Littérature scientifique sur le sujet « Silicates »
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Articles de revues sur le sujet "Silicates"
Wooden, Diane H. « Cometary Silicates : Interstellar and Nebular Materials ». Highlights of Astronomy 13 (2005) : 495–97. http://dx.doi.org/10.1017/s1539299600016403.
Texte intégralNiciu, H., Dorel Radu, C. Onose, A. Ioncea, Daniela Niciu, H. Stroescu et C. S. Onose. « The Permanently Bonded Glass Decor from Chemical Precursors ». Advanced Materials Research 39-40 (avril 2008) : 579–82. http://dx.doi.org/10.4028/www.scientific.net/amr.39-40.579.
Texte intégralHeckmann, W., F. Ramsteiner et Ch Mehler. « Morphology of Poly Amide Nanocomposites Characterized by Transmission Electron Microscopy (TEM) and Electron Spectroscopic Imaging (ESI). » Microscopy and Microanalysis 7, S2 (août 2001) : 502–3. http://dx.doi.org/10.1017/s1431927600028580.
Texte intégralMolster, F. J. « Astromineralogy : Crystalline silicates ». Symposium - International Astronomical Union 209 (2003) : 291–98. http://dx.doi.org/10.1017/s0074180900208796.
Texte intégralKemmitt, T., et NB Milestone. « The Ring Size Influence on 29Si N.M.R. Chemical Shifts of Some Spirocyclic Tetra- and Penta-coordinate Diolato Silicates ». Australian Journal of Chemistry 48, no 1 (1995) : 93. http://dx.doi.org/10.1071/ch9950093.
Texte intégralLii, Kwang-Hwa. « High-T, High-P Hydrothermal Synthesis of Uranium Silicates and Germanates ». Acta Crystallographica Section A Foundations and Advances 70, a1 (5 août 2014) : C759. http://dx.doi.org/10.1107/s2053273314092407.
Texte intégralLiang, Jian-Jie, Alexandra Navrotsky, Thomas Ludwig, Hans J. Seifert et Fritz Aldinger. « Enthalpy of Formation of Rare-earth Silicates Y2SiO5 and Yb2SiO5 and N-containing Silicate Y10(SiO4)6N2 ». Journal of Materials Research 14, no 4 (avril 1999) : 1181–85. http://dx.doi.org/10.1557/jmr.1999.0158.
Texte intégralP. C. Bennett, J. R. Rogers, W. J. « Silicates, Silicate Weathering, and Microbial Ecology ». Geomicrobiology Journal 18, no 1 (janvier 2001) : 3–19. http://dx.doi.org/10.1080/01490450151079734.
Texte intégralIliushchenko, V., L. Kalina, P. Hruby, V. Bilek Jr, J. Fladr, P. Bily et J. Bojanovsky. « The treatment of cementitious surface by selected silicate sealers ». Journal of Physics : Conference Series 2341, no 1 (1 septembre 2022) : 012003. http://dx.doi.org/10.1088/1742-6596/2341/1/012003.
Texte intégralJakobsen, U. H. « A hydrated barium silicate in unmetamorphosed sedimentary rocks of central North Greenland ». Mineralogical Magazine 54, no 374 (mars 1990) : 81–89. http://dx.doi.org/10.1180/minmag.1990.054.374.08.
Texte intégralThèses sur le sujet "Silicates"
Villanova, de Benavent Cristina. « Compositional and structural characterisation of Ni-phyllosilicates in hydrous silicate type Ni-laterite deposits ». Doctoral thesis, Universitat de Barcelona, 2015. http://hdl.handle.net/10803/396616.
Texte intégralEls fil- losilicats de níquel (comunament anomenats "garnierites") són importants menes en molts jaciments laterítics de Ni del món. La seva caracterització, classificació i nomenclatura és complexa, ja que normalment es troben en forma de mescles íntimes de diferents fil- losilicats de gra molt fi i baixa cristal• linitat. L'objectiu d' aquesta tesi és avançar en el coneixement de la mineralogia dels fil- losilicats de Ni del dipòsit de laterites niquelíferes de Falcondo, a la República Dominicana, per mitjà de l'ús d'un ampli espectre de tècniques analítiques: difracció de pols de raig X, anàlisi tèrmica diferencial i termogravimetria, microscòpia òptica, microscòpia electrònica de rastreig, microsonda electrònica, microscòpia electrònica de transmissió, espectroscòpia Raman, espectroscòpia d' absorció de raigs X (EXAFS i XANES, amb radiació sincrotró) i per mitjà d'experiments de dissolució. Les garnierites de Falcondo es localitzen a la part baixa de l'horitzó saprolftic en forma de rebliment de fractures i vetes, i ciments i clasts en bretxes. Els principals resultats indiquen que hi ha cinc tipus de garnierites, segons el seu color, la seva mineralogia i la química mineral. La majoria són barreges de serpentina i talc hidratat (kerolita-pimelita), tot i que també hi ha fases de la sèrie sepiolita-falcondoita. La fase que concentra més Ni és la kerolita-pimelita, mentre que a la serpentina el Ni és sistemàticament molt baix i a la sepiolita-falcondoita és molt variable. Les imatges d' alta resolució obtingudes amb microscopi electrònic de transmissió indiquen que els fil- losilicats que componen les garnierites formen una gran varietat de textures: serpentina poligonal, tubs de crisòtil, lamel• les de lizardita, lamel• les de talc hidratat i cintes de sepiolita. A més, s'ha observat que la kerolita-pimelita (rica en Ni) reemplaça sistemàticament la serpentina (pobra en Ni). L'espectroscòpia Raman permet distingir els cinc tipus descrits de garnierites i per tant, s'ofereix com una tècnica ràpida, senzilla i no destructiva per analitzar aquest tipus de minerals al camp. L' absorció de raigs X per mitjà de radiació sincrotró ha permès identificar que tot el Fe contingut en les garnierites i en les serpentines de la saprolita està en forma de Fe3+, i que tot el Ni es troba acumulat formant clusters, i no pas en forma de solució sòlida homogènia, a la capa octaèdrica. Finalment, els experiments de dissolució suggereixen que les velocitats de dissolució són més ràpides en les garnierites que contenen molta serpentina, i que la dissolució no és congruent, sent el Mg el primer element en ser posat en solució, seguit del Si i del Ni.
Rogers, Jennifer Roberts. « Nutrient-driven colonization and weathering of silicates / ». Full text (PDF) from UMI/Dissertation Abstracts International, 2000. http://wwwlib.umi.com/cr/utexas/fullcit?p3004368.
Texte intégralClaireaux, Corinne. « Mobilité atomique dans les silicates vitreux et fondus ». Thesis, Paris 6, 2014. http://www.theses.fr/2014PA066401/document.
Texte intégralThis manuscript deals with the coupled diffusion in an industrial glass system containing four oxides (SiO2, Al2O3, CaO, Na2O). The temperature range extends from the glass transition temperature (650°C) to the liquidus (1200°C). The first results concern the macroscopic nature of diffusion. The matrix containing the diffusion coefficients quantifies the mobility of the components and highlights many interactions between them. Other information can be obtained at the microscopic scale. The exchange equations summarize the main diffusion paths followed by the system in reactions form. All the data from the literature are processed and they seem to converge towards preferential diffusion paths. Hypothesis about the mechanisms of diffusion of the species are proposed. The results obtained at low temperatures open a discussion of the relationship between transport properties and diffusion. The study of the structure of the material was based on Raman spectroscopy. Diffusion experiments provide a large number of glass compositions, which allowed us to develop a statistical tool for handling spectra. The spectral components thus obtained are discussed in the light of the many observations described in the literature. This approach allowed us to interpret the components through correlations between their relative intensities and the composition of the material and by studying their evolution along the diffusion profiles. The possibility of a Raman spectroscopy technique for quantifying species is discussed
Claireaux, Corinne. « Mobilité atomique dans les silicates vitreux et fondus ». Electronic Thesis or Diss., Paris 6, 2014. http://www.theses.fr/2014PA066401.
Texte intégralThis manuscript deals with the coupled diffusion in an industrial glass system containing four oxides (SiO2, Al2O3, CaO, Na2O). The temperature range extends from the glass transition temperature (650°C) to the liquidus (1200°C). The first results concern the macroscopic nature of diffusion. The matrix containing the diffusion coefficients quantifies the mobility of the components and highlights many interactions between them. Other information can be obtained at the microscopic scale. The exchange equations summarize the main diffusion paths followed by the system in reactions form. All the data from the literature are processed and they seem to converge towards preferential diffusion paths. Hypothesis about the mechanisms of diffusion of the species are proposed. The results obtained at low temperatures open a discussion of the relationship between transport properties and diffusion. The study of the structure of the material was based on Raman spectroscopy. Diffusion experiments provide a large number of glass compositions, which allowed us to develop a statistical tool for handling spectra. The spectral components thus obtained are discussed in the light of the many observations described in the literature. This approach allowed us to interpret the components through correlations between their relative intensities and the composition of the material and by studying their evolution along the diffusion profiles. The possibility of a Raman spectroscopy technique for quantifying species is discussed
Azenha, Marcelo Rodrigues [UNESP]. « Reparação óssea em alvéolos de ratas ovarectomizadas após implante com biovidro : análise histomorfométrica e imunoistoquímica ». Universidade Estadual Paulista (UNESP), 2013. http://hdl.handle.net/11449/123378.
Texte intégralObjetivos: Avaliar o processo de reparo alveolar em ratas ovarectomizadas após implante com Biosilicato cristalino. Materiais e Métodos: Sessenta ratas foram divididas em quatro grupos (n = 15) de acordo com o tratamento: Grupo 1- ratas submetidas à cirurgia sham com alvéolos preenchidos com coágulo; Grupo 2-ratas submetidas à cirurgia sham com alvéolos preenchidos com Biosilicato cristalino; Grupo 3-ratas ovarectomizadas com alvéolos preenchidos com coágulo; e Grupo 4- ratas ovarectomizadas com alvéolos preenchidos com Biosilicato cristalino. Após 7, 14 e 28 dias os animais foram sacrificados e análises histomorfométricas (histologia e histometria) e imunoistoquímicas (Osteopontina e Osteocalcina) foram realizadas. A comparação dos resultados foi realizada utilizando o programa estatístico Assistat 2013 para Windows através da Análise de Variância e teste de Mann-Whitney, com resultados significantes sendo encontrados quando p≤0.05. Resultados: No período de 7 dias, os Grupos 1 e 3 apresentaram resultados superiores e estatisticamente maiores do que os Grupos 2 e 4 (p<0.05) quanto à formação óssea. Após o período de 14 dias as diferenças estatísticas mantiveram-se, com os Grupos 1 e 3 apresentando diferença estatisticamente significante maiores aos Grupos 2 e 4 (p<0.05). Aos 28 dias, a diferença estatística significativa permaneceu entre os mesmo Grupos estudados, sendo que nos grupos implantados com o Biosilicato cerca de 60% do alvéolo já havia sido preenchido por osso novo. A imunoistoquímica revelou expressão das proteínas Osteocalcina e Osteopontina, principalmente nos animais submetidos à cirurgia de ovarectomia. Conclusões: Os Grupos 1 e 3 foram os que apresentaram os melhores resultados durante todo o estudo, com o Biosilicato cristalino apresentando resultado favorável na reparação...
Objectives: To evaluate the process of alveolar repair in ovariectomized rats after implantation with Biosilicate. Materials and Methods: Sixty rats were divided into four groups (n = 15) according to treatment: Group 1 - rats underwent sham surgery with alveoli filled with blood clot; Group 2 - rats underwent sham surgery with alveoli filled with crystalline Biosilicate; Group 3 - ovariectomized rats with alveoli filled with blood clot; Group 4 - ovariectomized rats with alveoli filled with crystalline Biosilicate. After 7, 14 and 28 days the animals were sacrificed and histomorphometric analysis (histology and histometric) and immunohistochemical (Osteopontin and Osteocalcin) were measured . The comparison of the results was performed using the statistical program Assistat 2013 for Windows by Analysis of Variance and Mann-Whitney tests, with significant results being found when p ≤ 0:05 . Results: During the 7- day period, Groups 1 and 3 showed better and significantly higher results in bone formation than Groups 2 and 4 (p<0.05). After 14 days the statistical differences remained between Groups 1 and 3 and Groups 2 and 4 (p<0,05). At 28 days, the statically difference remained significant between the same Groups, while the groups implanted with Biosilicate presented about 60% of the socket filled by new bone. Immunohistochemistry revealed expression of proteins osteocalcin and osteopontin, especially in animals subjected to ovariectomy surgery. Conclusions: Groups 1 and 3 were those with the best results throughout the study, with the crystalline Biosilicate presenting favorable result in bone repair without bioglass resorption. The immunohistochemical analysis showed that animals subjected to ovariectomy had a higher signaling in Ostecalcina and Osteopontin proteins
Azenha, Marcelo Rodrigues. « Reparação óssea em alvéolos de ratas ovarectomizadas após implante com biovidro : análise histomorfométrica e imunoistoquímica / ». Araçatuba, 2013. http://hdl.handle.net/11449/123378.
Texte intégralBanca: Celso Kooji Sonoda
Banca: Sonia Regina Panzarini Barioni
Banca: Luiz Guilherme Brentegani
Banca: Osny Ferreira Júnior
Resumo: Objetivos: Avaliar o processo de reparo alveolar em ratas ovarectomizadas após implante com Biosilicato cristalino. Materiais e Métodos: Sessenta ratas foram divididas em quatro grupos (n = 15) de acordo com o tratamento: Grupo 1- ratas submetidas à cirurgia sham com alvéolos preenchidos com coágulo; Grupo 2-ratas submetidas à cirurgia sham com alvéolos preenchidos com Biosilicato cristalino; Grupo 3-ratas ovarectomizadas com alvéolos preenchidos com coágulo; e Grupo 4- ratas ovarectomizadas com alvéolos preenchidos com Biosilicato cristalino. Após 7, 14 e 28 dias os animais foram sacrificados e análises histomorfométricas (histologia e histometria) e imunoistoquímicas (Osteopontina e Osteocalcina) foram realizadas. A comparação dos resultados foi realizada utilizando o programa estatístico Assistat 2013 para Windows através da Análise de Variância e teste de Mann-Whitney, com resultados significantes sendo encontrados quando p≤0.05. Resultados: No período de 7 dias, os Grupos 1 e 3 apresentaram resultados superiores e estatisticamente maiores do que os Grupos 2 e 4 (p<0.05) quanto à formação óssea. Após o período de 14 dias as diferenças estatísticas mantiveram-se, com os Grupos 1 e 3 apresentando diferença estatisticamente significante maiores aos Grupos 2 e 4 (p<0.05). Aos 28 dias, a diferença estatística significativa permaneceu entre os mesmo Grupos estudados, sendo que nos grupos implantados com o Biosilicato cerca de 60% do alvéolo já havia sido preenchido por osso novo. A imunoistoquímica revelou expressão das proteínas Osteocalcina e Osteopontina, principalmente nos animais submetidos à cirurgia de ovarectomia. Conclusões: Os Grupos 1 e 3 foram os que apresentaram os melhores resultados durante todo o estudo, com o Biosilicato cristalino apresentando resultado favorável na reparação...
Abstract: Objectives: To evaluate the process of alveolar repair in ovariectomized rats after implantation with Biosilicate. Materials and Methods: Sixty rats were divided into four groups (n = 15) according to treatment: Group 1 - rats underwent sham surgery with alveoli filled with blood clot; Group 2 - rats underwent sham surgery with alveoli filled with crystalline Biosilicate; Group 3 - ovariectomized rats with alveoli filled with blood clot; Group 4 - ovariectomized rats with alveoli filled with crystalline Biosilicate. After 7, 14 and 28 days the animals were sacrificed and histomorphometric analysis (histology and histometric) and immunohistochemical (Osteopontin and Osteocalcin) were measured . The comparison of the results was performed using the statistical program Assistat 2013 for Windows by Analysis of Variance and Mann-Whitney tests, with significant results being found when p ≤ 0:05 . Results: During the 7- day period, Groups 1 and 3 showed better and significantly higher results in bone formation than Groups 2 and 4 (p<0.05). After 14 days the statistical differences remained between Groups 1 and 3 and Groups 2 and 4 (p<0,05). At 28 days, the statically difference remained significant between the same Groups, while the groups implanted with Biosilicate presented about 60% of the socket filled by new bone. Immunohistochemistry revealed expression of proteins osteocalcin and osteopontin, especially in animals subjected to ovariectomy surgery. Conclusions: Groups 1 and 3 were those with the best results throughout the study, with the crystalline Biosilicate presenting favorable result in bone repair without bioglass resorption. The immunohistochemical analysis showed that animals subjected to ovariectomy had a higher signaling in Ostecalcina and Osteopontin proteins
Doutor
Boulliung, Julien. « Solubilité, spéciation et diffusion de l'azote dans les verres et silicates fondus ». Electronic Thesis or Diss., Université de Lorraine, 2020. http://www.theses.fr/2020LORR0254.
Texte intégralNitrogen (N) belongs to the volatile elements (like hydrogen and carbon) that are essential for life on Earth. The behavior of N during high temperature geological processes, such as during magmatic processes, remains poorly understood. This study focuses on N solubility, speciation, and diffusion in silicate glasses and melts to better understand the N behavior during these processes. N solubility in silicate melts was studied for different melt compositions and for a wide range of fO₂ (IW –8 to IW +4.1) at 1425°C and 1 atm. The data obtained highlight the fundamental control of fO₂ and the degree of polymerization of the silicate melt on N solubility. These new data suggest that a mafic to ultra-mafic magma ocean could have incorporated a similar or higher amount of N compared to the actual bulk silicate Earth, suggesting that N may have been to the atmosphere and/or stored in Earth's deep interior (i.e., deep mantle, core). For the study of N diffusion in silicate glasses and melts, experimental and analytical developments were necessary. The first diffusion coefficient of N (as N³⁻) in silicate melts was determined from uni-axial diffusion experiments in a basaltic andesitic melt (4.2 × 10⁻⁸ cm².s⁻¹). The data highlight that N³⁻ diffusivity depends on melt composition. This dependence on the melt composition is more important than that of argon (Ar). Furthermore, N³⁻ diffusion is significantly slower than that of Ar in similar silicate melts, implying that N/Ar ratios can be fractionated during reducing magmatic processes (e.g., during Earth's magma ocean stage)
Hazm, Jamal Eddine. « Silicates et aluminosilicates microporeux obtenus en milieu fluoré avec, comme structurants, le 1,4-diazabicyclo [2,2,2] octane (DABCO) ou le 1-azabicyclo [2,2,2] octane (quinuclidine) ». Mulhouse, 1992. http://www.theses.fr/1992MULH0238.
Texte intégralBartelmehs, Kurt Lane. « Modeling the properties of silicates ». Diss., This resource online, 1993. http://scholar.lib.vt.edu/theses/available/etd-05042006-164529/.
Texte intégralMcCollam, Bridget E. « Thermochemistry of a synthetic Na-Mg rich triple-chain silicate determination of thermodynamic variables and geological applications / ». Diss., Online access via UMI:, 2007.
Trouver le texte intégralLivres sur le sujet "Silicates"
Griffen, Dana T. Silicate crystal chemistry. New York : Oxford University Press, 1992.
Trouver le texte intégralMysen, B. O. Structure and properties of silicate melts. Amsterdam : Elsevier, 1988.
Trouver le texte intégralBabushkin, V. I. Thermodynamics of silicates. Berlin : Springer-Verlag, 1985.
Trouver le texte intégralBabushkin, V. I., G. M. Matveyev et O. P. Mchedlov-Petrossyan. Thermodynamics of Silicates. Sous la direction de O. P. Mchedlov-Petrossyan. Berlin, Heidelberg : Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-69320-5.
Texte intégralWebb, Sharon L. Silicate melts : With 33 figures. Berlin : Springer, 1997.
Trouver le texte intégralPotts, P. J. A Handbook of silicate rock analysis. London : Blackie Academic & Professional, 1987.
Trouver le texte intégralTagiev, D. B. Kristallicheskie ali͡u︡mosilikaty v katalize. Baku : Ėlm, 1989.
Trouver le texte intégralPotts, P. J. A handbook of silicate rock analysis. Glasgow : Blackie, 1987.
Trouver le texte intégralL, Perchuk L., Kushiro I. 1934- et Baker Donald R. 1927-, dir. Physical chemistry of magmas. New York : Springer-Verlag, 1991.
Trouver le texte intégralFarwell, Stebbins Jonathan, McMillan Paul Francis 1955- et Dingwell D. B, dir. Structure, dynamics, and properties of silicate melts. Washington, D.C : Mineralogical Society of America, 1995.
Trouver le texte intégralChapitres de livres sur le sujet "Silicates"
Okrusch, Martin, et Hartwig E. Frimmel. « Silicates ». Dans Springer Textbooks in Earth Sciences, Geography and Environment, 157–239. Berlin, Heidelberg : Springer Berlin Heidelberg, 2020. http://dx.doi.org/10.1007/978-3-662-57316-7_11.
Texte intégralCastroviejo, Ricardo. « Silicates ». Dans A Practical Guide to Ore Microscopy—Volume 1, 819–44. Cham : Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-12654-3_135.
Texte intégralEdler, Karen J. « Mesoporous Silicates ». Dans Porous Materials, 69–145. Chichester, UK : John Wiley & Sons, Ltd, 2010. http://dx.doi.org/10.1002/9780470711385.ch2.
Texte intégralFalcone, J. S., et J. G. Blumberg. « Anthropogenic Silicates ». Dans Detergents, 367–82. Berlin, Heidelberg : Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-540-47108-0_14.
Texte intégralVerma, Pramod K. « Non-silicates ». Dans Optical Mineralogy, 337–60. Cham : Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-40765-9_16.
Texte intégralLiebau, Friedrich. « Nomenclature and Structural Formulae of Silicate Anions and Silicates ». Dans Structural Chemistry of Silicates, 69–75. Berlin, Heidelberg : Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-50076-3_5.
Texte intégralBabushkin, V. I., G. M. Matveyev et O. P. Mchedlov-Petrossyan. « The Basic Concepts and Laws of Thermodynamics ». Dans Thermodynamics of Silicates, 1–54. Berlin, Heidelberg : Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-69320-5_1.
Texte intégralBabushkin, V. I., G. M. Matveyev et O. P. Mchedlov-Petrossyan. « Pyrosilicate Reactions ». Dans Thermodynamics of Silicates, 55–249. Berlin, Heidelberg : Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-69320-5_2.
Texte intégralBabushkin, V. I., G. M. Matveyev et O. P. Mchedlov-Petrossyan. « Hydration Reactions ». Dans Thermodynamics of Silicates, 251–335. Berlin, Heidelberg : Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-69320-5_3.
Texte intégralBabushkin, V. I., G. M. Matveyev et O. P. Mchedlov-Petrossyan. « Corrosion Reactions ». Dans Thermodynamics of Silicates, 337–53. Berlin, Heidelberg : Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-69320-5_4.
Texte intégralActes de conférences sur le sujet "Silicates"
Neufuss, K., J. Ilavsky, J. Dubsky, B. Kolman et P. Chraska. « Plasma Spraying of Silicates II ». Dans ITSC 1999, sous la direction de E. Lugscheider et P. A. Kammer. Verlag für Schweißen und verwandte Verfahren DVS-Verlag GmbH, 1999. http://dx.doi.org/10.31399/asm.cp.itsc1999p0636.
Texte intégralChráska, P., K. Neufuss, B. Kolman et J. Dubsky. « Plasma Spraying of Silicates ». Dans ITSC 1997, sous la direction de C. C. Berndt. ASM International, 1997. http://dx.doi.org/10.31399/asm.cp.itsc1997p0477.
Texte intégralCtibor, P., J. Sedláček, K. Neufuss, J. Dubský et P. Chráska. « Study of Dielectric Properties of Plasma Sprayed Silicates at Low Voltage ». Dans ITSC2002, sous la direction de C. C. Berndt et E. Lugscheider. Verlag für Schweißen und verwandte Verfahren DVS-Verlag GmbH, 2002. http://dx.doi.org/10.31399/asm.cp.itsc2002p0617.
Texte intégralQuet, A., L. Bianchi, E. Darthout, F. Gitzhofer, J. L. Leluan et F. Rebillat. « Yttrium Silicate Coatings by Sol Precursor Plasma Spraying for Environmental Barrier Applications ». Dans ITSC2011, sous la direction de B. R. Marple, A. Agarwal, M. M. Hyland, Y. C. Lau, C. J. Li, R. S. Lima et A. McDonald. DVS Media GmbH, 2011. http://dx.doi.org/10.31399/asm.cp.itsc2011p0581.
Texte intégralLipinska-Kalita, Krystyna E., et Leonard M. Proniewicz. « FTIR Spectra Of Amorphous Silicates ». Dans Intl Conf on Fourier and Computerized Infrared Spectroscopy, sous la direction de David G. Cameron. SPIE, 1989. http://dx.doi.org/10.1117/12.969442.
Texte intégralRinehart, S., D. Benford, E. Dwek, R. Henry, J. Nuth, R. Silverberg et E. Wollack. « Optical properties of astronomical silicates ». Dans SPIE Astronomical Telescopes + Instrumentation, sous la direction de Ian S. McLean et Mark M. Casali. SPIE, 2008. http://dx.doi.org/10.1117/12.789712.
Texte intégralSitarz, M., W. Mozgawa et M. Handke. « Vibrational spectroscopy of ring silicates ». Dans The eleventh international conference on fourier transform spectroscopy. AIP, 1998. http://dx.doi.org/10.1063/1.55860.
Texte intégralTan, Bee Chea, Ismail Mohd Saaid, Siti Qurratu'Aini Mahat, Suzalina Zainal, Petrus Tri Bhaskoro et Astriyana Anuar. « Evaluation of Polyamidoamine-Assisted Scale Inhibitors to Mitigate Silicate Scale Formation in Near Wellbore Region ». Dans SPE/IATMI Asia Pacific Oil & Gas Conference and Exhibition. SPE, 2023. http://dx.doi.org/10.2118/215266-ms.
Texte intégralHuang, Tzu Hao. « Sequential extraction of biogenic, authigenic and lithogenic silicas and silicates from marine sediments ». Dans Goldschmidt2021. France : European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6062.
Texte intégralBauer, S., P. Gronewald, J. Hamilton, D. LaPlant et A. Mansure. « High-Temperature Plug Formation With Silicates ». Dans SPE International Symposium on Oilfield Chemistry. Society of Petroleum Engineers, 2005. http://dx.doi.org/10.2118/92339-ms.
Texte intégralRapports d'organisations sur le sujet "Silicates"
Shen, Andy Anda. Analyzing Silicates in Los Alamos’s Water Supply. Office of Scientific and Technical Information (OSTI), juillet 2019. http://dx.doi.org/10.2172/1557154.
Texte intégralWereszczak, Andrew A., Kathryn J. Ham, Yogesh K. Vohra, Georgiy Tsoi, Brian A. Oistad, Brett S. Kuwik, Emily F. Steiner, Osama Jadaan et Benjamin L. Hackett. High-Pressure Mechanical Response of Two Vitreous Silicates. Office of Scientific and Technical Information (OSTI), novembre 2018. http://dx.doi.org/10.2172/1482450.
Texte intégralMichael G. Nelson. CARBON DIOXIDE SEQUESTRATION BY MECHANOCHEMICAL CARBONATION OF MINERAL SILICATES. Office of Scientific and Technical Information (OSTI), avril 2004. http://dx.doi.org/10.2172/826304.
Texte intégralBelt, R. F., et J. A. Catalano. Investigation of Single Crystal Silicates for Blue Tunable Lasers. Fort Belvoir, VA : Defense Technical Information Center, juin 1986. http://dx.doi.org/10.21236/ada171823.
Texte intégralOJI, LN. Conditions Conducive to Forming Crystalline Uranyl Silicates in SRS Evaporators. Office of Scientific and Technical Information (OSTI), avril 2004. http://dx.doi.org/10.2172/823370.
Texte intégralWilliam B. White, Michael R. Silsbee et B. Joe Kearns. REACTION MECHANISMS OF MAGNESIUM SILICATES WITH CARBON DIOXIDE IN MICROWAVE FIELDS. Office of Scientific and Technical Information (OSTI), février 2004. http://dx.doi.org/10.2172/826203.
Texte intégralFripiat, J. J. Aluminum coordination and active sites on aluminas, Y zeolites and pillared silicates. Office of Scientific and Technical Information (OSTI), janvier 1992. http://dx.doi.org/10.2172/6923291.
Texte intégralSchneider, E. Applications of high resolution NMR to geochemistry : crystalline, glass, and molten silicates. Office of Scientific and Technical Information (OSTI), novembre 1985. http://dx.doi.org/10.2172/6246018.
Texte intégralOJI, LAWRENCE. Conditions Conducive to Forming Crystalline Uranyl Silicates in High Caustic Nuclear Waste Evaporators. Office of Scientific and Technical Information (OSTI), novembre 2004. http://dx.doi.org/10.2172/835626.
Texte intégralFripiat, J. J. Aluminum coordination and active sites on aluminas, Y zeolites and pillared layered silicates. Office of Scientific and Technical Information (OSTI), janvier 1991. http://dx.doi.org/10.2172/5874814.
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