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The formation of organic sulfides by reaction of lipids with aqueous sulfides in three Holocene sediments.

机译:在三个全新世沉积物中,脂质与含水硫化物反应形成有机硫化物。

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摘要

This thesis focuses on the formation of organic-sulfide compounds in recent sediments by the chemical reaction of sedimentary lipids and dissolved pore-water sulfides. This chemical reaction, termed natural sulfidization, converts individual organic compounds into high-molecular-weight, sulfide-rich sedimentary organic material and discrete organic-sulfides which are thought to be more resistant to the degradative conditions of early diagenesis than the original organic compounds. This process is widely accepted as an important diagenetic pathway for enhancing the preservation of organic matter during sediment burial. The analyses of sediments from two marine environments, the Santa Barbara Basin and the Peru margin upwelling zone, and a sulfate-containing lacustrine environment, Mud Lake, FL are the focus of these investigations. The concentrations and stable carbon-isotopic compositions of sulfidized compounds and unreacted compounds with the same carbon skeleton are compared in these sediments to determine reaction pathways for the sulfidization of lipids. Additionally, a laboratory sulfidization study of the reaction of model compounds containing functional groups that are structurally similar to those found in recent sediments with aqueous solutions of sodium tetrasulfide and H;Despite the high organic carbon contents in each of the environments and high concentrations of reactive lipid components, organic-sulfide formation was not extensive in the Peru margin or Santa Barbara Basin sediments or the uppermost sediments from Mud Lake. For example, the upper 100 cm of Mud Lake contains high concentration of n-alkenes, which were shown to be reactive in the model compound study under aqueous conditions, but no evidence for their sulfidization was found.;Direct evidence for the role of polysulfides in the sulfidization of lipids in Mud Lake sediments below 100 cm was provided by the discovery of polysulfide-bound n-alkanes and C
机译:本文的研究重点是通过沉积脂质与溶解的孔隙水硫化物的化学反应在新近的沉积物中形成有机硫化物。这种称为自然硫化的化学反应将单个有机化合物转化为高分子量,富含硫化物的沉积有机材料和离散的有机硫化物,它们被认为比原始有机化合物对早期成岩作用的降解条件更具抵抗力。该过程被广泛接受为重要的成岩途径,可增强沉积物在埋藏过程中有机物的保存。这些研究的重点是对圣塔芭芭拉盆地和秘鲁边缘上升流地区以及含硫酸盐的湖泊环境(佛罗里达州泥湖)这两种海洋环境中的沉积物进行分析。比较这些沉积物中硫化化合物和具有相同碳骨架的未反应化合物的浓度和稳定的碳同位素组成,以确定脂质硫化的反应途径。此外,实验室进行了硫化研究,研究了结构上类似于近期沉积物中发现的官能团的模型化合物与四硫化钠和H的水溶液的反应;尽管每种环境中有机碳含量高且反应物浓度高秘鲁边缘或圣巴巴拉盆地沉积物或泥湖最上层的沉积物中脂质成分,有机硫化物的形成并不广泛。例如,Mud Lake的上部100 cm含有高浓度的正烯,在模型化合物的研究中,在含水条件下它们具有反应性,但未发现其硫化的证据。直接证明了多硫化物的作用。多硫化物结合的正构烷烃和碳的发现为100 cm以下泥浆湖沉积物中脂质的硫化提供了新的途径

著录项

  • 作者

    Filley, Timothy Raymond.;

  • 作者单位

    The Pennsylvania State University.;

  • 授予单位 The Pennsylvania State University.;
  • 学科 Geochemistry.;Biogeochemistry.
  • 学位 Ph.D.
  • 年度 1997
  • 页码 363 p.
  • 总页数 363
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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