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Artigos de revistas sobre o assunto "Carbonate"

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Rouillé, Gaël, Johannes Schmitt, Cornelia Jäger, and Thomas Henning. "Gas-phase Condensation of Carbonated Silicate Grains." Astrophysical Journal 966, no. 2 (2024): 191. http://dx.doi.org/10.3847/1538-4357/ad381d.

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Abstract Reports on the detection of carbonates in planetary nebulae (PNe) and protostars have suggested the existence of a mechanism that produces these compounds in stellar winds and outflows. A subsequent laboratory study has reported a possible mechanism by presenting the non-thermodynamic-equilibrium (TE), gas-phase condensation of amorphous silicate grains with amorphous calcium carbonate inclusions. The authors concluded that water vapor was necessary for the formation of the carbonates. We present a laboratory study with pulsed laser ablation of a MgSi target in O2 and CO2 gases and re
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Yaxley, Gregory M., Bruce A. Kjarsgaard, and A. Lynton Jaques. "Evolution of Carbonatite Magmas in the Upper Mantle and Crust." Elements 17, no. 5 (2021): 315–20. http://dx.doi.org/10.2138/gselements.17.5.315.

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Carbonatites are the most silica-poor magmas known and are amongst Earth’s most enigmatic igneous rocks. They crystallise to rocks dominated by the carbonate minerals calcite and dolomite. We review models for carbonatite petrogenesis, including direct partial melting of mantle lithologies, exsolution from silica-undersaturated alkali silicate melts, or direct fractionation of carbonated silicate melts to carbonate-rich residual melts. We also briefly discuss carbonatite–mantle wall-rock reactions and other processes at mid-to upper crustal depths, including fenitisation, overprinting by carbo
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Korinevsky, V. G., and E. V. Korinevsky. "Isotopic evidences of magmatic nature of the dolomite-calcite bodies of the Ilmeny Mountains and the Plastovsky district of the South Urals." Vestnik of Geosciences 11 (2020): 3–19. http://dx.doi.org/10.19110/geov.2020.11.1.

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The data obtained for the first time on the isotopic composition of oxygen and carbon of calcites and graphites of dolomitecalcite rocks of the Ilmeny Mountains and dykes of a similar composition in the Plastovsky district have confirmed their magmatic genesis. The temperature of formation of carbonate bodies (590—1000 °Ñ), determined from the isotopic ratios of C and O in calcite and graphite, corresponds to the temperature range (600—900 °Ñ) of the formation of carbonatite associations. According to the same ratios of isotopes in calcites, the protoliths of carbonate rocks are located within
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Tang, Guowang, Feng Huang, Guihe Wang, et al. "Valorization of Water-Based Drill Cuttings through the Bio-Carbonation Approach." Advances in Materials Science and Engineering 2022 (May 6, 2022): 1–10. http://dx.doi.org/10.1155/2022/3836863.

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This study proposed a novel bio-carbonation method to recycle water-based drill cutting (WDC) to prepare samples, which contains reactive magnesia (MgO) cement (RMC), ground granulated blast furnace slag (GGBS), and fly ash (FA), with the adoption of microbially induced carbonate precipitation (MICP). Through the investigation of some parameters (i.e., GGBS content, FA content, and curing time), the microstructures and strength development of bio-carbonated RMC-based WDC samples were evaluated. The preliminary results revealed that bio-carbonated RMC-based WDC samples outperformed the control
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Nikiforov, Anatoly V., Elena O. Dubinina, Nikolay A. Polyakov, Amina M. Sugorakova, and Aylan K. Khertek. "Influence of Host Marble Rocks on the Formation of Intrusive Alkaline Rocks and Carbonatites of Sangilen (E. Siberia, Russia)." Minerals 11, no. 7 (2021): 666. http://dx.doi.org/10.3390/min11070666.

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The study of the O and C isotope composition of calcite from nepheline syenites, ijolites and carbonatites of the Chik intrusion and the intrusions of the Erzin–Tarbagatay group of Sangilen (Eastern Siberia, Russia) showed derivation from alkaline melts enriched with a carbonate component from the host marbleized sedimentary rocks. The calculations showed that about 40% of the initial mass of carbonates involved in the interaction with silicate melts have remained after decarbonation. During the assimilation of the carbonate, an oxygen isotope exchange took place between the residual carbonate
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Xiang, Wanli, Jan-Peter Duda, Andreas Pack, Mark van Zuilen, and Joachim Reitner. "Were early Archean carbonate factories major carbon sinks on the juvenile Earth?" Biogeosciences 21, no. 24 (2024): 5653–84. https://doi.org/10.5194/bg-21-5653-2024.

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Abstract. Paleoarchean carbonates in the Pilbara Craton (Western Australia) are important archives for life and environment on early Earth. Amongst others, carbonates occur in interstitial spaces of ca. 3.5–3.4 Ga pillow basalts (North Star, Mount Ada, Apex, and Euro Basalt, Dresser Formation) and are associated with bedded deposits (Dresser and Strelley Pool Formation, Euro Basalt). This study aims to understand the formation and geobiological significance of those early Archean carbonates by investigating their temporal–spatial distribution, petrography, mineralogy, and geochemistry (e.g., t
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El Howayek, Alain, Antonio Bobet, and Marika Santagata. "Microstructure and cementation of two carbonatic fine-grained soils." Canadian Geotechnical Journal 56, no. 3 (2019): 320–34. http://dx.doi.org/10.1139/cgj-2018-0059.

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This paper presents an investigation of the microstructure and cementation of two carbonatic fine-grained soils obtained from a deposit of lacustrine origin formed during the Wisconsin glaciation. The two soils differ in the degree of cementation (with average total carbonate contents of ∼55% and ∼38%), the dominating carbonate mineral (calcite versus dolomite), and the forms of carbonates present. The study is founded on observations of the microstructure using scanning electron microscopy (SEM) equipped with energy-dispersive X-ray (EDX) spectrometry, and examination of the effects of carbon
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Casola, Valentin, Lydéric France, Albert Galy, Nordine Bouden, and Johan Villeneuve. "No evidence for carbon enrichment in the mantle source of carbonatites in eastern Africa." Geology 48, no. 10 (2020): 971–75. http://dx.doi.org/10.1130/g47629.1.

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Abstract Carbonatites are unusual, carbon-rich magmas thought to form either by the melting of a carbon-rich mantle source or by low-degree partial melting of a carbon-poor (<80 ppm C) mantle followed by protracted differentiation and/or immiscibility. Carbonate-bearing mantle xenoliths from Oldoinyo Lengai (East African Rift), the only active volcano erupting carbonatites, have provided key support for a C-rich mantle source. Here, we report unique microscale O and C isotopic analyses of those carbonates, which are present as interstitial grains in the silicate host lava, veins in the
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Jorge Pinto, André, Nuria Sánchez-Pastor, and Angeles Fernández-González. "The Controlling Effect of CaCO3 Supersaturation over Zn Carbonate Assemblages: Co-Crystallization in Silica Hydrogel." Minerals 14, no. 12 (2024): 1274. https://doi.org/10.3390/min14121274.

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Weathering products of sphalerite-bearing ores play an important role in controlling the fate of Zn in the environment. In this framework, the relative stability of Zn carbonates is of special relevance for the common case of ore weathering by carbonated groundwater in the presence of calcium carbonates. We investigated the experimental (co)nucleation and growth of Zn and Ca carbonates at 25 °C in finite double diffusion silica hydrogel media with the purpose of deciphering the system’s reactive pathway and unraveling the major governing factors behind the obtained mineral assemblages. The cry
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Clarke, M. G. C., and B. Roberts. "Carbonated melilitites and calcitized alkalicarbonatites from Homa Mountain, western Kenya: a reinterpretation." Geological Magazine 123, no. 6 (1986): 683–92. http://dx.doi.org/10.1017/s0016756800024195.

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AbstractHoma Mountain is a well developed ijolite/carbonatite complex of Miocene to Quaternary age. Late stage olivine melilitite occurs as a satellite plug, parts of which show strong deuteric alteration to carbonate resulting in complete pseudomorphing of the melilite.A second satellite centre exposes a grey carbonate tuff and accompanying dykes, all of which exhibit relic textures after an elongate, rectangular mineral also formerly believed to be melilite. Comparison with other recently described occurrences indicates however that the second centre erupted alkali-carbonatite and that the c
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Teses / dissertações sobre o assunto "Carbonate"

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MOURA, Carlos Henrickson Barbalho de. "Estimativa de permeabilidade de rocha carbonáticas a partir de parâmetros do espaço poroso." Universidade Federal de Campina Grande, 2018. http://dspace.sti.ufcg.edu.br:8080/jspui/handle/riufcg/1615.

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Submitted by Emanuel Varela Cardoso (emanuel.varela@ufcg.edu.br) on 2018-08-30T23:05:10Z No. of bitstreams: 1 CARLOS HENRICKSON BARBALHO DE MOURA – DISSERTAÇÃO (PPGEPM) 2018.pdf: 10493787 bytes, checksum: 063013097342f1433f86bc8ac8434722 (MD5)<br>Made available in DSpace on 2018-08-30T23:05:10Z (GMT). No. of bitstreams: 1 CARLOS HENRICKSON BARBALHO DE MOURA – DISSERTAÇÃO (PPGEPM) 2018.pdf: 10493787 bytes, checksum: 063013097342f1433f86bc8ac8434722 (MD5) Previous issue date: 2018-03-28<br>Capes<br>A petrofísica computacional é uma técnica que vem sendo utilizada cada vez mais na indústria
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Shaikh, A. G. "Synthesis and characterization of poly (aryl carbonate)s and poly (arylester- carbonate)s via carbonate interchange reactions with dialkylcarbonate." Thesis(Ph.D.), CSIR-National Chemical Laboratory, Pune, 1994. http://dspace.ncl.res.in:8080/xmlui/handle/20.500.12252/3073.

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Champagne, Julie. "Diagenèse associée aux discontinuités sédimentaires émersives sur les plates-formes carbonatées : étude intégrée à l'affleurement et en subsurface de la Formation Natih (Cretacé, Oman), évolution des propriétés réservoir." Thesis, Bordeaux 3, 2012. http://www.theses.fr/2012BOR30059/document.

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En domaine de plate-forme carbonatée épicontinentale peu profonde, la production sédimentaire est étroitement liée aux variations eustatiques, au climat et à la position paleogéographique. Les périodes d’émersion constituent des phases de non-dépôt durant lesquelles l’arrêt de l’enregistrement sédimentaire peut être relayé par un enregistrement diagénétique. Les transformations associées aux discontinuités (réarrangement des porosités, modifications lithologiques, circulations tardives…) peuvent avoir un rôle déterminant sur les propriétés pétrophysiques des réservoirs carbonatés. La détection
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Dale, Annabel Rebecca. "Carbonate clumped isotopes : a new tool to assess carbonate cementation in clastic sediments." Thesis, Imperial College London, 2014. http://hdl.handle.net/10044/1/39782.

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Carbonate cements in clastic rocks capture a geochemical record of burial processes. As such, much of our understanding of clastic diagenesis and subsurface microbial activity is influenced by studies of carbonate cemented horizons and concretions. Furthermore, their presence can have a significant impact on clastic reservoir quality. However, the formation of cement bodies is poorly understood. A part of this problem is that studies investigating carbonate cements have historically been limited by the δ18Ocarbonate being dependent on both the carbonate precipitation temperature and δ18Oporewa
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Easley, Regina Anita. "The Spectrophotometric Analysis of Lead Carbonate Complexation and Carbonate Saturation States in Seawater." Scholar Commons, 2013. http://scholarcommons.usf.edu/etd/4668.

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The carbon dioxide (CO2) system is the primary buffer in seawater which controls oceanic pH. Changes in the marine CO2 system affect a number of processes such as metal speciation, mineral saturation states, auditory responses in fish, and primary productivity rates. Increased atmospheric concentrations of CO2 from human activities (e.g. burning of fossil fuels, deforestation, and cement production) has led to a global decrease in surface ocean pH termed anthropogenic ocean acidification. One particular concern in response to increased oceanic CO2 is a substantial decrease in the calcium carbo
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Tanimoto, Kazumi. "Studies on optimization of carbonate compositions for long life molten carbonate fuel cells." 京都大学 (Kyoto University), 2008. http://hdl.handle.net/2433/136372.

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Salter, Michael A. "The production and preservation of fish-derived carbonates in shallow sub-tropical marine carbonate provinces." Thesis, Manchester Metropolitan University, 2013. http://e-space.mmu.ac.uk/314039/.

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Recent studies have demonstrated that marine bony fish (teleosts) precipitate inorganic calcium carbonate in their gut as a by-product of osmoregulation, subsequently excreting it into the open water column as loosely aggregated millimetre-scale pellet. These studies have primarily focused on physiological aspects of this process and the fate of resulting carbonates in pelagic settings, which is likely to be dissolution at depth. However, the implications of such carbonate production in shallow tropical and sub-tropical carbonate provinces has also begun to be considered, and it is thought tha
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Hait, S. B. "Synthesis and characterization of homo and copoly(aryl carbonate)s via carbonate interchange reaction." Thesis(Ph.D.), CSIR-National Chemical Laboratory, Pune, 1997. http://dspace.ncl.res.in:8080/xmlui/handle/20.500.12252/3365.

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Lanteaume, Cyprien. "Couplage de la modélisation stratigraphique et diagénétique : développements numériques et applications aux systèmes carbonatés." Thesis, Aix-Marseille, 2017. http://www.theses.fr/2017AIXM0344.

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Les systèmes sédimentaires carbonatés forment à la fois des archives géologiques uniques des changements globaux-locaux des enveloppes externes de la Terre et renferment plus de 75 % des réserves d'hydrocarbure conventionnelles. Ils sont complexes et très difficiles à comprendre et à prédire. Cette complexité à toutes les échelles spatio-temporelles rend nécessaire l'intégration de méthodes naturalistes et quantitatives pour les étudier. La modélisation numérique basée processus permet de réduire les incertitudes des prédictions des propriétés des réservoirs carbonatés.Le manuscrit présente un
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Safa, Ali Ibrahim 1953. "Catalytic Calcination of Calcium Carbonate." Thesis, North Texas State University, 1985. https://digital.library.unt.edu/ark:/67531/metadc330965/.

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The calcination of calcium carbonate in a cement or a lime kiln uses approximately two to four times the theoretical quantity of energy predicted from thermodynamic calculation depending upon the type of the kiln used (1.4 x 10^6 Btu/ton theoretical to 6 x 10^6 Btu/ton actual). The objective of this research was to attempt to reduce the energy required for the calcination by 1. decreasing the calcination temperature of calcium carbonate, and/or 2. increasing the rate of calcination at a specific temperature. Assuming a catalytic enhancement of 20 percent in the industrial applications, an ener
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Livros sobre o assunto "Carbonate"

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E, Tucker Maurice, and Bathurst Robin G. C, eds. Carbonate diagenesis. Blackwell Scientific Publications, 1990.

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Ibrahim, Palaz, and Marfurt K. J, eds. Carbonate seismology. Society of Exploration Geophysicists, 1997.

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S, Sagyndykov K., Turdukeev I. D та Institut geologii im. M.M. Adysheva., ред. Litologii͡a︡ i rudonosnostʹ uglerodistykh format͡s︡ii verkhnego dokembrii͡a︡-nizhnego paleozoi͡a︡ Ti͡a︡nʹ-Shani͡a︡. Ilim, 1991.

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London, Geological Society of, ed. Advances in carbonate exploration and reservoir analysis. Published by the Geological Society, 2012.

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Bathurst, Robin G. C. Carbonate sediments and their diagenesis. 2nd ed. Elsevier, 1986.

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Morse, John W. Geochemistry of sedimentary carbonates. Elsevier, 1990.

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S, Presser T., Carothers W. W, and Geological Survey (U.S.), eds. CA-MG carbonate deposits, Warnick Canyon, Colusa County, California. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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S, Presser T., Carothers W. W, and Geological Survey (U.S.), eds. CA-MG carbonate deposits, Warnick Canyon, Colusa County, California. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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S, Presser T., Carothers W. W, and Geological Survey (U.S.), eds. CA-MG carbonate deposits, Warnick Canyon, Colusa County, California. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Tegethoff, F. Wolfgang, ed. Calcium Carbonate. Birkhäuser Basel, 2001. http://dx.doi.org/10.1007/978-3-0348-8245-3.

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Capítulos de livros sobre o assunto "Carbonate"

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Bährle-Rapp, Marina. "carbonate." In Springer Lexikon Kosmetik und Körperpflege. Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-71095-0_1660.

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Arndt, Nicholas. "Carbonate." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-44185-5_234.

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Arndt, Nicholas. "Carbonate." In Encyclopedia of Astrobiology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-11274-4_234.

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Allison, L. E., and C. D. Moodie. "Carbonate." In Agronomy Monographs. American Society of Agronomy, Soil Science Society of America, 2016. http://dx.doi.org/10.2134/agronmonogr9.2.c40.

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Geyssant, Jacques. "Features and characteristics of calcium carbonate." In Calcium Carbonate. Birkhäuser Basel, 2001. http://dx.doi.org/10.1007/978-3-0348-8245-3_1.

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Heß, Peter. "Plastics." In Calcium Carbonate. Birkhäuser Basel, 2001. http://dx.doi.org/10.1007/978-3-0348-8245-3_10.

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Strauch, Dieter. "Surface Coatings." In Calcium Carbonate. Birkhäuser Basel, 2001. http://dx.doi.org/10.1007/978-3-0348-8245-3_11.

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Kuhlmann, Ralph. "Calcium Carbonate - A Versatile Mineral." In Calcium Carbonate. Birkhäuser Basel, 2001. http://dx.doi.org/10.1007/978-3-0348-8245-3_12.

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Geyssant, Jacques. "The limestones - development and classification." In Calcium Carbonate. Birkhäuser Basel, 2001. http://dx.doi.org/10.1007/978-3-0348-8245-3_2.

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Geyssant, Jacques. "Limestone deposits." In Calcium Carbonate. Birkhäuser Basel, 2001. http://dx.doi.org/10.1007/978-3-0348-8245-3_3.

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Trabalhos de conferências sobre o assunto "Carbonate"

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Natsi, P. D., and P. G. Koutsoukos. "Calcium Carbonate Biofouling." In CORROSION 2019. NACE International, 2019. https://doi.org/10.5006/c2019-12930.

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Abstract Biofouling is the formation of composite deposits consisting of living organic matter and inorganic salts. So far there is little mechanistic information on biofouling. In this work, the role of the presence of microalgae on the nucleation and growth of calcium carbonate from aqueous supersaturated solutions was investigated with free drift and constant supersaturation batch experiments, at 25°C. Living and dead microalgae colonies were used to inoculate aqueous solutions supersaturated with respect to calcium carbonate. The presence of algae accelerated the crystal growth of calcium
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Cho, Yung-Zun, In-Tae Kim, Hee-Chul Yang, Hee-Chul Eun, Hwan-Seo Park, and Eung-Ho Kim. "Removal of Alkaline-Earth Elements by a Carbonate Precipitation in a Chloride Molten Salt." In The 11th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2007. http://dx.doi.org/10.1115/icem2007-7288.

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Separation of some alkaline-earth chlorides (Sr, Ba) was investigated by using carbonate injection method in LiCl-KCl eutectic and LiCl molten salts. The effects of the injected molar ratio of carbonate ([K2 (or Li2)CO3/Sr (or Ba)Cl2]) and the temperature (450–750 °C) on the conversion ratio of the Sr or Ba carbonate were determined. In addition, the form of the Sr and Ba carbonate resulting from the carbonation reaction with carbonates was identified via XRD and SEM-EDS analysis. In these experiments, the carbonate injection method can remove Sr and Ba chlorides effectively over 99% in both L
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Schofield, Alex. "Coral Carbonate." In ACADIA 2020: Distributed Proximities. ACADIA, 2020. http://dx.doi.org/10.52842/conf.acadia.2020.1.048.

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Ren, Nan, Yu-ting Wu, and Chong-fang Ma. "Preparation and Experimental Study of Mixed Carbonates With High Maximum Using Temperature." In ASME 2012 6th International Conference on Energy Sustainability collocated with the ASME 2012 10th International Conference on Fuel Cell Science, Engineering and Technology. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/es2012-91401.

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In order to meet the demands of future high-temperature solar thermal power generation, 37 kinds of mixed carbonate molten salts were prepared by mixing potassium carbonate, lithium carbonate, sodium carbonate in accordance with different proportions in this paper. Melting point of molten salt, as the most important basic character, is the primary parameter to select molten salt. Melting point and decomposition temperature are measured by Simultaneous Thermal Analyzer. The results show that melting points of major ternary carbonates are close at around 400°C and decomposition temperatures of m
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Wozencraft, Jennifer M., and Jennifer L. Irish. "SHOALS Surveys and Carbonate Beaches." In First International Symposium on Carbonate Sand Beaches. American Society of Civil Engineers, 2002. http://dx.doi.org/10.1061/40640(305)3.

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Asta, Maria, Arthur Adams, Torsten Vennemann, and Anders Meibom. "Oxygen isotope fractionation in carbonates: the role of amorphous calcium carbonate." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.16631.

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Oleksiy, Nazarenko, Berezovska Alona, Ischenko Oleksiy, Zhvan Viktor, and Kulik Michailo. "Prospects for the Use of Light Carbonate Slag Carbonate." In The 9th World Congress on Civil, Structural, and Environmental Engineering. Avestia Publishing, 2024. http://dx.doi.org/10.11159/icsect24.127.

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Liu, Winnie, Shawn Riechers, Sebastian Mergelsberg, Nabajit Lahiri, and Sebastien Kerisit. "Nickel Hydroxide–Nickel Carbonate Competitive Growth on Carbonate Surfaces." In Goldschmidt 2024. Geochemical Society, 2024. https://doi.org/10.46427/gold2024.23177.

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Zhi, Suo-Hong, Bo Zhang, Qiang Zhu, et al. "Mineralized Poly (Vinylidene Fluoride)-Based Ultrafiltration Membranes with Sodium Carbonate and Ammonium Carbonate as Carbonate Source." In 2016 International Conference on Mechanics and Materials Science (MMS2016). WORLD SCIENTIFIC, 2017. http://dx.doi.org/10.1142/9789813228177_0108.

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Sain, Ratnanabha, Ganglin Chen, Shiyu Xu, Michael A. Payne, and Akmal Awas Sultan. "Carbonate rock physics: Geophysical and petrophysical pore types of carbonate rocks from an offshore carbonate field." In SEG Technical Program Expanded Abstracts 2008. Society of Exploration Geophysicists, 2008. http://dx.doi.org/10.1190/1.3059226.

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Relatórios de organizações sobre o assunto "Carbonate"

1

Simandl, G. J., R. J. D'Souza, S. Paradis, and J. Spence. Rare-earth element content of carbonate minerals in sediment-hosted Pb-Zn deposits, southern Canadian Rocky Mountains. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328001.

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Paleozoic platform carbonate rocks of the Rocky Mountains host Mississippi Valley-type (MVT), magnesite, barite, and REE-barite-fluorite deposits. Farther west, platform carbonate rocks of the Kootenay Arc host MVT and fracture-controlled replacement (FCR) deposits. This is the first systematic LA-ICP-MS study of carbonates in MVT and FCR deposits. We investigated seven MVT deposits in the Rocky Mountains, and five MVT deposits in the Kootenay Arc. None of the post-Archean Australian shale (PAAS)-normalized REE profiles show light REE (LREE) depletion and strong negative Ce anomalies character
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2

Carter, T. R., C E Logan, and H. A. J. Russell. Three-dimensional model of dolomitization patterns in the Salina Group A-1 Carbonate and A-2 Carbonate units, Sombra Township, Lambton County, southern Ontario. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/332363.

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Dolomitization of carbonate rocks is a subject of considerable interest due to association with oil and gas reservoirs and Mississippi Valley Type ore deposits. Conceptual two-dimensional models of dolomitization are common in the literature, however numeric models supported by high quality data are rare to nonexistent. This paper presents three-dimensional (3-D) dolomitization patterns in the Salina Group A-1 Carbonate Unit and A-2 Carbonate Unit located in Sombra Township, Lambton County. The source data consists of percent dolomite measurements collected from 9727 drill cutting samples, sta
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Chidsey, Thomas C., David E. Eby, Michael D. Vanden Berg, and Douglas A. Sprinkel. Microbial Carbonate Reservoirs and Analogs from Utah. Utah Geological Survey, 2021. http://dx.doi.org/10.34191/ss-168.

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Multiple oil discoveries reveal the global scale and economic importance of a distinctive reservoir type composed of possible microbial lacustrine carbonates like the Lower Cretaceous pre-salt reservoirs in deepwater offshore Brazil and Angola. Marine microbialite reservoirs are also important in the Neoproterozoic to lowest Cambrian starta of the South Oman Salt Basin as well as large Paleozoic deposits including those in the Caspian Basin of Kazakhstan (e.g., Tengiz field), and the Cedar Creek Anticline fields and Ordovician Red River “B” horizontal play of the Williston Basin in Montana and
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Robert, F. Quartz-carbonate vein gold. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/208002.

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Jansa, L. F. Lithostratigraphy 10: carbonate buildup morphology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210648.

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6

Yuh, C. Y., C. M. Haung, and R. Johnsen. Carbonate fuel cell matrix strengthening. Office of Scientific and Technical Information (OSTI), 1995. http://dx.doi.org/10.2172/171342.

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7

Mills, R., and R. Coyle. DTA/DSC studies of phase equilibria in binary mixtures of barium carbonate with alkali carbonates. Office of Scientific and Technical Information (OSTI), 1987. http://dx.doi.org/10.2172/6302654.

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8

Salad Hersi, O., and D. Lavoie. Pre-Cairnside Formation carbonate-rich sandstone: evidence for a Cambrian carbonate platform in southwestern Quebec? Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/211172.

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9

Kishore K. Mohanty. Dilute Surfactant Methods for Carbonate Formations. Office of Scientific and Technical Information (OSTI), 2004. http://dx.doi.org/10.2172/910178.

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Kishore K. Mohanty. Dilute Surfactant Methods for Carbonate Formations. Office of Scientific and Technical Information (OSTI), 2004. http://dx.doi.org/10.2172/910179.

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