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The chemical composition of sinking particles and their vertical dynamics in the open ocean.

机译:在远洋中下沉粒子的化学成分及其垂直动力学。

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摘要

Sinking particles are one of the main vehicles for transporting chemical species, including carbon, from surface waters to the deep ocean and sediments. This process reduces the partial pressure of carbon dioxide in the surface mixed layer, and plays an important role in the oceanic carbon cycle. This thesis focuses on the vertical dynamics of sinking particles, and their chemical compositions and degradation trajectories.;A new method, based on fitting Fourier series to time-series data from sediment traps, was developed to estimate settling velocities (SV's) of sinking particles in the open ocean. The results showed that estimation of SV's is more reliable when single-elements, rather than element ratios, are used as tracers. Modal settling velocities estimated using single-tracer fluxes with good temporal resolution, averaged separately for each tracer, are 205+/-74 m/d. This new estimate is in essential accord with measurements made using Indented Rotating Sphere sediment traps in "setting velocity" mode at the same site.;Three-dimensional Principal Components Analysis (PCA) was applied to data on the organic composition of sinking particles collected in MedFlux. The results showed that constructing a 1-dimensional "degradation index" is oversimplified, and the trajectory from the first 2 or 3 axes is more informative.;Masses were summed with all the major chemical components, including organic matter (OM), opal, CaCO3, and lithogenic minerals, for sinking particles. The summed mass is often less than the mass that is directly measured. This mass deficit is also observed for sinking particles at the Ross Sea, but not for those collected from other US JGOFS deep ocean sites. OM was found to be directly related to mass deficit, especially in shallow water where OM content in particles is high. I hypothesize that water bound to organic molecules or minerals particles, especially in samples from shallow depths, may not be totally dehydrated after oven drying.
机译:下沉颗粒是从地表水向深海和沉积物运输包括碳在内的化学物质的主要工具之一。该过程降低了表面混合层中二氧化碳的分压,并且在海洋碳循环中起着重要作用。本文主要研究沉降颗粒的垂直动力学及其化学组成和降解轨迹。;一种基于傅立叶级数拟合沉积物时间序列数据的新方法来估算沉降颗粒的沉降速度(SV)在大海中。结果表明,当使用单元素而不是元素比率作为示踪剂时,SV的估计更加可靠。使用具有良好时间分辨率的单示踪剂通量估算的模式沉降速度为205 +/- 74 m / d,分别对每个示踪剂进行平均。这一新的估算值与在同一位置以“设定速度”模式使用缩进的旋转球形沉积物捕集阱进行的测量结果基本一致。三维主成分分析(PCA)应用于收集的沉没颗粒有机成分数据MedFlux。结果表明,构建一维“降解指数”的过程过于简单,并且从前2个或3个轴开始的轨迹提供了更多信息。;对质量进行了归纳,包括所有主要化学成分,包括有机物(OM),蛋白石, CaCO3和成岩矿物,用于下沉颗粒。总质量通常小于直接测量的质量。在罗斯海沉没的颗粒中也观察到这种质量不足,但从美国JGOFS其他深海场所收集到的那些则没有。发现OM与质量不足直接相关,特别是在颗粒中OM含量高的浅水中。我假设与有机分子或矿物质颗粒结合的水,特别是在浅深度的样品中,在烤箱干燥后可能不会完全脱水。

著录项

  • 作者

    Xue, Jianhong.;

  • 作者单位

    State University of New York at Stony Brook.;

  • 授予单位 State University of New York at Stony Brook.;
  • 学科 Physical Oceanography.;Biogeochemistry.
  • 学位 Ph.D.
  • 年度 2008
  • 页码 188 p.
  • 总页数 188
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 海洋物理学;生物地球化学、气体地球化学;
  • 关键词

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