Abstract
The particle and void sizes distributions of the soil are related with the assumption that a void constant relationship at all different scales and a relationship between pore and particle size of a given packing. In the relationship between pore and particle sizes, a particle elongation factor is applied based on the Arya and Paris model. A flow trajectory tortuosity factor based on the Fuentes model can also be applied. Since the void size distribution is associated to the soil water retention curve, the proposed relationship can be used to estimate this curve from particle size distribution.
| Original language | Spanish |
|---|---|
| Pages (from-to) | 197-205 |
| Number of pages | 9 |
| Journal | Revista Mexicana de Fisica |
| Volume | 64 |
| Issue number | 2 |
| DOIs | |
| State | Published - 2018 |
Bibliographical note
Publisher Copyright:© 2018, Sociedad Mexicana de Fisica.
Types Minciencias
- Artículos de investigación con calidad Q3
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