Ice was grown from melts of tap water and low salinity NaCl brines. The melts could, be heated from below and stirred, so that the rate of freezing, the temperature gradient below the solid-liquid (S-L) interface, and the initial concentration of the melt could be varied independently. The morphology of the S-L interface was observed at various stages of growth. [...]
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.73613 |
| Date | January 1966 |
| Creators | Kvajic, George |
| Contributors | Pounder, E. (Supervisor) |
| Publisher | McGill University |
| Source Sets | Library and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada |
| Language | English |
| Detected Language | English |
| Type | Electronic Thesis or Dissertation |
| Format | application/pdf |
| Coverage | Master of Science (Department of Physics) |
| Rights | All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. |
| Relation | alephsysno: 000481212, proquestno: AAINK00291, Theses scanned by UMI/ProQuest. |
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