Are Internet Stocks the Trigger of Internet Bubble Bursting?

2007 ◽  
Author(s):  
Jerry W. Chen
Keyword(s):  
Bubble Bursting

scholarly journals Experimental evidence of plastic particles transfer at the water-air interface through bubble bursting

2021 ◽  
Vol 280 ◽  
pp. 116949
Author(s):  
Maria Masry ◽  
Stéphanie Rossignol ◽  
Brice Temime Roussel ◽  
David Bourgogne ◽  
Pierre-Olivier Bussière ◽  
...  
Keyword(s):  
Experimental Evidence ◽  
Bubble Bursting ◽  
Air Interface

scholarly journals Patterns of bubble bursting and weak explosive activity in an active lava lake—Halema‘uma‘u, Kīlauea, 2015

2021 ◽  
Author(s):  
Bianca G. Mintz ◽  
Bruce F. Houghton ◽  
Edward W. Llewellin ◽  
Tim R. Orr ◽  
Jacopo Taddeucci ◽  
...  
Keyword(s):  
Lava Lake ◽  
Explosive Activity ◽  
Bubble Bursting

Aerosol generation by bubble bursting from a boiling pool

1989 ◽  
Vol 20 (8) ◽  
pp. 1405-1408 ◽  
Author(s):  
W. Schöck ◽  
M. Wagner-Ambs
Keyword(s):  
Bubble Bursting ◽  
Aerosol Generation

Collecting amino acids in the Enceladus plume

2018 ◽  
Vol 18 (1) ◽  
pp. 47-59 ◽  
Author(s):  
Melissa Guzman ◽  
Ralph Lorenz ◽  
Dana Hurley ◽  
William Farrell ◽  
John Spencer ◽  
...  
Keyword(s):  
Amino Acids ◽  
Particle Size ◽  
Particle Size Distribution ◽  
Size Distribution ◽  
Free Amino Acids ◽  
Free Amino ◽  
Deep Ocean ◽  
Mass Rate ◽  
Bubble Bursting ◽  
Deep Ocean Water

AbstractWe numerically model the dynamics of the Enceladus plume ice grains and define our nominal plume model as having a particle size distributionn(R) ~R−qwithq= 4 and a total particulate mass rate of 16 kg s−1. This mass rate is based on average plume brightness observed by Cassini across a range of orbital positions. The model predicts sample volumes of ~1600 µg for a 1 m2collector on a spacecraft making flybys at 20–60 km altitudes above the Enceladus surface. We develop two scenarios to predict the concentration of amino acids in the plume based on these assumed sample volumes. We specifically consider Glycine, Serine, α-Alanine, α-Aminoisobutyric acid and Isovaline. The first ‘abiotic’ model assumes that Enceladus has the composition of a comet and finds abundances between 2 × 10−6to 0.003 µg for dissolved free amino acids and 2 × 10−5to 0.3 µg for particulate amino acids. The second ‘biotic’ model assumes that the water of Enceladus's ocean has the same amino acid composition as the deep ocean water on Earth. We compute the expected captured mass of amino acids such as Glycine, Serine, and α-Alanine in the ‘biotic’ model to be between 1 × 10−5to 2 × 10−5µg for dissolved free amino acids and dissolved combined amino acids and about 0.0002 µg for particulate amino acids. Both models consider enhancements due to bubble bursting. Expected captured mass of amino acids is calculated for a 1 m2collector on a spacecraft making flybys with a closest approach of 20 km during mean plume activity for the given nominal particle size distribution.

Emission and local ventilation control of droplets generated by condensation and bubble-bursting during pickling

2021 ◽  
pp. 103491
Author(s):  
Jia-Ning Fan ◽  
Yang Yang ◽  
Yi Wang ◽  
Yuming Zhang ◽  
Yingrong Wei ◽  
...  
Keyword(s):  
Ventilation Control ◽  
Bubble Bursting ◽  
Local Ventilation

Experimental Observation of Nucleate Boiling Entrainment in a Liquid Film

2021 ◽  
Author(s):  
Junpei Tabuchi ◽  
Yuki Narushima ◽  
Kenichi Katono ◽  
Tomio Okawa
Keyword(s):  
Liquid Film ◽  
Forced Convection ◽  
Vapor Bubble ◽  
Water Surface ◽  
Annular Flow ◽  
Nucleate Boiling ◽  
Vapor Bubbles ◽  
Droplet Entrainment ◽  
Bubble Bursting ◽  
Filament Breakup

Abstract Many studies have been conducted on droplet entrainment in an annular flow regime, but little is known about droplet entrainment caused by nucleate boiling. In this report, visualization results of droplet entrainment caused by nucleate boiling are described. We observed two processes of droplet entrainment. The first one causes bubble bursting at a water surface. The second one causes filament breakup which occurs when the vapor bubble reaches and collapses at the interface between air and liquid. From comparison of the phenomena for the two processes, we found that the diameters of the droplets and vapor bubbles were considerably different. Using the results of this research allows the effect of forced convection to be taken into account. In the future, we plan to expand the amount of data and develop a boiling entrainment model under forced convection conditions.

Primary Marine Aerosol Produced during Bubble Bursting Experiments Using Baltic Sea, North Sea, and Atlantic Waters

2007 ◽  
pp. 1093-1097
Author(s):  
Kim Hultin ◽  
E. Douglas Nilsson ◽  
Radovan Krejci ◽  
Gerrit de Leeuw ◽  
Monica Mårtensson
Keyword(s):  
Baltic Sea ◽  
North Sea ◽  
Marine Aerosol ◽  
Bubble Bursting

Submicron Salt Particle Production in Bubble Bursting

2006 ◽  
Vol 40 (9) ◽  
pp. 664-671 ◽  
Author(s):  
Lynn M. Russell ◽  
Elizabeth G. Singh
Keyword(s):  
Particle Production ◽  
Salt Particle ◽  
Bubble Bursting
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