Investigation of detonation suppression in aluminum suspensions of micro- and nanoparticles by inert particle clouds

2019 ◽  
Author(s):  
Sergey Lavruk
Keyword(s):  
Inert Particle ◽  
Detonation Suppression ◽  
Particle Clouds

The propagation of reacting blast waves through inert particle clouds

1976 ◽  
Vol 3 (7-8) ◽  
pp. 517-529 ◽  
Author(s):  
Tateyuki Suzuki ◽  
Shigeharu Ohyagi ◽  
Fumio Higashino ◽  
Akira Takano
Keyword(s):  
Blast Waves ◽  
Inert Particle ◽  
Particle Clouds

scholarly journals Spherical turbulent flame propagation of pulverized coal particle clouds in an O2/N2 atmosphere

2019 ◽  
Vol 37 (3) ◽  
pp. 2935-2942 ◽  
Author(s):  
Khalid Hadi ◽  
Ryo Ichimura ◽  
Nozomu Hashimoto ◽  
Osamu Fujita
Keyword(s):  
Flame Propagation ◽  
Coal Particle ◽  
Turbulent Flame ◽  
Pulverized Coal ◽  
N2 Atmosphere ◽  
Particle Clouds

Formation and Characterization of Sub-Micron Inert Particle Embedded Nickel Composite Coatings

2017 ◽  
Vol 77 (11) ◽  
pp. 1029-1034
Author(s):  
Olgun Yilmaz ◽  
Metehan Erdogan ◽  
Ishak Karakaya
Keyword(s):  
Composite Coatings ◽  
Inert Particle

Thin cirrus clouds that extinct supercooled water clouds in the Arctics

2021 ◽  
Author(s):  
Suginori Iwasaki ◽  
Hajime Okamoto ◽  
Kaori Sato
Keyword(s):  
Radiative Forcing ◽  
Supercooled Water ◽  
Terminal Velocity ◽  
Cirrus Clouds ◽  
The Arctic ◽  
Significant Feature ◽  
Orthogonal Polarization ◽  
Cloud Particle ◽  
Particle Clouds ◽  
Moderate Resolution Imaging Spectroradiometer

<p><span><span>We show that thin cirrus clouds, whose particle radius is greater than 50 μm and number concentration is less than 10 /L, extinct supercooled water clouds (SC) by use of the data of the space-borne lidar, Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP), and the space-borne 94-GHz cloud profiling radar (CPR). We call the cirrus Large-and-Sparse-particle Clouds (LSC). </span></span></p><p><span><span>The space-borne imagers, such as Moderate Resolution Imaging Spectroradiometer (MODIS), cannot measure LSC; hence, LSC had been difficult to be found by satellites. CALIOP is less sensitive to LSC than CPR though CALIOP is usually more sensitive to clouds than CPR because of the cloud particle size distribution of LSC.</span></span></p><p><span><span>The most significant feature of LSC is that LSC extinct SC and cloud particles of SC are changed into pristine ice particles. This is because (1) SC and LSC do not tend to coexist while horizontally oriented ice particle clouds (2D) and LSC tend to coexist, (2) the cloud top height of LSC is higher than that of SC, and (3) the terminal velocity of LSC particles is about 1 km/h.</span></span></p><p><span><span>Because 10-20% of clouds in the Arctic are LSC, LSC would indirectly impact on radiative forcing in the Arctics.</span></span></p>

Structure Controls of Fine-Particle Clouds in DC Discharge Plasmas

2000 ◽  
pp. 329-336 ◽  
Author(s):  
Noriyoshi Sato ◽  
Giichiro Uchida ◽  
Ryoichi Ozaki ◽  
Satoru Iizuka ◽  
Tetsuo Kamimura
Keyword(s):  
Fine Particle ◽  
Discharge Plasmas ◽  
Dc Discharge ◽  
Particle Clouds
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