Transient analysis of direct contact evaporation and condensation within packed beds

2011 ◽  
Vol 54 (15-16) ◽  
pp. 3381-3393 ◽  
Author(s):  
Fadi Alnaimat ◽  
James F. Klausner ◽  
Renwei Mei
2006 ◽  
Vol 49 (25-26) ◽  
pp. 4751-4761 ◽  
Author(s):  
Yi Li ◽  
James F. Klausner ◽  
Renwei Mei ◽  
Jessica Knight

2020 ◽  
Vol 179 ◽  
pp. 115629 ◽  
Author(s):  
Raid Alrowais ◽  
Chen Qian ◽  
Muhammad Burhan ◽  
Doskhan Ybyraiymkul ◽  
Muhammad Wakil Shahzad ◽  
...  

2017 ◽  
Vol 96 (1) ◽  
pp. 404-413 ◽  
Author(s):  
Yunfa Hu ◽  
Yiping Wang ◽  
Qunwu Huang ◽  
Yong Cui

1984 ◽  
Vol 75 ◽  
pp. 597
Author(s):  
E. Grün ◽  
G.E. Morfill ◽  
T.V. Johnson ◽  
G.H. Schwehm

ABSTRACTSaturn's broad E ring, the narrow G ring and the structured and apparently time variable F ring(s), contain many micron and sub-micron sized particles, which make up the “visible” component. These rings (or ring systems) are in direct contact with magnetospheric plasma. Fluctuations in the plasma density and/or mean energy, due to magnetospheric and solar wind processes, may induce stochastic charge variations on the dust particles, which in turn lead to an orbit perturbation and spatial diffusion. It is suggested that the extent of the E ring and the braided, kinky structure of certain portions of the F rings as well as possible time variations are a result of plasma induced electromagnetic perturbations and drag forces. The G ring, in this scenario, requires some form of shepherding and should be akin to the F ring in structure. Sputtering of micron-sized dust particles in the E ring by magnetospheric ions yields lifetimes of 102to 104years. This effect as well as the plasma induced transport processes require an active source for the E ring, probably Enceladus.


1978 ◽  
Vol 39 (C6) ◽  
pp. C6-194-C6-195
Author(s):  
S. Ohta ◽  
Y. Sawada

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