In this, Part II of a two-part study, the oxidation kinetics in air of the
ternary compounds Ti2AlC, Ti2AlC0.5N0.5, Ti4AlN2.9, and Ti3AlC2 are reporte
d. For the first two compounds, in the 1000-1100 degreesC temperature range
and for short times (approximate to 20 h) the oxidation kinetics are parab
olic. The parabolic rate constants are k(x) (m(2)/s) = 2.68 x 10(5) exp - 4
91.5 (kJ/mol)/RT for Ti2AlC, and 2.55 x 10(5) exp - 458.7 (kJ/mol)/RT for T
i2AlC0.5N0.5. At 900 degreesC, the kinetics are quasi-linear, and up to 100
h the outermost layers that form are almost pure rutile, dense, and protec
tive. For the second pair, at short times (<10 h) the oxidation kinetics ar
e parabolic at all temperatures examined (800-1100<degrees>C), but become l
inear at longer times. The k(x) values are 3.2 x 10(5) exp - 429 (kJ/mol)/R
T, for Ti4AlN2.9 and 1.15 x 10(5) exp - 443 (kJ/mol)/RT for Ti3AlC2. In all
cases, the scales that form are comprised mainly of a rutile-based solid s
olution, (Ti1-yAly)O2-y/2 where y < 0.05, and some Al2O3. The oxidation occ
urs by the inward diffusion of oxygen and the outward diffusion of Al and T
i. The C and N atoms are presumed to also diffuse outward through the oxide
layer. At the low oxygen partial pressure side, the Al3+ ions dissolve in
and diffuse through the (Ti1-yAly)O2 -y/2 layer and react with oxygen to fo
rm Al2O3 at the high oxygen pressure side. This demixing results in the for
mation of pores that concentrate along planes, especially at longer times a
nd higher temperatures. These layers of porosity impede the diffusion of Al
, but not those of Ti and oxygen, which results in the formation of highly
striated scales where three layers, an Al2O3-rich, a TiO2-rich, and a porou
s layer repeat multiple (>10) times. The presence of oxygen also reduces th
e decomposition (into TiXx and Al) temperatures of Ti4AlN2.9 and Ti3AlC2 fr
om a T > 1400 degreesC, to one less than 1100 degreesC. (C) 2001 The Electr
ochemical Society.