Isotope-ratio detection for gas chromatography

被引:214
作者
Sessions, Alex L. [1 ]
机构
[1] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
关键词
combustion interface; compound-specific isotope analysis; GC-isotope-ratio mass spectrometry; isotope-ratio-monitoring; pyrolysis interface;
D O I
10.1002/jssc.200600002
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Instrumentation and methods exist for highly precise analyses of the stable-isotopic composition of organic compounds separated by GC. The general approach combines a conventional GC, a chemical reaction interface, and a specialized isotoperatio mass spectrometer (IRMS). Most existing GC hardware and methods are amenable to isotope-ratio detection. The interface continuously and quantitatively converts all organic matter, including column bleed, to a common molecular form for isotopic measurement. C and N are analyzed as CO2 and N-2, respectively, derived from combustion of analytes. H and O are analyzed as H-2 and CO produced by pyrolysis/reduction. IRMS instruments are optimized to provide intense, highly stable ion beams, with extremely high precision realized via a system of differential measurements in which ion currents for all major isotopologs are simultaneously monitored. Calibration to an internationally recognized scale is achieved through comparison of closely spaced sample and standard peaks. Such systems are capable of measuring C-13/C-12 ratios with a precision approaching 0.1 parts per thousand (for values reported in the standard delta notation), four orders of magnitude better than that typically achieved by conventional "organic" mass spectrometers. Detection limits to achieve this level of precision are typically < 1 nmol C (roughly 10 ng of a typical hydrocarbon) injected on-column. Achievable precision and detection limits are correspondingly higher for N, O, and H, in that order.
引用
收藏
页码:1946 / 1961
页数:16
相关论文
共 98 条
[91]   Hydrogen isotope fractionation during H2/CO2 acetogenesis: hydrogen utilization efficiency and the origin of lipid-bound hydrogen [J].
Valentine, D. L. ;
Sessions, A. L. ;
Tyler, S. C. ;
Chidthaisong, A. .
GEOBIOLOGY, 2004, 2 (03) :179-188
[92]   GC/multiple collector-ICPMS method for chlorine stable isotope analysis of chlorinated aliphatic hydrocarbons [J].
Van Acker, Marc R. M. D. ;
Shahar, Anat ;
Young, Edward D. ;
Coleman, Max L. .
ANALYTICAL CHEMISTRY, 2006, 78 (13) :4663-4667
[93]   Hydrogen isotope fractionation of low molecular weight n-alkanes during progressive vaporization [J].
Wang, Y ;
Huang, YS .
ORGANIC GEOCHEMISTRY, 2001, 32 (08) :991-998
[94]   Referencing strategies and techniques in stable isotope ratio analysis [J].
Werner, RA ;
Brand, WA .
RAPID COMMUNICATIONS IN MASS SPECTROMETRY, 2001, 15 (07) :501-519
[95]   The online 18O/16O analysis:: Development and application [J].
Werner, RA .
ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES, 2003, 39 (02) :85-104
[96]   Carbon position-specific isotope analysis of alanine and phenylalanine analogues exhibiting nonideal pyrolytic fragmentation [J].
Wolyniak, CJ ;
Sacks, GL ;
Pan, BS ;
Brenna, JT .
ANALYTICAL CHEMISTRY, 2005, 77 (06) :1746-1752
[97]   On-line measurement of intramolecular carbon isotope distribution of acetic acid by continuous-flow isotope ratio mass spectrometry [J].
Yamada, K ;
Tanaka, M ;
Nakagawa, F ;
Yoshida, N .
RAPID COMMUNICATIONS IN MASS SPECTROMETRY, 2002, 16 (11) :1059-1064
[98]   Compound-specific carbon isotope analysis of volatile organic compounds in the low-microgram per liter range [J].
Zwank, L ;
Berg, M ;
Schmidt, TC ;
Haderlein, SB .
ANALYTICAL CHEMISTRY, 2003, 75 (20) :5575-5583