Clay Seals of Oil and Gas Deposits

V. I. Osipov, V.N. Sokolov and V.V. Eremeev
- Published on Monday, 17 October 2011 20:05
In this work, the formation of clay deposits in sedimentary basins and the transformation of their mineral composition, microstructure and water content in the course of lithogenesis are treated in relation to the occurrence of oil and gas deposits.
Major topics discussed in this book comprise revealing of the main regularities in the variation of physical, mechanical, and seepage properties of clay in relation to its occurrence depth. In addition, a close relationship is demonstrated between clay deposit transformations and clay composition, thermodynamic conditions, pore space, structural bonds and geo-chemical composition of porous solutions. Facies conditions of clay seal development are also analysed and the relation between the cyclic structure of sedimentary massifs and sedimentary basin evolution is described. To this end, seven facies types of clay seals that differed with regard to composition, formation conditions, and screening properties have been distinguished by facies analysis of more than forty sedimentary oil-and-gas bearing basins within the former USSR territory. Also the correlation between clay properties and clay occurrence depth per seal type and the main factors controlling intensification and degradation of screening properties are described and it is shown that the maximum clay screening effect depth is an important indicator in the occurrence of oil and gas deposits. Information on modelling of the structure, properties and transformations of clay seals at various depths is included in the final part of the work. In this respect, also data like clay porosity graphs and strength variation at different lithogenesis stages are provided and the prediction of screening properties of clay seals with the help of software that was developed by the authors is treated.
This practical and informative book is intended for (post)graduate students, researchers and professionals in oil and gas geology, lithology, enineering geology and hydrogeology worldwide.
Contents
Introduction | VII | |
PART I | FORMATION OF CLAY SEAL PROPERTIES: THEORETICAL FUNDAMENTALS | 1 |
Chapter 1 | Composition of Clay Sediments and Their Structure Formation in Sedimentogenesis | 3 |
1.1. Composition of clay sediments | 3 | |
1.2. Structure of clay sediments | 7 | |
1.3. The theory of structure formation in clay dispersions | 17 | |
1.4. Structural bonds | 26 | |
1.5. Formation of primary microstructures in clay sediments | 30 | |
Chapter 2 | Lithogenesis of Clay Sediments | 37 |
2.1. General information | 37 | |
2.2. The stages of lithogenesis | 38 | |
2.3. Boundaries between the stages and substages of lithogenesis | 64 | |
Chapter 3 | Formation of the Properties of Clay Seals in Lithogenesis | 71 |
3.1. Density and porosity | 71 | |
3.2. Water content and consistence | 83 | |
3.3. Permeability | 90 | |
3.4. Physical-mechanical properties | 97 | |
3.5. Rheological properties | 109 | |
3.6. General regularities in the formation of clay properties in the process of lithogenesis | 112 | |
PART II | CHARACTERISTIC OF THE FACIES TYPES OF CLAY SEALS | 119 |
Chapter 4 | Depositional Environments of Clay Seal Formation | 121 |
4.1. The cyclic structure of sedimentary basin sequences | 121 | |
4.2. Source provinces r , | 123 | |
4.3. Evolution of sedimentation basins | 125 | |
4.4. Classification of clay seals according to their depositional environments and screening properties | 131 | |
Chapter 5 | Facies Analysis of Clay Seals in Oil-and Gas-Bearing Basins | 137 |
5.1. The principal criteria for facies analysis | 137 | |
5.2. Facies analysis of clay seals in sedimentary basins | 139 | |
VI CONTENTS | ||
Chapter 6 | The Composition of the Facies Types of Clay Seals and Its Change with Depth |
147 |
6.1. The composition of the facies types of clay seals | 147 | |
6.2. A comparative characteristic of the composition of clay seals of various facies types |
158 | |
Chapter 7 | Structure and Properties of the Facies Types of Clay Seals | 163 |
7.1. The influence of depositional environments on the structure formation |
163 | |
7.2. Porosity | 172 | |
7.3. Microfracturing | 181 | |
7.4. Permeability | 188 | |
7.5. Destruction of clay seals of different facies types | 190 | |
PART III | MODELING OF THE CHANGE IN THE CLAY SEAL PROPERTIES IN LITHOGENESIS | 195 |
Chapter 8 | Physicochemical Models of Clay Rock Microstructures | 197 |
8.1. The concepts of the physicochemical mechanics of clay rocks as a basis for modeling |
197 | |
8.2. Calculation of the number of contacts | 198 | |
8.3. Strength of individual contacts between clay particles | 204 | |
Chapter 9 | Development of a Mathematical Model for Estimating the Strength of Clay Seals | 211 |
9.1. Theoretical calculation of the change in the strength of individual contacts with depth | 211 | |
9.2. Calculation of the change in the number of contacts in clay seals with depth | 225 | |
9.3. Theoretical calculation of tensile and compressive strength of clay seals | 229 | |
Chapter 10 | Comparison of Theoretical Calculation Results and Experimental Data on the Mechanical Strength of Clay Seals | 239 |
10.1. Experimental data base | 239 | |
10.2. Comparison of theoretical and experimental data | 239 | |
References | 259 | |
Subject Index | 275 |