be described as catalysis, for both the phenol and phosphate
products are released into solution and not adsorbed.
However, at pH 4 most of the phosphate remains adsorbed
on to the oxide, and added phosphate inhibits the NPP
hydrolysis reaction.
are consistent with a role for surface hydroxyl groups acting
as nucleophiles in the hydrolysis mechanism. This would be
an analogous process to that observed for intramolecular
hydrolysis of phosphate esters in discrete metal complexes
in homogeneous aqueous solution (for example, ref 22).
Manganese dioxide is unusual among the oxides previ-
ously surveyed for catalytic activity because it does not adsorb
significant amounts of NPP prior to the release of NP into
solution. Examples of related heterogeneous catalysis in
which there is no significant adsorption of the substrate to
the catalytic surface are known. These include the hydrolysis
of phenyl picolinate by goethite and titania (15), the oxidation
of As(III) to As(V) by manganese dioxide (16), and the
oxidation of 1,4-dihydroxybenzene by manganese dioxide
p-Nitrophenyl phosphate has been used as a substrate to
measure what is believed to be the activity of phosphatase
enzymes in soils (23, 24). Hence, it is possible to compare
“
enzymatic” activity measured in soil systems with the abiotic
rates measured for manganese dioxide in this work. In one
study with phosphomonoesterase at its optimum pH between
6
h
and 7, approximately 1 µmol of p-nitrophenol was released
(g of soil) at 37 °C. This can be compared with the rate
-1
-1
at pH 6 shown in Figure 1 of about 50 µmol of NP/ g of
amorphous manganese. In another study, the maximum
hydrolysis rate calculated from the integrated Michaelis-
(
17). All of these reactions involve the adsorption of the
substrate to the surface of the oxide. The fact that there is
little net absorption of the primary reactant prior to ap-
pearance of the product implies that either the equilibrium
binding constant is low or that the rate of the primary
adsorption process is slower than that of the subsequent
reaction of the adsorbed species (that is, the adsorption
process is rate limiting). Previous workers have suggested
that anion adsorption onto amorphous manganese dioxide
is weak because of the net negative surface charge above pH
-1
Menten equation was of the order 10-100 µmol h (g of
-1
soil) (23), comparable to the abiotic rates observed here.
While there are many assumptions made in these compari-
sons, it seems clear that the abiotic process is potentially
competitive with the inferred activity of phosphatase en-
zymes. Similar conclusions have been reached in a parallel
study on the hydrolysis of tripolyphosphate also facilitated
by amorphous manganese dioxide (12).
2
(18-20).
The second acid dissociation of NPP has a pKa2 of 5.18.
Acknowledgments
At pH 4, therefore, the monoanion predominates, while at
pH 6 and above the dianion is the dominant species. The
probably accounts for the limited adsorption of the NPP to
the manganese dioxide surface below pH 6 and no measur-
able adsorption above this pH. The pH dependence of the
rate constants for the catalyzed hydrolysis of NPP thus reflects
two factors: differences between the monoanion and dianion
of NPP and the pH dependence of the surface charge of the
manganese oxide. The data do not allow a distinction between
the two effects to be made. What is clear is that the reaction
is fastest at pH 4, where some of the NPP monoanion is
adsorbed and where the surface charge of the oxide is less
negative than at higher pH values.
The financial support of the Australian Research Council
Small Grants Scheme is gratefully acknowledged.
Literature Cited
(
(
1) Yao, W.; Millero, F. J. Environ. Sci. Technol. 1996, 30, 536.
2) Baldwin, D. S.; Beattie, J. K.; Jones, D. R. Water Res. 1996, 30,
1
123.
(
3) Baldwin, D. S.; Beattie, J. K.; Coleman, L. M.; Jones, D. R. Environ.
Sci. Technol. 1995, 29, 1706.
(
(
(
4) Jambor, J. L.; Grew, E. S. Am. Mineral. 1990, 75, 931.
5) Stone, A. Environ. Sci. Technol. 1987, 21, 979.
6) Murphy, J.; Riley, J. P. Anal. Chim. Acta 1962, 27, 31.
The rate constants at pH values less than 6 decrease
significantly with increasing initial NPP concentration. At
pH 8, however, the rate constants are almost independent
of the NPP concentration. This behavior is consistent with
stronger adsorption of the monoanion than of the dianion.
At low pH, the surface of the oxide becomes saturated at low
NPP concentrations. As the concentration of NPP at the
surface increases, the net negative surface charge increases
making the adsorption of more NPP more difficult.
The inhibition by phosphate displays a similar pattern
with inhibition at pH 4 and no effect at pH 8. At the lower
pH, phosphate from the hydrolysis reaction remains adsorbed
to the surface. In addition, added phosphate also binds and
therefore blocks active surface sites. This effect should lead
to product inhibition and deviation from first-order kinetics
as phosphate is produced at pH 4, but the kinetics data were
not precise enough to observe this effect. The pKa2 of
orthophosphate is 7.2. At pH 8, all the phosphate produced
by the hydrolysis reaction is released into solution, reflecting
the weak interaction between the surface and the phosphate
dianion, and added phosphate does not inhibit the hydrolysis
reaction.
(7) Rossouw, M. H.; Liles, D. C.; Thackeray, M. M. Mater. Res. Bull.
992, 27, 221.
1
(8) Healy, T. W.; Herring, A. P.; Fuerstenau, D. W. J. Colloid Interface
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9) McKenzie, R. M. Aust. J. Soil Res. 1981, 19, 41.
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Res., in press.
(13) Balistrieri, L. S.; Chao, T. T. Geochim. Cosmochim. Acta 1990,
5
4, 739.
(14) Cox, J. R.; Ramsey, O. B. Chem. Rev. 1964, 64, 317.
(15) Torrents, A.; Stone, A. T. Environ. Sci. Technol. 1990, 25, 143.
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(
(
(
17) McBride, M. B. Clays Clay Miner. 1989, 37, 479.
18) McKenzie, R. M. Geochim. Cosmochim. Acta 1979.
19) Kawashima, M.; Tainaka, Y.; Hori, T.; Koyama, M.; Takamatsu,
T. Water Res. 1986, 20, 471.
(
20) Takematsu, T.; Kawashima, M.; Koyama, M. Water Res. 1985,
1
9, 1029.
(
(
21) Coleman, L. M. Ph.D. Thesis, University of Sydney, 1996.
The hydrolysis of NPP by amorphous manganese dioxide
is an order of magnitude more rapid, per gram of oxide, than
the same reaction facilitated by hydrous ferric oxide (2). This
difference is probably due to the increased acidity of the
surface hydroxyl groups of the manganese(IV) surface, with
pHpzc of 2.3, as compared with hydrous iron(III) oxide with
pHpzc of 8.2. Hence, the rate of reaction decreases from pH
22) Jones, D. R.; Lindoy, L. F.; Sargeson, A. M. J. Am. Chem. Soc.
1
983, 105, 7327.
(
(
23) Gerritse, R. G.; van Dijk, H. Soil Biol. Biochem. 1978, 10, 545.
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Received for review May 29, 2000. Revised manuscript re-
ceived November 9, 2000. Accepted November 14, 2000.
4
to pH 8 for the manganese system, but for the iron system
it reaches a maximum at pH 6.9 (21). The observed differences
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ENVIRONMENTAL SCIENCE & TECHNOLOGY / VOL. 35, NO. 4, 2001