Academic literature on the topic 'Bentonite – Wyoming'

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Journal articles on the topic "Bentonite – Wyoming"

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Laribi, S., J. M. Fleureau, and N. Kbir-Ariguib. "Filtration and standardized properties of Jebel Om El Khecheb clay (Tunisia) and Wyoming bentonite." Clay Minerals 42, no. 3 (2007): 319–28. http://dx.doi.org/10.1180/claymin.2007.042.3.05.

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AbstractThe rheological and filtration properties of a Tunisian clay are presented and compared with those of Wyoming bentonite. The study was part of an evauation of Tunisian mining resources in general, and of the bentonitic deposits in particular. Qualitatively, the two clays exhibit the same rheological and filtration behaviour but quantitatively the properties of purified Wyoming bentonite are distinctly better at the same concentration. The difference can be related to the mineralogical structure and the presence of 13% illite in the Tunisian clay. Standard tests show that the rheologica
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Sarkar, Grytan, Ashish Dey, and Sumi Siddiqua. "Preparation of Wyoming bentonite nanoparticles." Environmental Geotechnics 4, no. 5 (2017): 373–81. http://dx.doi.org/10.1680/jenge.15.00001.

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Thorson, Thomas A. "Aerial surveying of Wyoming bentonite." Applied Clay Science 11, no. 5-6 (1997): 329–35. http://dx.doi.org/10.1016/s0169-1317(96)00031-2.

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DOLATI, Samira, and Mohsen KALANI. "STRUCTURAL CHARACTERIZATION OF A BENTONITE DEPOSIT FROM THE EASTERN IRAN; COMPARISON WITH TWO REFERENCE BENTONITES." Carpathian Journal of Earth and Environmental Sciences 16, no. 1 (2021): 151–62. http://dx.doi.org/10.26471/cjees/2021/016/163.

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Mineralogically, bentonites are dominated by smectites and due to characteristic textural and physicochemical properties of smectites (e.g. very small particle sizes, high cation exchange capacity) are of a great use in industrial applications. In this study, a bentonite sample was characterized with regard to the particle size distribution, mineralogical composition and cation exchange capacity in comparison with the data for the two internationally well-known bentonites representative for Na- and Ca-bentonites: the Mx-80 bentonite of Wyoming, USA and that of Milos, Greece, respectively. Resu
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Brunton, George D. "Density and Compressibility of Wyoming Bentonite Particles." Clays and Clay Minerals 36, no. 1 (1988): 94–95. http://dx.doi.org/10.1346/ccmn.1988.0360112.

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Sauer, Kirsten, Florie Caporuscio, Marlena Rock, Michael Cheshire, and Carlos Jové-Colón. "HYDROTHERMAL INTERACTION OF WYOMING BENTONITE AND OPALINUS CLAY." Clays and Clay Minerals 68, no. 2 (2020): 144–60. http://dx.doi.org/10.1007/s42860-020-00068-8.

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Christidis, G., and A. C. Dunham. "Compositional Variations in Smectites: Part I. Alteration of Intermediate Volcanic Rocks. A Case Study from Milos Island, Greece." Clay Minerals 28, no. 2 (1993): 255–73. http://dx.doi.org/10.1180/claymin.1993.028.2.07.

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AbstractThe chemistry of smectites from some bentonite deposits derived from intermediate rocks has been examined by electron microprobe methods. A large variation in chemical composition within very short distances, principally controlled by a well-defined negative relationship between Si and A1, and between A1VI and Fe 3+ and A1VI and Mg has been observed. On the other hand, Mg does not vary systematically with either Si or Fe3+. In several bentonites beidellite coexists with montmorillonite and there is a compositional transition between the two smectite minerals, implying the existence of
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Hannon, Jeffrey S., Craig Dietsch, Warren D. Huff, and Davidson Garway. "Tracking 40 Million Years of Migrating Magmatism across the Idaho Batholith Using Zircon U-Pb Ages and Hf Isotopes from Cretaceous Bentonites." Minerals 11, no. 9 (2021): 1011. http://dx.doi.org/10.3390/min11091011.

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Cretaceous strata preserved in Wyoming contain numerous large bentonite deposits formed from the felsic ash of volcanic eruptions, mainly derived from Idaho batholith magmatism. These bentonites preserve a near-continuous 40 m.y. chronology of volcanism and their whole-rock and mineral chemistry has been used to document igneous processes and reconstruct the history of Idaho magmatism as emplacement migrated across the Laurentian margin. Using LA-ICP-MS, we analyzed the U-Pb ages and Hf isotopic compositions of nearly 700 zircon grains from 44 bentonite beds from the Bighorn Basin, Wyoming. Zi
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Jeong, Sueng-Won. "The Rheological Characteristics of Wyoming Bentonite: Role of Salinity." Journal of the Korean Geotechnical Society 27, no. 10 (2011): 81–92. http://dx.doi.org/10.7843/kgs.2011.27.10.081.

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XU, YONGFU. "SURFACE FRACTAL DIMENSION OF SWELLING CLAY MINERALS." Fractals 11, no. 04 (2003): 353–62. http://dx.doi.org/10.1142/s0218348x03002245.

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A simple method is proposed to determine the surface fractal dimension of swelling clay minerals. When swelling clay mineral is immersed into the water solution, swelling deformation and swelling pressure will occur. The swelling deformation and swelling pressure are proportional to the amount of water volume absorbed by swelling clay minerals. The water volume absorbed by swelling clay minerals is related to its surface fractality. The correlation of the normalized water volume by the volume of swelling clay minerals (Vw/Vm) to vertical overburden pressure (p) is obtained as Vw/Vm = KpDs-3, f
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Dissertations / Theses on the topic "Bentonite – Wyoming"

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Ferreira, Isabel Cristina Santos. "Tratamento terciário da indústria de laticinios através da adsorção de lactose em argila esmectítica." Universidade de São Paulo, 2007. http://www.teses.usp.br/teses/disponiveis/3/3137/tde-06072007-140835/.

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Este trabalho, propõe nova tecnologia para tratamento de efluentes gerados pelas indústrias de laticínios. Atualmente este tipo de efluente, quando tratado, utiliza o processo biológico para reduzir a carga orgânica, contudo, este método, algumas vezes, não garante a remoção completa dos compostos orgânicos. Assim, é sugerido a utilização de argila bentonitica sódica para a adsorção da lactose como tratamento terciário do efluente da indústria de laticínios. A comprovação deste evento assim como sua quantificação foi realizada através de duas técnicas distintas: análise térmica e difração de r
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Dumont, Matthieu. "Contribution à l'étude du comportement THM des sols partiellement saturés : aspects expérimentaux et modélisation." Le Havre, 2011. http://www.theses.fr/2011LEHA0017.

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Ce travail de recherche vise à améliorer les connaissances et à mieux cerner le comportement thermo-hydro-mécanique des sols fins. Un volet théorique présente un modèle simple de loi de comportement thermohydromécanique (THM). Le concept de contraintes effectives est élargi aux sols non saturés, avec l’introduction d’une contrainte capillaire. Cette contrainte capillaire est basée sur un modèle micro-structural et calculée à partir de forces d’attraction dues aux ménisques d’eau. Le phénomène d’écrouissage dû à la désaturation du matériau et à l’effet thermique sont modélisés avec un nombre ré
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Roubeuf, Véronique. "Interactions entre fluides et sédiments argileux naturels : étude expérimentale dans des conditions simulant un stockage souterrain de déchets radioactifs." Nancy 1, 2000. http://docnum.univ-lorraine.fr/public/SCD_T_2000_0190_ROUBEUF.pdf.

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Le comportement des argilites de l'oxfordien argileux de la haute-marne et des siltites de la serie albienne de marcoule (gard) a ete etudie experimentalement dans des conditions physico-chimiques simulant un stockage souterrain de dechets. Les diverses phases recrees sont l'interaction entre les fluides generes par l'oxydation des microsites a pyrites lors de l'entree de l'air dans les galeries et les mineraux constitutifs des sediments, l'alteration liee a une exposition aux intemperies climatiques (cycles d'humectation/dessiccation), des phases de rehydratation a 80 et 200\c simulant l'effe
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Books on the topic "Bentonite – Wyoming"

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SW Forest Health Act, bentonite mining in Wyoming, Pueblos of Santa Clara and Mt. Naomi Wilderness: Hearing before the Subcommittee on Public Lands and Forests of the Committee on Energy and Natural Resources, United States Senate, One Hundred Eighth Congress, first session on S. 32, S. 203, S. 246, S. 278, February 27, 2003. U.S. G.P.O., 2003.

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Chiou, Wen-An, Helmut Coutelle, Andreas Decher, et al. Bentonites -. Edited by Stephan Kaufhold. E. Schweizerbart Science Publishers, 2021. http://dx.doi.org/10.1127/bentonites/9783510968596.

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<p><b>Bentonites</b> are rocks mostly consisting of swelling clay minerals. They were first described from the Cretaceous Benton Shale near Rock River, Wyoming, USA. </p> <p> Because of their useful properties (e.g. highly adsorbent, cation exchanging, swelling), bentonites have many uses, in industry (among them as drilling mud, purification agent, binder, adsorbent, paper production), culture (for e.g. pottery) and medicine/cosmetics/cat litter, civil engineering, and in the future even in the disposal of high-level nuclear waste. </p> <p> Particular
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Wyoming. Dept. of Labor and Statistics., ed. Wyoming bentonite, trona, and uranium: A wage and employment survey, 1985. Wyoming Dept. of Labor & Statistics, 1985.

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Conference papers on the topic "Bentonite – Wyoming"

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Sauer, Kirsten, Marlena Rock, Florie Caporuscio, Katherine Telfeyan, and Edward Matteo. "Interaction of Wyoming Bentonite and Grimsel Granodiorite in High Temperature EBS Experiments." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2290.

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