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1

Funk, Tiffany. "A Musical Suite Composed by an Electronic Brain: Reexamining the Illiac Suite and the Legacy of Lejaren A. Hiller Jr." Leonardo Music Journal 28 (December 2018): 19–24. http://dx.doi.org/10.1162/lmj_a_01037.

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In 1956, Lejaren A. Hiller, Jr., and Leonard Isaacson debuted the Illiac Suite, the first score composed with a computer. Its reception anticipated Hiller’s embattled career as an experimental composer. Though the Suite is an influential work of modern electronic music, Hiller’s accomplishment in computational experimentation is above all an impressive feat of postwar conceptual performance art. A reexamination of theoretical and methodological processes resulting in the Illiac Suite reveals a conceptual and performative emphasis reflecting larger trends in the experimental visual arts of the
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2

Raghavendra and Prasanna Kumar. "Permutations on Illiac IV-Type Networks." IEEE Transactions on Computers C-35, no. 7 (1986): 662–69. http://dx.doi.org/10.1109/tc.1986.1676812.

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3

Babula, Gabriel, Wojciech Czarny, Zofia Ignasiak, Raja Chakraborty, and Slawomir Koziel. "Diversity of change in body mass index and skinfold thickness between different study courses within four years of study among the male students in a university in Poland." Anthropological Review 85, no. 3 (2022): 19–30. http://dx.doi.org/10.18778/1898-6773.85.3.02.

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Objective: This study examined whether there were significant changes (expectedly increase) in BMI (Body Mass Index), and relative subcutaneous body fat during the four years of study in a university and compared these changes between the students of different courses, viz., Computer science, Law and administration, Humanities and Physical education. Design: This was a prospective follow up study with measurements at two time points with gap of four years. Body mass index, Triceps, subscapular, mid-axillary, abdominal, supra-illiac and medial-calf skinfold thicknesses were measured at two poin
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4

Prado-Díaz, Alfredo, Andrés Castillo, Diana Marcela Rojas, and Mónica Chávez-Vivas. "Marcadores moleculares en el diagnóstico y pronóstico de sepsis, sepsis grave y choque séptico." Revista de la Facultad de Medicina 65, no. 1 (2017): 145–55. http://dx.doi.org/10.15446/revfacmed.v65n1.53876.

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Introducción. A pesar de los importantes avances en el entendimiento de la patofisiología de la sepsis, la mortalidad que genera sigue siendo alta.Objetivo. Describir el estado del arte de los biomarcadores moleculares propuestos hasta el momento como potenciales marcadores para el diagnóstico y pronóstico de sepsis, sepsis grave y choque séptico.Materiales y métodos. Se analizaron los registros de los últimos 14 años que se encontraban en PubMed, en The New England Journal of Medicine (NEJM) y en Illinois Automatic Computer (ILLIAC) con los términos sepsis, genetic polymorphisms, genetic vari
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5

Kotarba, M., and J. Środoń. "Diagenetic evolution of crystallite thickness distribution of illitic material in Carpathian shales, studied by the Bertaut-Warren-Averbach XRD method (MudMaster computer program)." Clay Minerals 35, no. 2 (2000): 383–91. http://dx.doi.org/10.1180/000985500546855.

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AbstractThe MudMaster computer program, based on the modified Bertaut-Warren- Averbach (BWA) XRD method, was used in the study of diagenetic evolution of illitic material in shales. The illitic material was characterized by XRD as a mixture of illite-smectite (I-S) and discrete illite. The experimental conditions for complete dehydration of swelling clays, necessary in this method, were established for a climate of high relative humidity (RH >40%). It was found that the distribution of crystallite thickness of dehydrated illitic material of shales is described by the lognormal law, as was e
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6

Muralidhar, Nikhil, Chen Wang, Nathan Self, et al. "illiad." ACM Transactions on Intelligent Systems and Technology 9, no. 3 (2018): 1–20. http://dx.doi.org/10.1145/3066167.

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7

Eberl, D. D., and B. Velde. "Beyond the Kubler Index." Clay Minerals 24, no. 4 (1989): 571–77. http://dx.doi.org/10.1180/claymin.1989.024.4.01.

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AbstractThe value of peak width at half-height for the illite 001 XRD reflection is known as the Kubler index or the illite ‘crystallinity’ index. This measurement, which has been related to the degree of metamorphism of very low-grade, pelitic rocks, is a function of at least two crystal-chemical factors: (1) illite X-ray scattering domain size; and (2) illite structural distortions (especially swelling). Reynolds' NEWMOD computer program is used to construct a grid with which these two contributions to illite peak width can be determined independently from measurements of the 001 peak width
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8

Hanafi, MohammadQ, Masoome Norouzi, and MohammadM Gharibvand. "Computed tomography-based age estimation of illiac crests calcification in 10-29 year-old individuals." Journal of Family Medicine and Primary Care 8, no. 6 (2019): 1947. http://dx.doi.org/10.4103/jfmpc.jfmpc_465_18.

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9

Rajic, Hrabri L., and Abderrafi M. Ougouag. "ILLICO: A Nodal Neutron Diffusion Method for Modern Computer Architectures." Nuclear Science and Engineering 103, no. 4 (1989): 392–408. http://dx.doi.org/10.13182/nse89-a23691.

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10

Drits, V. A., B. A. Sakharov, H. Lindgreen, and A. Salyn. "Sequential structure transformation of illite-smectite-vermiculite during diagenesis of Upper Jurassic shales from the North Sea and Denmark." Clay Minerals 32, no. 3 (1997): 351–71. http://dx.doi.org/10.1180/claymin.1997.032.3.03.

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AbstractFor mixed-layer clay fractions from the North Sea and Denmark, X-ray diffractograms have been recorded for specimens saturated with Mg, Ca, Na and NH4, both airdry and intercalated with ethylene glycol, and the patterns have been computer-simulated with a multicomponent program. The mixed-layer fractions consist of an illite-smectite-vermiculite (I-S-V) phase constituting ~90% of the fraction and a kaolinite-illite-vermiculite (K-I-V) phase. For each I-S-V, the degree of swelling in swelling interlayers depends on both interlayer cation and glycolation, whereas the amount of non-swelli
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11

Lindgreen, Holger. "Elemental and structural changes in illite/smectite mixed-layer clay minerals during diagenesis in Kimmeridgian- Volgian (- R yazanian) clays in the Central Trough, North Sea and the Norwegian ­Danish Basin." Bulletin of the Geological Society of Denmark 39 (October 25, 1991): 1–82. http://dx.doi.org/10.37570/bgsd-1991-39-01.

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. The literature on the diagenetic conversion of smectite layers to illite layers in mixed-layer illite/smectite is reviewed. According to this smectite layers are converted to illite layers during diagenesis at temperatures above 55°C and illite/smectites become IS ordered at about 100°C and at illite percentages of about 80%. Charge and elemental composition seem, beside temperature, to be of importance in the process. Investigations from metamorphic and hydrothermal areas have also found a conversion of smectite to illite layers with increasing temperature. In hydrothermal experiments, the
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12

Guthrie, George D. "High-Resolution Transmission Electron Microscopy of Mixed-Layer Illite/Smectite: Computer Simulations." Clays and Clay Minerals 37, no. 1 (1989): 1–11. http://dx.doi.org/10.1346/ccmn.1989.0370101.

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13

Liu, Xiwu, Zhiqi Guo, Qibin Zhang, Yuwei Liu, and Haifeng Chen. "Rock physical characterisation of microstructural fabrics and elastic anisotropy for a shale oil reservoir." Journal of Geophysics and Engineering 17, no. 2 (2020): 377–89. http://dx.doi.org/10.1093/jge/gxz123.

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Abstract Rock physics models are constructed to describe elastic anisotropy of various fabrics in shales. A method is developed to invert elastic properties of the clay mixture in shales. Inversion results indicate that the clay mixture has abnormally low Vs and consequently leads to a very high Vp/Vs ratio, which is related to the presence of the soft interparticle medium in the clay mixture. Accordingly, a model is constructed to describe anisotropy clay mixture that consists of layering distributed illite-smectite particles, and a more compliant interparticle medium that has a bulk modulus
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14

Klunk, Marcos Antonio, Leonardo Hax Damiani, Gustavo Feller, Rommulo Vieira Conceição, Mara Abel, and Luiz Fernando De Ros. "Geochemical modeling of diagenetic reactions in Snorre Field reservoir sandstones: a comparative study of computer codes." Brazilian Journal of Geology 45, suppl 1 (2015): 29–40. http://dx.doi.org/10.1590/2317-4889201530145.

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ABSTRACTDiagenetic reactions, characterized by the dissolution and precipitation of minerals at low temperatures, control the quality of sedimentary rocks as hydrocarbon reservoirs. Geochemical modeling, a tool used to understand diagenetic processes, is performed through computer codes based on thermodynamic and kinetic parameters. In a comparative study, we reproduced the diagenetic reactions observed in Snorre Field reservoir sandstones, Norwegian North Sea. These reactions had been previously modeled in the literature using DISSOL-THERMAL code. In this study, we modeled the diagenetic reac
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15

Jacob, Arne, Markus Peltz, Sina Hale, et al. "Simulating permeability reduction by clay mineral nanopores in a tight sandstone by combining computer X-ray microtomography and focussed ion beam scanning electron microscopy imaging." Solid Earth 12, no. 1 (2021): 1–14. http://dx.doi.org/10.5194/se-12-1-2021.

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Abstract. Computer X-ray microtomography (µXCT) represents a powerful tool for investigating the physical properties of porous rocks. While calculated porosities determined by this method typically match experimental measurements, computed permeabilities are often overestimated by more than 1 order of magnitude. This effect increases towards smaller pore sizes, as shown in this study, in which nanostructural features related to clay minerals reduce the permeability of tight reservoir sandstone samples. Focussed ion beam scanning electron microscopy (FIB-SEM) tomography was applied to determine
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16

Jacob, Arne, Markus Peltz, Sina Hale, et al. "Simulating permeability reduction by clay mineral nanopores in a tight sandstone by combining computer X-ray microtomography and focussed ion beam scanning electron microscopy imaging." Solid Earth 12, no. 1 (2021): 1–14. http://dx.doi.org/10.5194/se-12-1-2021.

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Abstract. Computer X-ray microtomography (µXCT) represents a powerful tool for investigating the physical properties of porous rocks. While calculated porosities determined by this method typically match experimental measurements, computed permeabilities are often overestimated by more than 1 order of magnitude. This effect increases towards smaller pore sizes, as shown in this study, in which nanostructural features related to clay minerals reduce the permeability of tight reservoir sandstone samples. Focussed ion beam scanning electron microscopy (FIB-SEM) tomography was applied to determine
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17

Qin, Xuan, De-Hua Han, and Luanxiao Zhao. "Elastic characteristics of overpressure due to smectite-to-illite transition based on micromechanism analysis." GEOPHYSICS 84, no. 4 (2019): WA23—WA42. http://dx.doi.org/10.1190/geo2018-0338.1.

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Characterizing the elastic signatures of overpressure of shale caused by the smectite-to-illite transition relies on a good understanding of this mechanism and is also necessary for pore-pressure prediction. Methods of pore-pressure prediction in shales that have undergone smectite-to-illite transition are mostly based on empirical fitting without a quantitative interpretation based on a micromechanism analysis. With upscaled wireline-logging data, two trends of smectite-to-illite transition are categorized by using the crossplot of sonic traveltime and density. Trend I associated with a fluid
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18

Mitcham, Carl. "In Memoriam Ivan Illich: Critic of Professionalized Design." Design Issues 19, no. 4 (2003): 26–30. http://dx.doi.org/10.1162/074793603322545037.

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19

Roush, James, David Biller, and Julie Gervais. "Evaluation of an overlapping pubic and ischiatic osteotomy for the improvement of acetabular ventroversion in dogs: an ex vivo study." Veterinary and Comparative Orthopaedics and Traumatology 29, no. 06 (2016): 499–506. http://dx.doi.org/10.3415/vcot-16-01-0018.

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SummaryObjectives: To assess the potential of a new single-session surgical procedure, the overlapping pubic and ischiatic osteotomy (OPIO) for modification of bilateral hip conformation. We hypothesized that OPIO would be simple to perform with currently available surgical equipment, through a single surgical approach, with minimal potential morbidity, and that it would allow adequate simultaneous bilateral improvement of coxofemoral joint conformation in patients at risk of canine hip dysplasia.Methods: The OPIO procedure was performed in the pelves of five large breed canine cadavers. Compu
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20

Dorriné, W., P. Van Espen, F. Adams, and B. Préat. "Characterisation and Classification of Individual Coal Mine Dust Particles by Computer-Controlled Electron Microprobe Analysis." Proceedings, annual meeting, Electron Microscopy Society of America 48, no. 2 (1990): 294–95. http://dx.doi.org/10.1017/s0424820100135071.

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Extremely dusty working conditions are a serious health risk for coal miners. Quartz and other minerals are known to cause lung diseases when inhaled over long periods of time. In this work, a study was made of the mineral content in coal mine dust. Individual particles were characterised using computer controlled electron microprobe analysis and then classified into different mineral categories using a multivariate classification procedure.Coal mine dust particles were collected from the Zolder coal mine, Belgium, using a BAT II cyclone sampling unit. Small quantities of the dust were suspend
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21

Dixon, D. A., J. Graham, and M. N. Gray. "Hydraulic conductivity of clays in confined tests under low hydraulic gradients." Canadian Geotechnical Journal 36, no. 5 (1999): 815–25. http://dx.doi.org/10.1139/t99-057.

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Clay barriers normally function at hydraulic gradients much lower than are commonly used in laboratory tests for hydraulic conductivity. This paper describes low-gradient tests on compacted illite, Na-bentonite, and sand-bentonite specimens at a range of dry densities. The tests examined the effects of deionized or saline pore fluid, the initial degree of saturation at the time of compaction, and back-pressuring to achieve saturation during permeation. No "critical" or "threshold" gradients were observed. In low-density materials, "transitional" gradients defined two separate regions of Darcia
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22

Smoliar-Zviagin, B. B. "Relationships between Structural Parameters and Chemical Composition of Micas." Clay Minerals 28, no. 4 (1993): 603–24. http://dx.doi.org/10.1180/claymin.1993.028.4.09.

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AbstractRegression analysis of high-precision structural and chemical data on trioctahedral and dioctahedral micas yielded interrelationships between unit-cell parameters, chemical composition and structural details. Regression equations relating b and csinβ parameters of micas to composition were used for estimating composition from cell data in order to analyse P-T conditions of rock formation. Algorithms for computing atomic coordinates for 2M1 37' and 1M dioctahedral micas having either centrosymmetric or non-centrosymmetric layers and 1M trioctahedral micas are presented. Deviations of co
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23

Zhao, Ping, Jie Li, Fanzi Zeng, Fu Xiao, Chen Wang, and Hongbo Jiang. "ILLIA: Enabling $k$ -Anonymity-Based Privacy Preserving Against Location Injection Attacks in Continuous LBS Queries." IEEE Internet of Things Journal 5, no. 2 (2018): 1033–42. http://dx.doi.org/10.1109/jiot.2018.2799545.

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24

Battaglia, S., F. Gherardi, G. Gianelli, L. Leoni, and F. Origlia. "Clay mineral reactions in an active geothermal area (Mt. Amiata, southern Tuscany, Italy)." Clay Minerals 42, no. 3 (2007): 353–72. http://dx.doi.org/10.1180/claymin.2007.042.3.08.

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AbstractThis study characterizes the effects of fluid migration into a predominantly shale cover which seals the active geothermal system of Mt. Amiata (Tuscany, Italy). During Alpine orogenesis the shale unit was affected by regional metamorphism at the limit of the diagenesis-anchizone. Subsequently, the phyllosilicate clay minerals of the shales underwent significant alteration at diagenetic temperatures (175±25ºC as determined by the geochemical model) by the pervasive circulation of fluids activated by the geothermal field. The overall mineralogical assemblages indicate that the main tran
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Sun, Guoqiang, Shuncun Zhang, Yetong Wang, Yaoliang Li, Hui Guo, and Shangshang Bo. "Eocene Sedimentary–Diagenetic Environment Analysis of the Pingtai Area of the Qaidam Basin." Applied Sciences 12, no. 14 (2022): 6850. http://dx.doi.org/10.3390/app12146850.

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Based on the petrological characteristics and elemental geochemical analysis of core samples from the Pingtai area in the northern structural belt of the Qaidam Basin, this study shows that the clay mineral assemblage of Lulehe Formation sandstone is dominated by high contents of smectite, chlorite and illite, and does not contain illite–smectite mixed layers or kaolinite. The chlorite and illite in the Xiaganchaigou Formation decreased gradually and the smectite disappeared. In addition, illite–smectite mixed layers began to appear and kaolinite was not present. These results indicate that th
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Jofre, Ana, Kristina Boylan, and Ibrahim Yucel. "Desarrollo de Herramientas de Educación Convivencial en el Siglo XXI." Espacio, Tiempo y Educación 9, no. 1 (2022): 6–26. http://dx.doi.org/10.14516/ete.492.

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Ivan Illich famously coined the term «tools for conviviality» in which he refers to tools that encourage individual creativity and expression, and that can be adapted to people’s needs and situations. This paper describes the design of an interactive adaptable tool, whose applications include education and game play, and contextualizes it within Illich’s framework. The Collaborative Interactive Tabletop for Education (CITE), currently being developed at SUNY Polytechnic, allows users to manipulate digital information through the manipulation of hand-held tabletop objects. Such interfaces, know
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Hoang-Minh, Thao, Jörn Kasbohm, Lan Nguyen-Thanh, et al. "Use of TEM-EDX for structural formula identification of clay minerals: a case study of Di Linh bentonite, Vietnam." Journal of Applied Crystallography 52, no. 1 (2019): 133–47. http://dx.doi.org/10.1107/s1600576718018162.

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Transmission electron microscopy linked with energy-dispersive X-ray spectroscopy (TEM-EDX) was applied to characterize mineralogical signals of weathering processes in the Di Linh bentonite deposit (Vietnam) and to visualize the effects of Na activation on the smectitic phases. Modelling of X-ray diffraction patterns (oriented mount) was applied in order to refine the computed structural formula. X-ray diffraction, X-ray fluorescence and Fourier-transform infrared spectroscopy (FT-IR) methods were also applied to verify the TEM-EDX results. An Excel-based routine has been developed in this re
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Wu, S., E. Jones, J. Gulley, et al. "Routine interval computed tomography in detecting new soft tissue disease in patients with androgen-independent prostate cancer (AIPC) and only bone metastasis." Journal of Clinical Oncology 24, no. 18_suppl (2006): 4621. http://dx.doi.org/10.1200/jco.2006.24.18_suppl.4621.

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4621 Background: Bone is the most common metastatic site in AIPC and the only site of metastasis for many patients. However, some pts with only bone metastasis will eventually develop soft tissue disease. Thus many clinical trials include CT monitoring to exclude new soft tissue disease as the only manifestation of disease progression. The true incidence of the asymptomatic development of soft tissue metastases without PSA or bone scan progression is unknown. Here we have identified pts with bone metastasis only at the time of protocol enrollment. We analyzed their disease progression pattern
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Martín, Domingo, Patricia Aparicio, Susana García, and María Mercedes Maroto-Valer. "Mixed-Layer Illite-Smectite Illitization under Supercritical CO2 Conditions." Applied Sciences 12, no. 22 (2022): 11477. http://dx.doi.org/10.3390/app122211477.

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The long-term safe storage of CO2 in geological reservoirs requires the understanding of the impact of CO2 on clay-rich sealing cap rocks. The reactivity of the mixed layer of illite-smectite was investigated to determine the reaction pathways under conditions of supercritical CO2 (scCO2) conditions in the context of geological CO2 storage. A common clay (blue marl from the Guadalquivir Tertiary basin, southern Spain) was tested under brine scCO2 conditions (100 bar and 35 °C) for 120 and 240 h. The clay sample (blue marl) contains calcite, quartz, illite, smectite, and the corresponding mixed
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Zhang, Luchuan, Shu Jiang, Dianshi Xiao, et al. "Controls on Pore Structures and Permeability of Tight Gas Reservoirs in the Xujiaweizi Rift, Northern Songliao Basin." Energies 13, no. 19 (2020): 5184. http://dx.doi.org/10.3390/en13195184.

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As significant components of tight gas reservoirs, clay minerals with ultrafine dimensions play a crucial role in controlling pore structures and permeability. XRD (X-ray diffraction), SEM (scanning electron microscopy), N2GA (nitrogen gas adsorption), and RMIP (rate-controlled mercury injection porosimetry) experiments were executed to uncover the effects of clay minerals on pore structures and the permeability of tight gas reservoirs, taking tight rock samples collected from the Lower Cretaceous Dengloukou and Shahezi Formations in the Xujiaweizi Rift of the northern Songliao Basin as an exa
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31

Pasero, Robert, and Paul Sabatier. "Linguistic Games for Language Learning: A Special Use of the ILLICO Library." Computer Assisted Language Learning 11, no. 5 (1998): 561–85. http://dx.doi.org/10.1076/call.11.5.561.5663.

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Lonardelli, Ivan, Hans-Rudolf Wenk, and Y. Ren. "Preferred orientation and elastic anisotropy in shales." GEOPHYSICS 72, no. 2 (2007): D33—D40. http://dx.doi.org/10.1190/1.2435966.

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Anisotropy in shales is becoming an important issue in exploration and reservoir geophysics. In this study, the crystallographic preferred orientation of clay platelets that contributes to elastic anisotropy was determined quantitatively by hard monochromatic X-ray synchrotron diffraction in two different shales from drillholes off the coast of Nigeria. To analyze complicated diffraction images with five different phases (illite/smectite, kaolinite, quartz, siderite, feldspar) and many overlapping peaks, we applied a methodology based on the crystallographic Rietveld method. The goal was to de
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33

Alves, Artur Matos. "Jacques Ellul’s “Anti-Democratic Economy:” Persuading Citizens and Consumers in the Information Society." tripleC: Communication, Capitalism & Critique. Open Access Journal for a Global Sustainable Information Society 12, no. 1 (2014): 169–201. http://dx.doi.org/10.31269/triplec.v12i1.465.

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Jacques Ellul's thoughts on the increasingly conspicuous role of persuasion techniques bring to the fore the persuasive and normative effects of new communication techniques at the core of contemporary consumer/citizen culture, as well as the limits of that instrumental stance towards mediated human communication. By drawing insights from authors who shared some of Ellul's concerns, such as Frankfurt School theorists, Vance Packard and Ivan Illich, this paper explores this “normative invasion” of human life by technique as a feature of contemporary information technology politics, specifically
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Alves, Artur Matos. "Jacques Ellul’s “Anti-Democratic Economy:” Persuading Citizens and Consumers in the Information Society." tripleC: Communication, Capitalism & Critique. Open Access Journal for a Global Sustainable Information Society 12, no. 1 (2014): 169–201. http://dx.doi.org/10.31269/vol12iss1pp169-201.

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Jacques Ellul's thoughts on the increasingly conspicuous role of persuasion techniques bring to the fore the persuasive and normative effects of new communication techniques at the core of contemporary consumer/citizen culture, as well as the limits of that instrumental stance towards mediated human communication. By drawing insights from authors who shared some of Ellul's concerns, such as Frankfurt School theorists, Vance Packard and Ivan Illich, this paper explores this “normative invasion” of human life by technique as a feature of contemporary information technology politics, specifically
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35

Drits, V. A., L. G. Dainyak, F. Muller, G. Besson, and A. Manceau. "Isomorphous cation distribution in celadonites, glauconites and Fe-illites determined by infrared, Mössbauer and EXAFS spectroscopies." Clay Minerals 32, no. 2 (1997): 153–79. http://dx.doi.org/10.1180/claymin.1997.032.2.01.

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AbstractCeladonite, glauconite and Fe-illite samples were studied by XRD, EXAFS, IR and Mössbauer spectroscopy. The samples were monomineralic and corresponded to 1M polytype. In the OH-stretching region of the IR spectra the content of each definite pair of cations bonded to OH groups was determined. The number of heavy (Fe) and light (Al, Mg) octahedral cations nearest to Fe was found by the EXAFS technique. The predicted quadrupole splitting values for each definite arrangement of cations nearest to Fe3+ were used to interpret the Mössbauer spectra. After the fitting procedure, the intensit
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Warren, E. A., and B. Ransom. "The Influence of analytical error upon the interpretation of chemical variations in clay minerals." Clay Minerals 27, no. 2 (1992): 193–209. http://dx.doi.org/10.1180/claymin.1992.027.2.05.

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AbstractUnderstanding the chemical variability of clay minerals depends on the analytical reliability of the techniques used. Uncertainties in clay mineral compositions were computed for common sources of analytical error such as those that arise from contaminant phases present in clay size-fractions in concentrations below the detection limit of routine XRD screening techniques, and the analytical limits of precision for TEM/AEM analysis. When plotted on standard diagrams used to represent clay mineral compositions, the calculated error envelopes were found to be of significant size, such tha
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Birk, Dieter. "Quantitative coal mineralogy of the Sydney Coalfield, Nova Scotia, Canada, by scanning electron microscopy, computerized image analysis, and energy-dispersive X-ray spectrometry." Canadian Journal of Earth Sciences 27, no. 2 (1990): 163–79. http://dx.doi.org/10.1139/e90-017.

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Automated image and X-ray analysis, with a scanning electron microscope, has been used to "fingerprint" mineral particles in bituminous coals of the Sydney Coalfield and catalogue their chemical class and size distribution. Four seams (Hub, Harbour, Phalen, and Gardiner) were analyzed quantitatively for some 32 000 mineral particles; these analyses revealed particle-size and weight distributions for 27 chemical classes. Manual searches augmented the computer-automated scans, covering eight seams and recording a total of 35 mineral species, their paragenesis, and sites for 28 elements.Sydney se
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38

Igelmo Zaldívar, Jon, and Patricia Quiroga Uceda. "“Las palabras son también hechos”: Quentin Skinner, el giro contextual y la Teoría de la Educación." Education in the Knowledge Society (EKS) 15, no. 4 (2015): 184–211. http://dx.doi.org/10.14201/eks.12351.

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Este artículo aborda la posibilidad de aplicar en la Teoría de la Educación el método para el estudio de las ideas de fundamento analítico propuesto por Quentin Skinner. La metodología del giro contextual es presentada como una herramienta hermenéutica apropiada para el esclarecimiento de las ideas desarrolladas por autores relevantes para el pensamiento educativo. Tomamos como referencia que profesar la Teoría de la Educación conlleva conocer para hacer; sin descartar la posibilidad de que conocer sea una forma de hacer. El objetivo que nos proponemos es incorporar un método riguroso para el
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Carcione, José M. "A model for seismic velocity and attenuation in petroleum source rocks." GEOPHYSICS 65, no. 4 (2000): 1080–92. http://dx.doi.org/10.1190/1.1444801.

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Petroleum source rock is modeled as a viscoelastic transversely isotropic medium composed of illite/smectite and organic matter. The wave velocities and attenuation of petroleum source rocks are obtained as a function of excess pore pressure, initial kerogen content, and water saturation. The model generalizes a previous approach based on a pure elastic formulation of Backus averaging and introduces the pressure effect and the presence of fluids (oil and water). The model allows the simulation of different maturation levels induced by pore‐pressure changes caused by the conversion of kerogen t
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Lu, Cheng, Yuxuan Xia, Xuwen Qin, et al. "Micro- and Nanoscale Pore Structure Characterization and Mineral Composition Analysis of Clayey-Silt Hydrate Reservoir in South China Sea." Geofluids 2022 (November 17, 2022): 1–10. http://dx.doi.org/10.1155/2022/2837193.

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Natural gas hydrate is a kind of environmentally friendly unconventional energy with large reserves, which attract increasing attention in recent years. The microscopic pore structure and mineral composition of natural gas hydrate reservoir have a great influence on its seepage characteristics during exploitation. In this study, computed tomography and scanning electron microscope are used to obtain digital images of three clayey-silt natural gas hydrate reservoir samples in the Shenhu area of South China Sea, and then, the pore structure and the mineral composition of the samples are obtained
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Pearce, Julie K., Grant K. W. Dawson, Silvano Sommacal, and Suzanne D. Golding. "Micro CT and Experimental Study of Carbonate Precipitation from CO2 and Produced Water Co-Injection into Sandstone." Energies 14, no. 21 (2021): 6998. http://dx.doi.org/10.3390/en14216998.

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Carbon dioxide geological storage involves injecting captured CO2 streams into a suitable reservoir. Subsequent mineral trapping of the CO2 as carbonate minerals is one of the most secure forms of trapping. Injection of CO2 dissolved in water or co-injection of CO2 with water may enhance trapping mechanisms. Produced waters are already re-injected into reservoirs worldwide, and their co-injection with CO2 could enhance mineral trapping in low reactivity rock by providing a source of cations. Sandstone drill core from a reservoir proposed for CO2 storage was experimentally reacted with supercri
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Kim, Sung-Man, In-Ho Yoon, Ilgook Kim, June-Hyun Kim, and So-Jin Park. "Hydrothermal Desorption of Cs with Oxalic Acid from Hydrobiotite and Wastewater Treatment by Chemical Precipitation." Energies 13, no. 12 (2020): 3284. http://dx.doi.org/10.3390/en13123284.

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A hydrobiotite (HBT) clay contains more cesium (Cs)-specific adsorption sites than illitic clay, and the capacity of frayed edge sites can increase as the weathering of micaceous minerals proceeds. Thus, Cs can be selectively adsorbed to HBT clay. In this study, we investigated the removal efficiency of non-radioactive (133Cs) and radioactive (137Cs) Cs from HBT, using oxalic acid. We found the minimum optimal concentration of 0.15 M oxalic acid removed more than 90% of Cs. Subsequently, cations and Cs ions were removed using Ca(OH)2 and sodium tetraphenylborate (NaTPB) to treat the washing wa
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Wang, Yong, Yunqian Long, Yeheng Sun, Shiming Zhang, Fuquan Song, and Xiaohong Wang. "Threshold Pore Pressure Gradients in Water-Bearing Tight Sandstone Gas Reservoirs." Energies 12, no. 23 (2019): 4578. http://dx.doi.org/10.3390/en12234578.

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Tight gas reservoirs commonly occur in clastic formations having a complex pore structure and a high water saturation, which results in a threshold pressure gradient (TPG) for gas seepage. The micropore characteristics of a tight sandstone gas reservoir (Tuha oilfield, Xinjiang, China) were studied, based on X-ray diffraction, scanning electron microscopy and high pressure mercury testing. The TPG of gas in cores of the tight gas reservoir was investigated under various water saturation conditions, paying special attention to core permeability and water saturation impact on the TPG. A mathemat
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VOLDMAN, GUSTAVO G., GUILLERMO L. ALBANESI, and MARGARITA DO CAMPO. "Conodont palaeothermometry of contact metamorphism in Middle Ordovician rocks from the Precordillera of western Argentina." Geological Magazine 145, no. 4 (2008): 449–62. http://dx.doi.org/10.1017/s001675680800455x.

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AbstractThe Yerba Loca Formation (Middle–Upper Ordovician), exposed in the Western Precordillera, San Juan, Argentina, is made up of clastic–carbonate turbidites, and basic–ultrabasic rocks. It is affected by regional Siluro-Devonian very low-grade metamorphism that locally reaches greenschist facies. At Ancaucha creek, 45 conodont samples were taken from two sections that include 30 to 50 m thick sills. In order to analyse the thermal alteration patterns produced by these intrusive bodies, conodont Colour Alteration Index (CAI) is contrasted with optical petrography and X-ray diffraction anal
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Tall, Andrej, Branislav Kandra, Milan Gomboš, and Dana Pavelková. "The influence of soil texture on the course of volume changes of soil." Soil and Water Research 14, No. 2 (2019): 57–66. http://dx.doi.org/10.17221/217/2017-swr.

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Volume changes of soil associated with soil moisture changes are caused by the presence of clay minerals from illite and montmorillonite groups. Clay minerals are found in the so-called clay soil component which can be quantified by laboratory analysis of the soil particle-size distribution. Consequently, the potential for volume changes in soil can be assessed from soil texture. In our study, 172 soil samples with different textures were used to measure dependencies between volume changes in soil and changes in soil moisture under laboratory conditions. The samples were collected from 11 site
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Ji, Qin, Lijun Zhou, and Hisham Nasr-El-Din. "Acidizing Sandstone Reservoirs With Aluminum-Based Retarded Mud Acid." SPE Journal 21, no. 03 (2016): 1050–60. http://dx.doi.org/10.2118/169395-pa.

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Summary Aluminum chloride (AlCl3) has been used as a retarding agent for mud acid for a long time; its applications are studied in the laboratory and tested in the field. The theory and mechanism of AlCl3 retardation were investigated in many works involving mud acidizing and reservoir-permeability enhancement. This paper furthers this investigation with solubility tests, coreflood tests, and 19F nuclear magnetic resonance (NMR) to better understand the mechanism of AlCl3 working as a retarding agent in mud acid. The reactivity of Al-based retarded mud acid (15 wt% HCl, 1.5 wt% HF, and 5 wt% A
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Salehi, M., and A. Salem. "Effect of moisture content on extrusion process of kaolinitic–illitic clay in manufacturing of ceramic Raschig ring." Journal of Materials Processing Technology 200, no. 1-3 (2008): 232–37. http://dx.doi.org/10.1016/j.jmatprotec.2007.09.013.

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Nekhlaoui, Souad, Hind Abdelaoui, Marya Raji, et al. "Assessment of thermo-mechanical, dye discoloration, and hygroscopic behavior of hybrid composites based on polypropylene/clay (illite)/TiO2." International Journal of Advanced Manufacturing Technology 113, no. 9-10 (2021): 2615–28. http://dx.doi.org/10.1007/s00170-021-06765-5.

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Carcione, José M. "AVO effects of a hydrocarbon source‐rock layer." GEOPHYSICS 66, no. 2 (2001): 419–27. http://dx.doi.org/10.1190/1.1444933.

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The organic content of petroleum source‐rock layers can be determined from seismic data with a suitable AVO technique. Since the source rock has a layered structure, the best forward model is a transversely isotropic layer between two isotropic half‐spaces, parameterized by the layer thickness and the amount of organic material. This limited number of parameters is essential to obtain a robust inversion method. Here, I compute the PP- and PS-reflection coefficients of the source bed as a function of layer thickness and organic content, including attenuation mechanisms related to different stag
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Zar, Aung Tay, I. Wayan Warmada, Lucas Donny Setijadji, and Koichiro Watanabe. "ALTERATION, VEIN TEXTURES AND FLUID INCLUSION PETROGRAPHY OF METAMORPHIC ROCK-HOSTED GOLD DEPOSIT AT ONZONKANBANI AREA, CENTRAL MYANMAR: IMPLICATION FOR ITS GENESIS." ASEAN Engineering Journal 8, no. 2 (2018): 48–63. http://dx.doi.org/10.11113/aej.v8.15502.

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Gold and base metal mineralization of Onzon-Kabani area is located at the western part of Mogok Metamorphic Belt in central Myanmar, where the well-known Sagaing Fault serves as its western boundary. Artisanal and small-scale gold operations started here three decades ago on gold mineralization hosted in marble and gneiss. Mineralization occurs as fracture-filling veins of several types: gold-bearing quartz vein, base metal quartz-carbonate vein, and carbonate base metal sulfides vein. Three types of hydrothermal alteration zones develop from the proximal to distal zone of hydrothermal conduit
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