1990
DOI: 10.1016/0146-6380(90)90025-u
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A new method for the measurement of kinetic parameters of hydrocarbon generation from source rocks

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Cited by 36 publications
(16 citation statements)
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“…The real kinetic variations are at right angles to the iso-temperature lines, so the lines can be annotated with the revised values of the activation energies. These range from approximately 195 to 225 kJ/mol for the main oil generating reactions, and from 225 to 270 kJ/mol for oil cracking and gas generating reactions, which are in line with the results of Klomp and Wright (1990), whose step-wise pyrolysis experiments were specifically designed to extract accurate overall activation energies of the main petroleum-generating reactions.…”
Section: Approximate Correction Of Literature Kineticsmentioning
confidence: 94%
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“…The real kinetic variations are at right angles to the iso-temperature lines, so the lines can be annotated with the revised values of the activation energies. These range from approximately 195 to 225 kJ/mol for the main oil generating reactions, and from 225 to 270 kJ/mol for oil cracking and gas generating reactions, which are in line with the results of Klomp and Wright (1990), whose step-wise pyrolysis experiments were specifically designed to extract accurate overall activation energies of the main petroleum-generating reactions.…”
Section: Approximate Correction Of Literature Kineticsmentioning
confidence: 94%
“…The model is within approximately AE0.1% VR of the interpreted data for the oil-prone source rocks, and within approximately AE0.15% VR for the coaly source rock. The interpreted transformation ratios of the real source rocks are themselves subject to substantial errors, up to approximately AE0.1% VR (e.g., Klomp and Wright, 1990). Fig.…”
Section: Transformation Of Kerogen Versus Thermal Maturitymentioning
confidence: 99%
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“…Yet the thermal degradation process is still incompletely understood due to the complicated kerogen structure. At present, the reported chemical kinetic models describing hydrocarbon generation include: (1) overall reaction model (Allred, 1966); (2) Friedman type model which assumes the kinetic parameters will be changed with the process of reaction (Dieckmann, 2005;Dieckmann and Keym, 2006;Friedman, 1963;Klomp and Wright, 1990); (3) parallel reaction model (Burnham et al, 1988(Burnham et al, , 1995Lu, 1996;Quigley and Mackenzie, 1988;Tissot et al, 1987;Ungerer, 1990); (4) consecutive reaction model (Behar et al, 1992(Behar et al, , 2008 etc., and each model can be divided into several sub-models. For example, the parallel reaction model can be divided into an infinite parallel reactions model (Quigley and Mackenzie, 1988) and a finite parallel reactions model (Burnham et al, 1988(Burnham et al, , 1995Lu, 1996;Ungerer, 1990), which again can be divided into a model with a single frequency factor (A) and a distribution of activation energies (E) and the model with multiple frequency factors and a distribution of activation energies based on whether the frequency is identical or not.…”
Section: Introductionmentioning
confidence: 99%