Impact of temperature on the low salinity EOR effect for sandstone cores containing reactive plagioclase, Iván D. Piñerez Torrijos, Tina Puntervold, Skule Strand, Tor Austad, Vinh Vuong Tran and Kaia Olsen. Submitted to JPSE, 2016.
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For the sandstones we use the experimental coreflood data of Reynolds and Krevor ; Reynolds et al. and for the carbonate rocks, the data set of Manoorkar et al. . The sandstones exhibit distinctly orientated planar bedding, whereas the carbonates are characterized by isotropic cementation of varying length scale.
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/carbonate will be equilibrated together before running the capillary trapping experiment. The apparatus used for sandstone rocks was modified so that the geochemical reaction between CO 2 /rock was accounted for. Samples are taken and analysed to ensure that the brine/CO 2 mixture is saturated with carbonate minerals. In Indiana, the CO 2
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The proposed Vivian Sand Facility Project is within the RM of Springfield, south of Vivian, Manitoba on land designated for aggregate and industrial activities. The location was selected as it is adjacent to, and can make use of, the existing CN rail infrastructure.
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This dataset contains digital models of three carbonate (Indiana limestone, Estaillades limestone and Edwards Brown Dolomite) and two sandstone (Bentheimer and Bunter) cores with varying degrees of heterogeneity types and length scales. The models define the spatial distribution of porosity and capillary heterogeneity, and can simulate core floods.
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In this study, coreflood experiments were conducted on Bandera sandstone cores (1.5 in. × 6 in.) at a flow rate of 4 cm3/ min and temperature of 140°F. A mixture of formic acid and HF was used as an organic mud acid. Preflush of hydrochloric and formic acid was employed to remove carbonate minerals. Bandera sandstone cores contain a
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For the sandstones we use the experimental coreflood data of Reynolds and Krevor ; Reynolds et al. and for the carbonate rocks, the data set of Manoorkar et al. . The sandstones exhibit distinctly orientated planar bedding, whereas the carbonates are characterized by isotropic cementation of varying length scale.
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After this period of time, sandstone cores were removed from the crude oil and placed in an oven until dried. The aged sandstone core pieces were immersed into an aqueous solution of 0.3% NaCl containing different concentrations of silica materials (100 or 200 mg/L) for 24 h. Afterward, the samples were removed and placed in an oven until dried.
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In this study, coreflood experiments were conducted on Bandera sandstone cores (1.5 in. × 6 in.) at a flow rate of 4 cm3/ min and temperature of 140°F. A mixture of formic acid and HF was used as an organic mud acid. Preflush of hydrochloric and formic acid was employed to remove carbonate minerals. Bandera sandstone cores contain a
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the potential of recovering additional oil in sandstone and carbonate reservoirs. Sandstone and carbonate rocks are composed of completely different minerals, with varying degree of complexity and heterogeneity, but wettability alteration has been widely considered as the consequence rather than the cause of brine-dependent recovery.
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The cores were sourced from Kocurek Industries Ltd at a depth of ~ 183 m, and they are believed to have their origin from Texas, USA. The leopard sandstone and Edward brown carbonate core samples are identified as LPn and EDn, respectively, where n (1–15) is the sample number.
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Carbonate-cemented sandstones may have any of the sedimentary structures seen in other kinds of sandstone. Two kinds of carbonate cement are common in Carboniferous coal fields: (64X CaCO 3) Calcite-cemented sandstone (64X FeCO 3) Siderite-cemented sandstone; Both varieties are generally harder than typical gray sandstones, which they resemble.
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Simulating Core Floods in Heterogeneous Sandstone and Carbonate Rocks Abstract The characterisation of multiphase flow properties is essential for predicting large-scale fluid behaviour in the subsurface.
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Carbonate Classification. Rock s are classified in order to communicate inform ation about them. All classifications of limestone s are arbitrary and they frequently overlap or do not fit ones particular needs. Since binocular microscopes or hand lenses are the tools that are commonly available to the explorationist, a practical classification
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Core Laboratories developed the Yemen Rock Catalog which focuses on the spectrum of clastic and carbonate rock types found in the Republic of Yemen. The objectives of the Yemen Rock Catalog are the same as for the Worldwide Rock Catalog: Provide a reference manual containing "analog" sandstone and carbonate rock types for more accurate
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the potential of recovering additional oil in sandstone and carbonate reservoirs. Sandstone and carbonate rocks are composed of completely different minerals, with varying degree of complexity and heterogeneity, but wettability alteration has been widely considered as the consequence rather than the cause of brine-dependent recovery.
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Carbonate Classification. Rock s are classified in order to communicate inform ation about them. All classifications of limestone s are arbitrary and they frequently overlap or do not fit ones particular needs. Since binocular microscopes or hand lenses are the tools that are commonly available to the explorationist, a practical classification
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Known sandstone reservoirs are in Upper Jurassic–Lower Cretaceous deltaic sandstones on the Scotian Shelf and deep-water turbidites in salt-bound minibasins on the Scotian Slope, which host natural gas and minor oil. Detrital supply differs between the eastern, central and western parts of the basin (Tsikouras et al., 2011, Zhang et al., 2014).
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Our wide array of services includes cutting carbonate,marble, granite, shale and sandstone core samples. Along with cutting samples from stone provided by the customer, we also stock a large variety of stones quarried from locations around the world.
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Lecture 10: Carbonate sequence stratigraphy (Prof. P.D.W. Haughton) Outline of the principles behind the application of sequence stratigraphy to carbonate environments; contrasts between carbonate and clastic sediment production and supply and the way supply is coupled to sea level fluctuations. Sequence stratigraphy of main carbonate platform
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"Sandstone Cores as Reaction Vessels: Synthesis of Calcium Carbonate Particles for Artificial Formation Damage in the Qualification of Matrix-Acidizing Solutions." Paper presented at the SPE International Symposium on Oilfield Chemistry, The Woodlands.
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Our wide array of services includes cutting carbonate,marble, granite, shale and sandstone core samples. Along with cutting samples from stone provided by the customer, we also stock a large variety of stones quarried from locations around the world.
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In this paper, it is intended to investigate how do carbonate and sandstone cores are affected when smart carbonated water is injected by using core flooding tests and mineral analysis. It is found that rock dissolution depends on brine concentration and rock minerals.
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carbonate pore types with the relatively simple pore structure of sandstones, given the variability of the sandstone cementation exponent, m. However, a cementation exponent value of two (m =2) is a good choice for carbonate rocks whose porosity is dominantly intercrystalline as shown by numerous core measurements and log
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Core samples (70 mm × 35 mm) were selected from the carbonate and sandstone core samples of various Malaysian fields and characterized by different ranges of permeability and porosity. Most of the carbonate cores have a different pore space distribution known as vugs, shown in figure 1.
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Core Laboratories developed the Yemen Rock Catalog which focuses on the spectrum of clastic and carbonate rock types found in the Republic of Yemen. The objectives of the Yemen Rock Catalog are the same as for the Worldwide Rock Catalog: Provide a reference manual containing "analog" sandstone and carbonate rock types for more accurate
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Core samples (70 mm × 35 mm) were selected from the carbonate and sandstone core samples of various Malaysian fields and characterized by different ranges of permeability and porosity. Most of the carbonate cores have a different pore space distribution known as vugs, shown in figure 1.
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74 For the sandstones we use the experimental core ood data of Reynolds and Krevor (2015); 75 Reynolds et al. (2018) and for the carbonate rocks, the dataset of Manoorkar et al. (2021). 76 The sandstones exhibit distinctly-orientated planar bedding, whereas the carbonates are 77 characterised by isotropic cementation of varying length scale.
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Sandstone and carbonate-rock aquifers In scattered places in the United States, carbonate rocks are interbedded with almost equal amounts of water-yielding sandstone. In most places where these two rock types are interbedded, the carbonate rocks yield much more water than the sandstone.
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74 For the sandstones we use the experimental core ood data of Reynolds and Krevor (2015); 75 Reynolds et al. (2018) and for the carbonate rocks, the dataset of Manoorkar et al. (2021). 76 The sandstones exhibit distinctly-orientated planar bedding, whereas the carbonates are 77 characterised by isotropic cementation of varying length scale.
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