25.01.2013 Views

Hydro-Mechanical Properties of an Unsaturated Frictional Material

Hydro-Mechanical Properties of an Unsaturated Frictional Material

Hydro-Mechanical Properties of an Unsaturated Frictional Material

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

186 CHAPTER 9. NUMERICAL SIMULATION OF COLUMN TEST BY FEM<br />

9.2 Model used for Numerical Investigation<br />

Based on the suction-water content model developed by Parker & Lenhard (1987) numerical<br />

investigation are carried out. The model is <strong>an</strong> empirical scaling hysteresis approach that c<strong>an</strong><br />

produce a realistic representation <strong>of</strong> sc<strong>an</strong>ning curves <strong>an</strong>d hysteresis loops. For prediction <strong>of</strong><br />

main drainage <strong>an</strong>d main imbibition curve Parker & Lenhard (1987) used the suction-water<br />

content model by v<strong>an</strong> Genuchten (1980). Their concept introduces <strong>an</strong> apparent saturation in<br />

order to account for the effect <strong>of</strong> residual trapped non-wetting phase saturation. Thus they<br />

distinguish between the effective <strong>an</strong>d the apparent wetting phase saturation. The effective<br />

saturation ¯ Sw is considered as the mobile part <strong>of</strong> the phase. The apparent saturation ¯ Sw is<br />

the sum <strong>of</strong> the effective saturation ¯ Sw <strong>an</strong>d the trapped effective saturation ¯ Snt <strong>of</strong> the non-<br />

wetting phase (see Fig. 9.1). If there is non-wetting phase entrapment ( ¯ S nr(i)), the soil-water<br />

characteristic curve for drainage <strong>an</strong>d imbibition do not form closed loops. The formation <strong>of</strong><br />

closed loops is possible by substitution <strong>of</strong> the effective by the apparent saturation (Fig. 9.1),<br />

that also accounts for fluid entrapment. Consequently, hysteresis is formed by scaling the<br />

apparent saturation. For example, saturation at point ζ that lies on <strong>an</strong> imbibition sc<strong>an</strong>ning<br />

curve (see Fig. 9.1, right) c<strong>an</strong> be scaled as follows:<br />

¯Sw(ζ) =<br />

¯S7 − ¯ S6<br />

¯S5 − ¯ · (<br />

S6<br />

¯ S4 − ¯ S3) + ¯ S3. (9.1)<br />

For simulation <strong>of</strong> flow in unsaturated porous media <strong>an</strong>d considering hysteresis effect in<br />

these simulations the model by Parker & Lenhard (1987) was implemented into MUFTE-<br />

UG by Sheta (1999) <strong>an</strong>d Papafotiou (2008).<br />

Capillary Pressure<br />

i<br />

S w(i)<br />

j<br />

S nt(ij)<br />

S w(j)<br />

S w(j)<br />

S nr<br />

S nr(i)<br />

Effective Saturation Apparent Saturation 1<br />

Figure 9.1: Hysteresis <strong>an</strong>d phase entrapment properties <strong>of</strong> the soil-water characteristic curve<br />

Capillary Pressure<br />

5<br />

7<br />

2<br />

6<br />

4<br />

ζ ξ<br />

3

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!