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Relevant bibliographies by topics / Marine carbonate system

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Academic literature on the topic 'Marine carbonate system'

Author: Grafiati

Published: 4 June 2021

Last updated: 8 February 2022

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Journal articles on the topic "Marine carbonate system"

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Mahjoubi, Rachida, Saïd Kamel, Yves Noack, Annie Michard, Daniel Nahon, and Christian Carruesco. "Sr isotopic tracing in a lagoonal system : example of surficial carbonate sediments in the Nador lagoon (northeastern Morocco)." Bulletin de la Société Géologique de France 176, no. 4 (2005): 373–80. http://dx.doi.org/10.2113/176.4.373.

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Abstract The Nador lagoon is the largest one in Morocco and along the Mediterranean. It is located on the northeastern coast near the Rif chain (North Morocco), and it is surrounded by volcanic and sedimentary rocks of various lithofacies. The watershed has an area of about 2200 km2 and is drained by a dense river network. The lagoon dimension is of 115 km2 (25 x 7.5 km) with a depth not exceeding 8 m. The island barrier is 25 km in length and 350 m in average width. The carbonate fraction is the dominant component of the present-day sedimentation in the Nador lagoon. It represents 13 to 48 %

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triyulianti, iis, I. Nyoman Radiarta, Agung Yunanto, Novia Arinda Pradistya, Fikhrul Islami, and Mutiara R Putri. "The Marine Carbonate System at Maluku and Sulawesi Seas." JFMR-Journal of Fisheries and Marine Research 2, no. 3 (2018): 192–207. http://dx.doi.org/10.21776/ub.jfmr.2018.002.03.8.

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van Loevezijn, Gerard B. S., and J. G. M. Raven. "Facies patterns and depositional processes in two Frasnian mixed siliciclastic-carbonate systems in the Cantabrian Mountains, northwest Spain." Geologos 26, no. 1 (2020): 1–23. http://dx.doi.org/10.2478/logos-2020-0001.

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AbstractRelative sea level fluctuations during the Frasnian generated two shallow-marine, mixed siliciclastic-carbonate successions in the Devonian Asturo-Leonese Basin. Each system represents a third-order sequence-stratigraphical unit deposited in the same basin during comparable extreme greenhouse conditions without nearby fluvial entry points. Depositional control on the siliciclastic and carbonate distribution was driven by relative sea level fluctuations, basin geometry, availability of sand and the way sediment was distributed by shelf currents. Early Variscan flexural bending of the co

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Melzner, Frank, Felix C. Mark, Brad A. Seibel, and Lars Tomanek. "Ocean Acidification and Coastal Marine Invertebrates: Tracking CO2 Effects from Seawater to the Cell." Annual Review of Marine Science 12, no. 1 (2020): 499–523. http://dx.doi.org/10.1146/annurev-marine-010419-010658.

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In the last few decades, numerous studies have investigated the impacts of simulated ocean acidification on marine species and communities, particularly those inhabiting dynamic coastal systems. Despite these research efforts, there are many gaps in our understanding, particularly with respect to physiological mechanisms that lead to pathologies. In this review, we trace how carbonate system disturbances propagate from the coastal environment into marine invertebrates and highlight mechanistic links between these disturbances and organism function. We also point toward several processes relate

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PIROUZ, MORTAZA, GUY SIMPSON, ABBAS BAHROUDI, and ALI AZHDARI. "Neogene sediments and modern depositional environments of the Zagros foreland basin system." Geological Magazine 148, no. 5-6 (2011): 838–53. http://dx.doi.org/10.1017/s0016756811000392.

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AbstractA sedimentological investigation of the Neogene deposits of the Zagros foreland basin in SW Iran reveals a continuous and largely gradational passage from supratidal and sabkha sediments at the base (represented by the Gachsaran Formation) to carbonates and marine marls (Mishan Formation with basal Guri carbonate member) followed by coastal plain and meandering river deposits (Agha Jari Formation) and finally to braided river gravel sheets (Bakhtyari Formation). This vertical succession is interpreted to represent the southward migration of foreland basin depozones (from distal foredee

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Schulz, K. G., J. Barcelos e Ramos, R. E. Zeebe, and U. Riebesell. "CO<sub>2</sub> perturbation experiments: similarities and differences between dissolved inorganic carbon and total alkalinity manipulations." Biogeosciences 6, no. 10 (2009): 2145–53. http://dx.doi.org/10.5194/bg-6-2145-2009.

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Abstract. Increasing atmospheric carbon dioxide (CO2) through human activities and invasion of anthropogenic CO2 into the surface ocean alters the seawater carbonate chemistry, increasing CO2 and bicarbonate (HCO3−) at the expense of carbonate ion (CO32−) concentrations. This redistribution in the dissolved inorganic carbon (DIC) pool decreases pH and carbonate saturation state (Ω). Several components of the carbonate system are considered potential key variables influencing for instance calcium carbonate precipitation in marine calcifiers such as coccolithophores, foraminifera, corals, mollus

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Dubiel, Stanisław, Adam Zubrzycki, Czesław Rybicki, and Michał Maruta. "Application of Dst Interpretation Results by Log – Log Method in the Pore Space Type Estimation for the Upper Jurassic Carbonate Reservoir Rocks of the Carpathian Foredeep Basement / Interpretacja Testów Wykonywanych Rurowymi Próbnikami Złoża – Rpz w Skałach Węglanowych Górnej Jury Podłoża Zapadliska Przedkarpackiego." Archives of Mining Sciences 57, no. 2 (2012): 413–24. http://dx.doi.org/10.2478/v10267-012-0027-0.

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Abstract In the south part of the Carpathian Foredeep basement, between Bochnia and Ropczyce, the Upper Jurassic (Oxfordian, Kimmeridian and Tithonian) carbonate complex plays important role as a hydrocarbon bearing formation. It consists of shallow marine carbonates deposited in environments of the outer carbonate ramp as reef limestones (dolomites), microbial - sponge or coral biostromes and marly or micrite limestones as well. The inner pore space system of these rocks was affected by different diagenetic processes as calcite cementation, dissolution, dolomitization and most probably by tec

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Kaczmarek, K., G. Langer, G. Nehrke, et al. "Boron incorporation in the foraminifer <i>Amphistegina lessonii</i> under a decoupled carbonate chemistry." Biogeosciences 12, no. 6 (2015): 1753–63. http://dx.doi.org/10.5194/bg-12-1753-2015.

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Abstract. A number of studies have shown that the boron isotopic composition (δ11B) and the B / Ca ratio of biogenic carbonates (mostly foraminifers) can serve as proxies for two parameters of the ocean's carbonate chemistry, rendering it possible to calculate the entire carbonate system. However, the B incorporation mechanism into marine carbonates is still not fully understood and analyses of field samples show species-specific and hydrographic effects on the B proxies complicating their application. Identifying the carbonate system parameter influencing boron incorporation is difficult due

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Kaczmarek, K., G. Langer, G. Nehrke, et al. "Boron incorporation in the foraminifer <i>Amphistegina lessonii</i> under a decoupled carbonate chemistry." Biogeosciences Discussions 11, no. 12 (2014): 16743–71. http://dx.doi.org/10.5194/bgd-11-16743-2014.

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Abstract. A number of studies have shown that the boron isotopic composition (δ11B) and the B/Ca ratio of biogenic carbonates (mostly foraminifers) can serve as proxies for two parameters of the ocean's carbonate chemistry, rendering it possible to calculate the entire carbonate system. However, the B incorporation mechanism into marine carbonates is still not fully understood and analyses of field samples show species specific and hydrographic effects on the B proxies complicating their application. Identifying the carbonate system parameter influencing boron incorporation is difficult due to

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Preiss-Daimler, Inga, Stergios D. Zarkogiannis, George Kontakiotis, Rüdiger Henrich, and Assimina Antonarakou. "Paleoceanographic Perturbations and the Marine Carbonate System during the Middle to Late Miocene Carbonate Crash—A Critical Review." Geosciences 11, no. 2 (2021): 94. http://dx.doi.org/10.3390/geosciences11020094.

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This study intends to review and assess the middle to late Miocene Carbonate Crash (CC) events in the low to mid latitudes of the Pacific, Indian, Caribbean and Atlantic Oceans as part of the global paleoceanographic reorganisations between 12 and 9 Ma with an emphasis on record preservation and their relation to mass accumulation rates (MAR). In the Eastern Pacific the accumulation changes in carbonate and opal probably reflect an El-Niño-like state of low productivity, which marks the beginning of the CC-event (11.5 Ma), followed by decreased preservation and influx of corrosive bottom water

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Dissertations / Theses on the topic "Marine carbonate system"

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Beer, Christopher James. "Planktic foraminifera, ocean sediments and the palaeo-marine carbonate system." Thesis, University of Southampton, 2010. https://eprints.soton.ac.uk/208361/.

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Chanson, Mareva. "The Changes of the Carbonate Parameters in the Ocean: Anthropogenic and Natural Processes." Scholarly Repository, 2009. http://scholarlyrepository.miami.edu/oa_dissertations/275.

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Since the industrial revolution, CO sub 2 has increased in the atmosphere and about 40% of the increase has been taken up by the ocean. An artifact of increasing CO sub 2 in the ocean is ocean acidification; it changes the calcium carbonate saturation state, which in turn alters the calcification rate of shelled organisms. The purpose of this dissertation is to estimate the changes in the carbonate system in the oceans, and whether these changes are due to natural (biological activity, chemical transformation or mixing of water masses) or anthropogenic (human activities) perturbations. The

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Weston, Keith. "The effect of coccolithophores and non-calcifying phytoplankton on the marine dissolved inorganic carbonate system." Thesis, University of Southampton, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.242503.

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Gregor, Luke. "Seasonality of the marine carbonate system in the southern Benguela nutrient stoichiometry, alkalinity production, and CO flux." Master's thesis, University of Cape Town, 2012. http://hdl.handle.net/11427/10570.

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Includes bibliographical references.<br>An observational study was undertaken to determine the seasonality of the marine carbonate system of the southern Benguela focusing on three key points: the processes driving bulk stoichiometry, alkalinity production on the continental shelf, and the air-sea flux of CO2. Monthly samples were taken along the St. Helena Bay Monitoring Line in the southern Benguela for ten of the months in 2010. Samples were analysed for dissolved inorganic carbon (DIC) and total alkalinity (TA). Temperature, salinity, oxygen and nutrients were also measured.

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Kaczmarek, Karina [Verfasser], Jelle [Akademischer Betreuer] Bijma, Andrea [Akademischer Betreuer] Koschinsky-Fritsche, and Ingo [Akademischer Betreuer] Horn. "Boron in marine biogenic carbonates as a proxy for the carbonate system / Karina Kaczmarek. Betreuer: Jelle Bijma. Gutachter: Jelle Bijma ; Andrea Koschinsky-Fritsche ; Ingo Horn." Bremen : IRC-Library, Information Resource Center der Jacobs University Bremen, 2015. http://d-nb.info/1087325706/34.

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Cochrane, Dylan. "Stratigraphic and Carbon Isotope Evolution of an Ediacaran Mixed Siliciclastic Deep-Marine Base-of-Slope System, First Isaac Carbonate, Windermere Supergroup, Canadian Cordillera, British Columbia." Thesis, Université d'Ottawa / University of Ottawa, 2018. http://hdl.handle.net/10393/37363.

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The first Isaac carbonate (FIC) is a mixed siliciclastic-carbonate base-of-slope succession in the Neoproterozoic Windermere Supergroup (WSG). Outstanding outcrop exposure at three study areas provided an excellent opportunity to observe the stratigraphic and isotopic evolution of an ancient deepwater mixed turbidite system. Based on lithological and stratal dimensions, the FIC can be subdivided into lower and upper parts suggesting temporal changes in patterns of sediment transport and deposition. δ13Ccarb also changes from -5.2‰ at the base of the FIC to 2.5‰ in the middle and then decreases

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Weeber, Amy. "Seasonal and interannual variability of the marine carbonate system at the ice shelf in the eastern Weddell Gyre and its sensitivity to future ocean acidification." Master's thesis, University of Cape Town, 2012. http://hdl.handle.net/11427/9807.

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Includes bibliographical references.<br>Ocean Acidification through the uptake of anthropogenic CO₂ is resulting in a decrease in surface water carbonate ion concentration, a critical compound for marine calcifying organisms (Fabry et al., 2008; Orr et al., 2005). Natural seasonal variability is predicted to hasten the effects of Ocean Acidification in the Southern Ocean, resulting in possible surface water wintertime aragonite (the more soluble form of calcium carbonate) undersaturation (Ωarag< 1) south of the Antarctic Polar Front by the year 2030 (McNeil and Matear, 2008). An Ocean Acidific

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Wit, Francisca [Verfasser], Ulrich [Akademischer Betreuer] Saint-Paul, Ulrich [Gutachter] Saint-Paul, and Boris [Gutachter] Koch. "Carbon footprints of peatland Degradation : Impacts on soil carbon leaching, aquatic CO2 emissions and the marine carbonate system in Indonesia / Francisca Wit ; Gutachter: Ulrich Saint-Paul, Boris Koch ; Betreuer: Ulrich Saint-Paul." Bremen : Staats- und Universitätsbibliothek Bremen, 2017. http://d-nb.info/114921998X/34.

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Dempsey, Alexandra C. "Global Evaluation of Platform-Top Sedimentary Features." NSUWorks, 2013. http://nsuworks.nova.edu/occ_stuetd/170.

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Remote sensing has transformed coral reef science in the last decades. It is now possible to audit reef health and geomorphology at global scale and very high spatial resolution. This work utilizes the vast and no-cost archive of imagery housed within Google Earth (GE). GE was used to interrogate the morphometric properties (size, shape, complexity, etc) of the components that combine to yield a reef environment (reef structures, sediment sheets, and so forth). The data populated a morphometric database for reefs globally that are partitioned by their architecture. The database has been invest

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Domeij, Hilliges Isak, and Cecilia Stendahl. "Ocean acidification effects on marine organisms : a study of Littorina littorea and Balanus improvisus." Thesis, Högskolan i Halmstad, Sektionen för ekonomi och teknik (SET), 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:hh:diva-17445.

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The world’s oceans are becoming more acid in a process called ocean acidification. The pH of the ocean have already decreased by 0.1 units from pre-industrial time until today. Scientists predict that by the year of 2100 the pH will decrease by as much as 0.4 units. This is a big potential problem to many marine species, because they have developed in such a stable environment that has not changed for millions of years. It is difficult to predict how they might be affected by such a decrease in pH during a relatively short time period. Several studies have been made on marine species exposed t

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Books on the topic "Marine carbonate system"

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Ostermann, Dorinda R. Automated system to measure the carbonate concentration of sediments. Woods Hole Oceanographic Institution, 1990.

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Westphal, Hildegard, Bernhard M. Riegl, and Gregor Paul Eberli. Carbonate depositional systems: Assessing dimensions and controlling parameters : the Bahamas, Belize and the Persian/Arabian Gulf. Springer, 2010.

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Kirchman, David L. Introduction to geomicrobiology. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0013.

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Geomicrobiology, the marriage of geology and microbiology, is about the impact of microbes on Earth materials in terrestrial systems and sediments. Many geomicrobiological processes occur over long timescales. Even the slow growth and low activity of microbes, however, have big effects when added up over millennia. After reviewing the basics of bacteria–surface interactions, the chapter moves on to discussing biomineralization, which is the microbially mediated formation of solid minerals from soluble ions. The role of microbes can vary from merely providing passive surfaces for mineral format

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Book chapters on the topic "Marine carbonate system"

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Millero, F. J. "The Carbonate System in Marine Environments." In Chemical Processes in Marine Environments. Springer Berlin Heidelberg, 2000. http://dx.doi.org/10.1007/978-3-662-04207-6_2.

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Monaco, André, and Patrick Prouzet. "Marine Biosphere, Carbonate Systems and the Carbon Cycle." In Marine Ecosystems. John Wiley & Sons, Inc., 2015. http://dx.doi.org/10.1002/9781119116219.ch1.

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Henriet, J. P., and S. Guidard. "Carbonate Mounds as a Possible Example for Microbial Activity in Geological Processes." In Ocean Margin Systems. Springer Berlin Heidelberg, 2002. http://dx.doi.org/10.1007/978-3-662-05127-6_27.

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Browne, Nicola K., Michael Cuttler, Katie Moon, et al. "Predicting Responses of Geo-ecological Carbonate Reef Systems to Climate Change: A Conceptual Model and Review." In Oceanography and Marine Biology. CRC Press, 2021. http://dx.doi.org/10.1201/9781003138846-4.

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Morse, J. W. "Sedimentary Geochemistry of the Carbonate and Sulphide Systems and their Potential Influence on Toxic Metal Bioavailability." In Chemistry of Marine Water and Sediments. Springer Berlin Heidelberg, 2002. http://dx.doi.org/10.1007/978-3-662-04935-8_7.

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Pomar, Luis, and William C. Ward. "Sea-Level Changes, Carbonate Production and Platform Architecture: The Llucmajor Platform, Mallorca, Spain." In Coastal Systems and Continental Margins. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-015-8583-5_4.

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Osleger, David A. "Depositional Sequences on Upper Cambrian Carbonate Platforms: Variable Sedimentologic Responses to Allogenic Forcing." In Coastal Systems and Continental Margins. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-015-8583-5_9.

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Mallinson, David J., and John S. Compton. "Mixed Carbonate-Siliciclastic Sequence Stratigraphy Utilizing Strontium Isotopes: Deciphering the Miocene Sea-Level History of the Florida Platform." In Coastal Systems and Continental Margins. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-015-8583-5_2.

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Subramanyam, K. S. V., V. Balaram, C. Manikyamba, et al. "Geochemistry of Marine Carbonates from Hole 1394, off the Coast of Montserrat, IODP Expedition-340; Implications on Provenance, Paleoenvironment and Lesser Antilles Arc Migration." In Dynamics of the Earth System: Evolution, Processes and Interactions. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40659-2_6.

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"The Marine Carbonate System." In Oceanography. CRC Press, 1996. http://dx.doi.org/10.1201/9781840765472-18.

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Conference papers on the topic "Marine carbonate system"

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Basurto, Maria-Teresa, Pericles Pilidis, and Richard Hales. "Molten Carbonate Fuel Cell Gas Turbine Combined Cycle for Marine Propulsion: Part A — Design Point Operation." In ASME Turbo Expo 2002: Power for Land, Sea, and Air. ASMEDC, 2002. http://dx.doi.org/10.1115/gt2002-30114.

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Molten Carbonate Fuel Cell/Gas Turbine (MCFC/GT) hybrid power systems could represent a modern, efficient and clean alternative to the currently used marine propulsion systems. The objective of this paper is to present the results of the study of a MCFC/GT hybrid power systems used on marine propulsion. The results are quite promising, but they are subjected to the current uncertainties derived from MCFCs early stage of development. Therefore, the interest of the authors is to summarise the research work done and the results, providing the understanding and a general view of the main concerns,

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Basurto, Maria-Teresa, Pericles Pilidis, and Richard Hales. "Molten Carbonate Fuel Cell Gas Turbine Combined Cycle for Marine Propulsion: Part B — Part Load Operation." In ASME Turbo Expo 2002: Power for Land, Sea, and Air. ASMEDC, 2002. http://dx.doi.org/10.1115/gt2002-30113.

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Molten Carbonate Fuel Cell/Gas Turbine (MCFC/GT) hybrid power systems represent a modern, efficient and clean alternative to the currently used marine propulsion systems. The objective of this paper is to present the results found from the application of MCFC/GT hybrid power systems to marine propulsion, and in particular to present the results of the off-design performance of a COGAFC system (Combined Gas Turbine and Fuel Cell System). The results presented are subjected to the current uncertainties on MCFC power systems derived from its early stage of development. It is, then, the interest o

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Kumar, Pramod, Pratul Kumar Saraswati, Santanu Banerjee, and Anupam Ghosh. "equence Stratigraphic Analysis of a Shallow Marine, Mixed Carbonate-Siliciclastic System, Early Miocene, Kutch." In Recent Studies on the Geology of Kachchh. Geological Society of India, 2016. http://dx.doi.org/10.17491/cgsi/2016/105411.

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Blättler, Clara, John A. Higgins, and Peter K. Swart. "CALCIUM ISOTOPE RATIOS SHOW SPATIAL PATTERNS OF OPEN-SYSTEM MARINE DIAGENESIS IN MALDIVES CARBONATE SEDIMENTS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355991.

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Balsamo, F., D. R. Gröcke, and F. Storti. "Palaeo-fluid Flow History of an Extensional Fault System from Carbonate Concretions in Shallow Marine Sediments, Italy." In 3rd EAGE International Conference on Fault and Top Seals. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143039.

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Orekhova, Natalia, Natalia Orekhova, Eugene Medvedev, Eugene Medvedev, Sergey Konovalov, and Sergey Konovalov. "CARBONATE SYSTEM TRANSFORMATION IN THE SEVASTOPOL BAY (THE BLACK SEA)." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b431683c672.

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A 20% increase of the carbon dioxide concentration in the atmosphere during the last century and a dramatic increase in nutrient load to marine systems due to human activity have resulted in pronounced carbon cycle transformation in coastal areas. Acidification and carbon dioxide increasing in the water column and appearance of oxygen minimum zones are reported for the worldwide coast. This makes ecological assessment of aquatic systems, including key cycles of elements, an important social and scientific task. In this study, we present information on the inorganic part of the carbon cycle and

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Orekhova, Natalia, Natalia Orekhova, Eugene Medvedev, Eugene Medvedev, Sergey Konovalov, and Sergey Konovalov. "CARBONATE SYSTEM TRANSFORMATION IN THE SEVASTOPOL BAY (THE BLACK SEA)." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b93867499f8.32847275.

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A 20% increase of the carbon dioxide concentration in the atmosphere during the last century and a dramatic increase in nutrient load to marine systems due to human activity have resulted in pronounced carbon cycle transformation in coastal areas. Acidification and carbon dioxide increasing in the water column and appearance of oxygen minimum zones are reported for the worldwide coast. This makes ecological assessment of aquatic systems, including key cycles of elements, an important social and scientific task. In this study, we present information on the inorganic part of the carbon cycle and

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Cunningham, Kevin J., Cameron Walker, and Richard L. Westcott. "Near-Surface, Marine Seismic-Reflection Data Define Potential Hydrogeologic Confinement Bypass in the Carbonate Floridan Aquifer System, Southeastern Florida." In SEG Technical Program Expanded Abstracts 2012. Society of Exploration Geophysicists, 2012. http://dx.doi.org/10.1190/segam2012-0638.1.

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Nickens, Anthony, Donald Hoffman, Mark Cervi, and Edward House. "Installation and Planned Testing of the 625 kW Molten Carbonate Ship Service Fuel Cell." In ASME Turbo Expo 2004: Power for Land, Sea, and Air. ASMEDC, 2004. http://dx.doi.org/10.1115/gt2004-54307.

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The U.S. Navy Ship Service Fuel Cell (SSFC) program is approaching the testing phase of the 625 KW molten carbonate ship service fuel cell generator. Testing is scheduled to occur in fiscal year 2005. The objective of the SSFC program is to develop diesel fueled shipboard fuel cell power systems with optimized performance characteristics (cost, weight, volume, and efficiency) which, when considered in the total ship environment, provide superior performance at a competitive cost compared to traditional shipboard generators. Emphasis has been placed on adapting commercially developed fuel cell

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Ghezel-Ayagh, Hossein, Anthony J. Leo, Hans Maru, and Mohammad Farooque. "Overview of Direct Carbonate Fuel Cell Technology and Products Development." In ASME 2003 1st International Conference on Fuel Cell Science, Engineering and Technology. ASMEDC, 2003. http://dx.doi.org/10.1115/fuelcell2003-1697.

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Significant progress has been made in development of power generation products based on carbonate fuel cells. Carbonate fuel cell systems provide high efficiency and ultra-clean power generation from a variety of gaseous, liquid, and solid carbonaceous fuels. The high operating temperature of 650 °C in carbonate fuel cell allows significant system simplification by integrating the internal reforming feature into the fuel cell stack as well as use of the byproduct heat in an efficient bottoming cycle. Direct FuelCell® (DFC®) is a unique version of the carbonate fuel cell, which generates electr

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