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Статті в журналах з теми "Atmospheric carbon dioxide on plants"

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Tamás, András. "The effect of rising concentration of atmospheric carbone dioxide on crop production." Acta Agraria Debreceniensis, no. 67 (February 3, 2016): 81–84. http://dx.doi.org/10.34101/actaagrar/67/1758.

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In the atmosphere, the amount of carbon dioxide and other greenhouse gases are rising in gradually increasing pace since the Industrial Revolution. The rising concentration of atmospheric carbon dioxide (CO2) contributes to global warming, and the changes affect to both the precipitation and the evaporation quantity. Moreover, the concentration of carbon dioxide directly affects the productivity and physiology of plants. The effect of temperature changes on plants is still controversial, although studies have been widely conducted. The C4-type plants react better in this respect than the C3-type plants. However, the C3-type plants respond more richer for the increase of atmospheric carbon dioxide and climate change.
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Arens, Nan Crystal, A. Hope Jahren, and Ronald Amundson. "Can C3 plants faithfully record the carbon isotopic composition of atmospheric carbon dioxide?" Paleobiology 26, no. 1 (2000): 137–64. http://dx.doi.org/10.1666/0094-8373(2000)026<0137:ccpfrt>2.0.co;2.

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Atmospheric carbon dioxide is the raw material for the biosphere. Therefore, changes in the carbon isotopic composition of the atmosphere will influence the terrestrial δ13C signals we interpret. However, reconstructing the atmospheric δ13C value in the geologic past has proven challenging. Land plants sample the isotopic composition of CO2 during photosynthesis. We use a model of carbon isotopic fractionation during C3 photosynthesis, in combination with a meta–data set (519 measurements from 176 species), to show that the δ13C value of atmospheric CO2 can be reconstructed from the isotopic composition of plant tissue. Over a range of pCO2 (198–1300 ppmv), the δ13C value of plant tissue does not vary systematically with atmospheric carbon dioxide concentration. However, environmental factors, such as water stress, can influence the δ13C value of leaf tissue. These factors explained a relatively small portion of variation in the δ13C value of plant tissue in our data set and emerged strongly only when the carbon isotopic composition of the atmosphere was held constant. Members of the Poaceae differed in average δ13C value, but we observed no other differences correlated with plant life form (herbs, trees, shrubs). In contrast, over 90% of the variation the carbon isotopic composition of plant tissue was explained by variation in the δ13C value of the atmosphere under which it was fixed. We use a subset of our data spanning a geologically reasonable range of atmospheric δ13C values (−6.4‰ to −9.6‰) and excluding C3 Poaceae to develop an equation to reconstruct the δ13C value of atmospheric CO2 based on plant values. Reconstructing the δ13C value of atmospheric CO2 in geologic time will facilitate chemostratigraphic correlation in terrestrial sediments, calibrate pCO2 reconstructions based on soil carbonates offer a window into the physiology of ancient plants.
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Cerling, T. E., J. R. Ehleringer, and J. M. Harris. "Carbon dioxide starvation, the development of C4 ecosystems, and mammalian evolution." Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 353, no. 1365 (January 29, 1998): 159–71. http://dx.doi.org/10.1098/rstb.1998.0198.

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The decline of atmospheric carbon dioxide over the last 65 million years (Ma) resulted in the ‘carbon dioxide–starvation’ of terrestrial ecosystems and led to the widespread distribution of C 4 plants, which are less sensitive to carbon dioxide levels than are C 3 plants. Global expansion of C 4 biomass is recorded in the diets of mammals from Asia, Africa, North America, and South America during the interval from about 8 to 5 Ma. This was accompanied by the most significant Cenozoic faunal turnover on each of these continents, indicating that ecological changes at this time were an important factor in mammalian extinction. Further expansion of tropical C 4 biomass in Africa also occurred during the last glacial interval confirming the link between atmospheric carbon dioxide levels and C 4 biomass response. Changes in fauna and flora at the end of the Miocene, and between the last glacial and interglacial, have previously been attributed to changes in aridity; however, an alternative explanation for a global expansion of C 4 biomass is carbon dioxide starvation of C 3 plants when atmospheric carbon dioxide levels dropped below a threshold significant to C 3 plants. Aridity may also have been a factor in the expansion of C 4 ecosystems but one that was secondary to, and perhaps because of, gradually decreasing carbon dioxide concentrations in the atmosphere. Mammalian evolution in the late Neogene, then, may be related to the carbon dioxide starvation of C 3 ecosystems.
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McElwain, J. C. "Do fossil plants signal palaeoatmospheric carbon dioxide concentration in the geological past?" Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 353, no. 1365 (January 29, 1998): 83–96. http://dx.doi.org/10.1098/rstb.1998.0193.

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Fossil, subfossil, and herbarium leaves have been shown to provide a morphological signal of the atmospheric carbon dioxide environment in which they developed by means of their stomatal density and index. An inverse relationship between stomatal density/index and atmospheric carbon dioxide concentration has been documented for all the studies to date concerning fossil and subfossil material. Furthermore, this relationship has been demonstrated experimentally by growing plants under elevated and reducedcarbon dioxide concentrations. To date, the mechanism that controls the stomatal density response to atmospheric carbon dioxide concentration remains unknown. However, stomatal parameters of fossil plants have been successfully used as a proxy indicator of palaeo–carbon dioxide levels. This paper presents new estimates of palaeo–atmospheric carbon dioxide concentrations for the Middle Eocene (Lutetian), based on the stomatal ratios of fossil Lauraceae species from Bournemouth in England. Estimates of atmospheric carbon dioxide concentrations derived from stomatal data from plants of the Early Devonian, Late Carboniferous, Early Permian and Middle Jurassic ages are reviewed in the light of new data. Semi–quantitative palaeo–carbon dioxide estimates based on the stomatal ratio (a ratio of the stomatal index of a fossil plant to that of a selected nearest living equivalent) have in the past relied on the use of a Carboniferous standard. The application of a new standard based on the present–day carbon dioxide level is reported here for comparison. The resultant ranges of palaeo–carbon dioxide estimates made from standardized fossil stomatal ratio data are in good agreement with both carbon isotopic data from terrestrial and marine sources and long–term carbon cycle modelling estimates for all the time periods studied. These data indicate elevated atmospheric carbon dioxide concentrations during the Early Devonian, Middle Jurassic and Middle Eocene, and reduced concentrations during the Late Carboniferous and Early Permian. Such data are important in demonstrating the long–term responses of plants to changing carbon dioxide concentrations and in contributing to the database needed for general circulation model climatic analogues.
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Long, Stephen P., Elizabeth A. Ainsworth, Alistair Rogers, and Donald R. Ort. "RISING ATMOSPHERIC CARBON DIOXIDE: Plants FACE the Future." Annual Review of Plant Biology 55, no. 1 (June 2, 2004): 591–628. http://dx.doi.org/10.1146/annurev.arplant.55.031903.141610.

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Tamás, András, Ágnes Törő, Tamás Rátonyi, and Endre Harsányi. "Responses of pea (Pisum sativum L.) to the rising atmospheric concentration of carbon-dioxide." Acta Agraria Debreceniensis, no. 72 (May 16, 2017): 185–88. http://dx.doi.org/10.34101/actaagrar/72/1613.

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The atmospheric concentration of carbon dioxide increases from decade to decade in increasing pace. In 1957, atmospheric carbon dioxide levels were around 315 ppm, while in 2012 it amounted to 394.49 ppm concentration. In parallel, the global temperature is rising,which is projected to average 1.5–4.5 °C. The carbon dioxide concentration is a key factor – in interaction with the light – affects the plant's photosynthesis. Among the various factors significant interactions prevail: environmental factors affect - the growth and the development of plants, leaf area size and composition, the function of the photosynthetic apparatus, the duration of growing season.
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Radmilović-Radjenović, Marija, Martin Sabo, and Branislav Radjenović. "Transport Characteristics of the Electrification and Lightning of the Gas Mixture Representing the Atmospheres of the Solar System Planets." Atmosphere 12, no. 4 (March 29, 2021): 438. http://dx.doi.org/10.3390/atmos12040438.

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Electrification represents a fundamental process in planetary atmospheres, widespread in the Solar System. The atmospheres of the terrestrial planets (Venus, Earth, and Mars) range from thin to thick are rich in heavier gases and gaseous compounds, such as carbon dioxide, nitrogen, oxygen, argon, sodium, sulfur dioxide, and carbon monoxide. The Jovian planets (Jupiter, Saturn, Uranus, and Neptune) have thick atmospheres mainly composed of hydrogen and helium involving. The electrical discharge processes occur in the planetary atmospheres leading to potential hazards due to arcing on landers and rovers. Lightning does not only affect the atmospheric chemical composition but also has been involved in the origin of life in the terrestrial atmosphere. This paper is dealing with the transport parameters and the breakdown voltage curves of the gas compositions representing atmospheres of the planets of the Solar System. Ionization coefficients, electron energy distribution functions, and the mean energy of the atmospheric gas mixtures have been calculated by BOLSIG+. Transport parameters of the carbon dioxide rich atmospheric compositions are similar but differ from those of the Earth’s atmosphere. Small differences between parameters of the Solar System’s outer planets can be explained by a small abundance of their constituent gases as compared to the abundance of hydrogen. Based on the fit of the reduced effective ionization coefficient, the breakdown voltage curves for atmospheric mixtures have been plotted. It was found that the breakdown voltage curves corresponding to the atmospheres of Solar System planets follow the standard scaling law. Results of calculations satisfactorily agree with the available data from the literature. The minimal and the maximal value of the voltage required to trigger electric breakdown is obtained for the Martian and Jupiter atmospheres, respectively.
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Berner, Robert A. "The carbon cycle and carbon dioxide over Phanerozoic time: the role of land plants." Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 353, no. 1365 (January 29, 1998): 75–82. http://dx.doi.org/10.1098/rstb.1998.0192.

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A model (GEOCARB) of the long–term, or multimillion year, carbon cycle has been constructed which includes quantitative treatment of (1) uptake of atmospheric CO 2 by the weathering of silicate and carbonate rocks on the continents, and the deposition of carbonate minerals and organic matter in oceanic sediments; and (2) the release of CO 2 to the atmosphere via the weathering of kerogen in sedimentary rocks and degassing resulting from the volcanic–metamorphic–diagenetic breakdown of carbonates and organic matter at depth. Sensitivity analysis indicates that an important factor affecting CO 2 was the rise of vascular plants in the Palaeozoic. A large Devonian drop in CO 2 was brought about primarily by the acceleration of weathering of silicate rock by the development of deeply rooted plants in well–drained upland soils. The quantitative effect of this accelerated weathering has been crudely estimated by present–day field studies where all factors affecting weathering, other than the presence or absence of vascular plants, have been held relatively constant. An important additional factor, bringing about a further CO 2 drop into the Carboniferous and Permian, was enhanced burial of organic matter in sediments, due probably to the production of microbially resistant plant remains (e.g. lignin). Phanerozoic palaeolevels of atmospheric CO 2 calculated from the GEOCARB model generally agree with independent estimates based on measurements of the carbon isotopic composition of palaeosols and the stomatal index for fossil plants. Correlation of CO 2 levels with estimates of palaeoclimate suggests that the atmospheric greenhouse effect has been a major factor in controlling global climate over the past 600 million years.
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Koriesh, E. "ORNAMENTAL PLANTS AND CLIMATE CHANGE: CARBON DIOXIDE AND ATMOSPHERIC TEMPERATURE." Scientific Journal of Flowers and Ornamental Plants 7, no. 1 (March 1, 2020): 71–76. http://dx.doi.org/10.21608/sjfop.2020.91398.

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Martinez, Carlos Alberto, Eduardo Augusto Dias de Oliveira, Tathyana Rachel Palo Mello, and Ana Lilia Alzate-Marin. "Plants responses to increase in atmospheric carbon dioxide and temperature." Revista Brasileira de Geografia Física 8 (2015): 635–50. http://dx.doi.org/10.5935/1984-2295.20150020.

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Дисертації з теми "Atmospheric carbon dioxide on plants"

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Pangga, Ireneo B. "Effects of elevated CO2 on plant architecture of Stylosanthes scabra and epidemiology of anthracnose disease /." [St. Lucia, Qld.], 2001. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe16215.pdf.

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Cheng, Yufu. "Effects of manipulated atmospheric carbon dioxide concentrations on carbon dioxide and water vapor fluxes in Southern California chaparral /." For electronic version search Digital dissertations database. Restricted to UC campuses. Access is free to UC campus dissertations, 2003. http://uclibs.org/PID/11984.

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Анотація:
Thesis (Ph. D.)--University of California, Davis and San Diego State University, 2003.
Includes bibliographical references (leaves 95-101). Also available via the World Wide Web. (Restricted to UC campuses).
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McElwain, Jennifer Claire. "Fossil stomatal parameters as indicators of palaeo-atmospheric CO2 concentration through Phanerozoic time." Thesis, Royal Holloway, University of London, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.362713.

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Haworth, Matthew. "Mesozoic atmospheric carbon dioxide concentrations from fossil plant cutucles." Thesis, University of Oxford, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.442779.

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Sey, Benjamin Kweku. "Carbon dioxide and nitrous oxide production from corn and soybean agroecosystems." Thesis, McGill University, 2006. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=102726.

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Globally, an estimated 25% of the CO2 and 90% of the N2O is believed to come from agroecosystems. The objective of this study was to investigate the dynamics of the below-ground CO 2 and N2O concentrations and efflux in corn and soybean systems. In our field study, changes in the below-ground concentrations of CO 2 and N2O were closely related to seasonal changes in soil moisture, with the first two months of the growing season being particularly critical to the production of these gases. Tillage significantly increased CO2 content in the soil profile, however, this effect was greater in the soybean plots than in the corn plots. In our greenhouse studies, an average of about 79% of the soil respiration in corn came from rhizosphere respiration, compared to an estimated 58% in the case of soybean. Specific rhizosphere respiration was significantly higher in soybean (0.29 mg C g -1 root h-1) than corn (0.09 mg C g-1 root h-1), which supports previous observations made with regards to slower-growing plants (e.g. soybean) having relatively higher root respiration than faster growing plants. We observed a nonsignificant difference between N2O efflux in the soybean-planted soil and unplanted bulk soil, which is in contrast to the perception that legumes could stimulate more N 2O production from the soil by increasing the N pool through N 2 fixation. While corn had the greatest uptake of fertilizer N, N 2O efflux in corn pots was higher (2.84 mug N pot-1 h-1) than the soybean pots (0.06 mug N pot-1 h-1). In the laboratory setting, denitrification in the microaggregates proceeded at about 4.4 to 39.6 times higher rate than in large macroaggregates, small macroaggregates or the bulk soil, and showed the greatest response to high moisture levels (80% WFPS).
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Camenzuli, Michelle. "The effect of elevated atmospheric carbon dioxide mixing ratios on the emission of Volatile organic compounds from Corymbia citriodora and Tristaniopsis laurina." Master's thesis, Australia : Macquarie University, 2008. http://hdl.handle.net/1959.14/45386.

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Анотація:
Thesis (MSc) -- Macquarie University, Division of Environmental and Life Sciences, Dept. of Chemistry and Biomolecular Sciences, 2008.
Bibliography: p. 120-124.
Introduction -- Environmental factors affecting the emission of biogenic Volatile organic compounds -- Materials and experimental procedures -- Quantification using sold-phase microextraction in a dynamic system: technique development -- The emission profile of Tristaniopsis laurina -- Study of the effect of elevated atmospheric CO₂ levels on the emission of BVOCS from Australian native plants -- Conclusions and future work.
Biogenic Volatile Organic Compounds (BVOCs) emitted by plants can affect the climate and play important roles in the chemistry of the troposphere. As ambient atmospheric carbon dioxide (CO₂) levels are rapidly increasing knowledge of the effect of elevated atmospheric CO₂ on plant BVOC emissions is necessary for the development of global climate models. -- During this study, the effect of elevated atmospheric CO2 mixing ratios on BVOC emissions from Corymbia citriodora (Lemon Scented Gum) and Tristaniopsis laurina (Water Gum) was determined for the first time through the combination of Solid-Phase Microextraction (SPME), Gas Chromatography-Flame Ionisation Detection (GC-FID), Gas Chromatography-Mass Spectrometry (GC-MS) and an environment chamber. For C. citriodora elevated atmospheric CO₂ led to a decrease in the emission rate of α-pinene, β-pinene, eucalyptol, citronellal and β-caryophyllene, however, elevated CO₂ had no effect on the emission rate of citronellol. The emission profile of T. laurina has been determined for the first time. For T. laurina elevated CO₂ led to a decrease in the emission rate of α-pinene but the emission rates of β-pinene, limonene, eucalyptol and citronellol were unaffected. The results obtained in this work confirm that the effect of elevated atmospheric CO₂ on plant BVOC emissions is species-specific.
Mode of access: World Wide Web.
124 leaves ill. (some col.)
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Pepper, David A. "Investigation of the long term physiological response of Huon pine (Lagarostrobos franklinii) to changes in atmospheric CO2 and climate using stable isotopes." Connect to full text, 1999. http://ses.library.usyd.edu.au/handle/2123/4032.

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Анотація:
Thesis (Ph. D.)--University of Sydney, 2000.
Title from title screen (viewed February 12, 2009). Submitted in fulfilment of the requirements for the degree of Doctor of Philosophy to the School of Biological Sciences, Faculty of Science. Degree awarded 2000; thesis submitted 1999. The 2 in the title is in subscript. Includes bibliographical references. Also available in print form.
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Nightingale, Joanne M. "Modelling carbon dynamics within tropical rainforest environments using the 3-PG and 3-PGS ecosystem process models /." [St. Lucia, Qld.], 2004. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe18498.pdf.

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Sharabaroff, Alexander M. "An assessment of the impact of the deregulation of the electric power sector in the U. S. on the efficiency of electricity generation and the level of emissions attributed to electricity generation." Ohio : Ohio University, 2008. http://www.ohiolink.edu/etd/view.cgi?ohiou1210903115.

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Cabena, Lori E. "Vascular land plant isolates from near-shore sediments and implications for stable isotope determination of the paleoatmosphere." Thesis, Georgia Institute of Technology, 1999. http://hdl.handle.net/1853/25882.

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Книги з теми "Atmospheric carbon dioxide on plants"

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Carbon dioxide and plant responses. Taunton, Somerset, England: Research Studies Press, 1997.

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W, Koch George, and Mooney Harold A, eds. Carbon dioxide and terrestrial ecosystems. San Diego: Academic Press, 1996.

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Kirkham, M. B. Elevated Carbon Dioxide: Impacts on Soil and Plant Water Relations. Hoboken: CRC Press, 2011.

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H, Allen L., Viney Marian K, ASA Working Group on Global Climate Changes., American Society of Agronomy. Division A-3., Crop Science Society of America. Division C-2., Crop Science Society of America. Division C-3., and Soil Science Society of America. Division S-7., eds. Advances in carbon dioxide effects research: Proceedings of a symposium. Madison, Wis: American Society of Agronomy, 1997.

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Symposium: Carbon Dioxide and Vegetation: Advanced International Approaches for Absorption of CO₂ and Responses to CO₂ (1999 Tsukuba Kenkyū Gakuen Toshi, Japan). Carbon Dioxide and Vegetation: Advanced International Approaches for Absorption of CO₂ and Responses to CO₂: The 13th Global Environment Tsukuba. [Tsukuba, Japan]: Center for Global Environmental Research, National Institute for Environmental Studies, Ministry of the Environment, 2001.

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DiNicola, Anthony. Carbon dioxide offset investment in the Asia-Pacific forestry sector: Opportunities and constraints. Bangkok, Thailand: Food and Agriculture Organization of the United Nations, 1998.

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Smith, Curtis Peter, and University of Michigan. Biological Station., eds. Belowground responses to rising atmospheric CO2: Implications for plants, soil biota, and ecosystem processes. Dordrecht: Kluwer Academic, 1995.

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Health, United States Congress House Committee on Resources Subcommittee on Forests and Forest. H. Con. Res. 151: Hearing before the Subcommittee on Forest and Forest Health of the Committee on Resources, House of Representatives, One Hundred Fifth Congress, first session, on H. Con. Res. 151 ... September 18, 1997, Washington, DC. Washington: U.S. G.P.O., 1998.

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Mackey, Brendan. Green Carbon: The role of natural forests in carbon storage. Canberra: ANU Press, 2008.

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Mackey, Brendan. Green carbon: The role of natural forests in carbon storage. Canberra, ACT: ANU E Press, 2008.

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Частини книг з теми "Atmospheric carbon dioxide on plants"

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Uprety, D. C., A. P. Mitra, S. C. Garg, B. Kimball, and D. Lawlor. "Rising Atmospheric Carbon Dioxide and Crop Responses." In Plant Breeding, 749–58. Dordrecht: Springer Netherlands, 2004. http://dx.doi.org/10.1007/978-94-007-1040-5_31.

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Agrawal, M., and S. S. Deepak. "Elevated Atmospheric Carbon Dioxide and Plant Responses." In Environmental Stress: Indication, Mitigation and Eco-conservation, 89–102. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-015-9532-2_8.

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Rozema, J., G. M. Lenssen, R. A. Broekman, and W. P. Arp. "Effects of Atmospheric Carbon Dioxide Enrichment on Salt-Marsh Plants." In Expected Effects of Climatic Change on Marine Coastal Ecosystems, 49–54. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-2003-3_7.

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O’Neill, Elizabeth G. "Responses of soil biota to elevated atmospheric carbon dioxide." In Belowground Responses to Rising Atmospheric CO2: Implications for Plants, Soil Biota, and Ecosystem Processes, 55–65. Dordrecht: Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-017-0851-7_6.

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Sivak, M. N. "Past and Present: Long Term Changes in Atmospheric CO2 Concentration and Plant Strategies for the Optimisation of Photosynthesis." In Carbon Dioxide as a Source of Carbon, 213–36. Dordrecht: Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-009-3923-3_12.

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Rogers, Hugo H., G. Brett Runion, Sagar V. Krupa, and Stephen A. Prior. "Plant Responses to Atmospheric Carbon Dioxide Enrichment: Implications in Root-Soil-Microbe Interactions." In Advances in Carbon Dioxide Effects Research, 1–34. Madison, WI, USA: American Society of Agronomy, Crop Science Society of America, Soil Science Society of America, 2015. http://dx.doi.org/10.2134/asaspecpub61.c1.

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Norby, Richard J. "Issues and perspectives for investigating root responses to elevated atmospheric carbon dioxide." In Belowground Responses to Rising Atmospheric CO2: Implications for Plants, Soil Biota, and Ecosystem Processes, 9–20. Dordrecht: Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-017-0851-7_2.

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Rozema, J. "Plant responses to atmospheric carbon dioxide enrichment: interactions with some soil and atmospheric conditions." In CO2 and biosphere, 173–92. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-1797-5_12.

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Idso, Keith E., and Sherwood B. Idso. "A Synopsis of a Major Review of Plant Responses to Rising Levels of Atmospheric Carbon Dioxide in the Presence of Unfavorable Growing Conditions." In Advances in Carbon Dioxide Effects Research, 131–39. Madison, WI, USA: American Society of Agronomy, Crop Science Society of America, Soil Science Society of America, 2015. http://dx.doi.org/10.2134/asaspecpub61.c6.

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Van De Geijn, Siebe C., and Paul Dijkstra. "Physiological effects of changes in atmospheric carbon dioxide concentration and temperature on growth and water relations of crop plants." In Potato Ecology And modelling of crops under conditions limiting growth, 89–99. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0051-9_6.

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Тези доповідей конференцій з теми "Atmospheric carbon dioxide on plants"

1

Heydari, Ali, and V. P. Carey. "Boiling Curve Measurement of Water Containing Dissolved Carbon Dioxide Around a Heated Wire." In ASME 2001 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2001. http://dx.doi.org/10.1115/imece2001/htd-24131.

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Анотація:
Abstract Proper thermal treatment of metals in metal processing plants is important both in terms of quality and economy of the final product. Addition of a highly soluble gas such as carbon dioxide to water has been shown to create an excellent quenching medium for metal objects in metal working processes. It causes slower rate of cooling due to the insulating effect of carbon dioxide on the surface of immersed metal objects which as a result hinders residual stress build up and warpage commonly observed in quenching metal objects in cold water. Additionally, absence of carbon dioxide-filled bubbles on the surface of quenching metal object causes cold water-like cooling of the surface, producing rapid cooling of the objects. In this study, boiling heat transfer characteristics of an electrically heated wire immersed in water mixed with different concentrations of carbon dioxide at various atmospheric and sub-atmospheric pressures are obtained and compared. The results indicate that the boiling behavior and heat transfer characteristics of carbon dioxide-water solution make it a favorable substitute to cold and hot water traditionally used as the heat transfer fluid in metal processing plants.
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2

Martinez-Frias, Joel, Salvador M. Aceves, J. Ray Smith, and Harry Brandt. "Thermodynamic Analysis of Zero-Atmospheric Emissions Power Plant." In ASME 2002 International Mechanical Engineering Congress and Exposition. ASMEDC, 2002. http://dx.doi.org/10.1115/imece2002-33199.

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This paper presents a thermodynamic analysis of a natural gas zero-atmospheric emissions power plant with a net electrical output of 400 MW. In this power plant, methane is combusted with oxygen in a gas generator to produce the working fluid for the turbines. The combustion produces a gas mixture composed of steam and carbon dioxide. These gases drive multiple turbines to produce electricity. The turbine discharge gases pass to a condenser where water is captured as liquid and gaseous carbon dioxide is pumped from the system. The carbon dioxide can be economically conditioned for enhanced recovery of oil, or coal-bed methane, or for sequestration in a subterranean formation. The analysis considers a complete power plant layout, including an air separation unit, compressors and intercoolers for oxygen and methane compression, a gas generator, three steam turbines, a reheater, a preheater, a condenser, and a carbon dioxide pumping system to pump the carbon dioxide to the pressure required for sequestration. The computer code is a powerful tool for estimating the efficiency of the plant, given different configurations and technologies. The efficiency of the power plant has been calculated over a wide range of conditions as a function of the two important power plant parameters of turbine inlet temperature and turbine isentropic efficiency. This simulation is based on a 400 MW electric power generating plant that uses turbines that are currently under development by a U.S. turbine manufacturer. The high-pressure turbine would operate at a temperature of 1089 K (1500 °F) with uncooled blades, the intermediate-pressure turbine would operate at 1478 K (2200 °F) with cooled blades and the low-pressure turbine would operate at 998 K (1336 °F). The corresponding turbine isentropic efficiencies for these three turbines were taken as 90, 91 and 93 percent. With these operating conditions, the zero-atmospheric emissions electric power plant has a net thermal efficiency of 46.5%. This net thermal efficiency is based on the lower heating value of methane, and includes the energy necessary for air separation and for carbon dioxide separation and sequestration.
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3

Jackson, Anthony J. B., Alcides Codeceira Neto, Matthew W. Whellens, and Harry Audus. "Gas Turbine Performance Using Carbon Dioxide as Working Fluid in Closed Cycle Operation." In ASME Turbo Expo 2000: Power for Land, Sea, and Air. American Society of Mechanical Engineers, 2000. http://dx.doi.org/10.1115/2000-gt-0153.

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The world’s main atmospheric “greenhouse gas” is carbon dioxide (CO2). The CO2 content of the atmosphere continues to rise due to increasing world demand for energy, and thus further means are needed to achieve its abatement. Most gas turbine powered electricity generating plants use hydro-carbon fuels and this inevitably produces CO2 in the engine exhaust. This paper discusses a scheme for concentrating the gas turbine exhaust CO2, thus facilitating its extraction. The scheme is a gas turbine operating synchronously in closed cycle, with CO2 as the working fluid. The additional CO2 and water produced in the combustion process are removed continuously. CO2 and air have substantially different gas properties. This significantly affects the performance of the gas turbine. It is shown that any gas turbine designed to use air, and operating synchronously, would need considerable modifications to its compressor and combustion systems to use carbon dioxide as its working fluid.
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Moore, J. Jeffrey, and Marybeth G. Nored. "Novel Concepts for the Compression of Large Volumes of Carbon Dioxide." In ASME Turbo Expo 2008: Power for Land, Sea, and Air. ASMEDC, 2008. http://dx.doi.org/10.1115/gt2008-50924.

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In order to reduce the amount of carbon dioxide (CO2) greenhouse gases released into the atmosphere, significant consideration has been given to the sequestration of CO2 from power plants and other major producers of greenhouse gas emissions. Integrated Gasification Combined Cycle (IGCC) power plants offer an alternative to pulverized coal plants because the carbon dioxide may be separated from the process gas stream prior to combustion. The compression of the captured carbon dioxide stream requires a sizeable amount of power, which impacts plant availability, capital expenditures and operational cost. Preliminary analysis has estimated that the CO2 compression process reduces the plant efficiency by 8% to 12% for a typical IGCC plant. The detailed thermodynamic analysis presented here examines methods to minimize the power penalty to the producer through integrated, low-power compression concepts. The goal of the present research is to reduce this penalty through novel compression concepts and integration with existing IGCC processes. The research supports the U.S. Department of Energy (DOE) National Energy Technology Laboratory (NETL) objectives of reducing the energy requirements for carbon capture and sequestration in electrical power production. The primary objective of this study is to boost the pressure of CO2 to pipeline pressures with the minimal amount of energy required. Fundamental thermodynamic analysis methods related to the compression of CO2 are used in the following paper to explore pressure and enthalpy rise in both liquid and gaseous states.
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Martinez-Frias, Joel, Salvador M. Aceves, J. Ray Smith, and Harry Brandt. "A Coal-Fired Power Plant With Zero Atmospheric Emissions." In ASME 2003 International Mechanical Engineering Congress and Exposition. ASMEDC, 2003. http://dx.doi.org/10.1115/imece2003-43923.

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This paper presents the thermodynamic analysis of a coal-based zero-atmospheric emissions electric power plant. The approach involves an oxygen-blown coal gasification unit. The resulting synthetic gas (syngas) is combusted with oxygen in a gas generator to produce the working fluid for the turbines. The combustion produces a gas mixture composed almost entirely of steam and carbon dioxide. These gases drive multiple turbines to produce electricity. The turbine discharge gases pass to a condenser where water is captured. A stream of carbon dioxide then results that can be used for enhanced oil recovery, or for sequestration. This analysis is based on a 400 MW electric power generating plant that uses turbines that are currently under development by a U.S. turbine manufacturer. The power plant has a net thermal efficiency of 42.6%. This efficiency is based on the lower heating value of the coal, and includes the energy necessary for coal gasification, air separation and for carbon dioxide separation and sequestration. The paper also presents an analysis of the cost of electricity (COE) and the cost of conditioning carbon dioxide for sequestration for the 400 MW power plant. Electricity cost is compared for three different gasification processes (Texaco, Shell, and Koppers-Totzek) and two types of coals (Illinois #6 and Wyodak). Cost of electricity ranges from 5.16 ¢/kWhr to 5.42 ¢/kWhr, indicating very little sensitivity to the gasification processes considered and the coal types used.
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Vyas, Dr Amit Kumar. "Potential Of Reduction Of Carbon Dioxide Gas Emissions In The Thar Desert By Kheemp (Leptadenia Pyrotechnia) Conservation Based Carbon Farming." In 7th GoGreen Summit 2021. Technoarete, 2021. http://dx.doi.org/10.36647/978-93-92106-02-6.3.

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Due to the climate change happening on the earth, the immunity of both humans and animals is decreasing along with this the plants are also getting affected. The main reason for which is the continuous increase in the temperature of the earth. The main reason for the increase in temperature is anthropogenic action, due to which carbon dioxide is emitted in high quantity in the atmosphere and this generates greenhouse effect. Due to the excessive emission of carbon dioxide, frequent changes in the climate are happening very fast and their ill effects are clearly visible. Due to this, the frequency of natural disasters is also increasing and their area is also increasing, due to which the biodiversity is also being lost. Because only natural plants have the amazing ability to prevent negative changes in the climate and adjust by absorbing carbon dioxide emitted in large quantities. In this sequence, there is an urgent need to implement the possibilities of reducing carbon dioxide emissions by cultivating carbon farming from the dry shrub Kheemp (Lepatadenia pyrotechnica), which is found abundantly in the Thar Desert.
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7

Hong, Jongsup, Ahmed F. Ghoniem, Randall Field, and Marco Gazzino. "Techno-Economic Evaluation of Pressurized Oxy-Fuel Combustion Systems." In ASME 2010 International Mechanical Engineering Congress and Exposition. ASMEDC, 2010. http://dx.doi.org/10.1115/imece2010-38002.

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Oxy-fuel combustion coal-fired power plants can achieve significant reduction in carbon dioxide emissions, but at the cost of lowering their efficiency. Research and development are conducted to reduce the efficiency penalty and to improve their reliability. High-pressure oxy-fuel combustion has been shown to improve the overall performance by recuperating more of the fuel enthalpy into the power cycle. In our previous papers, we demonstrated how pressurized oxy-fuel combustion indeed achieves higher net efficiency than that of conventional atmospheric oxy-fuel power cycles. The system utilizes a cryogenic air separation unit, a carbon dioxide purification/compression unit, and flue gas recirculation system, adding to its cost. In this study, we perform a techno-economic feasibility study of pressurized oxy-fuel combustion power systems. A number of reports and papers have been used to develop reliable models which can predict the costs of power plant components, its operation, and carbon dioxide capture specific systems, etc. We evaluate different metrics including capital investments, cost of electricity, and CO2 avoidance costs. Based on our cost analysis, we show that the pressurized oxy-fuel power system is an effective solution in comparison to other carbon dioxide capture technologies. The higher heat recovery displaces some of the regeneration components of the feedwater system. Moreover, pressurized operating conditions lead to reduction in the size of several other critical components. Sensitivity analysis with respect to important parameters such as coal price and plant capacity is performed. The analysis suggests a guideline to operate pressurized oxy-fuel combustion power plants in a more cost-effective way.
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8

Gambini, Marco, and Michela Vellini. "Conventional Power Plants Equipped With Systems for CO2 Emission Abatement." In ASME 2008 International Mechanical Engineering Congress and Exposition. ASMEDC, 2008. http://dx.doi.org/10.1115/imece2008-66471.

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This paper presents the results from an evaluation of the performance and cost of Italian power plants (a steam cycle power plants — 500 MW — fed by coal and a combined cycle power plant — 300 MW — fed by natural gas) with CO2 emissions control equipment to achieve a fixed reduction in atmospheric discharge of carbon dioxide (CO2) and so to accomplish the CO2 emission targets established by the Kyoto Protocol. The reduction of the CO2 content in the flue gas is achieved by amine scrubbing (CO2 removal), removal of water from CO2 (drying), compression to pipeline pressure; transport and storage are not considered. The paper presents an economic evaluation of the CO2 abatement cost and compares it with the cost of allowances in the Emission Trading System and with the payment of the penalty for the emissions in excess when there is no CO2 quota available on the market.
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9

Neithalath, Narayanan. "Keynote Speech: Climate and Construction: Chained by Carbon – A Perspective." In International Web Conference in Civil Engineering for a Sustainable Planet. AIJR Publisher, 2021. http://dx.doi.org/10.21467/proceedings.112.keynote2.

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The enormous amounts of carbon dioxide and other greenhouse gases emitted by various industries have resulted in global climate imbalance. The United Nations report that carbon dioxide levels have pushed passed another record threshold, after rising in 2019 at a rate faster than the average for the last 10 years. Climate impacts are compounding threats to human health, security and economic stability posed by COVID-19. Even with pandemic lockdowns slowing economic activity, atmospheric concentrations of greenhouse gases have continued to rise. It is now well known that, to limit global temperature rise to 1.5 degrees Celsius, global emissions must be reduced by 45% by 2030, from 2010 levels. This can be accomplished only through a collective effort where anthropogenic and natural systems are harmonized. From a perspective of construction, a large industry responsible for the well-being and progress of humanity, many actions can be adopted, some of which are listed here.
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Desideri, Umberto, and Stefania Proietti. "CO2 Capture and Removal System for a Gas-Steam Combined Cycle." In ASME 2002 International Mechanical Engineering Congress and Exposition. ASMEDC, 2002. http://dx.doi.org/10.1115/imece2002-33296.

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This paper presents the study of a natural gas fired power cycle which includes a carbon dioxide capture plant based on an absorption and scrubbing system. The interest in this integration is due to the widespread use of combined cycles in the power generation sector because of their high energy conversion efficiency. Energy consumption of the capture and removal system and its influence on the energetic performance of the power plant have been calculated. Mass and heat balance calculations are carried out by using the software tools GateCycle for the combined cycle and Aspen+ Software for the absorption process. Results of plant performance calculations, including compression of the captured carbon dioxide, are presented. The results, compared to the combined cycle power plant with no carbon dioxide capture, have also been compared to the more commonly known carbon dioxide capture process based on atmospheric absorption with MEA.
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Звіти організацій з теми "Atmospheric carbon dioxide on plants"

1

Berner, Robert A. Plants, Weathering, and the Evolution of Atmospheric Carbon Dioxide and Oxygen. Office of Scientific and Technical Information (OSTI), February 2008. http://dx.doi.org/10.2172/923048.

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2

Lincoln, D. Herbivore responses to plants grown in enriched carbon dioxide atmospheres. Office of Scientific and Technical Information (OSTI), May 1990. http://dx.doi.org/10.2172/6808774.

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Lincoln, D. E. [Plant responses to elevated atmospheric carbon dioxide and transmission to other trophic levels]. Final report. Office of Scientific and Technical Information (OSTI), October 1995. http://dx.doi.org/10.2172/108099.

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4

Lincoln, D. E. [Plant responses to elevated atmospheric carbon dioxide and transmission to other trophic levels]. Progress report, May 1991, DOE Grant DE-FG09-84ER60255. Office of Scientific and Technical Information (OSTI), May 1991. http://dx.doi.org/10.2172/113934.

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5

Trabalka, J. Atmospheric carbon dioxide and the global carbon cycle. Office of Scientific and Technical Information (OSTI), December 1985. http://dx.doi.org/10.2172/6048470.

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Firestine, M. W. Atmospheric carbon dioxide and the greenhouse effect. Office of Scientific and Technical Information (OSTI), May 1989. http://dx.doi.org/10.2172/5993221.

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Oechel, W. C., and N. E. Grulke. Response of tundra ecosystems to elevated atmospheric carbon dioxide. [Annual report]. Office of Scientific and Technical Information (OSTI), December 1988. http://dx.doi.org/10.2172/230285.

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Cooley, S. R., D. J. P. Moore, S. R. Alin, D. Butman, D. W. Clow, N. H. F. French, R. A. Feely, et al. Chapter 17: Biogeochemical Effects of Rising Atmospheric Carbon Dioxide. Second State of the Carbon Cycle Report. Edited by N. Cavallaro, G. Shrestha, R. Birdsey, M. A. Mayes, R. Najjar, S. Reed, P. Romero-Lankao, and Z. Zhu. U.S. Global Change Research Program, 2018. http://dx.doi.org/10.7930/soccr2.2018.ch17.

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Jacobson, A. R., J. B. Miller, A. Ballantyne, S. Basu, L. Bruhwiler, A. Chatterjee, S. Denning, and L. Ott. Chapter 8: Observations of Atmospheric Carbon Dioxide and Methane. Second State of the Carbon Cycle Report. Edited by N. Cavallaro, G. Shrestha, R. Birdsey, M. A. Mayes, R. Najjar, S. Reed, P. Romero-Lankao, and Z. Zhu. U.S. Global Change Research Program, 2018. http://dx.doi.org/10.7930/soccr2.2018.ch8.

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William Goddard. Low Cost Open-Path Instrument for Monitoring Atmospheric Carbon Dioxide at Sequestration Sites. Office of Scientific and Technical Information (OSTI), September 2008. http://dx.doi.org/10.2172/968337.

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