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Books on the topic 'Laser melting'

Author: Grafiati

Published: 4 June 2021

Last updated: 7 September 2024

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1

Wischeropp, Tim Marten. Advancement of Selective Laser Melting by Laser Beam Shaping. Berlin, Heidelberg: Springer Berlin Heidelberg, 2021. http://dx.doi.org/10.1007/978-3-662-64585-7.

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2

Lau, Marcus. Laser Fragmentation and Melting of Particles. Wiesbaden: Springer Fachmedien Wiesbaden, 2016. http://dx.doi.org/10.1007/978-3-658-14171-4.

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3

Wang, Jin Jimmy. Melting in Superheated Silicon Films Under Pulsed-Laser Irradiation. [New York, N.Y.?]: [publisher not identified], 2016.

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4

Wong, Vernon. 2-D Melting in Excimer-Laser Irradiated Polycrystalline Silicon Films. [New York, N.Y.?]: [publisher not identified], 2021.

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5

Choi, Min Hwan. Pulsed-Laser-Induced Melting and Solidification of Thin Metallic Films. [New York, N.Y.?]: [publisher not identified], 2012.

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6

Sing, Swee Leong. Selective Laser Melting of Novel Titanium-Tantalum Alloy as Orthopaedic Biomaterial. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-2724-7.

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7

Colloque international sur le soudage et la fusion par faisceaux d'électrons et laser (5e 1993 La Baule, Loire-Atlantique, France). 5ème Colloque international sur le soudage et la fusion par faisceaux d'électrons et laser =: 5th International Conference on Welding and Melting by Electron and Laser Beams, La Baule, 14-18 juin 1993. [Saclay]: Commissariat à l'énergie atomique, 1993.

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8

Glazer, Nathan. Beyond the melting pot: Thirty years later. Toronto: Robert F. Harney Professorship and Program in Ethnic, Immigration and Pluralism Studies, University of Toronto, 1991.

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9

Selective Laser Melting. MDPI, 2020. http://dx.doi.org/10.3390/books978-3-03928-579-2.

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10

Wischeropp, Tim Marten. Advancement of Selective Laser Melting by Laser Beam Shaping. Springer Berlin / Heidelberg, 2022.

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11

Lau, Marcus. Laser Fragmentation and Melting of Particles. Springer, 2016.

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12

Lau, Marcus. Laser Fragmentation and Melting of Particles. Springer London, Limited, 2016.

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13

Selective Laser Melting for Metal and Metal Matrix Composites. Elsevier, 2021. http://dx.doi.org/10.1016/c2018-0-01940-4.

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14

Shi, Yusheng, Chunze Yan, Qingsong Wei, Shifeng Wen, and Song Bo. Selective Laser Melting for Metal and Metal Matrix Composites. Elsevier Science & Technology, 2020.

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15

Shi, Yusheng, Chunze Yan, Qingsong Wei, Shifeng Wen, and Song Bo. Selective Laser Melting for Metal and Metal Matrix Composites. Elsevier Science & Technology Books, 2020.

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16

Preston, John Stewart. Nonequilibrium pattern formation in silicon during CW laser induced melting. 1987.

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17

Triply Periodic Minimal Surface Lattices Additively Manufactured by Selective Laser Melting. Elsevier, 2021. http://dx.doi.org/10.1016/c2020-0-01253-3.

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18

Hao, Liang, Lei Yang, Chunze Yan, Zhaoqing Li, and Young Philippe G. Triply Periodic Minimal Surface Lattices Additively Manufactured by Selective Laser Melting. Elsevier Science & Technology Books, 2021.

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19

Sing, Swee Leong. Selective Laser Melting of Novel Titanium-Tantalum Alloy as Orthopaedic Biomaterial. Springer, 2019.

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20

Hao, Liang, Yan Li, Lei Yang, Chunze Yan, Philippe G. Young, and Zhaoqing Li. Triply Periodic Minimal Surface Lattices by Selective Laser Melting Additive Manufacturing. Academic Press, 2021.

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21

Sing, Swee Leong. Selective Laser Melting of Novel Titanium-Tantalum Alloy as Orthopaedic Biomaterial. Springer, 2018.

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22

5eme Colloque international sur le soudage et la fusion par faisceaux d'electrons et laser =: 5th International Conference on Welding and Melting by Electron and Laser Beams, La Baule, 14-18 juin 1993. Commissariat a l'energie atomique, 1993.

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23

Lau, William K. M. Impacts of Aerosols on Climate and Weather in the Hindu-Kush-Himalayas-Gangetic Region. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.590.

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Situated at the southern edge of the Tibetan Plateau (TP), the Hindu-Kush-Himalayas-Gangetic (HKHG) region is under the clear and present danger of climate change. Flash-flood, landslide, and debris flow caused by extreme precipitation, as well as rapidly melting glaciers, threaten the water resources and livelihood of more than 1.2 billion people living in the region. Rapid industrialization and increased populations in recent decades have resulted in severe atmospheric and environmental pollution in the region. Because of its unique topography and dense population, the HKHG is not only a major source of pollution aerosol emissions, but also a major receptor of large quantities of natural dust aerosols transported from the deserts of West Asia and the Middle East during the premonsoon and early monsoon season (April–June). The dust aerosols, combined with local emissions of light-absorbing aerosols, that is, black carbon (BC), organic carbon (OC), and mineral dust, can (a) provide additional powerful heating to the atmosphere and (b) allow more sunlight to penetrate the snow layer by darkening the snow surface. Both effects will lead to accelerated melting of snowpack and glaciers in the HKHG region, amplifying the greenhouse warming effect. In addition, these light-absorbing aerosols can interact with monsoon winds and precipitation, affecting extreme precipitation events in the HKHG, as well as weather variability and climate change over the TP and the greater Asian monsoon region.

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24

Bridges, John C. Evolution of the Martian Crust. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190647926.013.18.

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This is an advance summary of a forthcoming article in the Oxford Encyclopedia of Planetary Science. Please check back later for the full article.Mars, which has a tenth of the mass of Earth, has cooled as a single lithospheric plate. Current topography gravity maps and magnetic maps do not show signs of the plate tectonics processes that have shaped the Earth’s surface. Instead, Mars has been shaped by the effects of meteorite bombardment, igneous activity, and sedimentary—including aqueous—processes. Mars also contains enormous igneous centers—Tharsis and Elysium, with other shield volcanoes in the ancient highlands. In fact, the planet has been volcanically active for nearly all of its 4.5 Gyr history, and crater counts in the Northern Lowlands suggest that may have extended to within the last tens of millions of years. Our knowledge of the composition of the igneous rocks on Mars is informed by over 100 Martian meteorites and the results from landers and orbiters. These show dominantly tholeiitic basaltic compositions derived by melting of a relatively K, Fe-rich mantle compared to that of the Earth. However, recent meteorite and lander results reveal considerable diversity, including more silica-rich and alkaline igneous activity. These show the importance of a range of processes including crystal fractionation, partial melting, and possibly mantle metasomatism and crustal contamination of magmas. The figures and plots of compositional data from meteorites and landers show the range of compositions with comparisons to other planetary basalts (Earth, Moon, Venus). A notable feature of Martian igneous rocks is the apparent absence of amphibole. This is one of the clues that the Martian mantle had a very low water content when compared to that of Earth.The Martian crust, however, has undergone hydrothermal alteration, with impact as an important heat source. This is shown by SNC analyses of secondary minerals and Near Infra-Red analyses from orbit. The associated water may be endogenous.Our view of the Martian crust has changed since Viking landers touched down on the planet in 1976: from one almost entirely dominated by basaltic flows to one where much of the ancient highlands, particularly in ancient craters, is covered by km deep sedimentary deposits that record changing environmental conditions from ancient to recent Mars. The composition of these sediments—including, notably, the MSL Curiosity Rover results—reveal an ancient Mars where physical weathering of basaltic and fractionated igneous source material has dominated over extensive chemical weathering.

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25

Orvell, Miles. Empire of Ruins. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780190491604.001.0001.

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Empire of Ruins explores the meaning of ruins in American culture, from the mid-nineteenth century to the twenty-first century, arguing that photographs have been the chief means by which the significance of ruins has been created in American culture. The book traces a historical argument that begins in the nineteenth century, when Americans yearned for the ruins of Europe, then moves to the discovery of Native American ruins in the Southwest. Later chapters explore the visualization of inner city ruins, abandoned factories, and shopping malls, and the “creative destruction” of buildings in order to make way for bigger ones. In addition, it analyzes the imagery of the 9/11 World Trade Center disaster; the ruins of the industrial landscape through mining operations; the ruins created by natural disasters like Hurricanes Katrina and Sandy; and the ruins produced by climate change, including the melting of the ice caps. Empire of Ruins considers, in conclusion, the way the picturing of ruins has served to mark revolutionary moments in political culture, symbolizing the choices societies must make. Empire of Ruins focuses mainly on photography, but it encompasses painting, literature, and popular films as well, in order to provide a larger picture of the cultural meaning of ruins. At the same time, it examines the powerful aesthetic attraction of ruin imagery in photographs and films, showing how the Destructive Sublime, a new category of experience, evokes contrary responses in viewers.

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26

Omstedt, Anders. The Development of Climate Science of the Baltic Sea Region. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.654.

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Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realization that fisheries themselves have strongly negative effects on the marine environment, calling for international assessment efforts. Scientists later introduced the concept of regime shifts when interpreting their data, attributing these to various causes. The increasing amount of anoxic deep water in the Baltic Sea and eutrophication have prompted debate about what is natural and what is anthropogenic, and the scientific outcome of these debates now forms the basis of international management efforts to reduce nutrient leakage from land. The observed increase in atmospheric CO2 and its effects on global warming have focused the climate debate on trends and generated a series of international and regional assessments and research programs that have greatly improved our understanding of climate and environmental changes, bolstering the efforts of earth system science, in which both climate and environmental factors are analyzed together.Major achievements of past centuries have included developing and organizing regular observation and monitoring programs. The free availability of data sets has supported the development of more accurate forcing functions for Baltic Sea models and made it possible to better understand and model the Baltic Sea–North Sea system, including the development of coupled land–sea–atmosphere models. Most indirect and direct observations of the climate find great variability and stochastic behavior, so conclusions based on short time series are problematic, leading to qualifications about periodicity, trends, and regime shifts. Starting in the 1980s, systematic research into climate change has considerably improved our understanding of regional warming and multiple threats to the Baltic Sea. Several aspects of regional climate and environmental changes and how they interact are, however, unknown and merit future research.

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27

Liu, Xiaodong, and Libin Yan. Elevation-Dependent Climate Change in the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.593.

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As a unique and high gigantic plateau, the Tibetan Plateau (TP) is sensitive and vulnerable to global climate change, and its climate change tendencies and the corresponding impact on regional ecosystems and water resources can provide an early alarm for global and mid-latitude climate changes. Growing evidence suggests that the TP has experienced more significant warming than its surrounding areas during past decades, especially at elevations higher than 4 km. Greater warming at higher elevations than at lower elevations has been reported in several major mountainous regions on earth, and this interesting phenomenon is known as elevation-dependent climate change, or elevation-dependent warming (EDW).At the beginning of the 21st century, Chinese scholars first noticed that the TP had experienced significant warming since the mid-1950s, especially in winter, and that the latest warming period in the TP occurred earlier than enhanced global warming since the 1970s. The Chinese also first reported that the warming rates increased with the elevation in the TP and its neighborhood, and the TP was one of the most sensitive areas to global climate change. Later, additional studies, using more and longer observations from meteorological stations and satellites, shed light on the detailed characteristics of EDW in terms of mean, minimum, and maximum temperatures and in different seasons. For example, it was found that the daily minimum temperature showed the most evident EDW in comparison to the mean and daily maximum temperatures, and EDW is more significant in winter than in other seasons. The mean daily minimum and maximum temperatures also maintained increasing trends in the context of EDW. Despite a global warming hiatus since the turn of the 21st century, the TP exhibited persistent warming from 2001 to 2012.Although EDW has been demonstrated by more and more observations and modeling studies, the underlying mechanisms for EDW are not entirely clear owing to sparse, discontinuous, and insufficient observations of climate change processes. Based on limited observations and model simulations, several factors and their combinations have been proposed to be responsible for EDW, including the snow-albedo feedback, cloud-radiation effects, water vapor and radiative fluxes, and aerosols forcing. At present, however, various explanations of the mechanisms for EDW are mainly derived from model-based research, lacking more solid observational evidence. Therefore, to comprehensively understand the mechanisms of EDW, a more extensive and multiple-perspective climate monitoring system is urgently needed in the areas of the TP with high elevations and complex terrains.High-elevation climate change may have resulted in a series of environmental consequences, such as vegetation changes, permafrost melting, and glacier shrinkage, in mountainous areas. In particular, the glacial retreat could alter the headwater environments on the TP and the hydrometeorological characteristics of several major rivers in Asia, threatening the water supply for the people living in the adjacent countries. Taking into account the climate-model projections that the warming trend will continue over the TP in the coming decades, this region’s climate change and the relevant environmental consequences should be of great concern to both scientists and the general public.

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