Note on the Oxidisable Organic Matter of Sea Water

In a former paper (1922) it was shown that the pH value of stored sea water decreased owing to the production of carbonic acid by organisms in it, and the oxidisable matter as indicated by this biological method appeared to be higher than the result obtained by oxidation with permanganate, according...

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Published in:Journal of the Marine Biological Association of the United Kingdom
Main Author: Atkins, W. R. G.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1923
Subjects:
Online Access:http://dx.doi.org/10.1017/s0025315400010973
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0025315400010973
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spelling crcambridgeupr:10.1017/s0025315400010973 2024-03-03T08:43:33+00:00 Note on the Oxidisable Organic Matter of Sea Water Atkins, W. R. G. 1923 http://dx.doi.org/10.1017/s0025315400010973 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0025315400010973 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of the Marine Biological Association of the United Kingdom volume 13, issue 1, page 160-163 ISSN 0025-3154 1469-7769 Aquatic Science journal-article 1923 crcambridgeupr https://doi.org/10.1017/s0025315400010973 2024-02-08T08:37:29Z In a former paper (1922) it was shown that the pH value of stored sea water decreased owing to the production of carbonic acid by organisms in it, and the oxidisable matter as indicated by this biological method appeared to be higher than the result obtained by oxidation with permanganate, according to various analyses available for comparison. These, however, were not done on the same water, so an attempt was made to determine this quantity on water of the English Channel off Plymouth. As is well known the permanganate method gives results which vary appreciably, according to the conditions of the experiment. Article in Journal/Newspaper Carbonic acid Cambridge University Press Journal of the Marine Biological Association of the United Kingdom 13 1 160 163
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Aquatic Science
spellingShingle Aquatic Science
Atkins, W. R. G.
Note on the Oxidisable Organic Matter of Sea Water
topic_facet Aquatic Science
description In a former paper (1922) it was shown that the pH value of stored sea water decreased owing to the production of carbonic acid by organisms in it, and the oxidisable matter as indicated by this biological method appeared to be higher than the result obtained by oxidation with permanganate, according to various analyses available for comparison. These, however, were not done on the same water, so an attempt was made to determine this quantity on water of the English Channel off Plymouth. As is well known the permanganate method gives results which vary appreciably, according to the conditions of the experiment.
format Article in Journal/Newspaper
author Atkins, W. R. G.
author_facet Atkins, W. R. G.
author_sort Atkins, W. R. G.
title Note on the Oxidisable Organic Matter of Sea Water
title_short Note on the Oxidisable Organic Matter of Sea Water
title_full Note on the Oxidisable Organic Matter of Sea Water
title_fullStr Note on the Oxidisable Organic Matter of Sea Water
title_full_unstemmed Note on the Oxidisable Organic Matter of Sea Water
title_sort note on the oxidisable organic matter of sea water
publisher Cambridge University Press (CUP)
publishDate 1923
url http://dx.doi.org/10.1017/s0025315400010973
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0025315400010973
genre Carbonic acid
genre_facet Carbonic acid
op_source Journal of the Marine Biological Association of the United Kingdom
volume 13, issue 1, page 160-163
ISSN 0025-3154 1469-7769
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0025315400010973
container_title Journal of the Marine Biological Association of the United Kingdom
container_volume 13
container_issue 1
container_start_page 160
op_container_end_page 163
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