1973
DOI: 10.1016/0001-6160(73)90082-5
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A model for second-stage liquid-phase sintering with a partially wetting liquid

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Cited by 60 publications
(33 citation statements)
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“…No model accounts for this complexity. A similar treatment by Gessinger et al [127,128] assumed the liquid layer wets the grain boundary with a small dihedral angle, giving essentially the same sintering shrinkage as Kingery. Solid-state diffusion by grain boundary diffusion in the grain contact is another densification mechanism.…”
Section: Densificationmentioning
confidence: 96%
See 1 more Smart Citation
“…No model accounts for this complexity. A similar treatment by Gessinger et al [127,128] assumed the liquid layer wets the grain boundary with a small dihedral angle, giving essentially the same sintering shrinkage as Kingery. Solid-state diffusion by grain boundary diffusion in the grain contact is another densification mechanism.…”
Section: Densificationmentioning
confidence: 96%
“…39c [127,128]. The contact zone enlarges to change the grain shape with simultaneous shrinkage of the grains.…”
Section: Densificationmentioning
confidence: 99%
“…The driving force is usually described in terms of the effect of capillary pressure on the grain-boundary formation process. [172][173][174] The capillary forces contemplated result from the menisci at liquid-vapor interfaces between contacting particles that drive sintering by pulling particles together. An important concept is that, despite the compressive force induced across particle contacts, enough of the liquid-forming material must remain adsorbed at the boundaries to provide the high boundary diffusion required to account for enhanced rates of densification via grain-boundary formation.…”
Section: (7) Equilibrium Intergranular and Surficial Filmsmentioning
confidence: 99%
“…Representing soil PSD in terms of statistical PDF, and considering aggregate deformation and porosity loss in wet soils as a solid diffusion process [Gessinger et al, 1973], enables modeling soil pore space changes as evolution of soil PDF governed by external forcing and soil deformation processes. A well-developed theory already exists for representing stochastic diffusion processes by the Kolmogorov forward equation or the FPE [Gardiner, 1985;Hara, 1984].…”
Section: Fokker-planck Equation (Fpe)mentioning
confidence: 99%