about one-half the value of these characteristics for available
resins. The steady state effluent concentration of a 2-m
column with a flow rate of 5 gpm and an influent of 115 µM
MTBE (10 mg/ L) would be 0.06 µM (0.005 mg/ L). This
evaluation suggests that adding a strong acid functionality
to carbonaceous resins may result in a material that would
be effective at transforming MTBE in a reasonably sized
treatment system. According to the resin vendors questioned,
such a resin does not currently exist. The assumption that
the sorbed MTBE is available for transformation needs to be
tested.
The effluent would contain the two alcohol products. This
technology would not be suitable for drinking water treatment
but could have applicability for pump and treat systems where
the effluent is discharged to a POTW. Understanding the fate
of the alcohol products will be important in assessing the
impact of these findings on groundwater protection and
possible treatment processes. Methanol should be readily
degraded under either aerobic or anaerobic conditions (50,
potentially impacted by the current findings is the role of
anaerobic microbial degradation of MTBE. To date, all of the
isolated MTBE-degrading microbial cultures are aerobic
(59, 60), and this is consistent with a role for oxygenase
enzymes in the initial cleavage of the ether bond (61, 62).
However, there have been some limited indications of
anaerobic MTBE degradation (51, 52, 63, 64). In these
instances, the mechanism of MTBE degradation is unknown.
While anaerobic conditions obviously exclude the possibility
of an oxygenation reaction directed at MTBE, an enzyme-
catalyzed hydrolysis of MTBE could potentially occur under
either aerobic or anaerobic conditions. The enzymes that
may be involved in the anaerobic degradation of MTBE are
not known at this time. However, it is possible that hydrolytic
enzymes catalytically similar to serine-containing peptidases
and carboxylic ester hydrolases could catalyze the hydrolysis
of MTBE. For example, the imidazole group associated with
the active site histidine residue in chymotrypsin functions
as an acid catalyst and also promotes the nucleophilic attack
of activated substrates by water (65). It is also notable that
the cleavage of the C-O-C bond in glycosidic bonds involves
an enzyme-catalyzed hydrolysis (6). For example, lysozyme
hydrolytically cleaves the â-(1-4) glycosidic bonds between
N-acetylglucosamine and N-acetylmuramic acid, the two
carbohydrate derivatives found in bacterial cell walls (65).
White et al. (66) also discussed the possibility of a hydrolytic
enzymatic mechanism in their review of the biological
scission of ether bonds. Although they presented limited
examples of ether hydrolyses, they felt that they may not
have much importance since, as they state, “ethers are ...
highly stable to hydrolysis even in the presence of mild acids”.
The results presented in this present study suggest that ether
oxygenates may be sufficiently susceptible to hydrolysis to
be subject to enzymatic cleavage.
5
1). In contrast, TBA degrading activity is less well character-
ized, although it has been detected at some (50, 52), but not
all (51), sites that have been investigated for biodegradation
processes.
The rate of MTBE hydrolysis in aqueous solution at near
neutral pH is too slow to have a significant impact on the
fate of this compound. At pH 7, the half-life of MTBE is
thousands of years. The observation of surface-catalyzed
hydrolysis may have implications for MTBE fate in the some
subsurface environments. The role of soils in catalyzing the
hydrolysis of organic compounds has been recently discussed
(
53, 54). Wei et al (53) studied the influence of clay minerals
on the hydrolysis of carbamate pesticides. A dilute suspension
10 mg/ L) of montmorillonite clay, a common soil constitu-
(
ent, resulted in a 100-fold increase in the rate of hydrolysis
at pH 6. These and other published results (57) suggest a
surface acidity of clay that can be 2 to 4 pH units lower than
the bulk solution. The high acidity of clays is due to both
Br o˜ nsted and Lewis acid sites (58). Although the acidity of
clays decreases as water content increases, clays can be used
as solid acids in aqueous solutions (58). The observed rate
of clay-catalyzed hydrolysis is higher in drier soils (57). The
similarity of clay to the ion-exchange resins evaluated in this
study is highlighted by the observation that clays can catalyze
the same MTBE synthesis reaction as IR-36WET (58).
Although the stability of MTBE at many sites indicates that
abiotic transformation may not be common, the high surface
area of clays, coupled with the high solids-to-water ratio of
the subsurface, suggests a possibility of surface-catalyzed
reactions.
Monitoring TBA concentrations in groundwater is be-
coming increasingly important due to both requests from
regulators and its role in evaluating the fate of MTBE.
California has proposed an action level for TBA in drinking
water of 0.16 µM or 12 µg/ L (55). Groundwater samples
collected for the analysis of volatile organic compounds are
typically preserved by lowering the pH to 2 or less by the
addition of a strong acid (56). Equation 1 can be used to
estimate the generation of TBA in preserved samples. At pH
Acknowledgments
A portion of this work was funded by the American Petroleum
Institute. The opinions expressed are those of the authors
and not necessarily those of the funding agency.
Literature Cited
(
1) Squillace, P. J.; Pankow, J. F.; Korte, N. E.; Zogorski, J. S.
Environmental Behavior and Fate of Methyl tert-Butyl Ether
(
MTBE); U. S. Geological Survey: Washington, DC, 1998.
(
2) Howard, P. H.; Boethling, R. S.; Jarvis, W. F.; Meylan, W. M.;
Michalenko, E. M. Handbook of Environmental Degradation
Rates; Lewis Publishers: Chelsea, MI, 1991.
(3) Burwell, R. L., Jr. Chem. Rev. 1954, 54, 615-685.
(
4) Zogorski, J. S.; Morduchowitz, A.; Baehr, A. L.; Bauman, B. M.;
Conrad, D. L.; Drew, R. T.; Korte, N. E., Lapham, W. W.; Pankow,
J. F.; Washington, E. R. In Interagency Assessment of Oxygenated
Fuels; National Science and Technology Council Committee on
Environment and Natural Resources: Washington, DC, 1997;
Chapter 2.
(
(
5) Mill, T. Environ. Tox. Chem. 1982, 1, 135-141.
6) Wallenfels, K.; Diekmann, H. In The Chemistry of the Ether
Linkage; Patai, S., Ed.; Interscience: London, 1967; pp 207-
2
42.
(
7) Butlerow, A. Ann. 1861, 118, 325-330.
(8) Silva, R. Ber. 1875, 8, 1352-1353.
2
, a sample with 115 µM MTBE (10 000 µg/ L) would result
(9) Lippert, W. Ann. 1893, 276, 148-199.
(
(
(
(
(
10) Baeyer, A. Ber. 1893, 26, 2558-2565.
in generation of 0.27 µM TBA (20 µg/ L) in 24 h at 25 °C. Since
the hydrolysis rate is dependent on pH, temperature, and
MTBE concentration, the fraction of TBA measured that
comes from MTBE hydrolysis in a given preserved sample
cannot be determined with precision. Measurements of low
TBA concentrations from preserved samples with moderate
MTBE concentrations should be viewed with caution.
Although this discussion has focused largely on abiotic
transformations of MTBE, results presented here also have
potential implications for our understanding of the biodeg-
radation of ether oxygenates. One area of research that is
11) Hughes, E. D.; Ingold, C. K. J. Chem. Soc. 1935, 244-255.
12) Skarabal, A.; Skarabal, R. Z. Physik. Chem. 1938, 130, 154-163.
13) Norris, J. F.; Rigby, G. W. J. Am. Chem. Soc. 1932, 54, 2088-2100.
14) Mitra, R. P.; Malhotra, H. C.; Jain, D. V. S. Trans. Faraday Soc.
1966, 62, 173-181.
(15) March, J. Advanced Organic Chemistry, 2nd ed.; McGraw-Hill:
New York, 1977; pp 349-353.
(
16) Ingold, C. K. Structure and Mechanism in Organic Chemistry,
nd ed., Cornell University Press: Ithaca, NY, 1969.
17) Arnett, E. M.; Wu, C. Y. J. Am. Chem. Soc. 1962, 84, 1680-1684.
2
(
(18) Cordes, E. H. In Prog. Phys. Org. Chem. Vol. 4, Streitweiser, A.
Jr.; Taft, R. W., Eds.; Interscience: New York, 1967; pp 1-44.
3
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