Quantification of ikaite in first and multi year sea ice

dc.contributor.authorKyle, Heather Marie
dc.contributor.examiningcommitteeFayek, Mostafa (Geological Sciences) Wang, Feiyue (Environment & Geography)en_US
dc.contributor.supervisorRysgaard, Søren (Geological Sciences)en_US
dc.date.accessioned2017-08-29T17:07:04Z
dc.date.available2017-08-29T17:07:04Z
dc.date.issued2017
dc.degree.disciplineGeological Sciencesen_US
dc.degree.levelMaster of Science (M.Sc.)en_US
dc.description.abstractIkaite (CaCO₃•6H₂O) is a metastable calcium carbonate mineral that forms in all types of sea ice that may play a significant role in the sea ice driven carbon pump, particularly with the increasing abundance of seasonal sea ice in the Arctic. Due to difficulties in determining its concentration and abundance, the spatial and temporal dynamics, and therefore the significance, of ikaite are poorly understood. To improve knowledge of ikaite in sea ice, a new method of quantification using dissolved inorganic carbon (DIC) analysis was developed and tested at the Sea-ice Environmental Research Facility (SERF), at Station Nord, Greenland, and at Cambridge Bay, Nunavut. Environmental parameters, including temperature, salinity, total alkalinity (TA), and DIC were also measured at all sampling sites. Ikaite concentrations ranged from 8 to 2595 μmol kg⁻¹ and were generally highest in low temperature, high salinity sea ice with high TA:DIC ratios. Results indicate that the new method of ikaite quantification is an effective technique that can be used in the future to improve understanding of ikaite and its role in carbon dynamics in ice covered seas.en_US
dc.description.noteOctober 2017en_US
dc.identifier.urihttp://hdl.handle.net/1993/32387
dc.language.isoengen_US
dc.rightsopen accessen_US
dc.subjectIkaiteen_US
dc.subjectSea iceen_US
dc.subjectArcticen_US
dc.subjectCarbon fluxesen_US
dc.subjectCarbonate systemen_US
dc.subjectClimate changeen_US
dc.titleQuantification of ikaite in first and multi year sea iceen_US
dc.typemaster thesisen_US
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