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Temporal variations of dimethylsulfide and dimethylsulfoniopropionate in the southern Yellow Sea in spring and autumn

机译:春季和秋季,黄海南部的二甲基硫醚和二甲基磺酸丙酸甲酯的时间变化

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摘要

Temporal distributions of dimethylsulfide (DMS) and dimethylsulfoniopropionate (DMSP) were studied in the southern Yellow Sea (SYS) during April and September 2010. The mean concentrations (range) of DMS, dissolved and particulate DMSP (DMSPd and DMSPp) in the surface waters in spring are 1.69 (0.48–4.92), 3.18 (0.68–6.75) and 15.81 (2.82–52.33) nmol/L, respectively, and those in autumn are 2.80 (1.33–5.10), 5.45 (2.19–11.30) and 30.63 (6.24–137.87) nmol/L. On the whole, the distributions of DMS and DMSP in spring are completely different from those in autumn. In the central part of the SYS, the concentrations of DMS and DMSP in spring are obviously higher than those in autumn, but the opposite situation is found on the south of 34°N, which can be attributed to the differences in nutrients and phytoplankton biomass and composition between spring and autumn. Besides, the seasonal variations of water column stability and the Changjiang diluted water also have significant impact on the distributions of DMS and DMSP in spring and autumn on the south of 34°N. DMS and DMSPp concentrations coincide well with chlorophylla (Chla) levels in the spring cruise, suggesting that phytoplankton biomass may play an important role in controlling the distributions of DMS and DMSPp in the study area. Annual DMS emission rates range from 0.015 to 0.033 Tg/a (calculated by S), respectively, using the equations of Liss and Merlivat (1986) and Wanninkhof (1992). This result implies a significant relative contribution of the SYS to the global oceanic DMS fluxes.
机译:在2010年4月至9月期间,在黄海南部(SYS)研究了二甲基硫醚(DMS)和二甲基磺丙酸甲酯(DMSP)的时间分布。地表水中DMS的平均浓度(范围),溶解的和颗粒状的DMSP(DMSPd和DMSPp)春季分别为1.69(0.48–4.92),3.18(0.68–6.75)和15.81(2.82–52.33)nmol / L,秋季为2.80(1.33–5.10),5.45(2.19–11.30)和30.63( 6.24–137.87)nmol / L。总体而言,春季的DMS和DMSP分布与秋季完全不同。在SYS的中部,春季DMS和DMSP的浓度明显高于秋季,但在34°N以南发现相反的情况,这可以归因于养分和浮游植物生物量的差异和春季和秋季之间的组成。此外,在北纬34°以南的春季和秋季,水柱稳定性和长江稀释水的季节变化也对DMS和DMSP的分布有显着影响。在春季巡游中,DMS和DMSPp的浓度与叶绿素(Chla)浓度非常吻合,表明浮游植物生物量可能在控制研究区域内DMS和DMSPp的分布中起重要作用。使用Liss和Merlivat(1986)和Wanninkhof(1992)的方程式,DMS的年排放速率分别为0.015-0.033 Tg / a(用S计算)。这一结果暗示了SYS对全球海洋DMS通量的重要相对贡献。

著录项

  • 来源
    《海洋学报(英文版)》 |2016年第2期|76-87|共12页
  • 作者单位

    Key Laboratory of Ministry of Education for Marine Chemistry Theory and Technology, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;

    Coastal Environment Engineering Technology Research Center of Shandong Province, Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai 264003, China;

    Key Laboratory of Ministry of Education for Marine Chemistry Theory and Technology, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;

    Key Laboratory of Ministry of Education for Marine Chemistry Theory and Technology, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;

    Key Laboratory of Ministry of Education for Marine Chemistry Theory and Technology, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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  • 入库时间 2022-08-19 03:57:51
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