Studentarrangementer - Side 93

Hydrogeological study of the Gvammsletta aquifers. Characterizing interconnections in a multiple aquifer system, Hjartdal, Norway

Is there a positive feedback between Arctic stratus and Arctic sea ice changes?

Restoration of the Third Law of Thermodynamics in a Quantum Refrigerator Model

Magnetisme i LDH og produktene etter dekomposisjon

Investigation of the growth process of silicon from the gas phase in the Dynatec Centrifuge and Free Space Reactor

Geochemical Comparison of Oils and Source Rocks from Barents Sea

Hydrotermisk stabilitet av mikroporøse materialer med CHA topologi

The first attempt to correlate the migrated bitumen from the Helgeland Basin cores to Devonian source rocks and oils from the UK Orcadian Basin - Is there a Devonian Orcadian type basin offshore Norway?

The lower crust and upper mantle beneath the western Barents Sea and Svalbard: evidence from combined active source and array seismology.

Monitoring CO2 behaviour during injection into reservoir sandstone

Experimental study on CO2 monitoring and saturation with combined acoustic  velocity and electrical resistivity in sandstone reservoirs

Receiver function analysis - Seismic imaging of the crust beneath TROLL seismic station in Queen Maud Land, Antarctica

Syntese og karakterisering av termoelektriske halv-Heusler materialer av typen (Ti,Zr,Hf)NiSn

Localization and analysis of calving-related seismicity at Kronebreen, Svalbard

Snow melt: Evaluation of an energy balance model

Geomechanical characterization of shale caprock of the Longyearbyen CO2 storage pilot

Repeatability and Detectability Requirements for 4D CSEM

Gas-dynamic computations of a small detonation using Large-Eddy Simulations

Optiske Mikrokaviteter og En-atom Lasere

The granulite-eclogite facies transition as developed in the Bergen Arcs, with focus on the minerals scapolite and spinel

Synthesis and Characterization of Homoepitaxial ZnO Thin Films

De-blending of marine seismic hydrophone and multicomponent data

Bioactive surfaces with atomic layer deposition

The role of the initial condition in numerical models of the present-day mantle flow field