September 2011
Corrosion of Alumina-Based Ceramics
3051
Table II. The Activation Energies of Dissolution of the Material AH, and Rate Constants Measured for Corrosion in Deionized
Water and in 0.5M NaCl Solution
Deionized water
0.5 mol/L NaCl
2
ꢂ1
2
ꢂ1
Specimen
k mmol(m ꢀ h)
E [kJ/mol]
k mmol(m ꢀ h)
E [kJ/mol]
Material A
2901C
2001C
1501C
0.002170.0001
0.00970.001
—
—w
0.01470.001
0.002670.0003
—
—w
Material AH
2
2
1
901C
001C
501C
5071
5.470.4
1.770.1
48.370.6
6772
9.773
2.170.3
49.070.1
wNot determined.
2
ꢂ
3ꢂ
4ꢂ
ꢂ
ꢂ
pH, Si(OH)
4
further dissociates into H SiO
2
4
/HSiO
4
/SiO
4
Al2O3 þ OH þ 2H2O ! AlðOHÞ þ AlOOH
(4)
(5)
4
1 18,19
ꢂ
and produces more H . In the presence of [Al(OH)
Ca , and Si(OH) various complexes such as Al(OH) H SiO
can be formed along with other corrosion products, e.g. anort-
hite (CaOꢀ Al ꢀ 2SiO ) confirmed by XRD at the surface of
AH corroded in deionized water. In the contrary, in aqueous
4
] ,
ꢂ
ꢂ
21
ꢂ
AlOOH þ OH þ H2O ! AlðOHÞ
4
4
3
3
4
with the second reaction being the faster of the two. According
to phase distribution diagram, the principal Al specie in the
presence of OH is the aluminate ion [Al(OH) ] . As our experi-
O
2 3
2
ꢂ
ꢂ 12
1
environment with Na ions, analcime (Na(Si Al)O ) was iden-
2 6
4
ments were carried out in the solutions with neutral pH,
amorphous Al(OH) precipitates can also form along with the
3
tified as the main reaction product (Table I), while calcium re-
mained in a soluble form. Calcium together with silicon were not
detected with EDX analysis in the corrosion affected, approxi-
mately 400 mm thick, layer. Similar dissolution rate constants
were acquired for deionized water and the NaCl solution.
aluminate ions: these can be hydrothermally aged to yield crys-
talline products. Speaking in terms of Al speciation, the pH
value 6.970.3 determined in deionized water after the corrosion
tests falls into the neutral solution range. The dissolution equa-
tion (Eq. (6)) is then proposed to proceed as follows:
V. Conclusion
ꢂ
3þ
2
Al2O3 þ 6H2O ! 3AlðOHÞ þ Al
(6)
4
(
1) Static Conditions
31
Precipitation of Al ions in the form of boehmite (AlOOH),
as the new secondary phase covering the surface of the specimen
A corroded in deionized water, was detected by various analyt-
ical techniques. Summarizing the weight loss measurements and
the solution chemistry, the corrosion of the specimen A in both
corrosion solutions comprised the mentioned dissolution pro-
cess with partial precipitation of aluminum hydroxid-oxides.
However, the process was rather slow when comparing to dis-
solution of the material AH.
Dissolution in both corrosion media of the material A was
found to be an extremely slow, temperature-dependent process.
Partial dissolution of alumina matrix grains was documented by
rounding of the surface grain edges. Loosening and detachment
of some matrix grains explained by grain-boundary attack and
possible dissolution of small amounts of silicon-containing grain
boundary segregated impurities is considered as the principal
mechanism of material degradation. Hydroxyaluminates, iden-
tified by XRD as boehmite, precipitate to form the discontinu-
ous layer at the surface of the specimens corroded at 2901C in
deionized water.
The hypothesis that corrosion of the AH ceramics proceeds
via dissolution of the grain-boundary glassy phase is supported
by the eluate chemistry together with the analysis of corroded
surfaces and newly formed secondary phases. The mechanism of
dissolution reported for aluminosilicate oxides and glasses can
be therefore applied, as the presence of calcium aluminosilicate
Corrosion of the material AH is by three orders of magnitude
faster than that of the material A, and attacks preferentially the
calcium alumino-silicate grain-boundary glass. The initial dis-
2
ꢂ1
9
solution rates of 50 and 67 mmol(m ꢀ h) were determined at
the temperature 2901C in deionized water and in the aqueous
sodium chloride solution, respectively. The apparent activation
energies 48.370.6 kJ/mol (deionized water) and 49.070.1 kJ/
mol (NaCl solution) suggest metal-proton exchange reactions
glass phase was confirmed at the grain boundaries. Jantzen
1
5
et al. treats dissolution of such glasses through activated com-
plex as a rapid removal of univalent and divalent cations from
the near surface by ion exchange followed by the slower ex-
31
1
change of Al for 3H protons in solution. Divalent metal–
oxygen bonds break faster than trivalent metal–oxygen bonds,
4
and dissolution of SiO tetrahedra as the rate-controlling disso-
1
6
31
lution mechanism. In deionized water saturation of the corro-
sion solution was observed, accompanied by precipitation of
anorthite-type compounds, and by significant depletion of the
corrosion solution of Ca. In the aqueous sodium chloride solu-
tion analcime, Na(Si Al)O , was detected by XRD as the main
2 6
precipitated phase after 480 h of corrosion. Precipitation of
analcime was accompanied by depletion of the eluate of Si.
which break faster than Si–O bonds. The Al —proton ex-
change does not destroy the glass framework but it partially
liberates three adjoining silica tetrahedra to which it is bonded.
It is the detachment of the partially liberated silica that is the
rate-determining step, that is, partially detached silica dissolves
more readily than bonded or ‘‘attached’’ tetrahedral silica.
After Ca, Al, and Si are released from the grain-boundary
glass of the attacked ceramic material, various reactions can oc-
cur due to the complex solution chemistry. The hydrolysis of
Al(III) is characterized by a series of mononuclear as well as
(
2) Quasi-Dynamic Conditions
The quasi-dynamic conditions applied during the tests were not
able to prevent completely the attainment of the equilibrium
resulting in precipitation of secondary phases and partially cov-
ering the surfaces of corroded specimens. Needle-like precipi-
tates of anorthite assembled to spherical aggregates were found
at surfaces corroded in deionized water and the lamellas aggre-
gated to globular clusters of analcime were observed at the sur-
faces of the material AH exposed to the aqueous sodium
3
1
polynuclear species. It has been shown that [Al(OH
2
)
6
]
under-
21
goes successive deprotonation steps to yield [Al(OH)]
,
Al(OH) ] , and Al(OH)3(aq). In neutral solution and upon in-
1
17
[
creasing pH the amorphous Al(OH)
2
dissolves and the alum-
(aq)
3
ꢂ
17
inate ion, [Al(OH)
mostly Si(OH) . It is a weak acid, of which the first degree dis-
sociation produces H SiO and H at a pH o9, and at higher
4
]
is formed. Dissolved Si(IV) specie is
4
ꢂ
4
1
3