Grain-size related nitrogen distribution in southern Yellow Sea surface sediments
Forty-eight surface sediments of the southern Yellow Sea are separated into three grain-size fractions. Four forms of extractable nitrogen (nitrogen in ion-exchangeable form (Nie), nitrogen in weak-acid extractable form (Nwa), nitrogen in strong-alkali extractable form (Nsa) and nitrogen in strong-o...
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Published in | Chinese journal of oceanology and limnology Vol. 23; no. 3; pp. 306 - 316 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Dordrecht
Springer Nature B.V
01.09.2005
The Graduate School of Chinese Academy of Sciences, Beijing 100039, China Institute of Oceanology, Chinese Academy of Sciences,No.7 Nanhai Road, Qingdao 266071, China College of Marine Geoscience, Ocean University of China, Qingdao 266003, China%Institute of Oceanology, Chinese Academy of Sciences,No.7 Nanhai Road, Qingdao 266071, China%Institute of Oceanology, Chinese Academy of Sciences,No.7 Nanhai Road, Qingdao 266071, China |
Subjects | |
Online Access | Get full text |
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Summary: | Forty-eight surface sediments of the southern Yellow Sea are separated into three grain-size fractions. Four forms of extractable nitrogen (nitrogen in ion-exchangeable form (Nie), nitrogen in weak-acid extractable form (Nwa), nitrogen in strong-alkali extractable form (Nsa) and nitrogen in strong-oxidant form (N50))are obtained by the sequential extraction. The results show that the contents and the distributions of the extractable nitrogen in the southern Yellow Sea surface sediments are closely related to sediment grain size. The distributions ofNie, Nso and total nitrogen (TN) present positive correlations with fine particles content, while Nwa and Nsa does not have such correlation. The net contents of all the forms of nitrogen increase with sediment grain size finer. |
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Bibliography: | X143 X522 37-1150/P ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0254-4059 2096-5508 1993-5005 2523-3521 |
DOI: | 10.1007/BF02847153 |