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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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8.2. SOIL-WATER CHARACTERISTIC CURVE MODEL 177<br />

Table 8.2: Constitutive parameters for the new SWCC model (calibrated against imbibition<br />

data)<br />

Experimental results β0 β1 β2 β3 s0<br />

Loose specimen, 2 nd imbibition process<br />

TDR/T 70 mm 38.86 −5.91 0.50 −33.12 3.49<br />

TDR/T 160 mm 38.56 −4.63 0.92 −32.62 3.11<br />

TDR/T 260 mm 38.28 −5.05 0.50 −30.42 2.81<br />

TDR/T 360 mm 38.55 −4.37 0.42 −20.92 1.92<br />

- Parameter β2 that also influences the slope <strong>of</strong> the curve <strong>an</strong>d is in all depth approximately<br />

β2 = 0.5.<br />

An influence according to the initial imbibition suction s0 was found for the scaling param-<br />

eter β3 that influences the minimum volumetric water content θmin. With increasing initial<br />

imbibition suction s0 the parameter β3 is decreasing. Further, it is now tried to replace β3<br />

with a term expression depending on s0, which incorporates the variation <strong>of</strong> this parameter<br />

for different layers. Simple linear term <strong>of</strong> s0 instead a const<strong>an</strong>t β3 showed the best fit over<br />

the trial models. The resulting hysteresis model is:<br />

θ(ψ) = β0 + (β 1 3 + β 2 3 · s0) exp(− ψβ1<br />

) (8.3)<br />

where: s0 is the initial imbibition suction measurement that has been recorded using ten-<br />

siometer sensor. Results <strong>of</strong> the proposed hysteresis model curve fit for both the 1 st <strong>an</strong>d 2 nd<br />

imbibition process are show in Fig. 8.5 for the loose specimen (<strong>an</strong>d in Fig. E.5 for curve fit <strong>of</strong><br />

dense specimen in Appendix E). In the 3D plots the initial imbibition suction s0 is introduced<br />

as 3rd dimension on the z-axis. Similar to the curve fit results from the drainage process the<br />

calculated results seem to be in good agreement to the experimental results for loose specimen<br />

(1 st imbibition <strong>an</strong>d 2 nd imbibition process). The identified parameters <strong>an</strong>d the coefficient <strong>of</strong><br />

linear regression R 2 are summarized in Tab. 8.3. For drainage as well as imbibition curve<br />

fitting procedure the Levenberg-Marquardt algorithm was used, that is <strong>an</strong> improvement <strong>of</strong><br />

the classical Gauss-Newton method for solving non-linear least-square regression problems.<br />

The plots given in Figs. 8.6 to 8.9 derived from regression <strong>an</strong>alysis <strong>of</strong> loose specimen<br />

are used to appreciate wether or not the model fits the experimental data well (see also the<br />

results derived from regression <strong>an</strong>alysis <strong>of</strong> dense specimen in Figs E.6 to E.9 in Appendix E).<br />

Both statistical techniques, coefficient <strong>of</strong> regression determination <strong>an</strong>d residual <strong>an</strong>alysis were<br />

used to validate the model <strong>an</strong>d to see the adequacy <strong>of</strong> different aspects <strong>of</strong> the model. The<br />

statistical results from model validation are shown in Figs. 8.6 <strong>an</strong>d 8.7 for the model fit<br />

<strong>of</strong> several drainage suction-water content measurements for loose specimens. The model<br />

validation results <strong>of</strong> the statistical <strong>an</strong>alysis derived from the 1 st as well as 2 nd imbibition<br />

β2

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