Hostname: page-component-cd9895bd7-dzt6s Total loading time: 0 Render date: 2024-12-22T17:36:36.316Z Has data issue: false hasContentIssue false
  • English
  • Français

Seasonal Changes in the Silica Content of Natural Waters in Relation to the Phytoplankton.

Published online by Cambridge University Press:  11 May 2009

W. R. G. Atkins
W. R. G. Atkins
Affiliation:
Head of the Department of General Physiology at the Plymouth Laboratory.
Get access Rights & Permissions [Opens in a new window]

Extract

1. The method of Dienert and Wandenbulcke permits of the estimation of silicate in solution down to the limit of 0-04 mg. of silica per litre, which cannot be distinguished from zero. The phosphate normally present does not interfere with the reaction.

2. All fresh waters examined were found to contain more silicate than does the water of the English Channel.

3. The water of Plymouth Sound is richer in silicate than that of the sea.

4. At Station El in the English Channel silicate decreases during spring, from a winter maximum of 200-240 mg. per cubic metre, so that from April to June, 1925, the amount left, recorded as 40 mg. per cubic metre, was indistinguishable from zero. At this time the water was stripped of phosphate also. Silicate increased again till early July, decreased in August and again in November ; the times of decrease are suggested as being those of diatom increase.

5. In deep Atlantic water silicate is much more abundant than in the English Channel; values from 360 mg. per cubic metre at 1000 metres to 1200 mg. at 3000 metres were obtained. In winter at any rate the surface value in the Atlantic is similar to that off Plymouth, about 110 mg.per m3 in 1925.

Type
Research Article
Information
Journal of the Marine Biological Association of the United Kingdom , Volume 14 , Issue 1 , March 1926 , pp. 89 - 99
Copyright
Copyright © Marine Biological Association of the United Kingdom 1926

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Atkins, W. R. G. 1923. The silica content of some natural waters and of culture media. Journ. Mar. Biol. Assoc. 13, 151–159.CrossRefGoogle Scholar
Atkins, W. R. G. and Harris, G. T. 1924. Seasonal changes in the water and heleoplankton of freshwater ponds. Sci. Proc. Roy. Dublin Soc., 18, 1–21, and Notes Bot. School, Trinity College, Dublin,1925, 3, No. 6, 281–301.Google Scholar
Atkins, W. R. G. and Harris, G. T. 1925. Abstract of above, with three figures. Journ. Mar. Biol. Assoc, 13, 750–754.CrossRefGoogle Scholar
Atkins, W. R. G. and Harvey, H. W. 1925. The variation with depth of certa salts utilised in plant growth in the sea. Nature, 116, 784.CrossRefGoogle Scholar
Brandt, K. 1920. Über den Stoffwechsel im Meere. 3 Abhandlung. Wiss. Meeresuntersuch. Abt. Kiel, 18, 185–430.Google Scholar
Dienert, F. and Wandenbulcke, F. 1923. Sur le dosage de la silice dans les eaux. C.R. Acad. des Sciences, Paris, 176, 1478–1480.Google Scholar
Thresh, J. C. and Beale, J. F. 1925. The examination of waters and water supplies. London.Google Scholar