Soil Organic Matter Characterization Using S3 and S4 Signals from Rock-Eval Pyrolysis
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Cited by (14)
Linking Rock-Eval parameters to soil heterotrophic respiration and microbial residues in a black soil
2023, Soil Biology and BiochemistryHistorical and post-ban releases of organochlorine pesticides recorded in sediment deposits in an agricultural watershed, France
2021, Environmental PollutionCitation Excerpt :The recorded RC/TOC ratio was constant (0.70 ± 0.02) and greater than the PC/TOC ratio, showing that the TOC was mainly composed by refractory Corg (Fig. 5). Thus, the temporal trends of β-HCH and aldrin are related to the inputs of refractory Corg which is the most stable fraction of OM (Sanei et al., 2005; Hetényi and Nyilas, 2014). As the proportion of labile Corg, the proportion of refractory Corg remained constant along the Eure Unit.
Thermal degradation features of soil humic acid sub-fractions in pyrolytic treatment and their relation to molecular signatures
2020, Science of the Total EnvironmentOn-line recovery system coupled to a Rock-Eval® device: An analytical methodology for characterization of liquid and solid samples
2020, Organic GeochemistryCitation Excerpt :The described recovery system can be used to characterize a wide range of geological solid and liquid samples, including source and reservoir rocks containing natural petroleum or contaminated with drilling additives and various petroleum products. Although the Rock-Eval® device was primarily developed to investigate sedimentary rocks and kerogens from the perspectives of the petroleum industry, this analytical technique has been used increasingly in other geo-applications including: (1) the characterization of organic matter in soils (e.g., Di-Giovanni et al., 2000; Disnar et al., 2003; Hetényi et al., 2005; Sebag et al., 2006; Graz et al., 2012; Saenger et al., 2013; Hétényi and Nyilas, 2014); (2) the study of recent lacustrine sediments (e.g., Campy et al., 1994; Di-Giovanni et al., 1998; Meyers and Lallier-Vergès, 1999; Ariztegui et al., 2001; Steinmann et al., 2003; Jacob et al., 2004; Sanei et al., 2005; Boussafir et al., 2012; Zocatelli et al., 2012; Lavrieux et al., 2013; Sebag et al., 2013); and (3) the evaluation of recent marine sediments (e.g., Peters and Simoneit, 1982; Hussain and Warren, 1991; Calvert et al., 1992; Combourieu-Nebout et al., 1999; Ganeshram et al., 1999; Ozcelik and Altunsoy, 2000; Holtvoeth et al., 2001, 2003, 2005; Tamburini et al., 2003; Baudin et al., 2007, 2010; Kim et al., 2007; Marchand et al., 2008; Tribovillard et al., 2008, 2009; Biscara et al., 2011; Riboulleau et al., 2011; Hare et al., 2014; Hatcher et al., 2014). Additional testing is needed to determine the applicability of the coupled Rock-Eval® – vacuum and on-line recovery system to these types of samples, as well as for material studies in other disciplines.
Calculation of the original abundance of organic matter at high-over maturity: A case study of the Lower Cambrian Niutitang shale in the Micangshan-Hannan Uplift, SW China
2019, Journal of Petroleum Science and EngineeringSpecifications for carbonate content quantification in recent marine sediments using Rock-Eval pyrolysis
2019, Journal of Analytical and Applied PyrolysisCitation Excerpt :Rock-Eval analyses are also widely used in the petroleum industry because they make it possible to obtain the percentage of organic matter in a rock and many other parameters that are useful for the characterization of oil potential. The Rock-Eval method was primarily developed by the Institut Français du Pétrole for compacted (fossil) sediments [3,4] but is now being increasingly used for the characterization of recent lacustrine and marine sediments [5–20] as well as soils [21–27]. In 2014, a qualitative and quantitative carbonate recognition method based on the results of Rock-Eval pyrolysis was proposed [1].
Supported by the Hungarian Scientific Research Fund (No. OTKA K-81181).