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南黄海沉积物中氮、磷的生物地球化学行为

BIOGEOCHEMICAL CHARACTERISTICS OF NITROGEN AND PHOSPHORUS IN THE SOUTH YELLOW SEA SEDIMENTS

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【作者】 宋金明李学刚邵君波贺志鹏张乃星

【Author】 SONG Jin-Ming, LI Xue-Gang, SHAO Jun-Bo,HE Zhi-Peng ,ZHANG Nai-Xing (Institute of Oceanology,Chinese Academy of Sciences,Qingdao,266071)(Zhoushan Marine Eco-environmental Monitoring Station of Zhejiang Province,Zhoushan,316004) (Institute of Oceanology,Chinese Academy of Sciences,Qingdao,266071;The Graduate School,Chinese Academy of Sciences,Beijing,100039)

【机构】 中国科学院海洋研究所浙江省舟山海洋生态环境监测站中国科学院北京研究生院北京100039中国科学院北京研究生院北京100039 青岛266071青岛266071舟山316004

【摘要】 于2004年10月采集南黄海4个站位的柱状沉积物和29个站位的表层沉积物,用氧化浸取分光光度法研究了自然粒度下沉积物中的氮、磷分布特征以及控制其分布的生物地球化学机制。结果表明,多数站位随着沉积深度的增加,沉积物中氮、磷浓度趋于稳定。4个站稳定时氮浓度平均约为289μg/g,磷约为329μg/g,平均稳定浓度出现的沉积层次分别为氮>30cm,磷>22cm。氮、磷垂直分布形状的规则性与沉积速率密切相关,沉积速率越小的站位,其氮、磷垂直分布愈规则;海洋沉积物中的氮主要来源自海洋生物的代谢,而磷与陆源碎屑输入密切相关。氮与沉积物粘土含量、浮游动物生物量干重有明显的正相关关系。海水中浮游动物干重每增加1mg/m3,则沉积物中氮浓度增加5.64μmol/g,磷不存在这样的关系。沉积物中氮的早期成岩速率远高于磷,在沉积物海水界面附近氮约为磷的7.4倍。海水浮游生物生物量与沉积物中氮的早期成岩类型密切相关,在所研究的2004年秋季海水中,浮游动物生物量干重19mg/m3是沉积物中氮早期成岩类型转变的界限值,小于这一界限值,水体中的氮趋向于向沉积物中凝聚;大于19mg/m3,则沉积物中的氮趋向于向水体释放。

【Abstract】 The distributions of nitrogen(N)and phosphorus(P)in sediment cores in the south Yellow Sea(SYS)were studied in detail in this paper.The core sediments from 4 stations and surface sediments from 29 stations were collected in SYS in October 2004.The peak concentrations of N and P in the sediments,occurred in depth of 5—35cm,and the phosphorus peak was close to the sediment-seawater interface.The concentrations gradually approach to constants with the depth increasing.The average constant concentrations were 289 and 329μg/g for N and P in depth of >30cm and >22cm,respectively.The vertical patterns of N and P distribution were closely related to the sedimentation rate in a regular pattern at the stations with low sedimentation rate.The N content in sediment was mainly from the metabolism of marine organisms,while that of P was mainly from input of terrestrial detritus.The ratio of N/P was controlled by N distribution in the sediments of SYS.A clear positive correlation has been revealed among N concentration,clay amount in the sediment and dry weight of zooplankton biomass.For every 1mg/m3 increased in dry weight,the N concentration would add 5.64μmol/g up;however,no such relation has been found for P.Early diagenesis rate of N was much higher than that of P, e.g.the rate of N was 7.4 times greater than that of P in sediments.The critical value of early diagenesis for N was 19mg/m3 calculated from the data of autumn 2004.In other words,below the value,N in seawater would incline to accumulate in sediments;while above the threshold,N would be released from sediment to seawater.

【基金】 中国科学院创新重大项目,KZCX1SW0108号;中国科学院“百人计划”资助项目,科人2003202号;青岛市科技将才专项计划项目,043JJ03号和052JC90
  • 【文献出处】 海洋与湖沼 ,Oceanologia et Limnologia Sinica , 编辑部邮箱 ,2006年04期
  • 【分类号】P736.41
  • 【被引频次】104
  • 【下载频次】872
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