Geokemiallinen malli pohjaveden olosuhteista ja kehityksestä Olkiluodon tutkimuspaikalla

Petteri Pitkänen, Ari Luukkonen, Paula Ruotsalainen, Hilkka Leino-Forsman, Ulla Vuorinen

Research output: Book/ReportReport

Abstract

An understanding of the geochemical evolution of groundwater is an essential part of the performance assessment and safety analysis of the final disposal of radioactive waste into the bedrock. The performance of technical barriers and migration of possibly released radionuclides depend on chemical conditions. A prerequisite for understanding these factors is the ability to specify the waterrock interactions which control chemical conditions in groundwater. The objective of this study is to interpret the processes and factors which control the hydrogeochemistry, such as pH and redox conditions. A model of the hydrogeochemical progress in different parts of the crystalline bedrock at Olkiluoto has been created and the significance of chemical reactions and groundwater mixing along different flowpaths calculated. Long term hydrodynamics have also been evaluated. The interpretation and modelling are based on water samples (63 altogether) obtained from precipitation, Baltic Sea, soil layer, shallow wells in the bedrock, and eight deep boreholes in the bedrock for which a comprehensive data set on dissolved chemical species and isotopes was available. Some analyses of dissolved gases and fracture calcite and their isotopic measurements were also utilised. The data covers the bedrock at Olkiluoto to a depth of 1 OOOm. The results from ground water chemistry, isotopes, petrography, hydrogeology of the site, geomicrobial studies, and PCA and speciation calculations were used in the evaluation of evolutionary processes at the site. The geochemical interpretation of water-rock interaction, isotope-chemical evolution and mixing of palaeo water types were approached by mass-balance calculations (NETPATH). Reaction-path calculations (EQ3/6) were used to verify the thermodynamic feasibility of the reaction models obtained. The interpretation and calculation of hydrochemical data from Olkiluoto reveals the complex nature of hydrogeochemical evolution at the site. Changes in external conditions such as glaciation, palaeo Baltic stages, land uplift and ancient hydrothermal events, have had a significant effect on local palaeohydrogeological conditions. They have caused great variability, which is observable in the chemical data notably in salinity (up to 70 g/1), water type and contents of conservative parameters, such as Cl, Br and stable isotopes of water (8H-2 and 80-18). However, their influence is also significant on the water-rock interaction that principally controls the pH and redox conditions - varying 7.5 to 8 and -200 to -300 mV, respectively - in the groundwater, although the calculated mass transfer in the reactions is minor compared with conservative mixing at the site. Calcite in fractures is interpreted to principally control pH level in groundwater. Sulphidic redox conditions dominate in the upper 500m in brackish and slightly saline groundwater. Deeper sulphur species are absent and methanic processes are obtained. The water types can be connected to certain palaeo stages. This enables to estimate mean residence time of groundwaters. Current meteoric recharge stage (< 2500 a) mainly dominates in the upper 150m. Groundwater from Litorina stage (7500-2500 a ago) forms the bulk at 100- 250 m. Glacial melt water (about 10 000 a old) is an important component of ground water between 100 - 500 m. However, any remarks of oxygen intrusion cannot be interpreted neither from mineralogy nor from groundwater. Deeper, subglacial and older saline groundwater predominates. Despite the current locations of different groundwater bodies it seems according to hydrogeochemical interpretation that dynamic flow conditions has been limited to upper 150 - 200 m.
Original languageEnglish
Place of PublicationHelsinki
PublisherPosiva
Number of pages184
ISBN (Print)951-652-048-0
Publication statusPublished - 1999
MoE publication typeD4 Published development or research report or study

Publication series

SeriesPosiva-raportti - Posiva Report
Volume98-10
ISSN1239-3096

Fingerprint

groundwater
bedrock
water-rock interaction
isotope
calcite
water
hydrogeochemistry
dissolved gas
chemical control
redox conditions
hydrogeology
petrography
meltwater
chemical reaction
radioactive waste
glaciation
radionuclide
residence time
recharge
mass balance

Keywords

  • groundwater chemistry
  • environmental isotopes
  • paleohydrogeology
  • water-rock interaction
  • mixing
  • geochemical modelling

Cite this

Pitkänen, P., Luukkonen, A., Ruotsalainen, P., Leino-Forsman, H., & Vuorinen, U. (1999). Geokemiallinen malli pohjaveden olosuhteista ja kehityksestä Olkiluodon tutkimuspaikalla. Helsinki: Posiva . Posiva-raportti - Posiva Report, Vol.. 98-10
Pitkänen, Petteri ; Luukkonen, Ari ; Ruotsalainen, Paula ; Leino-Forsman, Hilkka ; Vuorinen, Ulla. / Geokemiallinen malli pohjaveden olosuhteista ja kehityksestä Olkiluodon tutkimuspaikalla. Helsinki : Posiva , 1999. 184 p. (Posiva-raportti - Posiva Report, Vol. 98-10).
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Pitkänen, P, Luukkonen, A, Ruotsalainen, P, Leino-Forsman, H & Vuorinen, U 1999, Geokemiallinen malli pohjaveden olosuhteista ja kehityksestä Olkiluodon tutkimuspaikalla. Posiva-raportti - Posiva Report, vol. 98-10, Posiva , Helsinki.

Geokemiallinen malli pohjaveden olosuhteista ja kehityksestä Olkiluodon tutkimuspaikalla. / Pitkänen, Petteri; Luukkonen, Ari; Ruotsalainen, Paula; Leino-Forsman, Hilkka; Vuorinen, Ulla.

Helsinki : Posiva , 1999. 184 p. (Posiva-raportti - Posiva Report, Vol. 98-10).

Research output: Book/ReportReport

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T1 - Geokemiallinen malli pohjaveden olosuhteista ja kehityksestä Olkiluodon tutkimuspaikalla

AU - Pitkänen, Petteri

AU - Luukkonen, Ari

AU - Ruotsalainen, Paula

AU - Leino-Forsman, Hilkka

AU - Vuorinen, Ulla

N1 - LID

PY - 1999

Y1 - 1999

N2 - An understanding of the geochemical evolution of groundwater is an essential part of the performance assessment and safety analysis of the final disposal of radioactive waste into the bedrock. The performance of technical barriers and migration of possibly released radionuclides depend on chemical conditions. A prerequisite for understanding these factors is the ability to specify the waterrock interactions which control chemical conditions in groundwater. The objective of this study is to interpret the processes and factors which control the hydrogeochemistry, such as pH and redox conditions. A model of the hydrogeochemical progress in different parts of the crystalline bedrock at Olkiluoto has been created and the significance of chemical reactions and groundwater mixing along different flowpaths calculated. Long term hydrodynamics have also been evaluated. The interpretation and modelling are based on water samples (63 altogether) obtained from precipitation, Baltic Sea, soil layer, shallow wells in the bedrock, and eight deep boreholes in the bedrock for which a comprehensive data set on dissolved chemical species and isotopes was available. Some analyses of dissolved gases and fracture calcite and their isotopic measurements were also utilised. The data covers the bedrock at Olkiluoto to a depth of 1 OOOm. The results from ground water chemistry, isotopes, petrography, hydrogeology of the site, geomicrobial studies, and PCA and speciation calculations were used in the evaluation of evolutionary processes at the site. The geochemical interpretation of water-rock interaction, isotope-chemical evolution and mixing of palaeo water types were approached by mass-balance calculations (NETPATH). Reaction-path calculations (EQ3/6) were used to verify the thermodynamic feasibility of the reaction models obtained. The interpretation and calculation of hydrochemical data from Olkiluoto reveals the complex nature of hydrogeochemical evolution at the site. Changes in external conditions such as glaciation, palaeo Baltic stages, land uplift and ancient hydrothermal events, have had a significant effect on local palaeohydrogeological conditions. They have caused great variability, which is observable in the chemical data notably in salinity (up to 70 g/1), water type and contents of conservative parameters, such as Cl, Br and stable isotopes of water (8H-2 and 80-18). However, their influence is also significant on the water-rock interaction that principally controls the pH and redox conditions - varying 7.5 to 8 and -200 to -300 mV, respectively - in the groundwater, although the calculated mass transfer in the reactions is minor compared with conservative mixing at the site. Calcite in fractures is interpreted to principally control pH level in groundwater. Sulphidic redox conditions dominate in the upper 500m in brackish and slightly saline groundwater. Deeper sulphur species are absent and methanic processes are obtained. The water types can be connected to certain palaeo stages. This enables to estimate mean residence time of groundwaters. Current meteoric recharge stage (< 2500 a) mainly dominates in the upper 150m. Groundwater from Litorina stage (7500-2500 a ago) forms the bulk at 100- 250 m. Glacial melt water (about 10 000 a old) is an important component of ground water between 100 - 500 m. However, any remarks of oxygen intrusion cannot be interpreted neither from mineralogy nor from groundwater. Deeper, subglacial and older saline groundwater predominates. Despite the current locations of different groundwater bodies it seems according to hydrogeochemical interpretation that dynamic flow conditions has been limited to upper 150 - 200 m.

AB - An understanding of the geochemical evolution of groundwater is an essential part of the performance assessment and safety analysis of the final disposal of radioactive waste into the bedrock. The performance of technical barriers and migration of possibly released radionuclides depend on chemical conditions. A prerequisite for understanding these factors is the ability to specify the waterrock interactions which control chemical conditions in groundwater. The objective of this study is to interpret the processes and factors which control the hydrogeochemistry, such as pH and redox conditions. A model of the hydrogeochemical progress in different parts of the crystalline bedrock at Olkiluoto has been created and the significance of chemical reactions and groundwater mixing along different flowpaths calculated. Long term hydrodynamics have also been evaluated. The interpretation and modelling are based on water samples (63 altogether) obtained from precipitation, Baltic Sea, soil layer, shallow wells in the bedrock, and eight deep boreholes in the bedrock for which a comprehensive data set on dissolved chemical species and isotopes was available. Some analyses of dissolved gases and fracture calcite and their isotopic measurements were also utilised. The data covers the bedrock at Olkiluoto to a depth of 1 OOOm. The results from ground water chemistry, isotopes, petrography, hydrogeology of the site, geomicrobial studies, and PCA and speciation calculations were used in the evaluation of evolutionary processes at the site. The geochemical interpretation of water-rock interaction, isotope-chemical evolution and mixing of palaeo water types were approached by mass-balance calculations (NETPATH). Reaction-path calculations (EQ3/6) were used to verify the thermodynamic feasibility of the reaction models obtained. The interpretation and calculation of hydrochemical data from Olkiluoto reveals the complex nature of hydrogeochemical evolution at the site. Changes in external conditions such as glaciation, palaeo Baltic stages, land uplift and ancient hydrothermal events, have had a significant effect on local palaeohydrogeological conditions. They have caused great variability, which is observable in the chemical data notably in salinity (up to 70 g/1), water type and contents of conservative parameters, such as Cl, Br and stable isotopes of water (8H-2 and 80-18). However, their influence is also significant on the water-rock interaction that principally controls the pH and redox conditions - varying 7.5 to 8 and -200 to -300 mV, respectively - in the groundwater, although the calculated mass transfer in the reactions is minor compared with conservative mixing at the site. Calcite in fractures is interpreted to principally control pH level in groundwater. Sulphidic redox conditions dominate in the upper 500m in brackish and slightly saline groundwater. Deeper sulphur species are absent and methanic processes are obtained. The water types can be connected to certain palaeo stages. This enables to estimate mean residence time of groundwaters. Current meteoric recharge stage (< 2500 a) mainly dominates in the upper 150m. Groundwater from Litorina stage (7500-2500 a ago) forms the bulk at 100- 250 m. Glacial melt water (about 10 000 a old) is an important component of ground water between 100 - 500 m. However, any remarks of oxygen intrusion cannot be interpreted neither from mineralogy nor from groundwater. Deeper, subglacial and older saline groundwater predominates. Despite the current locations of different groundwater bodies it seems according to hydrogeochemical interpretation that dynamic flow conditions has been limited to upper 150 - 200 m.

KW - groundwater chemistry

KW - environmental isotopes

KW - paleohydrogeology

KW - water-rock interaction

KW - mixing

KW - geochemical modelling

M3 - Report

SN - 951-652-048-0

T3 - Posiva-raportti - Posiva Report

BT - Geokemiallinen malli pohjaveden olosuhteista ja kehityksestä Olkiluodon tutkimuspaikalla

PB - Posiva

CY - Helsinki

ER -

Pitkänen P, Luukkonen A, Ruotsalainen P, Leino-Forsman H, Vuorinen U. Geokemiallinen malli pohjaveden olosuhteista ja kehityksestä Olkiluodon tutkimuspaikalla. Helsinki: Posiva , 1999. 184 p. (Posiva-raportti - Posiva Report, Vol. 98-10).