St. 2 Ya % Frieg

Total Page:16

File Type:pdf, Size:1020Kb

St. 2 Ya % Frieg March 5, 1968 R. M. EVANS ET AL 3,372,083 COMPOSITIONS AND ARTICLES FROM THE REACTION OF AN ISOCYANATE TERMINATED POLYURETHANE AND THE ISOCYANATE ADDUCT OF BITUMEN Filed March ill, l964 522SE OO 4. P P 2 s O SA 33333 S ae 27 St.2 NVENTORS Afobert A4. A razzis Berraerdous Artzg S BY 7%67.24:ya % frieg 27 3,372,083 United States Patent Office Patented Mar. 5, 1968 1. 2 tion of a concrete pavement of a road showing the use of COMPOSITIONS AND3,372,083 ARTiciES FROM THE REAC. the composition of the present invention; TION OF AN SOCYANATE TERMINATED POLY. FIGURE 2 is a perspective view partly in section of a URETHANE AND THE SOCYANATE ADDUCT tile, brick or floor covering showing the use of the binder OF BITUMEN 5 sealant of the present invention; Robert M. Evans, Chesterland, and Bernardas Brizgys, FIGURE 3 is a sectional view of a portion of a thermal Lyndhurst, Ohio, assignors to The Master Mechanics type insulating window pane using the sealant of the Company, Cleveland, Ohio, a corporation of Ohio present invention; Filed Mar. 11, 1964, Ser. No. 351,065 20 Claims. (C. 161-190) FIGURE 4 is a sectional view of a portion of a window O sash using the present sealant; and FIGURE 5 is a sectional view of a portion of a metallic Wall or ceiling panel utilizing the present sealant. ABSTRACT OF THE DISCLOSURE; According to the present invention, it has been found Floor tile, and caulking for glass and concrete contain that if a bituminous substance be used which has a rela ing a polyurethane, cured by water from the air to a 5 tively low moisture content and which is pre-reacted with solid having an elongation capacity greater than 100%, a polyisocyanate and then the intermediate product result is made from the reaction of an isocyanate terminated ing therefrom is mixed with a polyurethane prepolymer, prepolymer and the isocyanate adduct of an unmodified the final product has excellent package stability, good ad tar. This may be prepackaged in a single container and hesion to wet concrete, better physical properties than the hardened only when exposed to the moisture from the air 20 polyurethane prepolymer without the bituminous-isocya at the point of use. Also chlorinated hydrocarbons and or nate adduct, and useful rheological properties of kinds ganic silicones may be included. The caulking materials not possessed by the polyurethane prepolymer itself. At may be applied to wet joints. the same time, material costs are substantially reduced as a result of the use of relatively large amounts of bitumens, 25 which are ordinarily low in price. When this mixture is This invention relates to compositions suitable for use exposed to the atmosphere it is vulcanized or cured by as construction joint sealants, caulking compounds, roof water vapor. Moreover, it is possible to produce the prod ing materials or the like, specifically a composition of this uct or mixture in a single operation. kind lending itself to shipment, sale and application in As shown in FIGURE 1 of the drawing sealant of ready-to-apply single package form without any particular 30 the present invention has been applied as a joint between requirement for mixing at the point of use and to articles concrete blocks 2-2 which are supported by packed made with Such compositions. Sand layer 3 and aggregate or rock layer 4 of roadway In the past, compositions have been suggested for pave 5, which may be of clay or other suitable road base mate ment joints and the like consisting largely of two prin rial. In FIGURE 2 of the drawing, there is shown a floor cipal ingredients mixed at the point of use, one of them 35 tile or section of a flooring in which bits of rock 10-10 a polymeric material and the other a bituminous material Such as chips of quartz, marble or shale, etc. have Such, for example, as a petroleum residue, a coke oven been mixed with composition 11 of this invention, cast, tar or a natural asphalt. Generally, the nature of these troWelled and cured. The tiles can be molded as such and compositions is such as to require that a curing agent be laid individually in a sealant of this invention or can be included with the bituminous portion to solidify the poly 40 cast in place over concrete, wood or other subflooring. meric material. From the standpoint of the user, mixing After curing, the tile or floor can be polished or its surface at the point of application is a disadvantage, as for ex made smooth, if desired. FIGURE 3 shows an insulating ample, When it requires the use of elaborate proportion type window pane in which two pieces of glass 15-15 ing apparatus and skilled attendants to operate it. In many are secured together at least along their inner edges by cases, the compositions have a decided tendency to foam; 45 means of Sealant 16 of the present invention to form dead in others, even if there is no foaming, the products have air space 17 which can be partially exhausted, filled with relatively poor physical properties, particularly as regards dry air and so forth. FIGURE 4 discloses a piece of glass strength, elongation and adhesion to wet surfaces. 20 Secured in metal channel 21 of a window sash by An even more serious weakness has characteristically means of sealant 22 of the present invention. FIGURE resided in the inability of such compositions to bond 50 5 discloses wall panel 25 comprising metal sheets such as tenaciously to new concrete of high water content or old Steel sheets 26-26 secured together by the present seal concrete wetted down by rain or melting snow. ant 27. Essentially all of the space between sheets 26-26 Accordingly, it is an object of the present invention to may be filled with sealant 27 or if desired only a portion provide Sealants, caulking compounds and roofing mate may be filled with sealant to secure the sheets together. rials and the like characterized by their ability to be easily 55 THE BITUMINOUS ADDUCT applied, by general freedom from foaming, by having im The bituminous substance employed in the practice of proved physicals, and by having improved dry and wet the present invention can be any natural or synthetic bi adhesive strength to concrete. tuminous Substance (bitumen, pyrobitumen, asphalt, as Another object of this invention is to provide products 60 phaltite, asphaltic pyrobitumen, nonasphaltic pyrobitumen, or articles of manufacture in which the parts or elements tar and/or pitch) containing asphaltene or tar-like com are Secured in place by the sealant or composition and the ponents. For example, there can be used pine tar or tar like of the present invention. which is used for cutting hard resins, coaltar, coke oven Another object is to provide a method for making a or gas plant tar, road tars or oils, pitches, roofing pitches, 65 other coal tar fractions, cracked, straight run or natural composition useful as a sealant, caulking compound, roof asphalts, petroleum distillation residues and asphalts, cut ing material and so forth. asphalts, albino asphalts and so forth as well as synthetic These and other objects and advantages of the present bituminous substances. Examples of many bituminous invention will become more apparent to those skilled in Substances which can be used are shown in the book by the art from the following detailed description, examples 70 Abraham, "Asphalts and Allied Substances, D. Van and drawing in which: Nostrand Co., Inc., New York, 5th ed., vol. 1, 1945, es FIGURE 1 is a vertical cross sectional view of a por pecially pages 56-69. Still other materials can be used such 3,372,083 3. 4. as the high boiling tar acids which may be obtained by and 2,6-tolylene diisocyanates or other polyisocyanate treating tars with caustic, neutralizing, and fractionating mixtures can be used. It will be appreciated that, where to get the portion boiling between about 195-340 C. con isocyanates are used having more than two isocyanato taining relatively a high percentage of beta naphthol, re groups, care should be observed to avoid too much cross sorcinol, and a small amount of xylenol and other Sub 5 linking which might give an undesirable increase in vis stances (the lower boiling fraction, 21.0-225 C., contains cosity of the bituminous substance or make it a solid or xylenol, phenols and so forth). The high boiling tar acids gel. If the bituminous substance has a sufficiently high are useful in making light colored or white products. Aro molecular weight or high isocyanate equivalent this prob matic resins such as coumarone-indene polymers or resins, lem may not be too serious. chlorinated biphenyl, cyclic unsaturated petroleum resins Isocyanates which are preferred for reaction with the and the like which contain, or to which have been added 10 bituminous substances are organic diisocyanates having high boiling tar acids can also be used. Thus, the bitumi at least 6 carbon atoms up and to a total of 18 carbon nous substances can be naturally occurring substances, or atoms in a chain between isocyanato groups. The chain their derivatives or by-products, synthetics, or they may be may be part of an aliphatic chain or of a cyclic or aro the products or by-products of the chemical, coal, petro 5 matic ring. A portion, 1 to 4, of the total hydrogen atoms leum or steel industries and so forth. It is preferred that of the total of these carbon atoms may be substituted the bituminous substance be a liquid at temperatures of with halogen atoms, i.e., Cl, Br, I and/or F atoms.
Recommended publications
  • Solvent-Pore Interactions in the Eagle Ford Shale Formation T Victoria H
    Fuel 238 (2019) 298–311 Contents lists available at ScienceDirect Fuel journal homepage: www.elsevier.com/locate/fuel Full Length Article ☆ Solvent-pore interactions in the Eagle Ford shale formation T Victoria H. DiStefanoa,b, Joanna McFarlanea, Andrew G. Stacka, Edmund Perfectc, David F.R. Mildnerd, Markus Bleueld, Steve J. Chiperae, Kenneth C. Littrella, Michael C. Cheshirea, ⁎ Katherine E. Manzb, Lawrence M. Anovitza, a Oak Ridge National Laboratory, Oak Ridge, TN 37830-6110, USA b Bredesen Center, University of Tennessee, Knoxville, TN 37996-3394, USA c Department of Earth and Planetary Science, University of Tennessee, Knoxville, TN 37996-1410, USA d Center for Neutron Research, National Institute of Standards and Technology, Gaithersburg, MD 20899, USA e Chesapeake Energy, Oklahoma City, OK 73154-0496, USA ABSTRACT The effect of solvent extraction on pore space was examined on a suite of samples from the Eagle Ford Shale Formation with varying lithologies andmaturities. Several solvents ─toluene, cyclohexane, methanol, dichloromethane, and hydrochloric acid─ were contacted with shale samples, extracting the compatible organic matter. The porosity in these extracted shale samples was compared to unmodified samples. The amount and type of organic matter extracted were determined using Gas Chromatography ─ Mass Spectrometry, and the porosity was determined by (Ultra) Small Angle Neutron Scattering. Mostly alkanes and aromatics were detected in the extracts, but other portions of bitumen may also have been present. Only higher molecular weight alkanes were extracted with hydrochloric acid, suggesting that physical dissolution of carbonate minerals may have liberated this portion of organic matter and the solvent was not able to penetrate the bitumen and kerogen to extract the lower molecular weight alkanes.
    [Show full text]
  • A Prediction Model of Oil Cracked Gas Resources and Its Application in the Gas Pools of Feixianguan Formation in NE Sichuan Basin, SW China
    Hindawi Publishing Corporation Journal of Geological Research Volume 2011, Article ID 592567, 11 pages doi:10.1155/2011/592567 Research Article A Prediction Model of Oil Cracked Gas Resources and Its Application in the Gas Pools of Feixianguan Formation in NE Sichuan Basin, SW China Tongshan Wang,1 Ansng Geng,2 Xia Li,1 Hongjun Wang,1 Zecheng Wang,1 and Li Qiufen1 1 Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China 2 The State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Science, Guangzhou 510640, China Correspondence should be addressed to Tongshan Wang, [email protected] Received 30 September 2010; Revised 21 January 2011; Accepted 8 February 2011 Academic Editor: Vicki Hansen Copyright © 2011 Tongshan Wang et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The prediction of oil cracked gas resources is necessary and urgent in the gas exploration of these basins at high to over stage in China. A marine crude oil sample was pyrolyzed using sealed gold tubes system in our study. The pyrolysates including gas, liquid, and solid were quantitatively analyzed. Based on the pyrolysis data and kinetic calculation, the yield correlativity among gas, liquid, and solid products was regressed with high correlative coefficients to establish a prediction model suitable for the resource estimation of oil cracked gas. The verification formula for this model was also established on the principle of mass conservation. The affecting factors and the application preconditions of this model were discussed.
    [Show full text]
  • Application of Organic Petrography in North American Shale Petroleum Systems: a Review
    International Journal of Coal Geology 163 (2016) 8–51 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo Application of organic petrography in North American shale petroleum systems: A review Paul C. Hackley a, Brian J. Cardott b a U.S. Geological Survey, MS 956 National Center, 12201 Sunrise Valley Dr, Reston, VA 20192, USA b Oklahoma Geological Survey, 100 E. Boyd St., Rm. N-131, Norman, OK 73019-0628, USA article info abstract Article history: Organic petrography via incident light microscopy has broad application to shale petroleum systems, including Received 13 April 2016 delineation of thermal maturity windows and determination of organo-facies. Incident light microscopy allows Received in revised form 10 June 2016 practitioners the ability to identify various types of organic components and demonstrates that solid bitumen Accepted 13 June 2016 is the dominant organic matter occurring in shale plays of peak oil and gas window thermal maturity, whereas Available online 16 June 2016 oil-prone Type I/II kerogens have converted to hydrocarbons and are not present. High magnification SEM obser- Keywords: vation of an interconnected organic porosity occurring in the solid bitumen of thermally mature shale reservoirs Organic petrology has enabled major advances in our understanding of hydrocarbon migration and storage in shale, but suffers Thermal maturity from inability to confirm the type of organic matter present. Herein we review organic petrography applications Shale petroleum systems in the North American shale plays through discussion of incident light photographic examples. In the first part of Unconventional resources the manuscript we provide basic practical information on the measurement of organic reflectance and outline Vitrinite reflectance fluorescence microscopy and other petrographic approaches to the determination of thermal maturity.
    [Show full text]
  • Organic Geochemistry of Marine Source Rocks and Pyrobitumen- Containing Reservoir Rocks of the Sichuan Basin and Neighbouring Areas, SW China
    Marine and Petroleum Geology 56 (2014) 147e165 Contents lists available at ScienceDirect Marine and Petroleum Geology journal homepage: www.elsevier.com/locate/marpetgeo Research Paper Organic geochemistry of marine source rocks and pyrobitumen- containing reservoir rocks of the Sichuan Basin and neighbouring areas, SW China Xiaodong Jin a, Changchun Pan a,*, Shuang Yu a, Ertin Li a, Jun Wang a, Xiaodong Fu b, Jianzhong Qin b, Zengye Xie c, Ping Zheng d, Lansheng Wang d, Jianping Chen e, Yuming Tan f a State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Wushan, Guangzhou 510640, China b Wuxi Institute of Petroleum Geology, Sinopec, Wuxi, Jiangsu 214151, China c Research Institute of Petroleum Exploration and Development-Langfang Branch, PetroChina Ltd, Langfang, Hebei 065007, China d Southwest Oil and Gas Field Company, PetroChina, Chengdu, Sichuan 610051, China e Research Institute of Petroleum Exploration and Development, PetroChina Ltd, Beijing 100083, China f Zhongyuan Oilfield Company, Sinopec, Puyang, Henan 457001, China article info abstract Article history: Three bitumen fractions were obtained and systematically analysed for the terpane and sterane Received 5 January 2014 composition from 30 Paleozoic source rocks and 64 bitumen-containing reservoir rocks within the Upper Received in revised form Sinian, Lower Cambrian, Lower Silurian, Middle Carboniferous, Upper Permian and Lower Triassic strata 22 April 2014 in the Sichuan Basin and neighbouring areas, China. These bitumen fractions include extractable oils Accepted 25 April 2014 (bitumen I), oil-bearing fluid inclusions and/or closely associated components with the kerogen or Available online 9 May 2014 pyrobitumen/mineral matrix, released during kerogen or pyrobitumen isolation and demineralization (bitumen II), and bound compounds within the kerogen or pyrobitumen released by confined pyrolysis Keywords: Sichuan basin (bitumen III).
    [Show full text]
  • Apbpet01 19..37
    Ugana, C. N., C. E. Snape, W. Meredith, A. D. Carr, I. C. Scotchman, and R. C. Davis, 2012, Retardation of hydrocarbon generation and maturation by water pressure in geologic basins: An experimental investigation, in K. E. Peters, D. J. Curry, and M. Kacewicz, eds., Basin Modeling: New Horizons in Research 1 and Applications: AAPG Hedberg Series, no. 4, p. 19 –37. Retardation of Hydrocarbon Generation and Maturation by Water Pressure in Geologic Basins: An Experimental Investigation Clement N. Ugana, Colin E. Snape, Iain C. Scotchman and Will Meredith Statoil (UK) Ltd., London, United Kingdom Department of Chemical and Environmental Engineering, Faculty of Engineering, University of Nottingham, Nottingham, United Kingdom Robert C. Davis Woodside Energy (USA) Inc., Houston, Texas, U.S.A. Andrew D. Carr1 Advanced Geochemical Systems Ltd., Leicestershire, United Kingdom ABSTRACT emperature-time–based first-order kinetic models are currently used to predict hydrocarbon generation and maturation in basin modeling. Physical chemical T theory, however, indicates that water pressure should exert significant control on the extent of these hydrocarbon generation and maturation reactions. We pre- viously heated type II Kimmeridge Clay source rock in the range of 310 to 3508Cata water pressure of 500 bar to show that pressure retarded hydrocarbon generation. This study extended a previous study on hydrocarbon generation from the Kimmeridge Clay that investigated the effects of temperature in the range of 350 to 4208C at water pres- sures as much as 500 bar and for periods of 6, 12, and 24 hr. Although hydrocarbon generation reactions at temperatures of 4208C are controlled mostly by the high tem- perature, pressure is found to have a significant effect on the phase and the amounts of hydrocarbons generated.
    [Show full text]
  • Formation and Thermal Evolution of Insoluble Reservoir Bitumen in Angolan Carbonate Reservoirs
    Formation and thermal evolution of insoluble reservoir bitumen in Angolan carbonate reservoirs. Andrew Mort, Fatima Laggoun-Défarge, Isabelle Kowalewski, Alain-Yves Huc, Jean-Noël Rouzaud, Fabrice Muller To cite this version: Andrew Mort, Fatima Laggoun-Défarge, Isabelle Kowalewski, Alain-Yves Huc, Jean-Noël Rouzaud, et al.. Formation and thermal evolution of insoluble reservoir bitumen in Angolan carbonate reservoirs.. 22th International Meeting Organic Geochemistry, 2005, Seville, Spain. hal-00085514 HAL Id: hal-00085514 https://hal-insu.archives-ouvertes.fr/hal-00085514 Submitted on 12 Jul 2006 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Formation and thermal evolution of insoluble reservoir bitumen in Angolan carbonate reservoirs Andrew Mort1, Fatima Laggoun-Défarge1, Isabelle Kowalewski2, Alain-Yves Huc2, Jean-Noël Rouzaud3, Fabrice Muller4 Pyrobitumen resulting from the thermal cracking of crude oil is a frequent occurrence in petroleum reservoirs. Despite the detrimental implications of pyrobitumen for the poroperm qualities of the reservoir; little is known about the evolution of pyrobitumen properties as a function of increasing thermal stress. A suite of pyrobitumen-bearing reservoir cores from the carbonate Jurassic Pinda formation in offshore Angola has been studied using geochemical and petrographic techniques (including elemental analysis, Rock Eval pyrolysis, GC, FTIR, XRD, SEM, TEM) in order to characterise the physical, chemical, and optical properties of the pyrobitumen as fully as possible.
    [Show full text]
  • Effect of Minerals on the Transformations of Organic Matter During Thermolysis in Benzene
    Chemistry for Sustainable Development 13 (2005) 569–574 569 Effect of Minerals on the Transformations of Organic Matter During Thermolysis in Benzene V. V. SAVELIEV Institute of Petroleum Chemistry, Siberian Branch of the Russian Academy of Sciences, Pr. Akademicheskiy 3, Tomsk 634021 (Russia) E-mail: [email protected] (Received February 1, 2005; in revised form May 6, 2005) Abstract The effect of minerals (montmorillonite, calcite, quartz) on the formation of group components of liquid products during pyrolysis of the kerogen of sapropel nature in benzene was investigated. It was established that the maximal amount of liquid products (with the mass concentration above 60 mass %) is formed in the presence of quartz and montmorillonite. It was established that carbonate and clayish rocks promote generation of high-molecular compounds in the pyrolyzate. INTRODUCTION Cuonam formation of bituminous sediments of the siliceous-carbonate-clayish and clayish- Investigation of the interaction between carbonate compositions is situated in the basins inorganic and organic components in of the Olenek and Yudoma rivers (Yakutia) [5]. sedimentary rocks shows that in the majority The bituminological analysis of these sediments of cases the effect of minerals manifests itself showed that this horizon of the Cambrian age is as adsorption and catalytic effects [1, 2]. In generally bitumen maternal with high potential. particular, for thermal destruction of organic Kerogen was obtained form shale oil by matter (OM), these effects promote an increase means of consecutive separation of the in the yield of liquid products, a decrease in chloroform, alcohol-benzene and “bound” (after the concentration of tarry and pyrobitumen acidic treatment) bitumoids.
    [Show full text]
  • Genesis of Solid Bitumen Hamed Sanei
    www.nature.com/scientificreports OPEN Genesis of solid bitumen Hamed Sanei This paper presents a new schematic model for generation and timing of multiple phases of solid bitumen throughout the continuum of organic matter maturation in source and tight reservoir rocks. Five distinct stages in the evolution of solid bitumen are proposed: (1) diagenetic solid bitumen (or degraded bituminite), which is not a secondary maceral resulting from the thermal cracking of kerogen. Instead it is derived from degradation of bituminite in the diagenesis stage (Ro < 0.5%); (2) initial-oil solid bitumen, is a consolidated form of early catagenetically generated bitumen at the incipient oil window (Ro ~ 0.5–0.7%); (3) primary-oil solid bitumen is derived from thermally generated bitumen and crude oil in the primary oil window (Ro ~ 0.7–1.0%); (4) late-oil solid bitumen (solid-wax) is derived from the waxy bitumen separated from the mature parafnic heavy oil in the primary- and late-oil windows; and (5) pyrobitumen, which is mainly a non-generative solid bitumen, is evolved from thermal cracking of the remaining hydrocarbon residue and other types of solid bitumen in the dry gas window and higher temperature (Ro > 1.4%). This model shows concurrence of multi-populations solid bitumen with oil, bitumen, and other phases of fuid hydrocarbon residue during most of the maturity continuum. Te evolution of organic matter immediately afer sinking through the water column and deposition in sedimen- tary basins involves a series of post-burial bacterial activities and low temperature chemical reactions during the diagenesis stage, followed by thermal maturation and thermal cracking during the catagenesis and metagenesis phases.
    [Show full text]
  • Pyrobitumen Occurrence and Formation in a Cambro–Ordovician Sandstone Reservoir, Fahud Salt Basin, North Oman
    Pyrobitumen occurrence and formation in a Cambro–Ordovician sandstone reservoir, Fahud Salt Basin, North Oman Alain-Yves Huc, Peter Nederlof, Romain Debarre, Bernard Carpentier, Mohammed Boussafir, Fatima Laggoun-Défarge, Arnaud Lenail-Chouteau, Nathalie Bordas-Le Floch To cite this version: Alain-Yves Huc, Peter Nederlof, Romain Debarre, Bernard Carpentier, Mohammed Boussafir, et al.. Pyrobitumen occurrence and formation in a Cambro–Ordovician sandstone reservoir, Fahud Salt Basin, North Oman. Chemical Geology, Elsevier, 2000, 168, pp.99-112. 10.1016/S0009- 2541(00)00190-X. hal-00115104 HAL Id: hal-00115104 https://hal-insu.archives-ouvertes.fr/hal-00115104 Submitted on 20 Mar 2007 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Pyrobitumen occurrence and formation in a Cambro– Ordovician sandstone reservoir, Fahud Salt Basin, North Oman Alain Y. Huc, a, Peter Nederlofb, Romain Debarrea, Bernard Carpentiera, Mohammed Boussafirc, Fatima Laggoun-Défargec, Arnaud Lenail-Chouteaua and Nathalie Bordas- Le Flocha a Institut Français du Pétrole, Division Geologie-Geochimie, 1 et 4 Avenue de Bois-Préau, 92852, Rueil-Malmaison, France b Petroleum Development of Oman, Oman c Université d'Orléans, UNR 6531 du CNRS, France : devient en janvier 200 ISTO-UMR6113 CNRS et Université d’Orléans – 45071 Orléans Cédex 2 Abstract The Cambro–Ordovician Barik Sandstone reservoirs in the Fahud Salt Basin in Oman contain bitumen which may fill up to 40% of the porosity.
    [Show full text]
  • Simple Kinetic Models of Petroleum Formation. Part II: Oil-Gas Cracking
    Marine and Petroleum Geology, Vol. 12, No. 3, pp. 321-340, 1995 Copyright 0 1995 Elsevier Science Ltd Printed in Great Britain. All rights reserved 0264-8172195 $10.00 + 0.00 Simple kinetic models of petroleum formation. Part II: oil-gas cracking Andrew S. Pepper* BP Research, Chertsey Road, Sunbury-on-Thames, Middlesex, UK Timothy A. Dodd t BP Exploration, Farburn Industrial Estate, Dyce, Aberdeen, UK Received 13 April 7993; revised 74 January 7994; accepted 20 April 1994 Kinetic schemes describing oil-gas cracking are a required component of models which predict the masses, compositions and phases of petroleum expelled from source rocks; an additional application is in predicting the temperature zone over which reservoired oil deposits will be degraded to gas. This simple first-order kinetic model, calibrated on closed-system laboratory pyrolysis of 16 different source rock samples, describes the bulk conversion of oil (Cc+ molecular range) to gas (r& molecular range). Cracking rates vary markedly between samples, defending on the saturate to aromatic ratio of the generated oil. The initial hydrogen index (HI ) of the sample, taken as an indirect measure of the saturate to aromatic ratio of the oil it generates, correlates strongly with optimized rate constants for oil cracking in individual samples. Thus cracking rates are predictable using a simple, routinely performed geochemical screening measurement. Source rocks with high HI0 tend to generate saturate-rich oils with a high mean activation energy and a tight distribution of bond energies, which crack relatively slowly over a high but relatively narrow temperature range. Source rocks with low HI0 generate aromatic-rich oils with a low mean activation energy and a broad distribution of bond energies, which crack relatively rapidly over a lower, but relatively wide, temperature range.
    [Show full text]
  • Formation of Bitumen in the Elgin/Franklin Complex, Central Graben, North Sea: Implications for Hydrocarbon Charging
    Downloaded from http://sp.lyellcollection.org/ by guest on January 31, 2019 Accepted Manuscript Geological Society, London, Special Publications Formation of bitumen in the Elgin/Franklin complex, Central Graben, North Sea: Implications for hydrocarbon charging Will Meredith, Clement N Uguna, Colin E Snape, Andrew D Carr & Iain C Scotchman DOI: https://doi.org/10.1144/SP484-2017-344 Received 15 December 2017 Revised 21 December 2018 Accepted 24 January 2019 © 2019 The Author(s). Published by The Geological Society of London. All rights reserved. For permissions: http://www.geolsoc.org.uk/permissions. Publishing disclaimer: www.geolsoc.org.uk/pub_ethics To cite this article, please follow the guidance at https://www.geolsoc.org.uk/onlinefirst#how-to-cite Manuscript version: Accepted Manuscript This is a PDF of an unedited manuscript that has been accepted for publication. The manuscript will undergo copyediting, typesetting and correction before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the book series pertain. Although reasonable efforts have been made to obtain all necessary permissions from third parties to include their copyrighted content within this article, their full citation and copyright line may not be present in this Accepted Manuscript version. Before using any content from this article, please refer to the Version of Record once published for full citation and copyright details, as permissions may be required. Downloaded from http://sp.lyellcollection.org/ by guest on January 31, 2019 Formation of bitumen in the Elgin/Franklin complex, Central Graben, North Sea: Implications for hydrocarbon charging W.
    [Show full text]
  • Organic Matter and Copper Mineralization at White Pine, Michigan, U.S.A
    Chemical Geology, 99 ( 1992 ) 189-211 189 Elsevier Science Publishers B.V., Amsterdam Organic matter and copper mineralization at White Pine, Michigan, U.S.A. Jeffrey L. Mauk a and G.B. Hieshimab'" aDepartment of Geological Sciences, University of Michtgan, Ann Arbor, M148109, USA bGeology Department, lndiana University, Bloomington, IN 47405, USA (Received May 21, 1991; revised and accepted February 20, 1992 ) ABSTRACT Mauk, J.L. and Hieshima, G.B., 1992. Organic matter and copper mineralization at White Pine, Michigan, U.S.A. In: P.A. Meyers. L.M. Pratt and B. Nagy (Guest-Editors), Geochemistry of Metalliferous Black Shales. Chem. Geol., 99: 189- 211. Indigenous and exogenous organic matter in sediments of the North American Midcontinent Rift were involved in precipitation of Cu-bearing minerals during main- and second-stage mineralization events at White Pine, Michigan. Sam- ples of the Proterozoic Nonesuch Formation from the White Pine mine and adjacent areas were investigated petrographi- cally and geochemically in order to determine the influence of organic matter on the precipitation of Cu and to determine whether mineralization influenced thermal maturity of organic matter. During main-stage mineralization, introduction of cupriferous fluids into the lower Nonesuch Fro. formed Cu-bearing sulfides by replacement of pyrite. Sulfur may have been added to the system via abiogenic sulfate reduction, with organic matter providing a direct source of reducing potential. In basal ore horizons where all sulfide had been incorporated into chalcocite during main-stage mineralization, native Cu also precipitated locally, with organic matter presumably acting as a direct reductant. Later compressional faulting at White Pine provided conduits for additional cupriferous fluids; these fluids deposited second-stage Cu mineralization.
    [Show full text]