Freezing Potentials and Currents in Potassium Fluoride Solutions at Constant Growth Rates

The Workman–Reynolds effect was studied in the growth of ice on a monocrystalline seed, at constant growth rates and under steady-state conditions, from KF solutions at concentrations from 2 × 10 −5 to 10 × 10 −5 Normal. Freezing potentials increased with growth rate to a maximum of 12 V at 11.2 μ m...

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Published in:Journal of Glaciology
Main Authors: Hanley, T. O’D., Weber, A. H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1973
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000031890
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031890
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spelling crcambridgeupr:10.1017/s0022143000031890 2024-03-03T08:46:08+00:00 Freezing Potentials and Currents in Potassium Fluoride Solutions at Constant Growth Rates Hanley, T. O’D. Weber, A. H. 1973 http://dx.doi.org/10.1017/s0022143000031890 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031890 en eng Cambridge University Press (CUP) Journal of Glaciology volume 12, issue 66, page 483-499 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1973 crcambridgeupr https://doi.org/10.1017/s0022143000031890 2024-02-08T08:37:11Z The Workman–Reynolds effect was studied in the growth of ice on a monocrystalline seed, at constant growth rates and under steady-state conditions, from KF solutions at concentrations from 2 × 10 −5 to 10 × 10 −5 Normal. Freezing potentials increased with growth rate to a maximum of 12 V at 11.2 μ m/s. Discharge currents through a 10 5 Ω shunt generally increased with freezing rate until a maximum of 1.5 μ A at 11.2 μ m/s. The charge transfer decreased with growth rate to 200 μ C at 10.3 μ m/s and then reached a maximum of 850 μ C at 11.2 μ m/s. Apparent diffusion coefficients of about 2 × 10 −3 mm 2 /s increased slowly with growth rate until a rapid increase began, apparently associated with interface breakdown. Distribution coefficients of the order of 10 −3 , calculated from a criterion for constitutional supercooling, increased with concentration. Parameters for LeFebre’s model of the interface showed an interface thickness of about 6 mm, an interface capacitance near one-half pF/mm 2 , and an interface resistance of about 6 × 10 4 Ω/mm 2 . Several empirical relations between these quantities were disclosed. Comparison with values obtained for KC1 solutions with the same freezing cell shows that the KF solutions yielded higher values of freezing potential, charge transfer, and distribution coefficient, and lower values of diffusion coefficient, interface capacitance, and interface resistance. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Workman ENVELOPE(-65.683,-65.683,-66.392,-66.392) Journal of Glaciology 12 66 483 499
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Hanley, T. O’D.
Weber, A. H.
Freezing Potentials and Currents in Potassium Fluoride Solutions at Constant Growth Rates
topic_facet Earth-Surface Processes
description The Workman–Reynolds effect was studied in the growth of ice on a monocrystalline seed, at constant growth rates and under steady-state conditions, from KF solutions at concentrations from 2 × 10 −5 to 10 × 10 −5 Normal. Freezing potentials increased with growth rate to a maximum of 12 V at 11.2 μ m/s. Discharge currents through a 10 5 Ω shunt generally increased with freezing rate until a maximum of 1.5 μ A at 11.2 μ m/s. The charge transfer decreased with growth rate to 200 μ C at 10.3 μ m/s and then reached a maximum of 850 μ C at 11.2 μ m/s. Apparent diffusion coefficients of about 2 × 10 −3 mm 2 /s increased slowly with growth rate until a rapid increase began, apparently associated with interface breakdown. Distribution coefficients of the order of 10 −3 , calculated from a criterion for constitutional supercooling, increased with concentration. Parameters for LeFebre’s model of the interface showed an interface thickness of about 6 mm, an interface capacitance near one-half pF/mm 2 , and an interface resistance of about 6 × 10 4 Ω/mm 2 . Several empirical relations between these quantities were disclosed. Comparison with values obtained for KC1 solutions with the same freezing cell shows that the KF solutions yielded higher values of freezing potential, charge transfer, and distribution coefficient, and lower values of diffusion coefficient, interface capacitance, and interface resistance.
format Article in Journal/Newspaper
author Hanley, T. O’D.
Weber, A. H.
author_facet Hanley, T. O’D.
Weber, A. H.
author_sort Hanley, T. O’D.
title Freezing Potentials and Currents in Potassium Fluoride Solutions at Constant Growth Rates
title_short Freezing Potentials and Currents in Potassium Fluoride Solutions at Constant Growth Rates
title_full Freezing Potentials and Currents in Potassium Fluoride Solutions at Constant Growth Rates
title_fullStr Freezing Potentials and Currents in Potassium Fluoride Solutions at Constant Growth Rates
title_full_unstemmed Freezing Potentials and Currents in Potassium Fluoride Solutions at Constant Growth Rates
title_sort freezing potentials and currents in potassium fluoride solutions at constant growth rates
publisher Cambridge University Press (CUP)
publishDate 1973
url http://dx.doi.org/10.1017/s0022143000031890
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000031890
long_lat ENVELOPE(-65.683,-65.683,-66.392,-66.392)
geographic Workman
geographic_facet Workman
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 12, issue 66, page 483-499
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000031890
container_title Journal of Glaciology
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container_issue 66
container_start_page 483
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