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This paper discusses the processes of migration and accumulation of petroleum, focusing on both primary and secondary migration mechanisms. Key factors influencing these processes include capillary action, bacterial action, differential specific gravity, and hydraulic movement. The paper highlights how different geological conditions affect the distance of oil migration and provides schematic diagrams to illustrate the concepts, contributing to a better understanding of petroleum reservoir dynamics.
Petroleum migration in highly permeable carrier beds and reservoir rocks is generally regarded as a buoyoncy-driven process called secondary migration. In contrast, the mechanisms which cause the expulsion of petroleum from source rocks are less well understood. Difficulties in understanding of this "primary migration" arise, because most source rocks are characterized by low permeabilities. Nevertheless oil molecules which are larger than pore throats are able to escape form these sedimentary rocks. Possible mechanisms were extensively discussed, e.g., by Durand (1988). As coals are known to be among the least permeable of all source rocks, the understanding of expulsion of oil and gas from coals is even more difficult than form clastic and carbonate source rocks. Primary migration in source rocks tbllows petroleum (= oil and gas) generation, which in turn is a function of rank and kerogen composition (Hunt, 1979; Tissot and Welte, 1984). Whether petroleum generation in coals is an economically important process was controversially discussed in the past (e.g.,
Journal of the Geological Society, 1987
This paper discusses the migration of petroleum from its formation in a source rock to its subsequent possible entrapment in a reservoir. The chemical and physical properties of petroleum gases and liquids are stressed, particularly their phase behaviour under subsurface conditions which is shown to be a very important factor in determining migration behaviour. Engineering correlations are presented for estimating the properties of petroleum fluids under geologically realistic conditions. The directions and magnitudes of the forces acting on migrating petroleum are deduced from the combined effects of buoyancy and water flow in compacting sediments. These forces are combined, using a fluid potential description. This procedure allows the direction of migration to be defined. The rate of migration is then estimated from the properties of the sediments involved, allowing a distinction to be made between 'lateral' and 'vertical' carrier beds. This simplified approach is suitable for rapid predictive calculations in petroleum exploration. It is compared with the more complex 3-D computer modelling approaches which are currently becoming available. Migration losses are related to the cumulative pore volume employed by the petroleum in establishing a migration pathway. The petroleum migration mechanism is shown to be predominantly by bulk flow, with a small diffusive contribution for light hydrocarbons over distances less than c. 100m. The loss factors involved in secondary migration are estimated from field evidence. The mechanism of reservoir filling is presented as a logical extension to those described for migration. This, together with the inefficiency of in-reservoir mixing by diffusion or convection, is shown to tend to cause significant lateral compositional gradients in reservoirs over and above the gravitationally induced vertical gradients described by other workers.
Paper Proceedings of the 4th Nigerian Association of Engineering Geology and the Environment (NAEGE) and Second African Regional Congress of the International Association of Engineering Geology and the Environment (IAEGE) , Abuja, Nigeria October, 27- 30, 2019 pp 48, Book of Abstract , 2019
Rock behavior in vertical and lateral successions, the effects of stress on the rock sequences which often cause compartmentalization and defining fluid communication within the basin is necessary for optimizing drilling , completion and production. Rock cores are seldom available for laboratory test hence dynamic method is used to derive the properties. The mechanical properties and local deformation in a depth interval of 1500m and 4500m have been determined using wireline logs. Results shows that the mechanical properties were influenced by rock mineralogy, porosity, depth of burial, pore pressure, effective stress, tectonics and temperature. Increase depth of burial and effective vertical stress favoured syndepositional compaction and paleotectonic stresses greater than yield strength of the rocks induced tensile fracturing and faulting culminating in kinematic translation an d creation of a depositional centre in the middle of the field. Rapid progradation of sandstones and shales sequences due to marine incursion created both stratigraphic and structural compartmentalization. This was accompanied by low rate of fluids diffusion and imposition of overburden load on the pore fluids, vertical transfer along the faults, grain sliding in shear; reduction in the rock compressibility and pore volume; and destruction of cement bonding causing compaction disequilibrium and generating excess pore pressure in the shales. Reorientation of the tectonic stresses led to elastic stretching of the ductile and high elasticity shales and microfracturing of the brittle sandstones forming growth faults and rollover anticlines that favoured hydrocarbon migration from the lower Akata source rock into the porous reservoirs and shale capping and smearing on the fault limbs providing the trapping mechanism.
Romanian Journal of Petroleum & Gas Technology, 2023
In the process of tertiary migration of crude oil, the phase that occurs after the cessation of primary exploitation of petroleum fluid deposits, the deposit is characterized by a state of maximum discontinuity of microscale phases and their abnormal gravitational positioning. This is precisely why it is necessary to discuss the blocking/unblocking mechanisms of wetting phase and non-wetting phase plugs in/out of capillary microtraps. The article presents for the first time a microfluidic behavior of crude oil through cores, with the analysis of polymer flow through rock pores and their filling with petroleum fluids.
Journal of Petroleum Geology, 2007
Estimates of hydrocarbon losses during migration are critical to petroleum resource assessments based on mass balance calculations. Using knowledge acquired from physical experiments, we conducted numerical experiments to qualitatively simulate migration processes on a basin scale, and we have estimated the proportions of oil lost along different parts of the migration pathway. Between the point where oil is expelled from a source rock and its arrival in a trap, migration pathways were divided into three sections, namely vertical and lateral pathways within the area of the effective source rock (W 1 ), and lateral pathways outside this area (W 2 ).
T'his report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United Statu Government nor any agency thereof. nor any of their employecs, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its UK would not infringe privately owned rights. Reference hmin to any specific commercial product, procss, or service by trade name, trademark, manufacturer, or otherwise dots not necessarily constitute or imply its endorsement. m r nmendation. or favoring by the United States Government or any agency thereof. The views and opinions of authors exprrssed herein do not necessarily state or reflect thosc of the United States Government or any agency thereof.
1993
T'his report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United Statu Government nor any agency thereof. nor any of their employecs, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its UK would not infringe privately owned rights. Reference hmin to any specific commercial product, procss, or service by trade name, trademark, manufacturer, or otherwise dots not necessarily constitute or imply its endorsement. m r nmendation. or favoring by the United States Government or any agency thereof. The views and opinions of authors exprrssed herein do not necessarily state or reflect thosc of the United States Government or any agency thereof.
The APPEA journal, 2018
The reliable mathematical modelling of secondary petroleum migration that incorporates structural geology and mature source rocks in the basin model, allows for prediction of the reservoir location, yielding the significant enhancement of the probability of exploration success. We investigate secondary petroleum migration with a significant composition difference between the source and oil pools. In our case study, the secondary migration period is significantly shorter than the time of the hydrocarbon pulse generation. Therefore, neither adsorption nor dispersion of components can explain the concentration difference between the source rock and the reservoir. For the first time, the present paper proposes deep bed filtration of hydrocarbons with component kinetics retention by the rock as a physics mechanism explaining compositional grading. Introduction of the component capture rate into mass balance transport equation facilitates matching the concentration difference for heavy hydrocarbons, and the tuned filtration coefficients vary in their common range. The obtained values of filtration coefficients monotonically increase with molecular weight and consequently affects the size of the oleic component, as predicted by the analytical model of deep bed filtration. The modelling shows a negligible effect of component dispersion on the compositional grading.
AAPG Bulletin, 1992
He received B.S. and M.S. degrees in petroleum engineering and development from the China University of Petroleum and his Ph.D. in petroleum geology from the Institute of Geology and Geophysics, Chinese Academy of Science. His interests now include theoretical and experimental analyses of secondary hydrocarbon migration, enhancement of oil recovery, and the use of nuclear magnetic resonance in the petroleum industry.
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