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...
Published in: | Journal of the Marine Biological Association of the United Kingdom |
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Cambridge University Press (CUP)
1923
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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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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 |
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Open Polar |
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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 |
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Journal of the Marine Biological Association of the United Kingdom |
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13 |
container_issue |
1 |
container_start_page |
160 |
op_container_end_page |
163 |
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1792498992389554176 |