Unsaturated Soils: Research &Amp; Applications 2014
DOI: 10.1201/b17034-73
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Modeling rainfall infiltration through coarse and fine-grained unsaturated geomaterials

Abstract: In this paper we study an imbibition test problem defined over a real two-dimensional soil domain subject to in-situ stresses and oedometric boundary conditions. Two different kinds of materials are tested, which are characterized by different pore-structures and hydro-mechanical properties. The aim is that of clarifying the behavior of real materials under real loading conditionss. The stress paths associated to rainfall infiltration processes are simulated by using the commercial code ABAQUS, endowed with an… Show more

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Cited by 5 publications
(5 citation statements)
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References 8 publications
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“…The mechanical behaviour of the solid skeleton is described with a Modified Cam Clay Model (MCCM) extended to unsaturated conditions [24]. The MCCM well-reproduces the response of fine-grained soils under a broad range of initial conditions during wetting and loading processes, as demonstrated for single elements by Casini [25] and Casini et al [26] as well as by other researchers [27][28][29] for boundary value problems. The model is characterised by a relatively simple mathematical formulation described in detail in Rotisciani et al [30].…”
Section: Constitutive Modellingmentioning
confidence: 68%
“…The mechanical behaviour of the solid skeleton is described with a Modified Cam Clay Model (MCCM) extended to unsaturated conditions [24]. The MCCM well-reproduces the response of fine-grained soils under a broad range of initial conditions during wetting and loading processes, as demonstrated for single elements by Casini [25] and Casini et al [26] as well as by other researchers [27][28][29] for boundary value problems. The model is characterised by a relatively simple mathematical formulation described in detail in Rotisciani et al [30].…”
Section: Constitutive Modellingmentioning
confidence: 68%
“…The second and third terms describe the strain-induced structure degradation using two separate negative exponential damage-type forms. The last term represents the simplest form of the hydraulic hardening that allows capturing most of the observed phenomena for unsaturated soils as, for example, the increase of the preconsolidation pressure with suction, and the wetting-induced collapse [17,35,49,51]. It worth noting that this expression is valid only when S r is not far from the unity and water menisci are homogeneously distributed over the soil volume [13], as assumed in the following.…”
Section: Constitutive Modelmentioning
confidence: 99%
“…This model is characterized by both a relatively simple mathematical formulation and few physically meaningful constitutive parameters. Despite its simplicity, the MCCM is capable of reproducing the hydro‐mechanical response observed during wetting for both REV and BVP …”
Section: Constitutive Modelmentioning
confidence: 99%
“…Despite its simplicity, the MCCM is capable of reproducing the hydro-mechanical response observed during wetting for both REV and BVP. [27][28][29][30][31] MCCM is formulated within the framework of critical soil mechanics in terms of Bishop's effective stresses, defined as σ ′ ij ¼ σ ij þ χ s δ ij , coinciding χ with S r . Since the saturation levels considered in this study are far from the residual values, Bishop's relation remains a valid expression for effective stresses, 32,33 if the constitutive model is suitably modified as is described here below.…”
Section: Constitutive Modelmentioning
confidence: 99%