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Hydro-Mechanical Properties of an Unsaturated Frictional Material

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214 APPENDIX A. DETAILS ZOU’S MODEL (2003, 2004)<br />

The average pore volume Vv0 per particle in a soil with pore ratio e, in proportion to r 3 s,<br />

c<strong>an</strong> be written as:<br />

Vv<br />

r3 s<br />

= 4π · e<br />

3<br />

(A.2)<br />

When the contact regions in a soil are wetted or dried to a position <strong>an</strong>gle α, according to<br />

the so-called capillary law (Fredlund & Rahardjo 1993b) the dimensionless suction σu(α) in<br />

pore water, in relation to α c<strong>an</strong> be expressed as follows:<br />

σu(α) = (ua − uw) · rs<br />

Ts<br />

=<br />

(2 − sin α − 2 cos α) · cos α<br />

1 − sin α(1 − cos α) − cos α(2 − cos α)<br />

(A.3)<br />

where ua <strong>an</strong>d uw are air <strong>an</strong>d water pressure respectively, Ts is the so-called surface tension <strong>of</strong><br />

capillary water (e.g. Ts = 72.75mN/m for the temperature T = 20C ◦ ).<br />

In Zou (2003), Zou (2004) it was proposed that the form <strong>of</strong> the ideal symmetrical frustum-<br />

shaped pores c<strong>an</strong> be described using a function y relating to the radius r (Fig. 2.22(b)) as<br />

following:<br />

y<br />

rs<br />

= a −<br />

b<br />

r 2 /r 2 s − c<br />

(0 ≤ y ≤ rs) (A.4)<br />

where a, b <strong>an</strong>d c are three const<strong>an</strong>ts that c<strong>an</strong> be determined according to geometrical <strong>an</strong>d<br />

physical boundary conditions using following equations:<br />

�<br />

�<br />

a 1 �ρ((αmax) a (a − 1) ln − + ξ)<br />

a − 1 a<br />

2 − ϱ 2 (αmax) �<br />

<strong>an</strong>d<br />

= 4e<br />

−<br />

3nf0<br />

nc · Vw1(αmax)<br />

2π · nf0 · r3 − ρ<br />

s<br />

2 (αmax)<br />

b = a (a − 1) �� ρ(αmax) + ξ) 2� − ρ 2 (αmax) �<br />

c = ρ 2 (αmax) − b<br />

(A.5)<br />

(A.6)<br />

(A.7)<br />

a<br />

where ρ(αmax) = (1−cos αmax)/ cos αmax <strong>an</strong>d ξ is a form parameter which describes the form<br />

<strong>of</strong> the symmetrical frustum-shaped pores.<br />

When a symmetrical frustum-shaped pore is filled with water up to y, from Eq. A.4 <strong>an</strong>d<br />

by integration the volume Vw1(y) <strong>of</strong> the pore water in the symmetrical frustum-shaped pore<br />

c<strong>an</strong> be written as:<br />

Vw1(y)<br />

r 3 s<br />

�<br />

= π c y<br />

+ b · ln<br />

rs<br />

a<br />

a − y/rs<br />

�<br />

(0 ≤ y ≤ rs) (A.8)<br />

The total volume Vw(y, α) <strong>of</strong> pore water per particle during the main imbibition <strong>an</strong>d<br />

drainage processes as well as during the secondary imbibition <strong>an</strong>d drainage processes, de-<br />

pending on y <strong>an</strong>d/or α, c<strong>an</strong> be written as:<br />

Vw(y, α)<br />

r 3 s<br />

= nf (y) Vw1(y)<br />

r 3 s<br />

+ nfi(y, α) Vw1(yi)<br />

r 3 s<br />

Vw1(α)<br />

+ nc<br />

2r3 s<br />

(A.9)

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