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Geochemical and physical processes influencing the composition of particles in diverse environments, eastern North Atlantic Ocean.

机译:影响北大西洋东部不同环境中颗粒组成的地球化学和物理过程。

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摘要

To understand global biogeochemical cycling in the oceans it is imperative to develop comprehensive models of the processes influencing elements in the suspended particulate phase. This thesis examines the character of particles from a wide variety of environments in the Eastern North Atlantic Ocean in order: (1) to enhance our knowledge of the physical and geochemical processes influencing resuspended matter; (2) to determine over what distances distinct water masses can transport characteristic particle suites; (3) to develop models for the formation and transformation of distinct mineral phases associated with hydrothermal plumes.;Particles were collected by filtering water from 30 liter Niskin bottles and by using in situ high-volume filtration equipment during the FLUXATLANTE (R/V Suroi t, 1985) and RRS Discovery 159 (1986) cruises. Particles were characterized using some or all of the following techniques: instrumental neutron activation (for Al, Ca, Fe, Mn, Cu, V, and/or I), scanning electron microscopy and energy dispersive x-ray analyses.;Differences between resuspended nepheloid materials and underlying surface sediments are attributed to preferential resuspension of fine-grained materials with a distinctive geochemical signature. Classical signs of early alteration processes such as dissolution of biogenic tests and remineralization of organic matter in the sediment column are observed.;Long-distance transport (to 800 km) of aluminosilicates occurs with advection of Mediterranean Outflow Water (MEDW). Mixing with Eastern North Atlantic Intermediate Water (ENAIW) accounts for an enhanced particulate Ca/Al and Mn/Al in intermediate waters with distance from Gibraltar and there is no evidence for adsorption of dissolved Mn introduced with the MEDW plume over distance scales ;Between 15 to 75% of the materials transported in the Trans-Atlantic Geotraverse hydrothermal plume (26
机译:为了了解海洋中的全球生物地球化学循环,必须开发出影响悬浮颗粒相中各元素的过程的综合模型。本文研究了北大西洋东部各种环境中的颗粒特征,以:(1)增强我们对影响重悬物质的物理和地球化学过程的了解; (2)确定不同的水团可以在多远的距离上传输特征粒子组; (3)建立与热液羽流相关的独特矿物相形成和转化的模型。;在FLUXATLANTE(R / V Suroi)期间通过过滤30升Niskin瓶中的水并使用现场大容量过滤设备收集颗粒,1985年)和RRS Discovery 159(1986年)巡游。使用以下一些或全部技术对颗粒进行表征:仪器中子活化(对于Al,Ca,Fe,Mn,Cu,V和/或I),扫描电子显微镜和能量色散X射线分析;重悬之间的差异肾小球物质和下面的表面沉积物归因于具有独特地球化学特征的细粒物质的优先重悬。观察到了早期改变过程的经典迹象,例如生物测试的溶解和沉积物柱中有机物的再矿化。;随着地中海流出水(MEDW)的平流发生了铝硅酸盐的长距离运输(至800 km)。与北大西洋东部中间水(ENAIW)混合导致距离直布罗陀的中间水域中的颗粒Ca / Al和Mn / Al增强,并且没有证据表明在距离范围内MEDW羽流引入了溶解的Mn的吸附; 15之间跨大西洋地缘热液羽流中运输的物料的75%(26

著录项

  • 作者

    Isley, Ann Elaine.;

  • 作者单位

    University of Rhode Island.;

  • 授予单位 University of Rhode Island.;
  • 学科 Geochemistry.;Geology.;Mineralogy.
  • 学位 Ph.D.
  • 年度 1990
  • 页码 173 p.
  • 总页数 173
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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