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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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174CHAPTER 8. NEW SWCC MODEL FOR SAND INCLUDING SCANNING CURVES<br />

θ 2<br />

ln θ<br />

ln ln θ<br />

ψ 2<br />

ln ψ<br />

ln ln ψ<br />

Figure 8.2: Results from data tr<strong>an</strong>sformation using experimental results (initial drainage, 1 st<br />

drainage, 2 nd drainage) from drainage tr<strong>an</strong>sient state column tests (loose specimen)<br />

where: the parameter β0 is the maximum volumetric water content, that is commonly the<br />

saturated volumetric water content θs <strong>an</strong>d β3 is related to the minimum volumetric water<br />

content, that is commonly the residual volumetric water content θr with θr = β0+β3 <strong>an</strong>d β1, β2<br />

are parameters. The new soil-water characteristic curve model was tested on experimental<br />

results measured in several depth in the tr<strong>an</strong>sient s<strong>an</strong>d column test (drainage process). The<br />

outcomes <strong>of</strong> the curve fits using the proposed model are given in Fig. 8.3 for loose specimen (see<br />

also Fig. E.3 in Appendix E for curve fits <strong>of</strong> experimental results from dense specimen). The<br />

Table 8.1: Constitutive parameters for the new SWCC model (calibrated against drainage<br />

data)<br />

Experimental results β0 β1 β2 β3 R 2<br />

Loose specimen, drainage process<br />

TDR/T 70 mm 39.00 −6.57 0.0146 −33.118 0.999<br />

TDR/T 160 mm 38.66 −5.69 0.0316 −33.106 0.999<br />

Dense specimen, drainage process<br />

TDR/T 260 mm 36.72 −8.07 0.0015 −28.592 0.999<br />

TDR/T 360 mm 34.21 −9.32 0.0003 −23.621 0.992

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