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Terrigenous dissolved organic matter persists in the energy-limited deep groundwaters of the Fennoscandian Shield

Nature communications, 2022-08, Vol.13 (1), p.4837-4837, Article 4837

2022

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Detecting the near-surface redox front in crystalline bedrock using fracture mineral distribution, geochemistry and U-series disequilibrium

Applied geochemistry, 2009-05, Vol.24 (5), p.1023-1039

2009

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Red-staining of the wall rock and its influence on the reducing capacity around water conducting fractures

Applied geochemistry, 2008-07, Vol.23 (7), p.1898-1920

2008

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Methodology for Hydrogeochemical Sampling to Characterise Groundwaters in Crystalline Bedrock: Developments Made within the Swedish Radwaste Programme

Geofluids, 2020, Vol.2020 (2020), p.1-13

2020

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Deep anoxic aquifers could act as sinks for uranium through microbial-assisted mineral trapping

Communications earth & environment, 2023-04, Vol.4 (1), p.128-11, Article 128

2023

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Hydrogeochemical characterisation of the groundwater in the crystalline basement of Forsmark, the selected area for the geological nuclear repositories in Sweden

Journal of hydrology (Amsterdam), 2023-09, Vol.624, p.129818, Article 129818

2023

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Uranium remobilisation in anoxic deep rock-groundwater system in response to late Quaternary climate changes – Results from Forsmark, Sweden

Chemical geology, 2021-12, Vol.584, p.120551-1-120551-16, Article 120551

2021

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Tracing the palaeoredox conditions at Forsmark, Sweden, using uranium mineral geochronology

Chemical geology, 2019-02, Vol.506, p.68-78

2019

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Distinguished multiple events of fracture mineralisation related to far-field orogenic effects in Paleoproterozoic crystalline rocks, Simpevarp area, SE Sweden

Lithos, 2009-06, Vol.110 (1), p.37-49

2009

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Paleohydrogeological events recorded by stable isotopes, fluid inclusions and trace elements in fracture minerals in crystalline rock, Simpevarp area, SE Sweden

Applied geochemistry, 2009-04, Vol.24 (4), p.715-732

2009

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Quaternary redox transitions in deep crystalline rock fractures at the western margin of the Greenland ice sheet

Applied geochemistry, 2017-01, Vol.76, p.196-209

2017

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Radium isotopes to trace uranium redox anomalies in anoxic groundwater

Chemical geology, 2020-01, Vol.531, p.119296, Article 119296

2020

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Natural uranium in Forsmark, Sweden: The solid phase

Applied geochemistry, 2015-08, Vol.59, p.178-188

2015

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Episodic fluid migration in the Fennoscandian Shield recorded by stable isotopes, rare earth elements and fluid inclusions in fracture minerals at Forsmark, Sweden

Chemical geology, 2009-08, Vol.266 (3), p.126-142

2009

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Extreme fractionation and micro-scale variation of sulphur isotopes during bacterial sulphate reduction in deep groundwater systems

Geochimica et cosmochimica acta, 2015, Vol.161, p.1-18

2015

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Variability of sulphur isotope ratios in pyrite and dissolved sulphate in granitoid fractures down to 1km depth – Evidence for widespread activity of sulphur reducing bacteria

Geochimica et cosmochimica acta, 2013-02, Vol.102 (1), p.143-161

2013

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Effect of Tunnel Excavation on Source and Mixing of Groundwater in a Coastal Granitoidic Fracture Network

Environmental science & technology, 2012-12, Vol.46 (23), p.12779-12786

2012

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Trace metal distribution and isotope variations in low-temperature calcite and groundwater in granitoid fractures down to 1km depth

Geochimica et cosmochimica acta, 2012-05, Vol.84, p.217-238

2012

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Palaeohydrogeology: A methodology based on fracture mineral studies

Applied geochemistry, 2008-07, Vol.23 (7), p.1881-1897

2008

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High cesium concentrations in groundwater in the upper 1.2km of fractured crystalline rock – Influence of groundwater origin and secondary minerals

Geochimica et cosmochimica acta, 2014-05, Vol.132, p.187-213

2014

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In situ tracer tests to determine retention properties of a block scale fracture network in granitic rock at the Äspö Hard Rock Laboratory, Sweden

Journal of contaminant hydrology, 2004-06, Vol.70 (3), p.271-297

2004

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Hydrogeochemical evaluation and modelling performed within the Swedish site investigation programme

Applied geochemistry, 2008-07, Vol.23 (7), p.1761-1795

2008

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Fracture-related hydrothermal alteration of metagranitic rock and associated changes in mineralogy, geochemistry and degree of oxidation: a case study at Forsmark, central Sweden

International journal of earth sciences : Geologische Rundschau, 2010, Vol.99 (1), p.1-25

2010

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Brittle tectonothermal evolution in the Forsmark area, central Fennoscandian Shield, recorded by paragenesis, orientation and (40)Ar/(39)Ar geochronology of fracture minerals

Tectonophysics, 2009-12, Vol.478 (3-4), p.158-174

2009

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Real system analyses/natural analogues

Applied geochemistry, 2012-02, Vol.27 (2), p.490-500

2012

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Terrigenous dissolved organic matter persists in the energy-limited deep groundwaters of the Fennoscandian Shield

Detecting the near-surface redox front in crystalline bedrock using fracture mineral distribution, geochemistry and U-series disequilibrium

Red-staining of the wall rock and its influence on the reducing capacity around water conducting fractures

Methodology for Hydrogeochemical Sampling to Characterise Groundwaters in Crystalline Bedrock: Developments Made within the Swedish Radwaste Programme

Deep anoxic aquifers could act as sinks for uranium through microbial-assisted mineral trapping

Hydrogeochemical characterisation of the groundwater in the crystalline basement of Forsmark, the selected area for the geological nuclear repositories in Sweden

Uranium remobilisation in anoxic deep rock-groundwater system in response to late Quaternary climate changes – Results from Forsmark, Sweden

Tracing the palaeoredox conditions at Forsmark, Sweden, using uranium mineral geochronology

Distinguished multiple events of fracture mineralisation related to far-field orogenic effects in Paleoproterozoic crystalline rocks, Simpevarp area, SE Sweden

Paleohydrogeological events recorded by stable isotopes, fluid inclusions and trace elements in fracture minerals in crystalline rock, Simpevarp area, SE Sweden

Quaternary redox transitions in deep crystalline rock fractures at the western margin of the Greenland ice sheet

Radium isotopes to trace uranium redox anomalies in anoxic groundwater

Natural uranium in Forsmark, Sweden: The solid phase

Episodic fluid migration in the Fennoscandian Shield recorded by stable isotopes, rare earth elements and fluid inclusions in fracture minerals at Forsmark, Sweden

Extreme fractionation and micro-scale variation of sulphur isotopes during bacterial sulphate reduction in deep groundwater systems

Variability of sulphur isotope ratios in pyrite and dissolved sulphate in granitoid fractures down to 1km depth – Evidence for widespread activity of sulphur reducing bacteria

Effect of Tunnel Excavation on Source and Mixing of Groundwater in a Coastal Granitoidic Fracture Network

Trace metal distribution and isotope variations in low-temperature calcite and groundwater in granitoid fractures down to 1km depth

Palaeohydrogeology: A methodology based on fracture mineral studies

High cesium concentrations in groundwater in the upper 1.2km of fractured crystalline rock – Influence of groundwater origin and secondary minerals

In situ tracer tests to determine retention properties of a block scale fracture network in granitic rock at the Äspö Hard Rock Laboratory, Sweden

Hydrogeochemical evaluation and modelling performed within the Swedish site investigation programme

Fracture-related hydrothermal alteration of metagranitic rock and associated changes in mineralogy, geochemistry and degree of oxidation: a case study at Forsmark, central Sweden

Brittle tectonothermal evolution in the Forsmark area, central Fennoscandian Shield, recorded by paragenesis, orientation and (40)Ar/(39)Ar geochronology of fracture minerals

Real system analyses/natural analogues

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