Hubert Chanson's Air Bubble Entrainment in Free-Surface Turbulent Shear Flows PDF

By Hubert Chanson

ISBN-10: 0121681106

ISBN-13: 9780121681104

Content material:

, Pages xiii-xvi,I-IV

, Page xvii
About the author

, Page xviii
List of symbols

, Pages xix-xxix

, Pages xxxi-xlix
Chapter 1 - Introduction

, Pages 2-16
Chapter 2 - Mechanisms of air bubble entrainment

, Pages 17-26
Chapter three - Similitude and experimental studies

, Pages 27-35
Chapter four - Air-water fuel transfer

, Pages 36-41
Chapter five - Plunging jet flows: Presentation

, Pages 44-52
Chapter 6 - Air entrainment by way of plunging jets

, Pages 53-72
Chapter 7 - Air entrainment in hydraulic jumps

, Pages 73-92
Chapter eight - Air entrainment in plunging jet flows: similar situations and fuel transfer

, Pages 93-101
Chapter nine - Self-aerated flows-presentation

, Pages 104-109
Chapter 10 - Air entrainment in steep chute flows

, Pages 110-132
Chapter eleven - Air entrainment in small-slope waterways

, Pages 133-143
Chapter 12 - Air entrainment in partially-filled conduits

, Pages 144-152
Chapter thirteen - Air entrainment in open channels: Discussion

, Pages 153-164
Chapter 14 - creation to high-velocity water jets discharging into the ambience and ventilated hollow space flows

, Pages 166-173
Chapter 15 - Air entrainment in high-velocity water jets

, Pages 174-188
Chapter sixteen - Ventilated hollow space flows

, Pages 189-199
Chapter 17 - Spillway program: Aeration devices

, Pages 200-214
Chapter 18 - precis: Air bubble diffusion in shear flows

, Pages 216-234
Chapter 19 - Conclusion

, Pages 235-238

, Pages 239-261
Appendix A - Constants and fluid properties

, Pages 263-270
Appendix B - Unit conversions

, Pages 271-273
Appendix C - Bubble upward thrust velocity

, Pages 274-277
Appendix D - Sound celerity in two-phase (gas-liquid) flow

, Pages 278-280
Appendix E - Air bubble diffusion at plunging water jets

, Pages 281-288
Appendix F - attribute parameters of boundary layer

, Pages 289-292
Appendix G - Air focus distributions in self-aerated flows

, Pages 293-303
Appendix H - Air-water stream in partially-filled pipes

, Pages 304-306
Appendix I - Air focus distributions in water jets discharging into the atmosphere

, Pages 307-315
Appendix J - Jet trajectory calculations

, Pages 316-322
Appendix okay - Air bubble dimension distribution characteristics

, Pages 323-326
Appendix L - Air-water move as mentioned by means of Leonardo da Vinci

, Pages 327-329
Appendix M - Corrections

, Pages 330-331
Index of authors

, Pages 333-337
Subject index

, Pages 339-348

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Additional info for Air Bubble Entrainment in Free-Surface Turbulent Shear Flows

Example text

R. WOOD is an Emeritus Professor in civil engineering at the University of Canterbury (New Zealand). Yunca : Indian of a group of South American tribes of which the Chimus and the Chinchas are the most important. The Yunca civilisation developed a pre-Inca culture on the coast of Peru. 1 Introduction Water^ constitutes the primary constituent of the oceans, theriversand streams, and subterraneous fluids on the Earth. e. 25 per cent of the water volume being in the oceans (BERNER and BERNER 1987).

The lift force is proportional to the flow velocity times the rotation speed of the cylinder. g. SWANSON 1961). MANNING : Robert MANNING (1816-1897) was Chief Engineer of the Office of Public Works, Ireland. In 1889, he presented two formulae (MANNING 1890). One was to become the so-called 'Gauckler-Manning formula' but Robert MANNING did prefer to use the second formula that he gave in his paper. G. GAUCKLER (GAUCKLER 1867). MARIOTTE : Abbe Edme MARIOTTE (1620-1684) was a French physicist and plant physiologist.

For a spherical bubble of diameter d^^, the increase of internal pressure necessary to balance the tensile force caused by surface tension equals : AP = A'^ald^^ where a is the surface tension. g. detergent) that, when added to a liquid, reduces its surface tension thereby increasing its wetting property. e. abrupt increase or decrease in depth). An abrupt increase in flow depth is called a 'positive surge' while a sudden decrease in depth is termed a 'negative surge'. A positive surge is also called (improperly) a 'moving hydraulic jump' or a 'hydraulic bore'.

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Air Bubble Entrainment in Free-Surface Turbulent Shear Flows by Hubert Chanson

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