1999
DOI: 10.1016/s0016-7037(99)00205-7
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Chemical forms of sulfur in geological and archeological asphaltenes from Middle East, France, and Spain determined by sulfur K- and L-edge X-ray absorption near-edge structure spectroscopy

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Cited by 119 publications
(102 citation statements)
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“…Table 1. Energy position of the sulphur K-edge white line for different sulphur compounds from literature data: coal [14], petroleum and asphaltenes [15], minerals [16], soils [19][20][21], residual oil fly ash [22,23]. After qualitative analysis, the relative proportions of the sulphur forms were estimated by means of a least-squares fitting procedure using Gaussian curves for the different sulphur forms peaks and an arctangent curve for the edge step at 2481 eV (oxidized S) [20].…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…Table 1. Energy position of the sulphur K-edge white line for different sulphur compounds from literature data: coal [14], petroleum and asphaltenes [15], minerals [16], soils [19][20][21], residual oil fly ash [22,23]. After qualitative analysis, the relative proportions of the sulphur forms were estimated by means of a least-squares fitting procedure using Gaussian curves for the different sulphur forms peaks and an arctangent curve for the edge step at 2481 eV (oxidized S) [20].…”
Section: Resultsmentioning
confidence: 99%
“…An alternative approach can be provided by X-ray absorption near edge spectroscopy (XANES), that has already been used to distinguish and measure species of S in several matrices such as coal [14], petroleum and asphaltenes [15], minerals [16], biological samples [17][18][19], soils [13,20,21], as well as in matrices similar to PM 10 like residual oil fly ash particulate matter [22,23].…”
Section: Introductionmentioning
confidence: 99%
“…Principal component analysis (17) of the spectra indicates at least six significant sulfur components, with mostly four types of reduced species contributing to the major peak at 2,473 eV (1 eV ϭ 1.602 ϫ 10 Ϫ19 J). Curve fitting with XANES spectra of standard compounds (15)(16)(17)(18) quantitatively reveals thiols (R-SH), disulfides (R-SS-RЈ with a characteristic doublepeak), and elemental sulfur (S 8 ) in all samples and in core 2 also pyrite (FeS 2 ) in sharply varying amount (Fig. 4 and Table 1).…”
Section: Sulfur and Iron Analysesmentioning
confidence: 96%
“…Differential reduction of organic S compounds to H 2 S does not identify the organic functional groups or the intermediate oxidation states of S. The pyrolysis -gas chromatography -mass spectrometry approach is used for coal, kerogens and aquatic humic substances, but is limited to speciation of thermally stable forms of S. Within this context, S K-and L-edge XANES spectroscopy are proving to be invaluable, non-destructive, and in some cases in situ, techniques for characterizing the S functional groups in natural organic matter. The method has been applied to coals (e.g., Hussain et al 1982, Spiro et al 1984, Huffman et al 1991, George et al 1991, Brown et al 1992, Kasrai et al 1990, 1996b, Olivella et al 2002, Huggins et al 1997, heavy petroleum asphalts (bitumens) and asphaltenes (George & Gorbaty 1989, Gorbaty et al 1991, Waldo et al 1991, Kasrai et al 1994, Vairavamurthy et al 1994, Sarret et al 1999, kerogens , Sarret et al 2002 and sediments, soils and humus (Vairavamurthy et al 1994, 1997, Morra et al 1997, Olivella et al 2002, Qian et al 2002, Beauchemin et al 2002, Solomon et al 2003, Jokic et al 2003. FIG.…”
Section: Organic Geochemistrymentioning
confidence: 99%