capacity (OH radicals and ozone) decreases in the system.
In addition, the presence of H2O2 leads to a partial reduction
of HOBr, which is an important intermediate in bromate
formation. These two factors reduced the bromate formation
by approximately a factor of 2, from 15.1 to 8.8 µg/ L.
Kinetic Modeling of MTBE Degradation by the AOP O3/
H2O2. A kinetic model was applied to predict the evolution
of MTBE and its degradation products in natural waters by
conventional ozonation and the AOP O3/ H2O2 and compared
to experimental results. For this, in addition to the rate
constants and the degradation product distribution, the
concentration of both oxidants ozone and OH radicals were
determined (k and Rct in Table 3). The contribution of several
degradation pathways must be considered to estimate the
transient formation of the degradation products. For that
purpose, the overall rate constants of MTBE and of each of
its degradation products with both oxidants have been split
up according to the partial contribution of each pathway
given in Figure 2. With the determined oxidant concentrations
and the split rate constants, the concentrations of MTBE
and its degradation products have been calculated from eq
1 with the help of the computer program ACUCHEM (39).
At higher ozone doses (4 mg/ L), an increased bromate
formation is found because of the increased overall oxidation
capacity in the system. An increase of the ozone dose leads
to an enhanced elimination of MTBE (by almost a factor of
2). This shows that the OH radical exposure is increased
significantly with the higher ozone dose. In addition, the
ozone exposure also increases. Both factors lead to an
increased bromate formation by about a factor of 2 (from 8.8
to 16.8 µg/ L). Therefore, MTBE oxidation in the LZ water is
restricted by bromate formation at pH 7. An oxidation of
about 50% can be achieved without exceeding the bromate
standard of 10 µg/ L when the AOP O3/ H2O2 is applied with
an initial bromide concentration of 50 µg/ L.
The data shown in Figures 3 and 4 allow comparisons of
the model calculations of MTBE degradation (lines) with
measured data (symbols) for various experimental conditions
and types of natural waters. It can be seen that MTBE
oxidation is well predictable. Figure 5 shows measured data
(symbols) and model calculations (lines) for MTBE removal
and formation of its degradation products during treatment
of LZ water (Figure 5a), WP water (Figure 5b), and LM water
(Figure 5c) at the respective experimental conditions (for
details, see figure captions). Experiments performed with
natural waters resulted in measurable concentrations of
MTBE, TBF, TBA, AC, and MA. Because of the low initial
concentration of MTBE (2 µM) and the interference of
thiosulfate in the analytical method, some aldehyde inter-
mediates could not be quantified. FA could only be measured
in the last reaction sample (after complete ozone depletion),
and the obtained values were very similar to those predicted
by model calculations. The concentrations of MMP (also a
primary degradation product) as predicted by the kinetic
model are also included in Figure 5 (dotted line), although
we cannot compare these values to measured data. The
dashed line in Figure 5 represents the mass balance including
measured concentrations of the primary degradation prod-
ucts MTBE, TBF, TBA, AC, and MA and the modeled
concentrations of MMP. Some control samples of natural
waters before and after ozonation have been analyzed, and
no MTBE degradation products were found (data not shown),
which indicates that the measured mass balance is in fact
due to MTBE degradation. The experimental mass balance
was well above 90% of the initial MTBE concentration in all
cases, indicating that the formation of the secondary
degradation products is not relevant until MTBE degradation
exceeds 50%. Note that measured concentrations of AC were
often slightly higher than the model predictions (mainly in
conventional ozonation experiments), which can be at-
tributed to the formation of AC from oxidation of NOM or
small interferences in the background signal of the GC/ MS
from the natural water. The otherwise good agreement
between the model calculations and the experimental results
validates the results of our study.
An increase in pH from 7 to 8 leads to a decrease of the
bromate formation for both conventional ozonation and the
AOP O3/ H2O2. To compare both pH values, however, the
elimination of MTBE has to be considered. In both cases,
less MTBE is eliminated at the higher pH, which is the result
of a lower OH radical exposure. In addition, the experiments
show that the ozone exposure is lower (k increases) at the
higher pH. Another reason for a reduced bromate formation
is the enhanced reduction of HOBr by H2O2 at the higher pH
value. The superposition of all three factors results in a lower
bromate formation (36). Only when normalized to the same
ozone exposure bromate formation increases with increasing
pH (35).
The two other waters (WP, LM) follow basically the same
trend (see Table 3) as discussed for LZ water. However, the
degree of bromate formation varied significantly. The
comparison of LZ water and WP water for the AOP O3/ H2O2
with an ozone dose of 4 mg/ L shows that the MTBE oxidation
was similar, whereas the bromate formation was almost twice
in WP water. In the DOC-poor WP water, the half-life of
ozone was substantially higher, which lead to a higher ozone
exposure. In addition, due to the high carbonate content,
carbonate radicals contributed to enhanced bromate forma-
tion (35). Therefore, in WP water only about 35% of MTBE
can be oxidized by the AOP O3/ H2O2 without exceeding the
bromate standard with the initial bromide concentration used
in these experiments (50 µg/ L). In LM water, about 50% of
MTBE can be oxidized without exceeding the bromate
standard, but a higher ozone dose is required due to the high
overall scavenging capacity of this water. In fact, the same
degree of MTBE oxidation can be achieved for LM water
with an ozone dose of 4 mg/ L (AOP O3/ H2O2) for LZ water
with an ozone dose of 2 mg/ L (AOP O3/ H2O2). The bromate
formation in both cases is identical at about 8.8 µg/ L, and
the ozone exposure is similar as well (1.4 × 10-4 M min-1).
The factor of 2 in ozone dosage needed to obtain similar
results is reflected in a 2-fold greater scavenging capacity for
LM water as compared to LZ water.
In conclusion, MTBE oxidation by conventional ozonation
and the AOP O3/ H2O2 has to be carefully optimized with
regard to bromate formation. To achieve a similar degree of
MTBE oxidation, the overall scavenging capacity has to be
considered and the ozone dose adapted accordingly. Once
a certain degree of MTBE oxidation has been set, the bromate
formation is a function of the resulting ozone exposure. The
oxidation of MTBE is an “unfortunate” case because of its
relatively low reactivity toward OH radicals. For other
compounds with higher rate constants with OH radical (e.g.,
aromatic compounds), better removal could be achieved,
and the optimization pollutant elimination/ bromate forma-
tion would be easier.
Overall, the combination of experimental kinetic data with
modeling enables to predict not only the time course of MTBE
removal but also the concomitant formation of its degradation
products during conventional ozonation and AOP treatment
of natural waters. In addition, our results allow a quantitative
prediction of the formation of primary degradation products
based on the degree of MTBE elimination. This is shown in
Figure 6 where the production of degradation products is
correlated to the MTBE elimination (molar basis). The data
shown in Figure 6 include both conventional ozonation and
the AOP O3/ H2O2 for the different water types investigated
in the present study. The slopes of the straight lines are 0.35
(TBF and FA), 0.23 (AC), 0.11 (TBA), and 0.07 mol/ mol (MA).
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