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A new yield function for geomaterials. - Ingegneria - Università degli ...

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278 Davide Bigoni, Andrea Piccolroaz<br />

Table 3. Correspondence between parameters of (6)-(9) and Deshpande and Fleck (2002) <strong>yield</strong><br />

<strong>function</strong>s —the latter shortened as ‘DF model’— to describe the behaviour of metallic foams.<br />

DF model<br />

Y ,α 2α<br />

Model (6)-(9) DF model<br />

M c pc Y α<br />

<br />

Y<br />

1+<br />

α<br />

<br />

α<br />

<br />

<br />

2 Y<br />

1+<br />

3 α<br />

Model (6)-(9)<br />

M,pc,c — — —<br />

<br />

α<br />

2 3<br />

<br />

2<br />

— —<br />

cM<br />

1+ M<br />

6<br />

where f is the void volume fraction (taking the values {0.01, 0.1, 0.3, 0.6 } in Fig. 10),<br />

σM is the equivalent flow stress in the matrix material and q1 =1.5, q2 =1and<br />

q3 = q 2 1 are the parameters introduced by Tvergaard (1981, 1982). A good agreement<br />

between the two models can be appreciated from Fig. 10, increasing when the void<br />

volume fraction f increases.<br />

q/ M<br />

1<br />

0.8<br />

0.6<br />

0.4<br />

0.2<br />

0.6<br />

0.3<br />

0.1<br />

0.5 1 1.5 2 2.5 3 3.5<br />

p/ <br />

Present model<br />

Gurson model<br />

f = 0.01<br />

Figure 10. Comparison with the Gurson model at different values of void volume fraction f.<br />

As far as the deviatoric section is regarded, we limit to two examples —reported<br />

in Fig. 11— concerning sandstone and dense sand, where the experimental data have<br />

been taken from Lade (1997, their Figs. 2 and 9a).<br />

Experimental data referred to the biaxial plane σ 3 =0<strong>for</strong> grey cast iron and concrete<br />

(taken respectively from Coffin and Schenectady, 1950, their Fig. 5 and Tasuji et<br />

al. 1978, their Figs. 1 and 2) are reported in Fig. 12.<br />

2<br />

M<br />

2

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