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Artykuły w czasopismach na temat "Gibbstie"
Gan, Bee K., Ian C. Madsen i James G. Hockridge. "In situX-ray diffraction of the transformation of gibbsite to α-alumina through calcination: effect of particle size and heating rate". Journal of Applied Crystallography 42, nr 4 (30.06.2009): 697–705. http://dx.doi.org/10.1107/s0021889809021232.
Pełny tekst źródłaChandran, P., S. K. Ray, T. Bhattacharyya, P. Srivastava, P. Krishnan i D. K. Pal. "Lateritic soils of Kerala, India: their mineralogy, genesis, and taxonomy". Soil Research 43, nr 7 (2005): 839. http://dx.doi.org/10.1071/sr04128.
Pełny tekst źródłaVendrame, Pedro Rodolfo Siqueira, Robélio Leandro Marchão, Osmar Rodrigues Brito, Maria de Fátima Guimarães i Thierry Becquer. "Relationship between macrofauna, mineralogy and exchangeable calcium and magnesium in Cerrado Oxisols under pasture". Pesquisa Agropecuária Brasileira 44, nr 8 (sierpień 2009): 996–1001. http://dx.doi.org/10.1590/s0100-204x2009000800031.
Pełny tekst źródłaBonato, J. A., i R. J. Morrison. "Weathering, bauxitisation and soil genesis from the Nakobalevu Basalt, South-East Viti Levu, Fiji". South Pacific Journal of Natural and Applied Sciences 30, nr 1 (2012): 1. http://dx.doi.org/10.1071/sp12001.
Pełny tekst źródłaCarducci, Carla Eloize, Geraldo César de Oliveira, Walmes Marques Zeviani, Henrique Aparecido Laureano, Samara Martins Barbosa, Eduardo da Costa Severiano i Nilton Curi. "Preconsolidation stress of gibbsitic and kaolinitic Oxisols under a multipractice conservationist coffee system". Semina: Ciências Agrárias 42, nr 3 (19.03.2021): 1049–68. http://dx.doi.org/10.5433/1679-0359.2021v42n3p1049.
Pełny tekst źródłaO'Connor, B. H., D. Y. Li i H. Sitepu. "Texture Characterisation in X-Ray Powder Diffraction using the March Formula". Advances in X-ray Analysis 35, A (1991): 277–83. http://dx.doi.org/10.1154/s0376030800008922.
Pełny tekst źródłaKew, G. A., i R. J. Gilkes. "Properties of regolith beneath lateritic bauxite in the Darling Range of south Western Australia". Soil Research 45, nr 3 (2007): 164. http://dx.doi.org/10.1071/sr06128.
Pełny tekst źródłaYANG, Hui-bin, Xiao-lin PAN, Hai-yan YU, Gan-feng TU i Jun-min SUN. "Dissolution kinetics and mechanism of gibbsitic bauxite and pure gibbsite in sodium hydroxide solution under atmospheric pressure". Transactions of Nonferrous Metals Society of China 25, nr 12 (grudzień 2015): 4151–59. http://dx.doi.org/10.1016/s1003-6326(15)64065-1.
Pełny tekst źródłaBhattacharyya, T., D. K. Pal i P. Srivastava. "Formation of gibbsite in the presence of 2:1 minerals: an example from Ultisols of northeast India". Clay Minerals 35, nr 5 (grudzień 2000): 827–40. http://dx.doi.org/10.1180/000985500547269.
Pełny tekst źródłaClemente, Celso Augusto, i Antonio Carlos de Azevedo. "Mineral weathering in acid saprolites from subtropical, southern Brazil". Scientia Agricola 64, nr 6 (grudzień 2007): 601–7. http://dx.doi.org/10.1590/s0103-90162007000600007.
Pełny tekst źródłaRozprawy doktorskie na temat "Gibbstie"
Gückel, Katharina. "Structural analysis of ternary actinyl(V/VI) sorption complexes on gibbsite". Doctoral thesis, Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2013. http://nbn-resolving.de/urn:nbn:de:bsz:14-qucosa-126300.
Pełny tekst źródłaSilva, Wellington Barbosa da. "Caracterização da cobertura superficial em encosta na Bacia do Rio das Pombas, Guarapuava - PR: bases para entendimento da gênese erosiva em túneis". Universidade Estadual do Oeste do Parana, 2011. http://tede.unioeste.br:8080/tede/handle/tede/119.
Pełny tekst źródłaCoordenação de Aperfeiçoamento de Pessoal de Nível Superior
On the Guarapuava Plateau/Palmas, in a low slope hillside of superficial covering from basaltic origins, on the right bank of the Rio das Pombas, Paraná state, processes of tunnel erosion (pipes) were identified. These are subsuperficial erosion processes with typical features, such as subsidence of the tunnel roof and rebate structures, which tend to evolve to superficial features. The emerging of this erosive process depends on a set of factors, being the main one, the properties of the superficial covering, such as: texture, macroporosity, granulometric composition (chemical matter make-up), density, porosity e chemical elements that make up the matter, those concerning the hydrological conditions and the topography of the hillside. In order to recognize and characterize the superficial covering in the sector of low hillside, sieve analysis was used, as well as real and apparent density, total porosity verified; toposequences were made and X-ray scattering techniques performed. The results showed that the matter which covers the low hillside sector, where the tunnels are, have a sandy texture due to the properties of microagregation generated by clay mineral, gibbsite; leaving the matter with a high porosity level, thus favoring the flowing of water through subsurfaces. The generated flows tend to be exfiltrated to a ditch wall-like surface, which causes the removal of small particles of matter (seepage). With the opening of small gullies through subsurface, the flow tend to become concentrated (tunnel scour) and consequently enlarge the subsuperficial channels by the mechanical action of the water. In a sequence of factors that can be used for the analysis of the process generation, which causes: alteration in basalt rocks, microaggregation of the matter, macroporosity and increase of water flow through subsurface. Therefore, the hydrology conditions in the hillside contributed for erosion mechanisms to emerge in subsurface, development of erosion process, formation of subsuperficial erosion and, ultimately, superficial erosion process development. These both chemical and physical features found in such field of study, show that the superficial covering is a determining factor for the subsuperficial tunnel erosion to originate in the hillside.
No Planalto de Guarapuava/Palmas, em encosta de baixa declividade e cobertura superficial de origem basáltica, à margem direita do Rio das Pombas em Guarapuava (Paraná), foram identificados processos de erosão em túneis (pipes). Trata-se de processos subsuperficiais de erosão que apresentam feições típicas, tais como, subsidência do teto do túnel e estruturas de abatimento, que tendem a evoluir para feições superficiais. A instalação desse processo erosivo depende de um conjunto de fatores, destacando-se como condicionantes, as propriedades da cobertura superficial como: textura, macroporosidade, composição granulométrica, densidade, porosidade e constituintes químicos dos materiais, e aqueles relativos às condições hidrológicas e à topografia da encosta. Buscando-se reconhecer e caracterizar a cobertura superficial do setor de baixa encosta, foram realizadas análises granulométricas, de densidade aparente, real e porosidade total, construção de topossequências e análises químicas de difração de raios-X. Os resultados indicaram que o material que recobre o setor de baixa encosta, onde aparecem os túneis, apresenta textura arenosa devido às propriedades de microagregação gerada pelo argilomineral gibbsita, deixando o material com porosidade alta, favorecendo assim a circulação de água em subsuperficie. Os fluxos gerados tendem a ser exfiltrados para uma superfície de exposição, o que provoca a remoção de pequenas partículas de material (seepage). Com a abertura de pequenos canais em subsuperfície, os fluxos tendem a se concentrar (tunnel scour) e consequentemente ampliar os canais subsuperficiais pela ação mecânica da água. Numa sequência de fatores que possam ser postos para análise da geração do processo, têm-se: alteração da rocha basáltica, microagregação do material, macroporosidade e aumento da circulação de água em subsuperfície. Assume-se que as condições hidrológicas da encosta propiciaram a instalação de mecanismos de erosão em subsuperfície, evolução do processo erosivo, formação de feições erosivas subsuperficiais e, por fim, instalação de feições erosivas superficiais. Essas características físicas e químicas encontradas na área de estudo, demonstram que a cobertura superficial é determinante para a instalação da erosão subsuperficial em túneis na encosta.
Fleming, Sean D. "Computer modelling of gibbsite crystallization". Curtin University of Technology, School of Applied Chemistry, 1999. http://espace.library.curtin.edu.au:80/R/?func=dbin-jump-full&object_id=10273.
Pełny tekst źródławere made. Different crystal habits were constructed by applying a range of defect surface coverage values to each of the faces appearing in the morphology. The resulting defect morphologies were in excellent agreement with crystal habits commonly observed by experimentalists. Also, the work provided an explanation for the earlier underestimation of the prismatic faces. Chapter Six documents molecular simulations of solutions containing the major species known to be present in industrial and experimental Bayer liquors. The structuring in two solutions, one containing sodium hydroxide and the other potassium hydroxide, was probed by constructing graphs of the radial distribution functions. These plots indicated that a significant degree of ion pairing was occurring between the alkali metal cations (Na+ and K+) and the aluminate monomer ([Al(OH)4(subscript)]-). Furthermore, these cations were found to be acting as 'bridges' which stabilize multiple aluminate monomers, allowing them to form clusters. This data was used to assist in explaining vibrational spectra, and to postulate that clustering may be the origin of the fine particle suspensions noted during the induction period.
Barbieri, Diogo Mazza [UNESP]. "Formas do relevo e variabilidade espacial de atributos químicos e mineralógicos de um argissolo cultivado com cana-de-açúcar". Universidade Estadual Paulista (UNESP), 2007. http://hdl.handle.net/11449/96884.
Pełny tekst źródłaConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
A agricultura de precisão implica a análise da variabilidade espacial dos fatores de produção e a aplicação dos insumos de forma localizada e em doses precisas. O presente trabalho teve por objetivo analisar a influência do relevo na variabilidade espacial dos atributos químicos e mineralógicos para aplicação de insumos em taxa variável. Duas parcelas de um hectare foram delimitadas em área côncava e convexa. Foram retiradas 121 amostras em cada área. Os teores de P disponível apresentaram-se diferenciados nas duas áreas estudadas, sendo que os menores valores médios de P se encontram na área convexa na qual estão presentes os maiores teores de gibsita. A formação dos minerais da fração argila é condicionada pelas variações do relevo, sendo que a área convexa apresentou ambiente mais favorável à formação da gibsita do que a área côncava, demonstrando que o relevo pode ser utilizado para a definição de limites de área mais homogênea. A gibsita foi o fator determinante para a maior capacidade de adsorção máxima de P e a menor disponibilidade de fósforo na área convexa. O uso da técnica de geoestatística possibilitou a precisa descrição das propriedades do solo.
Precision agriculture implies on the analysis of the spatial variability of the production factors and the application of inputs in a localized way and on precise doses. The present work aimed to analyze the influence of the relief on the spatial variability of the chemical and mineralogical attributes for the application of inputs in variable rates. Two parcels of one hectare were bounded in concave and convex area. 121 samples were taken from each area. The levels of available P have shown to be different on the two studied areas, being the lowest mean values of P on the convex area, where the highest levels of gibbsite are present. The formation of the minerals from the clay fraction is conditioned by the relief variations, being that the convex area has presented a more favorable environment for the formation of gibbsite than the concave area, showing that relief may be used for the definition of limits in more homogenous areas. Gibbsite was the determinant factor for the higher capacity of P maximum adsorption and lower availability of phosphorous on the convex area. The use of the geostatistics technique has made possible the precise description of the soil properties.
Mitchell, Scott Christian. "An Improved MUSIC Model for Gibbsite". Diss., CLICK HERE for online access, 2005. http://contentdm.lib.byu.edu/ETD/image/etd831.pdf.
Pełny tekst źródłaCamargo, Livia Arantes [UNESP]. "Mineralogia da argila e atributos físicos de um argissolo em curvaturas de relevo". Universidade Estadual Paulista (UNESP), 2009. http://hdl.handle.net/11449/96979.
Pełny tekst źródłaFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
Os atributos mineralógicos e físicos possuem dependência espacial e a distribuição espacial destes atributos possui relação com as formas do relevo. O objeto deste trabalho foi avaliar os atributos mineralógicos da fração argila e os atributos físicos de um argissolo em curvaturas do relevo, assim como avaliar a correlação entre esses atributos. Uma malha de dimensão 100 x 100 m foi delimitada em uma área caracterizada pela forma convexa e outra pela fôrma côncava. As malhas possuem espaçamento regular de 10 x 10 m e os pontos de cruzamento deste espaçamento determinaram os pontos de coleta das amostras, num total de 121 pontos amostrais georreferenciados em cada malha. Os atributos físicos foram avaliados nas profundidades 0,0- 0,2 e 0,2-0,4 m e os atributos mineralógicos na profundidade 0,0- 0,2 m. Os atributos físicos analisados foram diâmetro médio ponderado, diâmetro médio geométrico, agregados maiores que 2 mm, agregados entre 2 e 1 mm , agregados menores que 1 mm, microporos, macroporos, volume total de poros, densidade do solo, resistência do solo à penetração e teor de água no solo, já os atributos mineralógicos da fração argila foram largura a meia altura, diâmetro médio do cristal dos óxidos de ferro, da caulinita e gibbsita, substituição isomórfica e área de superfície específica da hematita e goethita. Os teores da goethita e hematita e razão goethita/(goethita+hematita) e razão caulinita/(caulinita+gibbsita) também foram calculados. Os dados foram submetidos às análises estatísticas e geoestatísticas para avaliação da variabilidade espacial e influência das curvaturas nestes atributos. Para avaliação da relação entre os atributos da mineralogia e físicos realizaram-se as análises de correlação simples e espacial. Os atributos físicos e mineralógicos apresentaram-se dependentes das curvaturas do relevo...
The mineralogicals and physical attributes have spatial dependence and the distribution of these attributes has relation with the forms of relief. The object of this study was to evaluate the attributes of clay mineralogy and the physical attributes of an argissol in curvatures of relief, as well as assess the correlation between these attributes. A grid size of 100 x 100 meters was defined in an area characterized by the convex shape and another in an area characterized by the concave shape. The grids have regular spacing of 10 x 10 m and the spacing of the points of intersection determine the points of collection of samples, a total of 121 georeferenced sample points in each grid. The physical attributes were evaluated in depth from 0.0 - 0.2 and 0.2 -0.4 m and the mineralogical attributes in depth 0,00-0,20 m. The physical attributes were analyzed: mean weight diameter, mean geometric diameter, aggregates larger than 2 mm, aggregates between 2 and 1 mm, aggregates smaller than 1 mm, microporosity, macroporosity, total porosity, bulk density, penetration resistance and water content in soil. The attributes of minerals were: width at half height, average diameter of crystals of iron oxides and kaolinite and gibbsite and isomorphic substitution and specific surface area of hematite and goethite. The contents of goethite and hematite and ratio goethite / (goethite + hematite) [Gt / (Gt + Hm)] and ratio kaolinite / (kaolinite + gibbsite) [Ct / (Ct + Gb)] were also calculated. Data were subjected to statistical and geostatistical analysis to evaluate the spatial variability and influence of these curvatures on these attributes. To assess the relation between mineralogy and physical attributes simple and spation correlation analysis where made. The physical and mineralogical attributes and depend on the curvature of the relief. There was also the influence of crystallinity of goethite and gibbsite in soil physical.
Chiang, Yu-Lun. "Antisolvent gibbsite crystallisation from synthetic Bayer liquor". Master's thesis, University of Cape Town, 2009. http://hdl.handle.net/11427/8927.
Pełny tekst źródłaThe current Bayer precipitation of gibbsite is notoriously slow and is considered to be the rate limiting step of the Bayer process. The present industrial reactor configuration involves precipitating gibbsite inside a series of large stainless steel agitated vessels due to the slow precipitation kinetics of gibbsite from pregnant Bayer liquor. The scope of this study is to investigate the effectiveness of using water as an antisolvent to increase the overall gibbsite yield and the associated particle behaviours under isothermal conditions. The experiments were performed in a series of batch experiments which were divided into two subsets. Firstly, the effect of different caustic concentrations present in the anti solvent on gibbsite yield was tested. Secondly, the effect of different seed loading (50 and 100 grams seeds per liter of synthetic liquor) on aggregation and fines formation were investigated. All batch experiments were conducted isothermally at 80°C under a closed system using a baffled stainless steel 316 agitated vessel. The experimental results indicated water to be a feasible medium for the isothermal antisolvent crystallisation of gibbsite from synthetic pregnant Bayer liquor. It was found that the extent of overall gibbsite yield exhibits a power law correlation to the change in the antisolvent caustic concentration with R2 ~1 (R2 = 0.99974). This finding is important as the regressed curve will be used to correlate gibbsite yield as a function of anti solvent purity. From the seed loading experiments, an Increase In seed loading under constant temperature and initial liquor supersaturation resulted in an overall decrease in product particle size due to a rise in inter-particulate attrition. However, crystal growth was not dominant during any period of the experiments with aggregation being more prominent for the system with the lower seed load. Gibbsite morphology determination from SEM revealed hexagonal solids which, in the presence of a higher seed loading indicated signs of fracture due to attrition. Quantitative evidence of this mechanism is shown USIng the discretised population balance method by Bramley et al. (1996) with the aid of the computational technique developed by Hounslow (2005) in Mathematica. Results generated using this method show decreasing aggregation with liquor de supersaturation and increased seed loading. The overall particle behaviours from the current investigation are validated by results obtained from previous gibbsite studies under very similar conditions. Although the gibbsite yield can be increased drastically in the presence of an anti solvent, the average particle size generated from this study is still too small to be commercially feasible due to the increase in initial supersaturation. Thus it is recommended that further particle size optimisation may be conducted inside a fluidised bed reactor where particles generally experience lower shear than inside a conventional agitated vessel.
Plagnieux, Virginie. "Influence des conditions d'agglomération sur la morphologie de la gibbsite et les propriétés d'usage de l'alumine". Vandoeuvre-les-Nancy, INPL, 2003. http://www.theses.fr/2003INPL088N.
Pełny tekst źródłaThe@improvement of the solidity of alumina which is produced for aluminium refinery and the reduction of fine particles generation which result of shocks during calcination and transport are essential points for the Bayer producers. The aim of this study is to link the gibbsite precipitation conditions to the morphology of the crystals and to verity their impact on alumina solidity. Analysis on industrial and lab-made products was done. We have focused our attention on the role of the agglomeration step. The experimental procedure was chosen to be as close as possible to the industrial process. Gibbsite morphology was quantified by using three visualization methods (optical microscopy with different immersion liquids, scanning electron microscopy on free powder and on polished section) and a setof different shape parameters. Five shape parameters quantify the two-dimensional shape of the crystals from the point of view of their roughness, elongation and concavity. Principal component analysis have enabled an information simplification for a better precision of the results and a better interpretation. The scanning electron microscope on free powder enables the tacet network visualization. Pseudo three dimensional parameters were calculated to describe the tacet network. On polished section, the crystal frames are weil defined and enable the sizing of the crystal sides related to the tacet sides. Alumina solidity was evaluated with a standardized fluidized bed and two indices. The attrition index quantifies the proportion of particles of size less than 45 1-1m which have been created du ring the test. The breakage index quantifies the evolution of the size distribution after the test
Siebentritt, Matthieu. "Étude de l'entartrage par la gibbsite influence d'un substituant halogéné sur l'adsorption de l'alcool benzylique sur l'acier et la gibbsite". Mémoire, Université de Sherbrooke, 2010. http://savoirs.usherbrooke.ca/handle/11143/4886.
Pełny tekst źródłaLee, Mei-yin. "The mechanism of gibbsite crystal growth in Bayer liquor". Curtin University of Technology, School of Applied Chemistry, 1998. http://espace.library.curtin.edu.au:80/R/?func=dbin-jump-full&object_id=10719.
Pełny tekst źródłathat E growth occurs by spiral growth mechanism. The growth of the basal face was found to follow the spiral growth mechanism below a relative supersaturation of 0.815 and the birth and spread mechanism above this level. The activation energies and kinetic coefficients for the individual prismatic faces were also determined.Growth rate dispersion was observed in these microscopic studies, but the question of size dependency remains unanswered.The overall growth rates of gibbsite crystal, determined using rapid dynamic light scattering, was found to be an exponential function of supersaturation indicative of a birth and spread growth mechanism.
Książki na temat "Gibbstie"
A, Dzombak David, red. Surface complexation modeling: Gibbsite. Hoboken, N.J: Wiley, 2010.
Znajdź pełny tekst źródłaApps, J. A. Thermochemical properties of gibbsite, bayerite, boehmite, diaspore, and the aluminate ion between 0 and 350C. Washington, DC: Division of Waste Management, Office of Nuclear Material Safety and Safeguards, U.S. Nuclear Regulatory Commission, 1989.
Znajdź pełny tekst źródłaReyhani, M. M. Investigations at the atomic level of interactions between gibbsite and sodium oxalate in the Bayer process. East Perth, WA: Minerals and Energy Research Institute of Western Australia, 2000.
Znajdź pełny tekst źródłaDzombak, David A., i Athanasios K. Karamalidis. Surface Complexation Modeling: Gibbsite. Wiley & Sons, Incorporated, John, 2010.
Znajdź pełny tekst źródłaDzombak, David A., i Athanasios K. Karamalidis. Surface Complexation Modeling: Gibbsite. Wiley & Sons, Incorporated, John, 2011.
Znajdź pełny tekst źródłaDzombak, David A., i Athanasios K. Karamalidis. Surface Complexation Modeling: Gibbsite. Wiley & Sons, Incorporated, John, 2011.
Znajdź pełny tekst źródłaCzęści książek na temat "Gibbstie"
Gooch, Jan W. "Gibbsite". W Encyclopedic Dictionary of Polymers, 340. New York, NY: Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-6247-8_5493.
Pełny tekst źródłaHarato, T., T. Ishida i K. Yamada. "Autoprecipitation of Gibbsite and Boehmite". W Essential Readings in Light Metals, 141–47. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118647868.ch18.
Pełny tekst źródłaHarato, T., T. Ishida i K. Yamada. "Autoprecipitation of Gibbsite and Boehmite". W Essential Readings in Light Metals, 141–47. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-48176-0_18.
Pełny tekst źródłaFutia, A., H. M. Ang i Dean Ilievski. "Yield Model of a Batch Gibbsite Precipitator". W Mixing and Crystallization, 215–26. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-017-2290-2_19.
Pełny tekst źródłaLi, Tian, Dean Ilievski i Iztok Livk. "Compartmental Modelling of an Aggregating Batch Gibbsite Precipitator". W Electrometallurgy and Environmental Hydrometallurgy, 1783–91. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118804407.ch53.
Pełny tekst źródłaZheng-gen, Liu, Chu Man-sheng, Tang Jue, Han Yuan-ting i Wu Xiang-long. "Appropriate Reduction and Fe-Al Separation of High Iron Gibbsite". W Light Metals 2013, 223–27. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118663189.ch39.
Pełny tekst źródłaLanga, J. M. "The Heat of Dissolution of Gibbsite at Bayer Digestion Temperatures". W Essential Readings in Light Metals, 170–75. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-48176-0_22.
Pełny tekst źródłaZheng-gen, Liu, Chu Man-sheng, Tang Jue, Han Yuan-ting i Wu Xiang-long. "Appropriate Reduction and Fe-Al Separation of High Iron Gibbsite". W Light Metals 2013, 223–27. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-65136-1_39.
Pełny tekst źródłaYamada, K., T. Harato, S. Hamano i K. Horinouchi. "Dehydration Products of Gibbsite by Rotary Kiln and Stational Calciner". W Essential Readings in Light Metals, 717–26. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118647868.ch100.
Pełny tekst źródłaLanga, J. M. "The Heat of Dissolution of Gibbsite at Bayer Digestion Temperatures". W Essential Readings in Light Metals, 170–75. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118647868.ch22.
Pełny tekst źródłaStreszczenia konferencji na temat "Gibbstie"
Legg, Benjamin A., i James J. DeYoreo. "ENERGY LANDSCAPE FOR GIBBSITE NUCLEATION AT THE MICA-WATER INTERFACE". W GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-341436.
Pełny tekst źródłaLu, Yi, Xu Zhang, Yanfeng Gao, Xin Wang, Shuochao Fan, Yuan Chen, Yan Li i in. "Characterization of Gibbsite Filler in HTV Silicone Rubber by Thermogravimetric Analysis". W 2019 IEEE 3rd International Electrical and Energy Conference (CIEEC). IEEE, 2019. http://dx.doi.org/10.1109/cieec47146.2019.cieec-2019207.
Pełny tekst źródłaLumetta, Gregg J., Brian M. Rapko i Herman M. Cho. "Studies of the Fundamental Chemistry of Hanford Tank Sludges". W ASME 2003 9th International Conference on Radioactive Waste Management and Environmental Remediation. ASMEDC, 2003. http://dx.doi.org/10.1115/icem2003-4633.
Pełny tekst źródłaCortez, L. A., J. Marques Júnior, R. G. Peluco, G. T. Pareira i L. A. Camargo. "Relações Espaciais entre Caulinita e Gibbsita e a Estabilidade dos Agregados de Latossolo". W I Simpósio de Geoestatística Aplicada em Ciências Agrárias. Botucatu, São Paulo, Brasil: FCA/UNESP, 2009. http://dx.doi.org/10.12702/i-sgea-a32.
Pełny tekst źródłaSowards, Kimberly F., Stephen T. Nelson, Stephen T. Nelson, John McBride, John McBride, David Tingey, David Tingey, Kevin A. Rey i Kevin A. Rey. "INVESTIGATING SMECTITE AS AN IMPORTANT INTERMEDIATE PRODUCT BETWEEN IGNEOUS MINEROLOGY AND A MATURE ASSEMBLAGE OF KAOLINITE-GROUP CLAYS, GIBBSITE, AND FE-OXIDES". W GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283454.
Pełny tekst źródłaRaporty organizacyjne na temat "Gibbstie"
Martino, C. J. Gibbsite/Bayerite and Uranium in Tank 41H. Office of Scientific and Technical Information (OSTI), styczeń 2003. http://dx.doi.org/10.2172/807384.
Pełny tekst źródłaDuff, M. C. Uranium Sorption on Sodium Aluminosilicates and Gibbsite. Office of Scientific and Technical Information (OSTI), luty 2003. http://dx.doi.org/10.2172/807916.
Pełny tekst źródłaRussell, Renee L., Harry D. Smith, Donald E. Rinehart i Reid A. Peterson. Development and Characterization of Gibbsite Component Simulant. Office of Scientific and Technical Information (OSTI), styczeń 2009. http://dx.doi.org/10.2172/967006.
Pełny tekst źródłaHerting, Daniel L. Effect of Phosphate, Fluoride, and Nitrate on Gibbsite Dissolution Rate and Solubility. Office of Scientific and Technical Information (OSTI), styczeń 2014. http://dx.doi.org/10.2172/1119691.
Pełny tekst źródłaPoirier, M., i P. Burket. Impact Of Sodium Oxalate, Sodium Aluminosilicate, and Gibbsite/Boehmite on ARP Filter Performance. Office of Scientific and Technical Information (OSTI), listopad 2015. http://dx.doi.org/10.2172/1235439.
Pełny tekst źródłaHay, M., K. Kofi Adu-Wusu i D. Daniel McCabe. DETERMINATION OF THE FRACTION OF GIBBSITE AND BOEHMITE FORMS OF ALUMINUM IN TANK 51H SLUDGE. Office of Scientific and Technical Information (OSTI), sierpień 2008. http://dx.doi.org/10.2172/939428.
Pełny tekst źródłaApps, J. A., J. M. Neil i C. H. Jun. Thermochemical properties of gibbsite, bayerite, boehmite, diaspore, and the aluminate ion between 0 and 350/degree/C. Office of Scientific and Technical Information (OSTI), styczeń 1989. http://dx.doi.org/10.2172/6481805.
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