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Books on the topic 'Dispersed phase'

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Author: Grafiati

Published: 4 June 2021

Last updated: 19 February 2022

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1

Meng, Haoran. On dispersed two phase flows past obstacles. Eindhoven: Eindhoven University of Technology, 1993.

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2

Pullum, Olwen J. The fabrication and analysis of hard Si3N4-based, dispersed phase composites. [s.l.]: typescript, 1993.

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3

Kalis, Aouni A. Liquid phase velocity of turbulent dispersed bubbles flow in large diameter horizontal pipes. Montreal: Ecole polytechnique de Montreal, Departement de genie mecanique, Section mecanique appliquee, 1988.

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4

International Symposium on Two-Phase Annular and Dispersed Flows (1984 University of Pisa). Two-phase annular and dispersed flows: Selected papers presented at the International Symposium on Two-Phase and Dispersed Flows, University of Pisa, Italy, 24-29 June 1984. Edited by Andreussi P, Azzopardi B. J, and Hanratty T. J. Oxford: Pergamon Press, 1985.

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5

Majumdar, Arunava. A study of the ostwald ripening phenomenon of a dispersed phase in a molten salt system. Ottawa: National Library of Canada, 1990.

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6

Morel, Christophe. Mathematical Modeling of Disperse Two-Phase Flows. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-20104-7.

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7

Mols, Bernard Marie. Particle dispersion and deposition in horizontal turbulent channel and tube flows =: Dispersie en depositie van deeltjes in horizontale, turbulente, kanaal- en buisstromingen. Delft: Delft University Press, 1999.

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8

Hanratty, T. Two Phase Annular and Dispersed Flow. Pergamon Pr, 1985.

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9

Sofiane Berrouk, Abdallah, ed. Stochastic Lagrangian Modeling for Large Eddy Simulation of Dispersed Turbulent Two-Phase Flows. BENTHAM SCIENCE PUBLISHERS, 2012. http://dx.doi.org/10.2174/97816080529671110101.

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10

Boer, T. C. de. Heat Transfer to a Dispersed Two Phase Flow and Detailed Quench Front Velocity Research (Nuclear Science and Technology). European Communities / Union (EUR-OP/OOPEC/OPOCE), 1985.

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11

Erez, Miriam. From Local to Cross-Cultural to Global Work Motivation and Innovation. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780190879228.003.0005.

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This chapter examines three phases of a programmatic research on work motivation. Phase one focuses on research on work motivation prior to considering the effect of culture on work motivation. This research identifies two boundary conditions of the goal-setting theory of motivation—knowledge of results, and goal commitment—two necessary conditions for goals to affect performance. It continues to examine the effect of participation in goal setting on goal acceptance and its consequent performance and discovers cross-cultural differences in the effect of participation on goal acceptance and performance. This has opened up phase two, which focuses on cross-cultural differences and similarities in work motivation. Phase three has paralleled the change toward a global, culturally diverse and geographically dispersed work context. This context stimulates new research questions and research paradigms that have specifically focused on understanding how to motivate employees’ behaviors in the global context and enhance their sense of belongingness to their multicultural teams.

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12

Dispersed flow film boiling: An investigation of the possibility to improve the models implemented in the NRC computer codes for the reflooding phase of the LOCA. Washington, DC: Office of Nuclear Regulatory Research, U.S. Nuclear Regulatory Commission, 1992.

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13

Morel, Christophe. Mathematical Modeling of Disperse Two-Phase Flows. Springer, 2015.

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14

Hook, Sharon, Graeme Batley, Michael Holloway, Paul Irving, and Andrew Ross, eds. Oil Spill Monitoring Handbook. CSIRO Publishing, 2016. http://dx.doi.org/10.1071/9781486306350.

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Oil spills can be difficult to manage, with reporting frequently delayed. Too often, by the time responders arrive at the scene, the slick has moved, dissolved, dispersed or sunk. This Oil Spill Monitoring Handbook provides practical advice on what information is likely required following the accidental release of oil or other petroleum-based products into the marine environment. The book focuses on response phase monitoring for maritime spills, otherwise known as Type I or operational monitoring. Response phase monitoring tries to address the questions – what? where? when? how? how much? – that assist responders to find, track, predict and clean up spills, and to assess their efforts. Oil spills often occur in remote, sensitive and logistically difficult locations, often in adverse weather, and the oil can change character and location over time. An effective response requires robust information provided by monitoring, observation, sampling and science. The Oil Spill Monitoring Handbook completely updates the Australian Maritime Safety Authority’s 2003 edition of the same name, taking into account the latest scientific advances in physical, chemical and biological monitoring, many of which have evolved as a consequence of major oil spill disasters in the last decade. It includes sections on the chemical properties of oil, the toxicological impacts of oil exposure, and the impacts of oil exposure on different marine habitats with relevance to Australia and elsewhere. An overview is provided on how monitoring integrates with the oil spill response process, the response organisation, the use of decision-support tools such as net environmental benefit analysis, and some of the most commonly used response technologies. Throughout the text, examples are given of lessons learned from previous oil spill incidents and responses, both local and international. General guidance of spill monitoring approaches and technologies is augmented with in-depth discussion on both response phase and post-response phase monitoring design and delivery. Finally, a set of appendices delivers detailed standard operating procedures for practical observation, sample and data collection. The Oil Spill Monitoring Handbook is essential reading for scientists within the oil industry and environmental and government agencies; individuals with responder roles in industry and government; environmental and ecological monitoring agencies and consultants; and members of the maritime sector in Australia and abroad, including officers in ports, shipping and terminals.

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15

Yakubov, I. T. Thermophysical and Electrophysical Properties of Low-Temperature Plasma with Condensed Disperse Phase (Thermophysical & Electrophysical Properties of Low-Temperatu). Routledge, 1989.

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16

Weninger, Bernhard, and Lee Clare. 6600–6000 cal BC Abrupt Climate Change and Neolithic Dispersal from West Asia. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199329199.003.0003.

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Recent advances in palaeoclimatological and meteorological research, combined with new radiocarbon data from western Anatolia and southeast Europe, lead us to formulate a new hypothesis for the temporal and spatial dispersal of Neolithic lifeways from their core areas of genesis. The new hypothesis, which we term the Abrupt Climate Change (ACC) Neolithization Model, incorporates a number of insights from modern vulnerability theory. We focus here on the Late Neolithic (Anatolian terminology), which is followed in the Balkans by the Early Neolithic (European terminology). From high-resolution 14C-case studies, we infer an initial (very rapid) west-directed movement of early farming communities out of the Central Anatolian Plateau towards the Turkish Aegean littoral. This move is exactly in phase (decadal scale) with the onset of ACC conditions (~6600 cal BC). Upon reaching the Aegean coastline, Neolithic dispersal comes to a halt. It is not until some 500 years later—that is, at the close of cumulative ACC and 8.2 ka cal BP Hudson Bay cold conditions—that there occurs a second abrupt movement of farming communities into Southeast Europe, as far as the Pannonian Basin. The spread of early farming from Anatolia into eastern Central Europe is best explained as Neolithic communities’ mitigation of biophysical and social vulnerability to natural (climate-induced) hazards.

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17

Martin, Colin. Wreck-Site Formation Processes. Edited by Ben Ford, Donny L. Hamilton, and Alexis Catsambis. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780199336005.013.0002.

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The environmental settings within which shipwrecks occur are matters of chance rather than of choice. It is primarily the wreck and not its physical context that is of consequence to nautical archaeologists. No two wreck-site formations are the same, since the complex and interacting variables that constitute the environmental setting, the nature of the ship, and the circumstances of its loss combine to create a set of attributes unique to each site. The dynamic phase, which begins with the event of shipwreck, is characterized by the wreck's status as an environmental anomaly. It is unstable, lacks integration with its surroundings, and is prone to further disintegration and dispersal by external influences. The chemical and physical properties of water cause reactions with the metals. Understanding these natural processes in the context of the distinctively anthropogenic inputs, this article characterizes archaeology as an essential prerequisite to the interpretation of any shipwreck.

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