mineralisation (regolith) associated with black shales at surface. In this study, Carboniferous shales on the west coast of Ireland are found to have higher than average shale concentrations of As, Cd, Cu, Co, Mo, Ni, Se, Te and U, similar to the laterally equivalent Bowland Shales, UK. Groundwater penetration and oxidative weathering of these pyritic black shales produces oxide deposits, dominated by goethite and jarosite, which are significantly enriched in As (44-468 ppm), Se (12-184 ppm), U (6-158 ppm) and other trace elements, compared to concentrations in the parent shales. Major elemental abundances vary in composition from 3.5-29.4 % sulphate, 0.6-9.1 % phosphate and 36.6-47.2 % iron-oxide. Phosphate substitution within jarosite is observed in these samples, formed under ambient pressure and temperature conditions.
The major and trace elements forming these secondary deposits are predominantly sourced from the underlying black shales through mobilisation by groundwater. This discovery is critical for the environmental assessment of black shale lithologies during shale gas exploration and production, where the demonstrated mobility of in situ elemental enrichments may indicate a significant source of produced- and groundwater contamination during and after hydraulic fracturing processes. The proportions of the major oxide phases exhibit a clear control on the trace elemental enrichments within the secondary deposits, where increasing Se and As concentrations correlate with increasing phosphate content of the jarosite mineralisation. This has implications for the remediation of acid mine drainage seeps, where phosphate-rich jarosite phases could be utilised for more efficient trace element removal.
Original languageEnglish
Article number104401
JournalApplied Geochemistry
Volume109
Early online date14 Aug 2019
DOIs
Publication statusPublished - Oct 2019

Fingerprint

Uranium
Selenium
Trace Elements
Arsenic
Trace elements
selenium
jarosite
mobilization
arsenic
uranium
trace element
Phosphates
phosphate
Groundwater
Deposits
Shale
Oxides
groundwater
oxide
mineralization

Keywords

  • black shale
  • carboniferous
  • regolith
  • secondary mineralisation
  • oxidation
  • jarosite
  • groundwater
  • leaching
  • fixation
  • hydraulic fracturing
  • AMD
  • selenium
  • arsenic
  • uranium
  • critical elements
  • Arsenic
  • Uranium
  • Groundwater
  • Oxidation
  • Selenium
  • Carboniferous
  • Black shale
  • Regolith
  • Leaching
  • Hydraulic fracturing
  • Critical elements
  • Fixation
  • Jarosite
  • Secondary mineralisation

ASJC Scopus subject areas

  • Pollution
  • Geochemistry and Petrology
  • Environmental Chemistry

Cite this

Mobilisation of arsenic, selenium and uranium from Carboniferous black shales in west Ireland. / Armstrong, Joseph G.T.; Parnell, John; Bullock, Liam A; Boyce, Adrian J; Perez, Magali; Feldmann, Jörg.

In: Applied Geochemistry, Vol. 109, 104401, 10.2019.

Research output: Contribution to journalArticle

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AU - Perez, Magali

AU - Feldmann, Jörg

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N2 - The fixation and accumulation of critical elements in the near surface environment is an important factor in understanding elemental cycling through the crust, both for exploration of new resources and environmental management strategies. Carbonaceous black shales are commonly rich in trace elements relative to global crustal averages, many of which have potential environmental impacts depending on their speciation and mobility at surface. This trace element mobility can be investigated by studying the secondary mineralisation (regolith) associated with black shales at surface. In this study, Carboniferous shales on the west coast of Ireland are found to have higher than average shale concentrations of As, Cd, Cu, Co, Mo, Ni, Se, Te and U, similar to the laterally equivalent Bowland Shales, UK. Groundwater penetration and oxidative weathering of these pyritic black shales produces oxide deposits, dominated by goethite and jarosite, which are significantly enriched in As (44-468 ppm), Se (12-184 ppm), U (6-158 ppm) and other trace elements, compared to concentrations in the parent shales. Major elemental abundances vary in composition from 3.5-29.4 % sulphate, 0.6-9.1 % phosphate and 36.6-47.2 % iron-oxide. Phosphate substitution within jarosite is observed in these samples, formed under ambient pressure and temperature conditions.The major and trace elements forming these secondary deposits are predominantly sourced from the underlying black shales through mobilisation by groundwater. This discovery is critical for the environmental assessment of black shale lithologies during shale gas exploration and production, where the demonstrated mobility of in situ elemental enrichments may indicate a significant source of produced- and groundwater contamination during and after hydraulic fracturing processes. The proportions of the major oxide phases exhibit a clear control on the trace elemental enrichments within the secondary deposits, where increasing Se and As concentrations correlate with increasing phosphate content of the jarosite mineralisation. This has implications for the remediation of acid mine drainage seeps, where phosphate-rich jarosite phases could be utilised for more efficient trace element removal.

AB - The fixation and accumulation of critical elements in the near surface environment is an important factor in understanding elemental cycling through the crust, both for exploration of new resources and environmental management strategies. Carbonaceous black shales are commonly rich in trace elements relative to global crustal averages, many of which have potential environmental impacts depending on their speciation and mobility at surface. This trace element mobility can be investigated by studying the secondary mineralisation (regolith) associated with black shales at surface. In this study, Carboniferous shales on the west coast of Ireland are found to have higher than average shale concentrations of As, Cd, Cu, Co, Mo, Ni, Se, Te and U, similar to the laterally equivalent Bowland Shales, UK. Groundwater penetration and oxidative weathering of these pyritic black shales produces oxide deposits, dominated by goethite and jarosite, which are significantly enriched in As (44-468 ppm), Se (12-184 ppm), U (6-158 ppm) and other trace elements, compared to concentrations in the parent shales. Major elemental abundances vary in composition from 3.5-29.4 % sulphate, 0.6-9.1 % phosphate and 36.6-47.2 % iron-oxide. Phosphate substitution within jarosite is observed in these samples, formed under ambient pressure and temperature conditions.The major and trace elements forming these secondary deposits are predominantly sourced from the underlying black shales through mobilisation by groundwater. This discovery is critical for the environmental assessment of black shale lithologies during shale gas exploration and production, where the demonstrated mobility of in situ elemental enrichments may indicate a significant source of produced- and groundwater contamination during and after hydraulic fracturing processes. The proportions of the major oxide phases exhibit a clear control on the trace elemental enrichments within the secondary deposits, where increasing Se and As concentrations correlate with increasing phosphate content of the jarosite mineralisation. This has implications for the remediation of acid mine drainage seeps, where phosphate-rich jarosite phases could be utilised for more efficient trace element removal.

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KW - arsenic

KW - uranium

KW - critical elements

KW - Arsenic

KW - Uranium

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KW - Oxidation

KW - Selenium

KW - Carboniferous

KW - Black shale

KW - Regolith

KW - Leaching

KW - Hydraulic fracturing

KW - Critical elements

KW - Fixation

KW - Jarosite

KW - Secondary mineralisation

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