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Titlebook: Drying ’85; Ryozo Toei,Arun S. Mujumdar Conference proceedings 1985 Springer-Verlag Berlin Heidelberg 1985 Drying.engine.flow.heat transfe

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发表于 2025-3-21 16:11:18 | 显示全部楼层 |阅读模式
书目名称Drying ’85
编辑Ryozo Toei,Arun S. Mujumdar
视频video
图书封面Titlebook: Drying ’85;  Ryozo Toei,Arun S. Mujumdar Conference proceedings 1985 Springer-Verlag Berlin Heidelberg 1985 Drying.engine.flow.heat transfe
描述It is a pleasure to present this volume consisting of a selection of papers presented at the 4th International Drying Symposium (IDS) held in Kyoto, July 9-12, 1984, under the sponsorship of the Society of Chemi­ cal Engineers, Japan. This book includes full texts of the ten keynote lectures and several papers which were presented in the technical sessions in the 4th IDS. As editors we had the arduous and unpleasant task of selecting papers for this volume. We were delighted with the high quality manuscripts sub­ mitted. We are grateful to the authors for their efforts in meeting the manuscript guidelines and also the deadlines. Aside from quality, we have attempted to maintain in this volume a balance of coverage in terms of topics as well as geography. Space restrictions prevented us from presenting all the high quality papers for publication in DRYING 85. Numerous papers of archival interest have been released for general publication in international journals. Several will no doubt appear in Drying Technology - An International Journal. Many others will find their way into other standard engineering journals as well. Over 120 papers from 30 countries were included in the Proceed
出版日期Conference proceedings 1985
关键词Drying; engine; flow; heat transfer; organization; quality; space; vapor; water
版次1
doihttps://doi.org/10.1007/978-3-662-21830-3
isbn_softcover978-3-662-21832-7
isbn_ebook978-3-662-21830-3
copyrightSpringer-Verlag Berlin Heidelberg 1985
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Another Attempt to Answer Our Questionng phases, including the constant surface water activity period, the period with decreasing surface water activity, the penetration period where the surface water concentration is in equilibrium with the surrounding gas phase and the central water concentration has still hardly changed and finally t
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Another Attempt to Answer Our Questionendent and diluted character of solar radiation. This involves problems requiring different means for their solution /heat Storer, auxiliary energy source, large collector surfaces, control system/ and so the investment cost are considerable..For the economical utilization of solar energy for drying
发表于 2025-3-22 07:21:20 | 显示全部楼层
Another Attempt to Answer Our Question dominant. Foaming and incorporation of an emulsified oil phase or surfactants all have substantial effects on volatiles loss. These effects can be interpreted through transport analyses..Particle inflation during drying requires entrainment or nucleation of an air bubble as a first step, and is the
发表于 2025-3-22 11:35:46 | 显示全部楼层
Junxia Guo,Qiyun Cao,Rilian Zhao,Zheng Lisolution of a system of three partial derivative, equations which are non-linear due to the variation of the phenomenological coefficients with moisture content..Such a model is resolved in a one-dimensional case and allows us to check the validity of the theoretical assumptions. The computed values
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Junxia Guo,Qiyun Cao,Rilian Zhao,Zheng Lig solution methods are inadequate..This paper presents a one-dimensional numerical solution technique for the transport of water, water vapor, and an inert gas through a porous medium. The fundamental equations follow from the application of volume averaging theory. These transient equations are fin
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Opportunities for Fundamental Research in Dryinged or about to be available instruments to measure and “see” the water molecule for a substrate (advanced electron microscopes), and high-speed, high-capacity computers (supercomputers)..The water molecule hp a diameter of 2 Å and a bond length of 0.9 Å. Water molecules are on a substrate which has
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Short-Cut Calculation for Non-Isothermal Drying of Shrinking and Non-Shrinking Particles and of Hollng phases, including the constant surface water activity period, the period with decreasing surface water activity, the penetration period where the surface water concentration is in equilibrium with the surrounding gas phase and the central water concentration has still hardly changed and finally t
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