The Rock-Eval Method : Principles and Application için kapak resmi
Başlık:
The Rock-Eval Method : Principles and Application
Yazar:
Baudin, François, 1964- editor, contributor.
ISBN:
9781394256235

9781394256211
Basım Bilgisi:
First edition.
Fiziksel Tanımlama:
1 online resource.
Seri:
Geoscience: the surface of the lithosphere and the biosphere
İçerik:
Cover -- Title Page -- Copyright Page -- Contents -- Presentation of Units, Symbols and Acronyms -- List of Formulae -- Chapter 1. Historical Perspectives -- 1.1. History of Rock-Eval® -- 1.2. Geographical distribution of Rock-Eval® devices worldwide and areas of application of the method -- Chapter 2. Principles and Methods -- 2.1. Analysis process -- 2.2. Schematic diagram of the Rock-Eval® 6 analyzer -- 2.3. Detectors -- 2.3.1. Flame ionization detector (FID) -- 2.3.2. CO-CO2-SO2 detectors -- 2.4. Thermograms -- 2.4.1. Pyrolysis: S1 parameter -- 2.4.2. Pyrolysis: S2 parameter -- 2.4.3. Pyrolysis: Tpeak/Tmax -- 2.4.4. Specificities of the S2 parameter: pyrolysis in an open medium -- 2.4.5. Pyrolysis: S3 and S3CO parameters -- 2.4.6. Oxidation: S4 parameters -- 2.4.7. Oxidation: S5 parameter -- 2.5. Methods and cycles -- 2.6. Rock-Eval® 7 Sulfur -- 2.7. Pollut-Eval® -- 2.7.1. Instrumentation -- 2.7.2. Pollut-Eval® method or multi-heating rate -- 2.7.3. Calculations and parameters used by the Pollut-Eval® method -- 2.7.4. Positioning of integration cursors -- Chapter 3. Parameters and Illustration of Results -- 3.1. Introduction -- 3.2. Rock-Eval® signals and basic parameters -- 3.2.1. Dividing thermograms into Rock-Eval® "signals" -- 3.2.2. Use of signals to calculate the organic and inorganic carbon contents of a sample -- 3.2.3. Case of contamination by thermolabile carbonates -- 3.2.4. Parameters indicating the elemental composition of the sample: hydrogen and oxygen indices -- 3.3. Key parameters for oil exploration -- 3.3.1. Rock-Eval® Bulk Rock -- Basic cycle parameters for the characterization of source rocks -- 3.3.2. Rock-Eval® Shale Play™ parameters for the characterization of liquid-rich source rocks -- 3.4. Parameters developed for soil analysis -- 3.4.1. HC thermal stability parameters.

3.4.2. Fine-tuning and generalization of thermal stability parameters -- 3.4.3. What should we do with the wealth of parameters on the thermal stability of soil organic matter? -- 3.5. Development in progress on the mathematical processing of thermograms -- Chapter 4. Guidance on Sampling, Effects of Mineral Matrix and Other Artifacts on Thermograms -- 4.1. Sample collection, preparation and conservation -- 4.1.1. Recent lacustrine or marine sediments -- 4.1.2. Sedimentary rocks -- 4.1.3. Cores and drill cuttings -- 4.1.4. Specific cases of reservoir rocks and oils -- 4.1.5. Soils and polluted soils -- 4.1.6. Kerogens -- 4.2. Mineral matrix effects -- 4.2.1. Identification of mineral matrix effects on hydrocarbon compounds -- 4.2.2. Impact of matrix effects on Rock-Eval® parameters -- 4.2.3. Measurement of the activity of a mineral matrix and means of correcting its effect -- 4.2.4. Conclusions on the effects of mineral matrices -- 4.3. Other artifacts on thermograms related to the presence of minerals -- 4.4. Other artifacts and abnormal signals of instrumental origin -- Chapter 5. Comparison with Other Methods -- 5.1. The Rock-Eval® method at the crossroads of classical analytical methods -- 5.2. Elemental analysis -- 5.3. Chromatography -- 5.4. Thermal analysis -- 5.5. Comparison with other analyzers of the same type -- 5.6. Comparison with other types of samples -- Chapter 6. Characterization of Petroleum Source Rocks -- 6.1. Introduction -- 6.2. Characterization of conventional oil source rocks and isolated organic matter (kerogens) -- 6.3. Characterization of oil samples -- 6.4. Characterization of hydrocarbons from source rocks -- 6.5. Composition of hydrocarbons detected by Rock-Eval® pyrolysis -- 6.6. Estimation of hydrocarbon reserves in place -- 6.7. Estimation of free hydrocarbons in porous media.

Chapter 7. Determining the Parameters of Thermal Cracking of Fossil Organic Matter -- 7.1. Introduction -- 7.2. Basic equations for thermal cracking -- 7.3. Experimental determination of kinetic parameters of kerogen -- 7.4. Calculation of the overall kinetic parameters of kerogen in an open system -- 7.5. Acquisition and optimization of kinetic parameters E and A -- 7.6. How are the absolute values of E and A, obtained in the laboratory, used to calculate the values of TR under geological conditions? -- 7.6.1. Effect of compensation between E and A under laboratory conditions -- 7.6.2. Shape of the curve of the error function optimized to calculate the value of A -- 7.7. Summary -- Chapter 8. Characterization of Sulfur Compounds -- 8.1. Introduction -- 8.2. Experimental device -- 8.3. Characterization of sulfur in kerogens -- 8.3.1. Thermograms -- 8.3.2. Origin of the analyzed sulfur compounds -- 8.3.3. Calculation of "sulfur" parameters -- 8.4. Characterization of sulfur in oil source rocks -- 8.5. Kinetics of cracking of the organosulfur compounds of organic matter -- 8.6. Characterization of sulfur in oils -- 8.7. Characterization of sulfur in reservoir rocks -- 8.8. Prospects for the application of Rock-Eval® 7 Sulfur in understanding the sulfur sedimentary cycle -- 8.9. Prospects for the application of Rock-Eval® 7S in industry -- Chapter 9. Study of Organic Matter in Recent Sediments -- 9.1. Introduction -- 9.2. Reminder of the principles of analysis of recent sediments by the Rock-Eval® method -- 9.3. Analysis of fresh organic matter and pure compounds -- 9.4. Continental archives as witnesses of environmental changes -- 9.4.1. Suspended particulate matter and fluvial archives -- 9.4.2. Lacustrine archives, reservoirs -- 9.4.3. Peatlands -- 9.5. Coastal and marine environments -- 9.5.1. Mangroves -- 9.5.2. Epicontinental seas.

9.5.3. Deep turbidite systems -- 9.5.4. Upwellings -- 9.5.5. Sapropel deposits -- 9.5.6. Marine sediments of coral origin -- 9.6. Relationships between organic matter and contaminant concentrations -- Chapter 10. Characterization and Evaluation of the Stability of Soil Organic Matter -- 10.1. Introduction -- 10.2. Relevance and general teachings of Rock-Eval® analysis of soil samples -- 10.2.1. Analyzing soils with Rock-Eval®, a reasonable diversion -- 10.2.2. A marked evolution in Rock-Eval® parameters with soil depth -- 10.2.3. Rock-Eval® signal specificities of certain soil types, soil horizons and soil aggregates -- 10.3. Difficulties in linking the Rock-Eval® signature and chemical composition of soil organic matter -- 10.3.1. Contributions of Rock-Eval® analysis of pure compounds -- 10.3.2. Links between chemical composition of soil organic matter determined by various methods and Rock-Eval® signature -- 10.4. Evaluation of soil organic carbon stability by Rock-Eval® -- 10.4.1. What is the biogeochemical stability of soil organic carbon? -- 10.4.2. Links between Rock-Eval® results and biogeochemical stability of soil organic matter observed in the field -- 10.4.3. Links between Rock-Eval® results and the usual techniques for quantifying the biogeochemical stability of soil organic carbon -- 10.5. Quantifying soil organic carbon stability using Rock-Eval® with a view to improving soil carbon dynamics models -- 10.5.1. Soil organic carbon dynamics models -- 10.5.2. Construction of the stable carbon model at the century scale -- 10.5.3. Using the PARTYSOC machine learning model to estimate the size of the stable kinetic compartment of the AMG soil C dynamics model -- 10.6. Conclusion -- Chapter 11. Study of Natural and Anthropogenic Events -- 11.1. Introduction -- 11.2. Events of geological origin -- 11.2.1. Hydrothermal circulations.

11.2.2. Radiolysis and other U/organic matter relationships -- 11.2.3. Magmatic and metamorphic events -- 11.3. Fires and signature of incomplete combustion residues -- 11.4. Weathering versus syndiagenetic oxidation -- 11.5. Artificial oxidation -- Chapter 12. Detection and Monitoring of Oil Pollution in the Environment -- 12.1. Introduction -- 12.2. The Pollut-Eval® method -- 12.2.1. Principle and equipment -- 12.2.2. Quantification and characterization of pollutants -- 12.2.3. Characteristic pyrograms of reference hydrocarbon cuts -- 12.2.4. Two characteristic examples extracted from the reference database -- 12.2.5. Examples of characteristic ratios for the diagnosis of contaminated soils -- 12.3. Influence of the natural organic matrix of soils on the observed responses -- 12.3.1. Types of samples and natural soils analyzed -- 12.3.2. Correlation between the different pyrolysis and oxidation signals -- Chapter 13. Analysis of Carbonates -- 13.1. Reminder of the principles of mineral carbon analysis using the Rock-Eval® method -- 13.2. Kinetic effects -- 13.3. Artifacts -- 13.4. Discrimination and quantification of different carbonate mineral species using the Rock-Eval® method -- 13.5. Corrections in case of the presence of siderite -- 13.6. From Rock-Eval® MinC to carbonate percentage -- 13.7. TOC and MinC relationships in sediments and sedimentary rocks -- 13.8. Concluding remarks -- Chapter 14. What's Next for Rock-Eval®? -- References -- List of Authors -- Index -- EULA.
Özet:
This book presents the Rock-Eval ® method, which was invented in France in the 1970s and is used by the oil industry worldwide to characterize source rocks and reservoir rocks as well as their petroleum potential. Rock Eval ® has also spread to other fields of application, including soil science, paleoceanography, paleoclimatology, environmental science (i.e. monitoring pollution remediation), material chemistry (i.e. carbonates, microplastics) and many others. The Rock-Eval Method presents a collection of chapters reviewing this method and its fields of application, and examines its possible developments. The authors are from either the academic or applied sector and have all contributed to the development of the Rock Eval ® apparatus and method. This instrument, which lies somewhere between a chromatographic, a thermal and an elemental analyzer, is now evolving to be an analytical platform, on which new fields of applications can be tested in the future.
Notlar:
John Wiley and Sons
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