基于原子力显微镜(AFM)的纳米级各向异性焦沥青的成熟度表征和形成机理

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Zhaoxi Zuo , Jian Cao , Wenxuan Hu , Ruijie Zhang , Xiaolin Wang , Suping Yao , Bing Luo , Jingkun Zhang
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引用次数: 0

摘要

高度演化的热沥青是表征古代和深埋有机物成熟度的一个重要而现实的对象,但由于其强烈的光学各向异性和纳米级的浮雕,对其反射率的测量具有挑战性。在此,我们对中国四川盆地的新元古代(埃迪卡拉纪)登瀛地层进行了案例研究。通过原子力显微镜(AFM)、激光拉曼光谱(LRM)和反射率研究,对储层火成岩进行了高分辨率、三维形态成像。研究结果表明,杨氏模量和附着力作为力学成熟度参数,可有效表征成熟度。由于焦沥青是由石油裂解形成的,比矾土更富含氢,因此焦沥青杨氏模量的增长滞后于矾土。杨氏模量、附着力与火成沥青亮区和暗区的反射率之间建立了定量关系,可用于成熟度表征。高温沥青杨氏模量的变化与有机物的凝结和微晶的定向排列有关。在有机质成熟度较高(Ro > 2.0 %)时,有机质的杨氏模量是一个可靠的机械成熟度指标,但必须注意各向异性的影响。与杨氏模量相比,粘附力受各向异性的影响较小。除了传统的光学和光谱方法外,杨氏模量和附着力等纳米力学性能将成为新的成熟度指标。有机物的纳米力学性能有望在进一步的研究中应用于有机岩石学领域的成熟度指标和宏观矿物分类。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Maturity characterization and formation mechanisms of nano-scale anisotropic pyrobitumen based on atomic force microscopy (AFM)
Highly evolved pyrobitumen is an important and realistic object for maturity characterization of ancient and deeply buried organic matter, but measurement of its reflectance is challenging due to its strong optical anisotropy and nano-scale relief. Here we conducted a case study in the Sinian (Ediacaran) Dengying Formation of the Sichuan Basin, China. High-resolution, three-dimensional, morphological imaging by atomic force microscopy (AFM), laser Raman (LRM) spectroscopy, and reflectance studies were conducted on the reservoir pyrobitumen. Our results show that Young’s modulus and adhesion, which are mechanical maturity parameter, provides effective characterization of maturity. The increase in Young’s modulus of pyrobitumen lags that of the vitrinite, given that pyrobitumen is formed by oil cracking and is more hydrogen-rich than vitrinite. A quantitative relationship between Young’s modulus, adhesion and reflectance in bright and dark areas of pyrobitumen was established, which can be used for maturity characterization. The changes in Young’s modulus of the pyrobitumen is related to the condensation of organic matter and directional arrangement of microcrystals. Young’s modulus of organic matter is a robust mechanical maturity index at high organic matter maturity (Ro > 2.0 %), but it is important to pay attention to the influence of anisotropy. Compared to Young’s modulus, adhesion is less affected by anisotropy. The nano-mechanics such as Young’s modulus and adhesion will be new maturity indicator in addition to conventional optical and spectroscopic method. The nano-mechanical properties of organic matter are expected to be applied to maturity indicators and macerals classification in the field of organic petrology in the further research.
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来源期刊
Organic Geochemistry
Organic Geochemistry 地学-地球化学与地球物理
CiteScore
5.50
自引率
6.70%
发文量
100
审稿时长
61 days
期刊介绍: Organic Geochemistry serves as the only dedicated medium for the publication of peer-reviewed research on all phases of geochemistry in which organic compounds play a major role. The Editors welcome contributions covering a wide spectrum of subjects in the geosciences broadly based on organic chemistry (including molecular and isotopic geochemistry), and involving geology, biogeochemistry, environmental geochemistry, chemical oceanography and hydrology. The scope of the journal includes research involving petroleum (including natural gas), coal, organic matter in the aqueous environment and recent sediments, organic-rich rocks and soils and the role of organics in the geochemical cycling of the elements. Sedimentological, paleontological and organic petrographic studies will also be considered for publication, provided that they are geochemically oriented. Papers cover the full range of research activities in organic geochemistry, and include comprehensive review articles, technical communications, discussion/reply correspondence and short technical notes. Peer-reviews organised through three Chief Editors and a staff of Associate Editors, are conducted by well known, respected scientists from academia, government and industry. The journal also publishes reviews of books, announcements of important conferences and meetings and other matters of direct interest to the organic geochemical community.
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