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1	Fluid-rock interaction in the Mirvalles geothermal field, Costa Rica : mineralogical and experimental studies Rochelle, Christopher Alyn January 1990 (has links) No description available. 551 Minerals fluid composition
2	Ionic regulation of blood and gastric fluid in Crustacea decapoda (Carcinus maenas, Cancer paguras, Maia squinado) : the role of the foregut Tentori, Ernestina January 1988 (has links) No description available. 551.46 Crab body fluid composition
3	Interpretation of the P-T-XCO2 environment during metamorphism of carbonates, central Utö, Stockholm archipelago. Lundin, Linnéa January 2013 (has links) This thesis attempts to interpret the metamorphic condition and fluid composition experienced by metacarbonates on Utö, located in the south-eastern parts of the Stockholm archipelago. Utö is a part of the Svecofennian domain, and the area Bergslagen, that has hosted several mines over the last millennia. The bedrock in this area has been dated by the U-Pb technique to 1.90-1.87 Ga, placing it in the Paleoproterozoic era (Allen et al. 1996, Lundström et al. 1998). The rocks, of the studied area on the island of Utö, are mainly metacarbonates with a varying purity and thin layers of volcanic ash. These rocks become more felsic towards the north-western coast as the layers of felsic ash become more dominant. To determine the P-T-XCO2 of metamorphism, metacarbonates were examined, in the field, in thin sections and mineral chemistry was determined by SEM analysis. Three samples were collected along a 1km transect, along which the assemblage calcite + dolomite + quartz + tremolite + diopside was observed. Petrographic and SEM analysis were performed to gather chemical data from coexisting calcite and dolomite in order to calculate temperature using the calcite-dolomite geothermometer. Chemical data from the SEM analysis were also run with AX and THERMOCALC together with pressure data received from a study by Engström (2011) of the adjacent island, Persholmen, to generate a T- XCO2 diagram. Pressure was estimated to 3.1 +/- 1.3 kbars, temperature calculated to 442°C 30°C and XCO2 to range from 0,00067-0,0038 with the standard deviation taken in to account. These results record equilibration with a CO2-bearing hydrous fluid at greenschist facies conditions. / Metamorphic map of Sweden Metacarbonates THERMOCALC Utö Calcite-Dolomite geothermometer Fluid composition SEM Greenschist facies.
4	Modelling of diamond precipitation from fluids in the lower mantle Crossingham, Alexandra 07 June 2012 (has links) M.Sc. / Please refer to full text to view abstract Thermodynamic calculations Lithospheric mantle Fluid composition Diamond precipitation Diamonds Kaapvaal Craton Lithosphere Geochemistry Groundwater flow Precipitation hardening
5	Thermal Snail : Design and Performance Evaluation of a Non-Electronic Autonomous Vehiclefor Harnessing Thermal Expansion of Volatile Fluid for Movement Chen, Xin, Velin, Benjamin January 2024 (has links) No description available. Energy Harvesting Temporal Gradient Energy Density Spring Constant Amount Of Work Mobile Robot Direct Sunlight Working Fluid Propionate Phase Transition Heat Transfer Phase Change Pressure Measurements Renewable Sources Thermal Energy Vapor Pressure Gas Constant Gas Pressure Specific Energy Hot State Vehicle Wheel Dust Storms Solar Panels Constant Returns Energy Harvesting System Fluid Composition Storage Devices Physical Sciences Fysik

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