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Kroner

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But because of cubic symmetry, c 66 = c 44 , so that <strong>Kroner</strong>’s coefficients ᾱ, ¯β, ¯γ<br />

are consistent with the above coefficients a, b, c, namely:<br />

ᾱ = 1 8 (5c 11 + 4c 12 ) = a (228)<br />

¯β = − c 44<br />

8 (7c 11 − 4c 12 ) = −b (229)<br />

¯γ = − c 44<br />

8 (c 11 + 2c 12 )(c 11 − c 12 ) = −c (230)<br />

as required, thus completing the derivation of <strong>Kroner</strong>’s cubic.<br />

13 Comparison with experimental data<br />

Hashin and Shtrikman [11], [12] have derived bounds for the isotropic shear<br />

modulus of aggregates of cubic crystals. Gschneider [13] provides experimental<br />

data, and Simmons [14] provides cubic crystal elastic coefficients in Mbar. Sisodia<br />

[15] compares some experimental data with calculated shear modulus and<br />

reports the formulation of the Hashin-Shtrikman bounds, G ∗ 1 and G ∗ 2 in terms<br />

of the single crystal cubic coefficients c ij as:<br />

where<br />

(<br />

) −1<br />

G ∗ 5<br />

1 = G 1 + 3 − 4β 1 (231)<br />

G 2 − G 1<br />

(<br />

G ∗ 2 = G 2 + 2<br />

5<br />

G 1 − G 2<br />

− 6β 2<br />

) −1<br />

(232)<br />

β 1 = − 3 K + 2G 1<br />

5 G 1 (3K + 4G 1 )<br />

β 2 = − 3 K + 2G 2<br />

5 G 2 (3K + 4G 2 )<br />

An anisotropy index à is defined by:<br />

K = c 11 + 2c 12<br />

3<br />

(233)<br />

(234)<br />

(235)<br />

G 1 = c 11 − c 12<br />

2<br />

(236)<br />

G 2 = c 44 (237)<br />

à = G 2<br />

G 1<br />

= 2c 44<br />

c 11 − c 12<br />

(238)<br />

which reduces to unity for isotropic material. Table 1 shows the cubic coefficients<br />

and the anisotropy index for several materials. Notice that Tungsten (W) and<br />

Molybdenum (Mo) come closest to being isotropic.<br />

To compare the shear modulus determined by <strong>Kroner</strong>’s cubic with experimental<br />

values, we use a simple iterative Newton’s method, beginning with a trial

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