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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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2.5. CONSTITUTIVE MODELS FOR HYDRAULIC FUNCTIONS 49<br />

responsible for the geometry <strong>of</strong> the frustums, the parameter nf0 describes the number<br />

<strong>of</strong> the frustums, <strong>an</strong>d the parameter µ describes the drainage process <strong>of</strong> some residual<br />

frustums, thus they are responsible for the volume <strong>of</strong> water in the frustum-shaped pores,<br />

<strong>an</strong>d influence mainly the saturated <strong>an</strong>d the unsaturated zone.<br />

Maximum contact <strong>an</strong>gle αmax: The maximum contact <strong>an</strong>gle αmax is reached, when ad-<br />

joining contractile skins are in contact <strong>an</strong>d the frustum-shaped pores are filled with wa-<br />

ter. As smaller the contact <strong>an</strong>gle αmax as higher the suction, which has to be applied for<br />

draining the contact regions. With decreasing contact <strong>an</strong>gle αmax the unsaturated zone<br />

is increasing <strong>an</strong>d the residual zone is decreasing during drainage process (see Fig. 2.23).<br />

Frustum number nf0 per sphere: When αmax is reached, the frustum-shaped pore be-<br />

tween the grains is filled with water. The remaining pore volume is taken into account<br />

by a function, describing the volume <strong>of</strong> a frustum. The largest volume <strong>of</strong> water is lo-<br />

cated in these pores. Thus the number <strong>of</strong> frustums nf0 is influencing the shape <strong>of</strong> the<br />

curve signific<strong>an</strong>tly in the saturated zone as well as unsaturated zone. With increasing<br />

nf0 the saturated zone <strong>an</strong>d unsaturated zone is shifting to higher suction values during<br />

drainage process. Same behavior c<strong>an</strong> be observed for the imbibition process. As larger<br />

nf0 as larger the air-entry value ψaev <strong>an</strong>d the water-entry value ψwev (see Fig. 2.24).<br />

Form parameter ξ: The form parameter ξ defines the geometry <strong>of</strong> the frustum <strong>an</strong>d<br />

estimates the upper diameter <strong>of</strong> the frustum. With increasing ξ the curve becomes<br />

flatter for drainage <strong>an</strong>d imbibition process. As smaller ξ as more distinct the air-entry<br />

value ψaev. The saturated zone is shifting to higher suction values for decreasing ξ while<br />

wetting the specimen (see Fig. 2.25).<br />

<strong>Material</strong> parameter ζ: The material parameter ζ is responsible for the form <strong>of</strong> the<br />

meniscus in the frustum-shaped pores <strong>an</strong>d thus it influences the suction (ua − uw)<br />

Contact points<br />

A<br />

Pore water in<br />

“contact regions”<br />

r s<br />

α<br />

Capillary menisci<br />

A<br />

y<br />

Frustum-shaped<br />

pores<br />

r 1<br />

y<br />

β 0<br />

r 1 + ξ r s<br />

β(y)<br />

r<br />

r s<br />

particle water air<br />

a) b)<br />

A - A<br />

Figure 2.22: Pore spaces <strong>an</strong>d pore water (Zou 2003)

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