Temperature compensation of electrical conductivity in glacial meltwaters
Abstract Temperature compensation built into many conductivity meters becomes inaccurate in low-temperature waters typical of glacial melt streams. Experiments using simulated glacial waters show a linear dependence of electrical conductivity on temperature from 0.3° to 25°C. The slope of the temper...
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Cambridge University Press (CUP)
1992
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Online Access: | http://dx.doi.org/10.1017/s0022143000009540 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009540 |
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crcambridgeupr:10.1017/s0022143000009540 2024-09-15T18:15:37+00:00 Temperature compensation of electrical conductivity in glacial meltwaters Smart, C. C. 1992 http://dx.doi.org/10.1017/s0022143000009540 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009540 en eng Cambridge University Press (CUP) Journal of Glaciology volume 38, issue 128, page 9-12 ISSN 0022-1430 1727-5652 journal-article 1992 crcambridgeupr https://doi.org/10.1017/s0022143000009540 2024-07-31T04:03:26Z Abstract Temperature compensation built into many conductivity meters becomes inaccurate in low-temperature waters typical of glacial melt streams. Experiments using simulated glacial waters show a linear dependence of electrical conductivity on temperature from 0.3° to 25°C. The slope of the temperature–conductivity relation is linearly dependent on the conductivity of the solution, allowing a numerical or analytical temperature correction to be made. To minimize error introduced by temperature compensation, measurements of electrical conductivity in glacial streams should be corrected to a low standard temperature, and 0°C is suggested. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 38 128 9 12 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract Temperature compensation built into many conductivity meters becomes inaccurate in low-temperature waters typical of glacial melt streams. Experiments using simulated glacial waters show a linear dependence of electrical conductivity on temperature from 0.3° to 25°C. The slope of the temperature–conductivity relation is linearly dependent on the conductivity of the solution, allowing a numerical or analytical temperature correction to be made. To minimize error introduced by temperature compensation, measurements of electrical conductivity in glacial streams should be corrected to a low standard temperature, and 0°C is suggested. |
format |
Article in Journal/Newspaper |
author |
Smart, C. C. |
spellingShingle |
Smart, C. C. Temperature compensation of electrical conductivity in glacial meltwaters |
author_facet |
Smart, C. C. |
author_sort |
Smart, C. C. |
title |
Temperature compensation of electrical conductivity in glacial meltwaters |
title_short |
Temperature compensation of electrical conductivity in glacial meltwaters |
title_full |
Temperature compensation of electrical conductivity in glacial meltwaters |
title_fullStr |
Temperature compensation of electrical conductivity in glacial meltwaters |
title_full_unstemmed |
Temperature compensation of electrical conductivity in glacial meltwaters |
title_sort |
temperature compensation of electrical conductivity in glacial meltwaters |
publisher |
Cambridge University Press (CUP) |
publishDate |
1992 |
url |
http://dx.doi.org/10.1017/s0022143000009540 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009540 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 38, issue 128, page 9-12 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000009540 |
container_title |
Journal of Glaciology |
container_volume |
38 |
container_issue |
128 |
container_start_page |
9 |
op_container_end_page |
12 |
_version_ |
1810453485634715648 |