𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Modelling of the transition zone porosity

✍ Scribed by B. Bourdette; E. Ringot; J.P. Ollivier


Publisher
Elsevier Science
Year
1995
Tongue
English
Weight
750 KB
Volume
25
Category
Article
ISSN
0008-8846

No coin nor oath required. For personal study only.

✦ Synopsis


The ion diffusion process in mortar is different from the one which occurs in cement paste. This difference is due to the presence of transition zones, which take place around the grains in mortar and which are very porous regions. Based on mercury intrusion porosimetry experimental data and on the analysis of percolation through a 3D mortar model, a computation of the transition zone porosity and of the bulk paste porosity has been carried out. The porosity of the transition zone has been analyzed as a function of the mortar composition and of the degree of hydration.


πŸ“œ SIMILAR VOLUMES


Excision of anal transition zone
✍ J. M. Enriquez; J. CamuΓ±as; M. R. B. Keighley; K. Yoshioka πŸ“‚ Article πŸ“… 1988 πŸ› John Wiley and Sons 🌐 English βš– 155 KB

A further 5 recurred within 6 1 0 years after surgery and only 1 recurrence occurred 11 years after surgery. On Hoffmann's criteria, 7 of our recurrences could be classified as transient/innocuous (35 per cent) and the remaining 13 as chronic/malevolent (65 per cent). This would give our series a ch

Monte Carlo Modelling of Structure and P
✍ P. N. Maya; S. P. Deshpande; M. Warrier πŸ“‚ Article πŸ“… 2006 πŸ› John Wiley and Sons 🌐 English βš– 166 KB

A 3-dimensional Monte Carlo model for growth of hydrocarbon films on surfaces having dangling bonds is presented. The model is microscopic in the sense that it incorporates the stereoscopic orientations of the deposited hydrocarbons and macroscopic in that it considers shadowing effects and porosity

Modelling of wetting and drying of shall
✍ B. van't Hof; E. A. H. Vollebregt πŸ“‚ Article πŸ“… 2005 πŸ› John Wiley and Sons 🌐 English βš– 685 KB

## Abstract A new method for wetting and drying in two‐dimensional shallow water flow models is proposed. The method is closely related to the artificial porosity method used by different authors in Boussinesq‐type models, but is further extended for use in a semi‐implicit (ADI‐type) time integrati