ON THE NUTRIENT SALTS OF THE SOUTHERN OCEAN IN THE SECTION BETWEEN QUEEN MAUD LAND AND SOUTH AFRICA (Reports read at the Symposium on Polar Oceanography)

The serial observations were carried out along 10°-15° E at every 5° in latitude in JARE-7. In the Antarctic Circumpolar Water, 24 μg-atoms/L of phosphate-P, 100 μg-atoms/L of silicate-Si and 35-38 μg-atoms/L of nitratc-N were observed There was difference between the distribution of phosphate-P and...

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Bibliographic Details
Main Author: Masaru SHIOZAKI
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 1966
Subjects:
geo
Online Access:https://doi.org/10.15094/00007424
https://doaj.org/article/4ff22503185f435c873683fea88cff23
Description
Summary:The serial observations were carried out along 10°-15° E at every 5° in latitude in JARE-7. In the Antarctic Circumpolar Water, 24 μg-atoms/L of phosphate-P, 100 μg-atoms/L of silicate-Si and 35-38 μg-atoms/L of nitratc-N were observed There was difference between the distribution of phosphate-P and that of silicate-Si, the maximum values of phosphate-P and mtrate-N were observed in 400-600m layer at 60°S, but that of silicate-Si was at a depth of 1,500m Regeneration of phosphate-P and nitrate-N was observed in 400-600m layer in the Antarctic zone and the Antarctic Intermediate Water, and the regeneration of almost all silicate-Si was estimated in the Antarctic zone