| Reference Type | Journal (article/letter/editorial) |
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| Title | Network Geometry of Veins in Polycrystalline Ice |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Langham, E. J. | Author |
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| Year | 1974 (September 1) | Volume | 11 |
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| Issue | 9 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e74-119Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 474206 | Long-form Identifier | mindat:1:5:474206:1 |
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| GUID | 0 |
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| Full Reference | Langham, E. J. (1974) Network Geometry of Veins in Polycrystalline Ice. Canadian Journal of Earth Sciences, 11 (9) 1274-1279 doi:10.1139/e74-119 |
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| Plain Text | Langham, E. J. (1974) Network Geometry of Veins in Polycrystalline Ice. Canadian Journal of Earth Sciences, 11 (9) 1274-1279 doi:10.1139/e74-119 |
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| In | (1974, September) Canadian Journal of Earth Sciences Vol. 11 (9) Canadian Science Publishing |
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| Abstract/Notes | Polycrystalline ice contains a three-dimensional network of water filled veins, whose size is a function of temperature among other parameters. In order to study heat transfer to and from these veins, a model of their arrangement around a crystal is necessary. The geometrical constraints of this arrangement are discussed and a model is proposed. This is compared to various other models, including that used by Frank (1968) for convection in the earth's mantle. |
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