A Free-Boundary Model of Corrosion

Author(s):  
F. Clarelli ◽  
B. De Filippo ◽  
R. Natalini
Keyword(s):  
2019 ◽  
Vol 481 ◽  
pp. 61-74 ◽  
Author(s):  
Ruth E Baker ◽  
Andrew Parker ◽  
Matthew J Simpson
Keyword(s):  

1996 ◽  
Author(s):  
Igor A. Lubashevsky ◽  
Alexander V. Priezzhev ◽  
Vasyl V. Gafiychuk ◽  
Meruzhan G. Cadjan

1996 ◽  
Author(s):  
Igor A. Lubashevsky ◽  
Alexander V. Priezzhev ◽  
V. V. Gafiychuk ◽  
Meruzhan G. Cadjan
Keyword(s):  

2002 ◽  
Vol 13 (1) ◽  
pp. 25-52 ◽  
Author(s):  
PAUL C. FIFE ◽  
XIAO-PING WANG

The free boundary model of diffusion-induced grain boundary motion derived in Cahn et al. [3], Fife et al. [6] and Cahn & Penrose [4] is extended, in the case of thin metallic films, to account for bidirectional motion, together with the appearance of S-shapes and double seam configurations. These are often observed in the laboratory. Computer simulations based on the extended model are given to illustrate these and other features of bidirectional motion. More generally, the extension accounts for the motion of grain boundaries whose traces on the film's surface are curved. The new free boundary model is one of forced motion by curvature, the forcing term possibly changing sign due to the bidirectionality. The thin film model is derived systematically under explicit assumptions, and an adjustment for grooving is included.


Author(s):  
Robert Yi ◽  
Yossi Cohen ◽  
Hansjörg Seybold ◽  
Eric Stansifer ◽  
Robb McDonald ◽  
...  

Valleys that form around a stream head often develop characteristic finger-like elevation contours. We study the processes involved in the formation of these valleys and introduce a theoretical model that indicates how shape may inform the underlying processes. We consider valley growth as the advance of a moving boundary travelling forward purely through linearly diffusive erosion, and we obtain a solution for the valley shape in three dimensions. Our solution compares well to the shape of slowly growing groundwater-fed valleys found in Bristol, Florida. Our results identify a new feature in the formation of groundwater-fed valleys: a spatially variable diffusivity that can be modelled by a fixed-height moving boundary.


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