Identification of alkenylbenzenes in pyrolyzates using GC-MS and GC-FTIR techniques: evidence for kerogen aromatic moieties with various binding sites

被引:21
作者
Ellis, L
Fisher, SJ
Singh, RK
Alexander, R
Kagi, RI
机构
[1] Curtin Univ Technol, Ctr Petr & Environm Organ Geochem, Australian Petr CRC, Perth, WA 6001, Australia
[2] Baseline Resolut Inc, Plano, TX 75074 USA
关键词
alkenylbenzene; alkylbenzene; kerogen aromatic moieties; GC-FTIR; pyrolysis-GC-MS; pyrolysis-GC-FTIR;
D O I
10.1016/S0146-6380(99)00013-3
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Pyrolysis products obtained from heating a shale under vacuum have been analyzed for alkenylbenzenes using GC-MS and GC-FTIR, The shale pyrolysate contains a homologous series (C-11-C-23) Of alkenylbenzenes with terminal unsaturations concomitant with lesser amounts of hitherto unknown trans alk-1-enylbenzenes. These latter compounds are unique constituents of kerogen pyrolyzates and are suggested to be derived from alkylbenzene moieties bound to kerogen at the benzylic position. The presence of these unsaturated compounds in pyrolyzates has been interpreted as evidence for site-specific binding of alkylbenzene moieties in kerogen. Formation of alkenylbenzene moieties is suggested to result from diagenetic cyclization/aromatization reactions of fatty acid precursors. Incorporation of structurally different lipid precursors such as saturated, mono- and polyunsaturated fatty acids is suggested to reflect the nature of the different alkenylbenzene products generated upon pyrolysis. The application of 'compound specific' GC-FTIR techniques, provides a new and complementary tool to the study of geochemical samples. Compound specific IR spectra in conjunction with electron impact mass spectra are shown to facilitate the structural identification of hydrocarbons in geochemical samples. (C) 1999 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:651 / 665
页数:15
相关论文
共 43 条
[1]   GEOSYNTHESIS OF ORGANIC-COMPOUNDS .2. METHYLATION OF PHENANTHRENE AND ALKYLPHENANTHRENES [J].
ALEXANDER, R ;
BASTOW, TP ;
FISHER, SJ ;
KAGI, RI .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1995, 59 (20) :4259-4266
[2]  
Allan J., 1980, ADV ORG GEOCHEM, V12, P599, DOI 10.1016/0079-1946(79)90142-3
[3]  
Baset ZH, 1980, ADV ORGANIC GEOCHEMI, P619
[4]   THERMOLYSIS OF SURFACE-ATTACHED 1,4-DIPHENYLBUTANE - THE ROLE OF HYDROGEN-TRANSFER REACTIONS ON THE SURFACE IN DETERMINING THE PRODUCT DISTRIBUTION [J].
BRITT, PF ;
BUCHANAN, AC .
JOURNAL OF ORGANIC CHEMISTRY, 1991, 56 (21) :6132-6140
[5]   STRUCTURAL TRANSFORMATIONS OF POLYLABDANOID RESINITES DURING MATURATION [J].
CLIFFORD, DJ ;
HATCHER, PG .
ORGANIC GEOCHEMISTRY, 1995, 23 (05) :407-418
[6]   THE MICROBIAL INPUT IN CARBONATE-ANHYDRITE FACIES OF A SABKHA PALEOENVIRONMENT FROM GUATEMALA - A MOLECULAR APPROACH [J].
CONNAN, J ;
BOUROULLEC, J ;
DESSORT, D ;
ALBRECHT, P .
ORGANIC GEOCHEMISTRY, 1986, 10 (1-3) :29-50
[7]  
COREY EJ, 1979, TETRAHEDRON LETT, V20, P399
[8]  
DAMSTE JSS, 1991, GEOCHIM COSMOCHIM AC, V55, P3677
[9]  
DELONG EF, 1986, APPL ENVIRON MICROB, V51, P730, DOI 10.1128/AEM.51.4.730-737.1986
[10]   CHARACTERIZATION OF ESTONIAN KUKERSITE BY SPECTROSCOPY AND PYROLYSIS - EVIDENCE FOR ABUNDANT ALKYL PHENOLIC MOIETIES IN AN ORDOVICIAN, MARINE, TYPE-II/I-KEROGEN [J].
DERENNE, S ;
LARGEAU, C ;
CASADEVALL, E ;
DAMSTE, JSS ;
TEGELAAR, EW ;
DELEEUW, JW .
ORGANIC GEOCHEMISTRY, 1990, 16 (4-6) :873-888