Experimental study and modeling of hindered one dimensional settling of spherical trifluroethyl methacrylate based polymer particles

2021 ◽  
pp. 52006
Author(s):  
Aravind Reghu ◽  
Timothy Butcher ◽  
Jui‐Ming Lin ◽  
James Russell ◽  
Jeremy Hammond
2007 ◽  
Vol 7 (15) ◽  
pp. 2200-2205 ◽  
Author(s):  
Almahdi Atteya Alhwaige ◽  
Siti Masrinda Tasiri . ◽  
Wan Ramli Wan Daud .

1995 ◽  
Vol 74 (9) ◽  
pp. 1673-1676 ◽  
Author(s):  
K. Takeda ◽  
K. Konishi ◽  
K. Nedachi ◽  
K. Mukai

2019 ◽  
Vol 1369 ◽  
pp. 012054
Author(s):  
V V Cheverda ◽  
I S Vozhakov ◽  
F V Ronshin

2009 ◽  
Vol 196 (1) ◽  
pp. 50-55 ◽  
Author(s):  
X.Z. An ◽  
C.X. Li ◽  
R.Y. Yang ◽  
R.P. Zou ◽  
A.B. Yu

2013 ◽  
Author(s):  
J. E. Lugo ◽  
Rafael Doti ◽  
Jocelyn Faubert ◽  
Noemi Sanchez ◽  
Javier Sanchez ◽  
...  

2008 ◽  
Vol 281 (14) ◽  
pp. 3681-3685 ◽  
Author(s):  
Liwei Zhang ◽  
Zhiguo Wang ◽  
Hong Chen ◽  
Hongqiang Li ◽  
Yewen Zhang

1967 ◽  
Vol 6 (47) ◽  
pp. 681-694 ◽  
Author(s):  
Andrew C. Palmer

When a surface layer of the soil freezes, both heat and water diffuse from the unfrozen soil beneath to the frozen region. Often the soil does not freeze homogeneously but distinct ice lenses form. An analysis of the diffusion and ice nucleation processes suggests conditions under which ice lensing can be expected; in particular, it is shown that multiple ice lenses cannot form unless the soil thermal diffusivity is greater than the water diffusion coefficient. Analysis of a simple one-dimensional case (a semi-infinite mass of homogeneous soil whose surface temperature is suddenly lowered) gives the temperature and water-content fields as functions of time; these agree with those observed in an experimental study of freezing clay.


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