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Artykuły w czasopismach na temat "Silicates"
Wooden, Diane H. "Cometary Silicates: Interstellar and Nebular Materials". Highlights of Astronomy 13 (2005): 495–97. http://dx.doi.org/10.1017/s1539299600016403.
Pełny tekst źródłaNiciu, H., Dorel Radu, C. Onose, A. Ioncea, Daniela Niciu, H. Stroescu i C. S. Onose. "The Permanently Bonded Glass Decor from Chemical Precursors". Advanced Materials Research 39-40 (kwiecień 2008): 579–82. http://dx.doi.org/10.4028/www.scientific.net/amr.39-40.579.
Pełny tekst źródłaHeckmann, W., F. Ramsteiner i Ch Mehler. "Morphology of Poly Amide Nanocomposites Characterized by Transmission Electron Microscopy (TEM) and Electron Spectroscopic Imaging (ESI)." Microscopy and Microanalysis 7, S2 (sierpień 2001): 502–3. http://dx.doi.org/10.1017/s1431927600028580.
Pełny tekst źródłaMolster, F. J. "Astromineralogy: Crystalline silicates". Symposium - International Astronomical Union 209 (2003): 291–98. http://dx.doi.org/10.1017/s0074180900208796.
Pełny tekst źródłaKemmitt, T., i 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, nr 1 (1995): 93. http://dx.doi.org/10.1071/ch9950093.
Pełny tekst źródłaLii, Kwang-Hwa. "High-T, High-P Hydrothermal Synthesis of Uranium Silicates and Germanates". Acta Crystallographica Section A Foundations and Advances 70, a1 (5.08.2014): C759. http://dx.doi.org/10.1107/s2053273314092407.
Pełny tekst źródłaLiang, Jian-Jie, Alexandra Navrotsky, Thomas Ludwig, Hans J. Seifert i Fritz Aldinger. "Enthalpy of Formation of Rare-earth Silicates Y2SiO5 and Yb2SiO5 and N-containing Silicate Y10(SiO4)6N2". Journal of Materials Research 14, nr 4 (kwiecień 1999): 1181–85. http://dx.doi.org/10.1557/jmr.1999.0158.
Pełny tekst źródłaP. C. Bennett, J. R. Rogers, W. J. "Silicates, Silicate Weathering, and Microbial Ecology". Geomicrobiology Journal 18, nr 1 (styczeń 2001): 3–19. http://dx.doi.org/10.1080/01490450151079734.
Pełny tekst źródłaIliushchenko, V., L. Kalina, P. Hruby, V. Bilek Jr, J. Fladr, P. Bily i J. Bojanovsky. "The treatment of cementitious surface by selected silicate sealers". Journal of Physics: Conference Series 2341, nr 1 (1.09.2022): 012003. http://dx.doi.org/10.1088/1742-6596/2341/1/012003.
Pełny tekst źródłaJakobsen, U. H. "A hydrated barium silicate in unmetamorphosed sedimentary rocks of central North Greenland". Mineralogical Magazine 54, nr 374 (marzec 1990): 81–89. http://dx.doi.org/10.1180/minmag.1990.054.374.08.
Pełny tekst źródłaRozprawy doktorskie na temat "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.
Pełny tekst źródłaEls 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.
Pełny tekst źródłaClaireaux, Corinne. "Mobilité atomique dans les silicates vitreux et fondus". Thesis, Paris 6, 2014. http://www.theses.fr/2014PA066401/document.
Pełny tekst źródłaThis 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.
Pełny tekst źródłaThis 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.
Pełny tekst źródłaObjetivos: 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.
Pełny tekst źródłaBanca: 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.
Pełny tekst źródłaNitrogen (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.
Pełny tekst źródłaBartelmehs, Kurt Lane. "Modeling the properties of silicates". Diss., This resource online, 1993. http://scholar.lib.vt.edu/theses/available/etd-05042006-164529/.
Pełny tekst źródłaMcCollam, 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.
Znajdź pełny tekst źródłaKsiążki na temat "Silicates"
Griffen, Dana T. Silicate crystal chemistry. New York: Oxford University Press, 1992.
Znajdź pełny tekst źródłaMysen, B. O. Structure and properties of silicate melts. Amsterdam: Elsevier, 1988.
Znajdź pełny tekst źródłaBabushkin, V. I. Thermodynamics of silicates. Berlin: Springer-Verlag, 1985.
Znajdź pełny tekst źródłaBabushkin, V. I., G. M. Matveyev i O. P. Mchedlov-Petrossyan. Thermodynamics of Silicates. Redaktor O. P. Mchedlov-Petrossyan. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-69320-5.
Pełny tekst źródłaWebb, Sharon L. Silicate melts: With 33 figures. Berlin: Springer, 1997.
Znajdź pełny tekst źródłaPotts, P. J. A Handbook of silicate rock analysis. London: Blackie Academic & Professional, 1987.
Znajdź pełny tekst źródłaTagiev, D. B. Kristallicheskie ali͡u︡mosilikaty v katalize. Baku: Ėlm, 1989.
Znajdź pełny tekst źródłaPotts, P. J. A handbook of silicate rock analysis. Glasgow: Blackie, 1987.
Znajdź pełny tekst źródłaL, Perchuk L., Kushiro I. 1934- i Baker Donald R. 1927-, red. Physical chemistry of magmas. New York: Springer-Verlag, 1991.
Znajdź pełny tekst źródłaFarwell, Stebbins Jonathan, McMillan Paul Francis 1955- i Dingwell D. B, red. Structure, dynamics, and properties of silicate melts. Washington, D.C: Mineralogical Society of America, 1995.
Znajdź pełny tekst źródłaCzęści książek na temat "Silicates"
Okrusch, Martin, i Hartwig E. Frimmel. "Silicates". W 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.
Pełny tekst źródłaCastroviejo, Ricardo. "Silicates". W 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.
Pełny tekst źródłaEdler, Karen J. "Mesoporous Silicates". W Porous Materials, 69–145. Chichester, UK: John Wiley & Sons, Ltd, 2010. http://dx.doi.org/10.1002/9780470711385.ch2.
Pełny tekst źródłaFalcone, J. S., i J. G. Blumberg. "Anthropogenic Silicates". W Detergents, 367–82. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-540-47108-0_14.
Pełny tekst źródłaVerma, Pramod K. "Non-silicates". W Optical Mineralogy, 337–60. Cham: Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-40765-9_16.
Pełny tekst źródłaLiebau, Friedrich. "Nomenclature and Structural Formulae of Silicate Anions and Silicates". W Structural Chemistry of Silicates, 69–75. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-50076-3_5.
Pełny tekst źródłaBabushkin, V. I., G. M. Matveyev i O. P. Mchedlov-Petrossyan. "The Basic Concepts and Laws of Thermodynamics". W Thermodynamics of Silicates, 1–54. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-69320-5_1.
Pełny tekst źródłaBabushkin, V. I., G. M. Matveyev i O. P. Mchedlov-Petrossyan. "Pyrosilicate Reactions". W Thermodynamics of Silicates, 55–249. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-69320-5_2.
Pełny tekst źródłaBabushkin, V. I., G. M. Matveyev i O. P. Mchedlov-Petrossyan. "Hydration Reactions". W Thermodynamics of Silicates, 251–335. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-69320-5_3.
Pełny tekst źródłaBabushkin, V. I., G. M. Matveyev i O. P. Mchedlov-Petrossyan. "Corrosion Reactions". W Thermodynamics of Silicates, 337–53. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-69320-5_4.
Pełny tekst źródłaStreszczenia konferencji na temat "Silicates"
Neufuss, K., J. Ilavsky, J. Dubsky, B. Kolman i P. Chraska. "Plasma Spraying of Silicates II". W ITSC 1999, redaktorzy E. Lugscheider i P. A. Kammer. Verlag für Schweißen und verwandte Verfahren DVS-Verlag GmbH, 1999. http://dx.doi.org/10.31399/asm.cp.itsc1999p0636.
Pełny tekst źródłaChráska, P., K. Neufuss, B. Kolman i J. Dubsky. "Plasma Spraying of Silicates". W ITSC 1997, redaktor C. C. Berndt. ASM International, 1997. http://dx.doi.org/10.31399/asm.cp.itsc1997p0477.
Pełny tekst źródłaCtibor, P., J. Sedláček, K. Neufuss, J. Dubský i P. Chráska. "Study of Dielectric Properties of Plasma Sprayed Silicates at Low Voltage". W ITSC2002, redaktorzy C. C. Berndt i E. Lugscheider. Verlag für Schweißen und verwandte Verfahren DVS-Verlag GmbH, 2002. http://dx.doi.org/10.31399/asm.cp.itsc2002p0617.
Pełny tekst źródłaQuet, A., L. Bianchi, E. Darthout, F. Gitzhofer, J. L. Leluan i F. Rebillat. "Yttrium Silicate Coatings by Sol Precursor Plasma Spraying for Environmental Barrier Applications". W ITSC2011, redaktorzy B. R. Marple, A. Agarwal, M. M. Hyland, Y. C. Lau, C. J. Li, R. S. Lima i A. McDonald. DVS Media GmbH, 2011. http://dx.doi.org/10.31399/asm.cp.itsc2011p0581.
Pełny tekst źródłaLipinska-Kalita, Krystyna E., i Leonard M. Proniewicz. "FTIR Spectra Of Amorphous Silicates". W Intl Conf on Fourier and Computerized Infrared Spectroscopy, redaktor David G. Cameron. SPIE, 1989. http://dx.doi.org/10.1117/12.969442.
Pełny tekst źródłaRinehart, S., D. Benford, E. Dwek, R. Henry, J. Nuth, R. Silverberg i E. Wollack. "Optical properties of astronomical silicates". W SPIE Astronomical Telescopes + Instrumentation, redaktorzy Ian S. McLean i Mark M. Casali. SPIE, 2008. http://dx.doi.org/10.1117/12.789712.
Pełny tekst źródłaSitarz, M., W. Mozgawa i M. Handke. "Vibrational spectroscopy of ring silicates". W The eleventh international conference on fourier transform spectroscopy. AIP, 1998. http://dx.doi.org/10.1063/1.55860.
Pełny tekst źródłaTan, Bee Chea, Ismail Mohd Saaid, Siti Qurratu'Aini Mahat, Suzalina Zainal, Petrus Tri Bhaskoro i Astriyana Anuar. "Evaluation of Polyamidoamine-Assisted Scale Inhibitors to Mitigate Silicate Scale Formation in Near Wellbore Region". W SPE/IATMI Asia Pacific Oil & Gas Conference and Exhibition. SPE, 2023. http://dx.doi.org/10.2118/215266-ms.
Pełny tekst źródłaHuang, Tzu Hao. "Sequential extraction of biogenic, authigenic and lithogenic silicas and silicates from marine sediments". W Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6062.
Pełny tekst źródłaBauer, S., P. Gronewald, J. Hamilton, D. LaPlant i A. Mansure. "High-Temperature Plug Formation With Silicates". W SPE International Symposium on Oilfield Chemistry. Society of Petroleum Engineers, 2005. http://dx.doi.org/10.2118/92339-ms.
Pełny tekst źródłaRaporty organizacyjne na temat "Silicates"
Shen, Andy Anda. Analyzing Silicates in Los Alamos’s Water Supply. Office of Scientific and Technical Information (OSTI), lipiec 2019. http://dx.doi.org/10.2172/1557154.
Pełny tekst źródłaWereszczak, Andrew A., Kathryn J. Ham, Yogesh K. Vohra, Georgiy Tsoi, Brian A. Oistad, Brett S. Kuwik, Emily F. Steiner, Osama Jadaan i Benjamin L. Hackett. High-Pressure Mechanical Response of Two Vitreous Silicates. Office of Scientific and Technical Information (OSTI), listopad 2018. http://dx.doi.org/10.2172/1482450.
Pełny tekst źródłaMichael G. Nelson. CARBON DIOXIDE SEQUESTRATION BY MECHANOCHEMICAL CARBONATION OF MINERAL SILICATES. Office of Scientific and Technical Information (OSTI), kwiecień 2004. http://dx.doi.org/10.2172/826304.
Pełny tekst źródłaBelt, R. F., i J. A. Catalano. Investigation of Single Crystal Silicates for Blue Tunable Lasers. Fort Belvoir, VA: Defense Technical Information Center, czerwiec 1986. http://dx.doi.org/10.21236/ada171823.
Pełny tekst źródłaOJI, LN. Conditions Conducive to Forming Crystalline Uranyl Silicates in SRS Evaporators. Office of Scientific and Technical Information (OSTI), kwiecień 2004. http://dx.doi.org/10.2172/823370.
Pełny tekst źródłaWilliam B. White, Michael R. Silsbee i B. Joe Kearns. REACTION MECHANISMS OF MAGNESIUM SILICATES WITH CARBON DIOXIDE IN MICROWAVE FIELDS. Office of Scientific and Technical Information (OSTI), luty 2004. http://dx.doi.org/10.2172/826203.
Pełny tekst źródłaFripiat, J. J. Aluminum coordination and active sites on aluminas, Y zeolites and pillared silicates. Office of Scientific and Technical Information (OSTI), styczeń 1992. http://dx.doi.org/10.2172/6923291.
Pełny tekst źródłaSchneider, E. Applications of high resolution NMR to geochemistry: crystalline, glass, and molten silicates. Office of Scientific and Technical Information (OSTI), listopad 1985. http://dx.doi.org/10.2172/6246018.
Pełny tekst źródłaOJI, LAWRENCE. Conditions Conducive to Forming Crystalline Uranyl Silicates in High Caustic Nuclear Waste Evaporators. Office of Scientific and Technical Information (OSTI), listopad 2004. http://dx.doi.org/10.2172/835626.
Pełny tekst źródłaFripiat, J. J. Aluminum coordination and active sites on aluminas, Y zeolites and pillared layered silicates. Office of Scientific and Technical Information (OSTI), styczeń 1991. http://dx.doi.org/10.2172/5874814.
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