Mathematical Modelling of Transport Processes During Wellbore Heating in Tar Sand and Bituminous Reservoirs

2004 ◽  
Vol 43 (09) ◽  
Author(s):  
K. Karmaker ◽  
B.B. Maini ◽  
A.A. Jeje
Author(s):  
Ν. N. Skvortsova ◽  
G. M. Batanov ◽  
A. E. Petrov ◽  
A. A. Pshenichnikov ◽  
K. A. Sarksyan ◽  
...  

2003 ◽  
Vol 24 (3) ◽  
pp. 380-389 ◽  
Author(s):  
Martin Pačes ◽  
Juraj Kosek ◽  
Miloš Marek ◽  
Ulrich Tallarek ◽  
Andreas Seidel-Morgenstern

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.


2012 ◽  
Author(s):  
Aleksandras Krylovas ◽  
Natalja Kosareva ◽  
Olga Navickiene

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