Grain boundary structures and O tracer diffusivities (table 6) were studied in transparent ceramics whose compositions varied from a 2% excess of Y2O3 to an 0.5% excess of Al2O3. In the former case, a second phase (yttrium aluminium perovskite) which contained Si was found in the grain boundaries. In the case of an Al2O3 excess, both Al-rich particles (alumina) and a Si-rich segregated layer were found in the grain boundaries. It was found that volume diffusion of the O tracer was little affected by the excesses. On the other hand, the grain boundary diffusion of O (table 7) was suppressed in Y2O3-excess specimens, as compared with Al2O3-excess specimens. These differences were attributed to the effect of chemical reactions between second phases and intergranular liquid during sintering.

I.Sakaguchi, H.Haneda, J.Tanaka, T.Yanagitani: Journal of the American Ceramic Society, 1996, 79[6], 1627-32

 

 

 

 

Table 6

Arrhenius Parameters for Bulk O Diffusion in Al5Y3O12

 

 

Condition

 

Addition

 

Do (m2/s)

 

Q (kJ/mol)

 

 

non-annealed

 

2%Y2O3

 

5.8 x 10-10

 

259.6

non-annealed

1%Y2O3

7.7 x 10-11

223.9

non-annealed

stoichiometric

4.3 x 10-8

304.1

non-annealed

0.5%Al2O3

3.9

519.4

annealed

2%Y2O3

2.1 x 10-7

348.2

annealed

1%Y2O3

2.2 x 10-9

286.1

annealed

stoichiometric

2.6 x 10-10

265.8

annealed

0.5%Al2O3

2.3 x 10-5

408.5

 

 

 

 

 

 

Table 7

Arrhenius Parameters for Grain Boundary O Diffusion in Al5Y3O12

 

 

Condition

 

Addition

 

Do (m2/s)

 

Q (kJ/mol)

 

 

non-annealed

 

stoichiometric

 

2.1 x 10-10

 

393.8

non-annealed

0.5%Al2O3

124

688.8

annealed

stoichiometric

1.1 x 10-8

463.9

annealed

0.5%Al2O3

5.6 x 10-9

459.2