Characterizing nonrigid aggregated soil-water medium using its shrinkage curve

By Erik Braudeau, J. Frangi, Rabi H. Mohtar. 2004

131 citations recorded by the source corpus.

Subfields: Atmospheric Science, Civil and Structural Engineering

View Paper: https://www.semanticscholar.org/paper/ca22344c937b7d815e64564c144dc50d230cccc4

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Xinhua Peng
2. R. Horn
3. M. Sène
4. Rabi H. Mohtar
5. Erik Braudeau

In Civil and Structural Engineering

1. Xinhua Peng
2. R. Horn
3. Wim Cornelis
4. M. Sène
5. Rabi H. Mohtar
6. Erik Braudeau
7. Donald Gabriëls

Citations in the corpus

• Prediction of Water Retention of Soils from the Humid Tropics by the Nonparametric k‐Nearest Neighbor Approach (2013, unknown): “…in the k-NN technique led to a slight increase of the RMSD. h ey indicated that the BD of Vertisols is known to change with soil water content (swelling-shrinking soils). h is particular behavior was observed and studied by various authors (e.g., Braudeau et al., 2004; Cornelis et al., 2006).”
• Identifying Six Types of Soil Shrinkage Curves from a Large Set of Experimental Data (2013, methodology): “org/publications/sssaj 373 Soil Physics and Haugen, 1998); (ii) models of the shrinkage curve without zero shrinkage (McGarry and Malafant, 1987); and (iii) models of the shrinkage curve with four shrinkage phases (Braudeau et al., 1999; Groenevelt and Grant, 2001; Tariq and Durnford, 1993a). In the”
• A simplified parametric model to describe the magnitude and geometry of soil shrinkage (2006, background): “For soils that swell and shrink, their changes in volume resulting from changes in water content greatly affect their macroporosity and to a lesser extent their microporosity (Braudeau et al., 2004).”
• Hydrostructural characteristics of two African tropical soils (2005, methodology): “…as a function of texture and Fe2O3 can be considered as pedotransfer functions, both for the agronomic properties (field capacity, wilting point, available water, air capacity) and for the curve for modelling the shrinkage properties of soil under field conditions (Braudeau et al., 2004b).”