Respected readers, authors and reviewers, you can add comments to this page on any questions about the contribution, review, editing and publication of this journal. We will give you an answer as soon as possible. Thank you for your support!
MA Hong-bo, SONG Jin-ming, LÜ Xiao-xia. Nitrogen forms and decomposition of organic carbon in the southern Bohai Sea core sediments[J]. Haiyang Xuebao, 2002, 24(5): 64-70.
Citation:
MA Hong-bo, SONG Jin-ming, LÜ Xiao-xia. Nitrogen forms and decomposition of organic carbon in the southern Bohai Sea core sediments[J]. Haiyang Xuebao, 2002, 24(5): 64-70.
MA Hong-bo, SONG Jin-ming, LÜ Xiao-xia. Nitrogen forms and decomposition of organic carbon in the southern Bohai Sea core sediments[J]. Haiyang Xuebao, 2002, 24(5): 64-70.
Citation:
MA Hong-bo, SONG Jin-ming, LÜ Xiao-xia. Nitrogen forms and decomposition of organic carbon in the southern Bohai Sea core sediments[J]. Haiyang Xuebao, 2002, 24(5): 64-70.
Sequential extraction process in natural grain size is used to study the existent forms of nitrogen of five core sediments in the southern Bohai Sea, and form characteristics of nitrogen and its diagenesis process are researched.Results indicate that transferable nitrogen accounts for 34.25% of total nitrogen(TN) and exists mainly in the form of OSF-N and IEF-N, which have different distributions and their early diagenesis varies distinctly.Organic nitrogen(ON) has the decomposition rate constant of 15.51×10-3a-3, and rate constant of C, N, P, Si has the sequence N > P > C > Si.The main reason for much lower C/N ratio than OC/ON is that abundant nitrogen is pr eserved during the early diagenesis.OC/ON ratio decreases with depth, which is due to two main reasons:abundant inactive components contained in ON and ON adsorption to clay minerals.In general, transferable nitrogen accounts for more proportion of TN in surface than in deep layer of core sediment.The stable forms can activate and become transfer able under some special circumstance, which induces the proportion of transferable nitrogen in TN in deep layer to he almost the same with in surface.
RUTTENBURG K C.Development of a sequential extraction method for different forms of phosphorus in marine sediments[J].Limnol Oceanogr,1992,37:1 460-1 482.
SMART M M,RADAR G,DONNERMEYER G N.Determination of total nitrogen in sediments and plants using persulfatedigestion[J].Water Res,1983,17(9):1 207-1 211.
GB 17378.4-1998,海洋监测规范[S].
ANDERSON L A,SARMIENTO J L.Redfield ratios of remineralization determined by nutrient data analysis[A].Global Biogeochemical Cycles(8)[M],1994.65-80.
HAMMOND D E,MCMANUS J,BERELSON W M,et al.Early diagenesis of organic material in equatorial Pacific sediments:stoichiometry and kinetics[J].Limnol Oceanogr,1996,43(4~6):1 365-1 412.
COWIE G,HEDGES J I,CALVERT S E.Sources and relative reactivities of amino acids,neutral sugars,and lignin in an intermittently anoxic marine environment[J].Geochimica &Cosmochimica Acta,1992,56:1 963-1 978.