| Reference Type | Journal (article/letter/editorial) |
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| Title | Phase Equilibria 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/e74-120Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 474209 | Long-form Identifier | mindat:1:5:474209:2 |
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| GUID | 0 |
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| Full Reference | Langham, E. J. (1974) Phase Equilibria of Veins in Polycrystalline Ice. Canadian Journal of Earth Sciences, 11 (9) 1280-1287 doi:10.1139/e74-120 |
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| Plain Text | Langham, E. J. (1974) Phase Equilibria of Veins in Polycrystalline Ice. Canadian Journal of Earth Sciences, 11 (9) 1280-1287 doi:10.1139/e74-120 |
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| In | (1974, September) Canadian Journal of Earth Sciences Vol. 11 (9) Canadian Science Publishing |
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| Abstract/Notes | The permeability of ice layers in the snowpack can have far reaching effects on its response to meltwater or rain. This permeability is due to the presence of veins of liquid water at the junctions of the crystals. It is shown that the size of these veins is very sensitive to changes of temperature, air pressure, and dissolved air or other material. |
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