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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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96 CHAPTER 5. MATERIAL USED AND EXPERIMENTAL PROGRAM<br />

5.2 Hostun S<strong>an</strong>d<br />

The experimental program for this study was conducted on Hostun S<strong>an</strong>d, a reference s<strong>an</strong>d<br />

well studied in the research literature (Biarez et al. 1989, Flavigny et al. 1990, Hammad 1991,<br />

Sch<strong>an</strong>z & Vermeer 1996, Sch<strong>an</strong>z 1998, Gennaro et al. 2004). Hostun S<strong>an</strong>d is a quartz s<strong>an</strong>d<br />

with grain sizes r<strong>an</strong>ging from 0.1 mm to 1.0 mm in diameter. According to the USCS classi-<br />

fication the material is a poorly-graded medium s<strong>an</strong>d SP (Fig. 5.1). The main classification<br />

properties as the density <strong>of</strong> the soil particles ϱs, the coefficient <strong>of</strong> uniformity Cu, the coeffi-<br />

cient <strong>of</strong> curvature Cc, the values <strong>of</strong> maximum <strong>an</strong>d minimum void ratio e max/min, as well as the<br />

corresponding values <strong>of</strong> maximum <strong>an</strong>d minimum specific weight γ max/min are summarized in<br />

Table 5.1. The saturated hydraulic conductivity <strong>of</strong> the s<strong>an</strong>d is required when computing the<br />

unsaturated hydraulic conductivity from the soil-water characteristic curve using the indirect<br />

method. The saturated hydraulic conductivity <strong>of</strong> the s<strong>an</strong>d for several initial void ratios was<br />

measured using const<strong>an</strong>t head permeability test (Lins et al. 2002, Lins & Sch<strong>an</strong>z 2005). The<br />

results are given in Table 5.1. Experimental results <strong>of</strong> the saturated hydraulic conductiv-<br />

ity are presented in Fig. 5.2. In further calculations <strong>an</strong>d predictions for loose Hostun s<strong>an</strong>d<br />

specimen (e = 0.89) saturated hydraulic conductivity <strong>of</strong> ks = 2.75 · 10 −4 m/s <strong>an</strong>d for dense<br />

Hostun s<strong>an</strong>d specimen (e = 0.66) ks = 2.03 · 10 −4 m/s were used. Shear strength parameters<br />

obtained by Hammad (1991) <strong>an</strong>d Sch<strong>an</strong>z & Vermeer (1996) under plain strain <strong>an</strong>d triaxial<br />

condition on saturated sample tests are given in Table 5.2. These parameters are necessary<br />

for prediction <strong>of</strong> unsaturated shear strength using indirect method <strong>an</strong>d also for prediction <strong>of</strong><br />

unsaturated bearing capacity.<br />

Percent passing by weight (%)<br />

100 80<br />

20 40 60<br />

0<br />

Silt medium Gravel S<strong>an</strong>d fine coarse Clay<br />

Reihe2<br />

Reihe3<br />

Grain size (mm)<br />

Hostun S<strong>an</strong>d (Flavigny et al. 1990) Hostun S<strong>an</strong>d (Lins & Sch<strong>an</strong>z 2005) 100 10 1 0.1 0.01 0.001<br />

Figure 5.1: Grain-size distribution <strong>of</strong> Hostun S<strong>an</strong>d

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