Page 172 - Advances in Forensic Applications of Mass Spectrometry - Jehuda Yinon
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1522_C04.fm  Page 155  Thursday, November 13, 2003  9:54 AM









                                Since the small variations of the heavier isotope habitually measured by
                             IRMS are of the order of –0.07 to +0.02 APE, the d-notation in units of per
                             mil (‰) has been adopted to report changes in isotopic abundance as a per
                             mil deviation compared to a designated isotopic standard:

                                               d  = ([R  – R ]/R ) ¥ 1000 [‰]                (3)
                                                s     s    std  std
                             where R  is the measured isotope ratio for the sample and R is the measured
                                    s                                           std
                             isotope ratio for the standard. To give a convenient rule-of-thumb approxi-
                                                     13
                             mation, in the d-notation, a  C abundance in the range of –0.033 to +0.0549
                                                 13
                             APE corresponds to a d C value range of –30‰ to +50‰. A change of +1‰
                             is approximately equivalent to a change of 0.001 APE and 0.0003 APE for
                                    15
                             13 C and  N, respectively.
                                Natural abundance applications for the most part require the high-pre-
                             cision techniques introduced in the late 1940s; these techniques dominated
                             IRMS for four decades. They focused initially on the analysis of bulk materials
                             of high chemical complexity such as plant extracts or petroleum reduced to
                             simple gases by combustion to CO  or conversion to N  or H . Analysis of
                                                            2                  2    2
                             chemically pure materials was much more common for compounds that
                             occur in relatively pure form in nature, such as water, because off-line sample
                             preparation is a time-consuming affair fraught with the risk of contamination
                             and subtle isotopic fractionation.


                             4.2.2  Dual-Inlet Isotope Ratio/Mass Spectrometry (IRMS)
                             However, until the commercial availability of continuous-flow isotope ratio
                             mass spectrometer (CF-IRMS) systems enabling on-line isotope analysis of
                             organic compounds in the late 1980s, initial attempts to exploit the informa-
                             tion locked into stable isotope ratios at natural abundance level for forensic
                             purposes were confined to employing dual-inlet IRMS systems. Typically, off-
                             line preparation involves multiple steps on custom-designed vacuum lines
                             equipped with high-vacuum and sample-compression pumps, concentrators
                             using cryogenic or chemical traps, reactions in furnaces using catalysts or
                             true reagents, and microdistillation steps. Contamination and isotopic frac-
                             tionation are a constant threat at any step, and, in general, manual off-line
                                                                                           7
                             methods are slow and tedious, usually requiring large sample amounts.  The
                             quality of the results depends considerably on operator skill and dedication.
                                The dual-adjustable volume inlet system facilitates sample/standard
                             comparison under the most nearly identical of circumstances. It is necessary
                             for highest precision to compensate for (a) normal fluctuations in instru-
                             mental response and (b) ion source nonlinearity which produces isotope
                             ratios that depend on the source gas pressure. The latter phenomenon can


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