2000
DOI: 10.1016/s0098-3004(00)00014-5
|View full text |Cite
|
Sign up to set email alerts
|

A spreadsheet program to optimize kinetic parameters of organic matter from laboratory pyrolysis data

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

0
4
0

Year Published

2004
2004
2020
2020

Publication Types

Select...
4

Relationship

0
4

Authors

Journals

citations
Cited by 4 publications
(4 citation statements)
references
References 6 publications
0
4
0
Order By: Relevance
“…The cumulative value of carbon isotopes at time t , δ 13 C cum ( t ), is the ratio of methane precursor conversion. There are the following formulas: The instantaneous value of the carbon isotope δ 13 C inst ( t ) is the ratio of the reaction rate at time t . Here The formula of the carbon isotope accumulated from time t – 1 to time t δ 13 C step ( t ) is as follows: where R std is the PDB standard ratio, δ 13 C 0 is the initial carbon isotope value, R o is the initial carbon isotope ratio of the methane precursor, F *­( t ) and F ( t ) are the conversion rates of heavy carbon methane and light carbon methane at time t , respectively, r *­( t ) and r ( t ) are the reaction rates of heavy carbon methane and light carbon methane at time t , respectively, and F *­( t – 1) and F ( t – 1) are the conversion rates of heavy carbon methane and light carbon methane at time t – 1, respectively.…”
Section: Experiments and Methodsmentioning
confidence: 99%
See 2 more Smart Citations
“…The cumulative value of carbon isotopes at time t , δ 13 C cum ( t ), is the ratio of methane precursor conversion. There are the following formulas: The instantaneous value of the carbon isotope δ 13 C inst ( t ) is the ratio of the reaction rate at time t . Here The formula of the carbon isotope accumulated from time t – 1 to time t δ 13 C step ( t ) is as follows: where R std is the PDB standard ratio, δ 13 C 0 is the initial carbon isotope value, R o is the initial carbon isotope ratio of the methane precursor, F *­( t ) and F ( t ) are the conversion rates of heavy carbon methane and light carbon methane at time t , respectively, r *­( t ) and r ( t ) are the reaction rates of heavy carbon methane and light carbon methane at time t , respectively, and F *­( t – 1) and F ( t – 1) are the conversion rates of heavy carbon methane and light carbon methane at time t – 1, respectively.…”
Section: Experiments and Methodsmentioning
confidence: 99%
“…Carbon isotope kinetics based on hydrocarbon generation kinetics can solve the scientific problems of carbon isotope evolution and fractionation regularity under certain geological conditions. Moreover, the kinetic process of natural gas generation and migration is objectively evaluated; the natural accumulation process is clarified; and the favorable blocks for gas accumulation are pointed out. Therefore, the study of the carbon isotope kinetics is of great significance for solving the problem of natural gas accumulation. In recent years, the carbon isotope kinetics of natural gas has become an important research focus in the field of petroleum geochemistry and has important application potential for explaining the process of natural gas accumulation. …”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…A Lotus 1-2-3 program was proposed for pyrolysis kinetics of sedimentary organic matter [13] by assuming the total reaction consisting of parallel degradation of several hypothetical components following the Arrhenius equation and first-order kinetics, each with a different E but the same A value. Later, the model was modified for different oil shale samples [14] where on the basis of TGA data, 11 values of E j were given in advance, and 11 values of A j and of total fractional conversions, x j , were unknown parameters.…”
Section: Non-isothermal Retortingmentioning
confidence: 99%