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  • Miljøteknologi
  • Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon
  • Fluid - solid interactions related to subsurface storage of CO2 : experimental tests of well cement
  • A field laboratory for monitoring CO2 leakage
  • Effect of CO2 interaction with Svalbard shale: Implications to caprock integrity for subsurface sequestration of CO2
  • A continuous process for manufacture of magnesite and silica from olivine, CO2 and H2O
  • A basin scale perspective on CO2 storage—short and long term risks
  • Experimental measurement of portlandite carbonation kinetics with supercritical CO2
  • Sources of dissolved mine drainage and atmospheric transported lead: A comparative case study in Japan and Sweden
  • Establishing the correlation between complexity and a reliability metric for software digital i&c-systems
  • Estimation of lithospheric extension by accounting for stretching and thinning of the sedimentary basin – An example from the Vøring margin, NE Atlantic
  • Physical principles of sedimentary basin analysis
 
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Miljøteknologi

Granitic magmatism by melting of juvenile continental crust: new constraints on the source of Palaeoproterozoic granitoids in Fennoscandia from Hf isotopes in zircon
Fluid - solid interactions related to subsurface storage of CO2 : experimental tests of well cement
A field laboratory for monitoring CO2 leakage
Effect of CO2 interaction with Svalbard shale: Implications to caprock integrity for subsurface sequestration of CO2
A continuous process for manufacture of magnesite and silica from olivine, CO2 and H2O
A basin scale perspective on CO2 storage—short and long term risks
Experimental measurement of portlandite carbonation kinetics with supercritical CO2
Sources of dissolved mine drainage and atmospheric transported lead: A comparative case study in Japan and Sweden
Establishing the correlation between complexity and a reliability metric for software digital i&c-systems
Estimation of lithospheric extension by accounting for stretching and thinning of the sedimentary basin – An example from the Vøring margin, NE Atlantic
Physical principles of sedimentary basin analysis
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