The density–salinity relation of standard seawater

The determination of salinity by means of electrical conductivity relies on stable salt proportions in the North Atlantic Ocean, because standard seawater, which is required for salinometer calibration, is produced from water of the North Atlantic. To verify the long-term stability of the standard s...

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Published in:Ocean Science
Main Authors: H. Schmidt, S. Seitz, E. Hassel, H. Wolf
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
G
Online Access:https://doi.org/10.5194/os-14-15-2018
https://doaj.org/article/e8b742a4a7c9483cbd4eacef953ff356
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spelling ftdoajarticles:oai:doaj.org/article:e8b742a4a7c9483cbd4eacef953ff356 2023-05-15T17:31:08+02:00 The density–salinity relation of standard seawater H. Schmidt S. Seitz E. Hassel H. Wolf 2018-01-01T00:00:00Z https://doi.org/10.5194/os-14-15-2018 https://doaj.org/article/e8b742a4a7c9483cbd4eacef953ff356 EN eng Copernicus Publications https://www.ocean-sci.net/14/15/2018/os-14-15-2018.pdf https://doaj.org/toc/1812-0784 https://doaj.org/toc/1812-0792 doi:10.5194/os-14-15-2018 1812-0784 1812-0792 https://doaj.org/article/e8b742a4a7c9483cbd4eacef953ff356 Ocean Science, Vol 14, Pp 15-40 (2018) Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2018 ftdoajarticles https://doi.org/10.5194/os-14-15-2018 2022-12-31T10:05:37Z The determination of salinity by means of electrical conductivity relies on stable salt proportions in the North Atlantic Ocean, because standard seawater, which is required for salinometer calibration, is produced from water of the North Atlantic. To verify the long-term stability of the standard seawater composition, it was proposed to perform measurements of the standard seawater density. Since the density is sensitive to all salt components, a density measurement can detect any change in the composition. A conversion of the density values to salinity can be performed by means of a density–salinity relation. To use such a relation with a target uncertainty in salinity comparable to that in salinity obtained from conductivity measurements, a density measurement with an uncertainty of 2 g m −3 is mandatory. We present a new density–salinity relation based on such accurate density measurements. The substitution measurement method used is described and density corrections for uniform isotopic and chemical compositions are reported. The comparison of densities calculated using the new relation with those calculated using the present reference equations of state TEOS-10 suggests that the density accuracy of TEOS-10 (as well as that of EOS-80) has been overestimated, as the accuracy of some of its underlying density measurements had been overestimated. The new density–salinity relation may be used to verify the stable composition of standard seawater by means of routine density measurements. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Ocean Science 14 1 15 40
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
spellingShingle Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
H. Schmidt
S. Seitz
E. Hassel
H. Wolf
The density–salinity relation of standard seawater
topic_facet Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
description The determination of salinity by means of electrical conductivity relies on stable salt proportions in the North Atlantic Ocean, because standard seawater, which is required for salinometer calibration, is produced from water of the North Atlantic. To verify the long-term stability of the standard seawater composition, it was proposed to perform measurements of the standard seawater density. Since the density is sensitive to all salt components, a density measurement can detect any change in the composition. A conversion of the density values to salinity can be performed by means of a density–salinity relation. To use such a relation with a target uncertainty in salinity comparable to that in salinity obtained from conductivity measurements, a density measurement with an uncertainty of 2 g m −3 is mandatory. We present a new density–salinity relation based on such accurate density measurements. The substitution measurement method used is described and density corrections for uniform isotopic and chemical compositions are reported. The comparison of densities calculated using the new relation with those calculated using the present reference equations of state TEOS-10 suggests that the density accuracy of TEOS-10 (as well as that of EOS-80) has been overestimated, as the accuracy of some of its underlying density measurements had been overestimated. The new density–salinity relation may be used to verify the stable composition of standard seawater by means of routine density measurements.
format Article in Journal/Newspaper
author H. Schmidt
S. Seitz
E. Hassel
H. Wolf
author_facet H. Schmidt
S. Seitz
E. Hassel
H. Wolf
author_sort H. Schmidt
title The density–salinity relation of standard seawater
title_short The density–salinity relation of standard seawater
title_full The density–salinity relation of standard seawater
title_fullStr The density–salinity relation of standard seawater
title_full_unstemmed The density–salinity relation of standard seawater
title_sort density–salinity relation of standard seawater
publisher Copernicus Publications
publishDate 2018
url https://doi.org/10.5194/os-14-15-2018
https://doaj.org/article/e8b742a4a7c9483cbd4eacef953ff356
genre North Atlantic
genre_facet North Atlantic
op_source Ocean Science, Vol 14, Pp 15-40 (2018)
op_relation https://www.ocean-sci.net/14/15/2018/os-14-15-2018.pdf
https://doaj.org/toc/1812-0784
https://doaj.org/toc/1812-0792
doi:10.5194/os-14-15-2018
1812-0784
1812-0792
https://doaj.org/article/e8b742a4a7c9483cbd4eacef953ff356
op_doi https://doi.org/10.5194/os-14-15-2018
container_title Ocean Science
container_volume 14
container_issue 1
container_start_page 15
op_container_end_page 40
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