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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Published in:Journal of Glaciology
Main Author: Smart, C. C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1992
Subjects:
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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spelling 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
institution Open Polar
collection Cambridge University Press
op_collection_id 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
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