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Phosphorus and silicon in sea water off Plymouth during the years 1950 tO 1953

Published online by Cambridge University Press:  11 May 2009

F. A. J. Armstrong
F. A. J. Armstrong
Affiliation:
The Plymouth Laboratory
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Extract

The analyses reported here refer to water from International Hydrographic Station E I (lat. 50° 02′ N., long. 4° 22′ W.). They extend the sequence begun in 1923 when sufficiently sensitive chemical methods were first applied at this station (Atkins, 1923 a), and reported thereafter in a series of papers from this Laboratory (Atkins, 1923a, b, 1924, 1926a, b, 1928, 1930, 1953; Cooper, 1933a, b, 1937, 1938; Harvey, 1948, 1950; Armstrong, 1951; Armstrong & Harvey, 1950). This is a factual report and interpretation and comparison with earlier years are deferred.

Type
Research Article
Information
Journal of the Marine Biological Association of the United Kingdom , Volume 33 , Issue 2 , June 1954 , pp. 381 - 392
Copyright
Copyright © Marine Biological Association of the United Kingdom 1954

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References

Armstrong, F. A. J., 1949. A source of error in the absorptiometric determination of inorganic and total phosphorus in sea water. J. Mar. Biol. Ass. U.K., Vol. 28, pp. 701–5.Google Scholar
Armstrong, F. A. J., 1951. The determination of silicate in sea water. J. Mar. Biol. Ass. U.K., Vol. 30, pp. 149–60.Google Scholar
Armstrong, F. A. J. & Atkins, W. R. G., 1950. The suspended matter of sea water. J. Mar. Biol. Ass. U.K., Vol. 29, pp. 139–43.Google Scholar
Armstrong, F. A. J. & Harvey, H. W., 1950. The cycle of phosphorus in the waters of the English Channel. J. Mar. biol. Ass. U.K., Vol. 29, pp. 145–62.Google Scholar
Atkins, W. R. G., 1923 a. The phosphate content of fresh and salt waters in its relationship to the growth of the algal plankton. J. Mar. biol. Ass. U.K., Vol. 13, pp. 119–50.Google Scholar
Atkins, W. R. G., 1923 b. The silica content of some natural waters and of culture media. J. Mar. biol. Ass. U.K., Vol. 13, pp. 151–9.Google Scholar
Atkins, W. R. G., 1924. Seasonal changes in the phosphate content of sea water in relation to the growth of the algal plankton during 1923 and 1924. J. Mar. biol. Ass. U.K., Vol. 13, pp. 700–20.Google Scholar
Atkins, W. R. G., 1926 a. Seasonal changes in the silica content of natural waters in relation to the phytoplankton. J. Mar. biol. Ass. U.K., Vol. 14, pp. 89–99.Google Scholar
Atkins, W. R. G., 1926 b. The phosphate content of sea water in relation to the growth of the algal plankton. Part III. J. Mar. biol. Ass. U.K., Vol. 14, pp. 447–67.Google Scholar
Atkins, W. R. G., 1928. Seasonal variations in the phosphate and silicate content of sea water during 1926 and 1927 in relation to the phytoplankton crop. J. Mar. biol. Ass. U.K., Vol. 15, pp. 191–205.Google Scholar
Atkins, W. R. G., 1930. Seasonal variations in the phosphate and silicate content of sea water in relation to the phytoplankton crop. Part V. November 1927 to April 1929, compared with earlier years from 1923. J. Mar. biol. Ass. U.K., Vol. 16, pp. 821–52.Google Scholar
Atkins, W. R. G., 1953. Seasonal variations in the phosphate and silicate content of sea water. Part VI. 1948 compared with the 1923–25 period. J. Mar. biol. Ass. U.K., Vol. 31, pp. 489–92.Google Scholar
Atkins, W. R. G., Jenkins, P. G. & Warren, F. J., 1954. The suspended matter in sea water and its seasonal changes as affecting the visual range of the Secchi disc. J. Mar. biol. Ass. U.K., Vol. 33, pp. 497–509.Google Scholar
Cooper, L. H. N., 1933 a. Chemical constituents of biological importance in the English Channel, November 1930 to January 1932. Part I. Phosphate, silicate, nitrate, nitrite, ammonia. J. Mar. biol. Ass. U.K., Vol. 18, pp. 677–728.Google Scholar
Cooper, L. H. N., 1933 b. Chemical constituents of biological importance in the English Channel. Part III. June-December, 1932. Phosphate, silicate, nitrite, hydrogen ion concentration, with a comparison with wind records. J. Mar. biol. Ass. U.K., Vol. 19, pp. 55–62.Google Scholar
Cooper, L. H. N., 1937. ‘Organic’ phosphorus in sea water from the English Channel. J. Mar. biol. Ass. U.K., Vol. 21, pp. 673–7.Google Scholar
Cooper, L. H. N., 1938. Phosphate in the English Channel, 1933–8, with a comparison with earlier years, 1916 and 1923–32. J. Mar. biol. Ass. U.K., Vol. 23, pp. 181–95.Google Scholar
Gorgy, S., Rakestraw, N. & Fox, D., 1948. Arsenic in the sea. J. Mar. Res., Vol. 7, pp. 22–32.Google Scholar
Hansen, A. L. & Robinson, R. J., 1953. The determination of organic phosphorus in sea water with perchloric acid oxidation. J. Mar. Res., Vol. 12, pp. 31–42.Google Scholar
Harvey, H. W., 1948. The estimation of phosphate and of total phosphorus in sea waters. J. Mar. biol. Ass. U.K., Vol. 27, pp. 337–59.Google ScholarPubMed
Cooper, L. H. N., 1950. On the production of living matter in the sea off Plymouth. J. Mar. biol. Ass. U.K., Vol. 29, pp. 97–137.Google Scholar
Redfield, A. C, Smith, H. & Ketchum, B. H., 1937. The cycle of organic phosphorus in the Gulf of Maine. Biol. Bull., Wood's Hole, Vol. 73, pp. 421–43.Google Scholar
Smales, A. A. & Pate, B. D., 1952. The determination of sub-microgram quantities of arsenic by radioactivation. Analyst, Vol. 77, pp. 188–95.Google Scholar