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Издание:Elsevier, 2020 г., 515 стр., ISBN: 978-0-12-819150-7
Язык(и)Английский
Petroleum Reservoir Simulation. The Engineering Approach / Моделирование нефтяных резервуаров. Инженерный подход

In this book the basics of reservoir simulation are presented through the modeling of single-phase fluid flow and multiphase flow in petroleum reservoirs using the engineering approach. This text is written for senior-level BSc students and first-yearMSc students studying petroleum engineering. The aim of this book is to restore engineering and physics sense to the subject. In this way the misleading impact of excess mathematical glitter, which has dominated reservoir simulation books in the past, is challenged. The engineering approach, used in this book, uses mathematics extensively, but it injects engineering meaning to differential equations and to boundary conditions used in reservoir simulation. It does not need to deal with differential equations as a means for modeling, and it interprets boundary conditions as fictitious wells that transfer fluids across reservoir boundaries. The contents of the book can be taught in two consecutive courses. The first undergraduate senior-level course includes the use of block-centered grid in rectangular coordinates in single-phase flow simulation. Thematerial ismainly included in Chapters 2, 3, 4, 6, 7, and 9. The second graduate-level course deals with block-centered grid in radial-cylindrical coordinates, point-distributed grid in both rectangular and radial-cylindrical coordinates, and the simulation of multiphase flow in petroleum reservoirs. The material is covered in Chapters 5, 8, 10, and 11 in addition to specific sections in Chapters 2, 4, 5, 6, and 7 (Sections 2.7, 4.5, 5.5, 6.2.2, 7.3.2, and 7.3.3).

Автор(ы):Ezekwe N.
Издание:Pearson Prentice Hall, 2011 г., 800 стр., ISBN: 0-13-715283-3
Язык(и)Английский
Petroleum reservoir. Engineering, practice / Углеводородные резервуары. Строение, практика

Porosity is defined as a measure of the capacity of reservoir rocks to contain or store fluids. The fluids stored in the pore spaces within the reservoir rocks could be gas, oil, and water. High porosity values indicate high capacities of the reservoir rocks to contain these fluids, while low porosity values indicate the opposite. Consequently, porosity data are routinely used qualitatively and quantitatively to assess and estimate the potential volume of hydrocarbons contained in a reservoir.

Издание 2
Автор(ы):Aadnoy B.S., Looyeh R.
Издание:Elsevier, 2019 г., 437 стр., ISBN: 978-0-12-815903-3
Язык(и)Английский
Petroleum rock mechanics drilling operations and well design / Механика буровых работ по нефтесодержащим породам и проектирование скважин

Engineering systems must be designed to withstand the actual and probable loads that may be imposed on them. Hence the wall of a dam must be of adequate strength to hold out mainly the reservoir water pressure but also to withstand other loads, such as seismic occasional shocks, thermal expansions/contractions, and many others. A tennis racket is designed to take dynamic and impact loads imposed by a fast-moving flying tennis ball. It must also be adequately designed to withstand impact loads when incidentally hitting a hard ground. An oil drilling equipment must be designed to suitably and adequately drill through different types of rock materials, but at the same time ensuring that its imposing loads would not cause rock formation integrity affecting the stability of the drilled well. <...>

Редактор(ы):AbuAli M.A., Bolas H.M.N., Moretti I.
Издание:American Association of Petroleum Geologists, 2017 г., 319 стр., ISBN: 978-0-89181-394-1
Язык(и)Английский
Petroleum systems analysis. Case studies / Анализ углеводородных систем. Учебные примеры

Petroleum systems analysis has come a long way from pure geochemical evaluation to integration of all petroleum elements, including source rock characteristics, hydrocarbon generation, expulsion and migration, traps, seals, and alterations of the hydrocarbon fluids and columns. Quantification of many of these processes is attempted by the use of more complex 3-D basin models.

Редактор(ы):Bartolini C., Ramos J.R.R.
Издание:American Association of Petroleum Geologists, 2009 г., 532 стр., ISBN: 978-0-89181-371-2
Язык(и)Английский
Petroleum systems in the Southern Gulf of Mexico / Нефтяные системы в южной части Мексиканского залива

The petroleum geology of Mexico remains relatively unknown to the international geoscience community because of the limited number of articles published in international forums by geoscientists from Petroleos Mexicanos (PEMEX) and the Mexican Petroleum Institute. Sensitive Pemex data have traditionally been treated with strict confidentiality.

Автор(ы):Slatt R.M., Weimer P.
Издание:Society of exploration geophysicists, 2004 г., 487 стр., ISBN: 1-56080-086-0
Язык(и)Английский
Petroleum systems of deepwater settings / Нефтяные системы глубоководных установок

This course provides the working geophysicist with a broad overview of the petroleum systems of deepwater settings. The six main elements of petroleum systems will be covered: reservoirs, traps, seals, source rocks, generation, migration, and timing. The course is designed to teach students approximately 80% of what is important. For those interested in further study of a specific topic, each chapter has extensive references for the current literature. About 10% of the current cutting-edge information remains proprietary and cannot be included. <...>

Автор(ы):McResth I., Sial A.N.
Издание:Salvador, 1984 г., 162 стр.
Язык(и)Португальский
Petrologia ignea. Volume 1. Os fundamentos e as ferramentas de estudo / Петрология изверженных пород. Том 1. Основы и инструменты обучения

Uma das maiores dificuldades encontradas pelos autores no ensino de disciplinas relacionadas à Petro-logia ígnea e áreas afins nos níveis de Graduação e Pós-Graduação é representada pela falta de textos em português. Entre a tradução de um livro texto já existente e a preparação de um texto novo, os autores optaram, em 1979, pela segunda alternativa, uma vez que os textos já disponíveis se encontraram algo desatualizados e, muito raramente, tocam em assuntos de grande importância para o Geólogo brasileiro.

Автор(ы):Kornprobst J.
Издание:Kluwer Academic Publishers, 2002 г., 224 стр., ISBN: 0-306-48097-2
Язык(и)Английский
Petrology and structural geology. Volume 12. Metamorphic rocks and their geodynamic significance. A petrological handbook / Петрология и структурная геология. Выпуск 12. Метаморфические породы и их геодинамическое значение. Петрологический справочник

Metamorphism is the sum of all transformations which cause a rearrangement of the elements of a rock at the atomic scale, leading to a recrystallization in the solid state (with or without a fluid phase), as a result of variations in temperature, pressure or of composition.

Автор(ы):Fischer G.W.
Издание:American Geophysical Union, 1989 г., 15 стр.
Язык(и)Английский
Petrology and structure of gneiss anticlines near Baltimore, Maryland. Field trip guidebook / Петрология и структура гнейсовой антиклинали возле Балтимора, Мэрилэнд. Путеводитель полевой экскурсии

This field trip will focus on the petrology and structure of basementcored anticlines in the central Appalachian Piedmont, near Baltimore, Maryland (Figure 1). These structures have long been interpreted as mantled gneiss domes in the sense of Eskola (1949). However, recent work suggests that they are recumbent nappes, arched by later folding about steeply dipping axial planes. <...>

Издание 2
Автор(ы):Mason R.
Издание:Springer Science+Business Media B.V., 1990 г., 240 стр., ISBN: 978-94-017-2590-3
Язык(и)Английский
Petrology of the metamorphic rocks / Петрология метаморфических пород

There are three categories of rocks- igneous, sedimentary and metamorphic. Igneous rocks have been formed by solidification of hot silicate melts known as magmas, which may be erupted at the Earth's surface as lavas from volcanoes. Sedimentary rocks form by a variety of processes at low temperatures near the surface, including the bottom of the seas and oceans. Metamorphic rocks, the third category, were originally either igneous or sedimentary, but their character has been changed by processes operating below the surface of the Earth. The constituent minerals of the rocks may be changed, or the shapes, sizes and mutual spatial relationships of the crystals may change. There are a variety of processes involved, and they are collectively described by the term metamorphism. <...>

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