Chemosphere, Vol°lT, No.2, Printed in G r e a t B r i t a i n
pp
395-398,
1988
0045-6535/88 $ 3 . 0 0 + .OO Pergamon Journals Ltd.
PITFALLS IN THE AQUATIC PHOTOCHEMISTRY TESTING OF CHLORINATED AROMATIC COMPOUNDS
Paul van Noort *'t, Ren4 Smit, Erik Zwaan, and Jelle Zijlstra
Laboratory for Ecotoxicology,
Environmental Chemistry,
and Drinking Water,
National Institute for Public Health and Environmental Hygiene, P.O.Box i, 3720 BA
Bilthoven,
The Netherlands
ABSTRACT
Eventual phototransformation of ehloroaromatics in water containing humie acid is proposed to result from unidentified trace impurities in the water introduced by the addition of concentrated solutions of humic acid to the irradiation mixtures, Humie acid itself does not seem to sensitise the phototransformation of these type of compounds. INTRODUCTION
The aquatic photochemistry of chlorinated aromatic compounds has been the subject of many investigations because of the adverse biological properties of compounds of In
the
aquatic
environment
many
of
these
compounds
this
type.
may in principle be transformed by
sunlight as a result of either direct light absorption by these compounds or by reaction with reactive
intermediates
direct photolysis reported
formed from e,g. humic materials on irradiation
is the incident light being absorbed by the compound.
combination
of
. A prerequisite for In
I
for direct photolysis although
transformation
was
reported
accelerate
phototransformation is
not
photochemically
yet
cases
the
2
'
Humic
material 3
mechanism
some
light source and molecular structure did not suggest possibilities
clear.
incorporated
of
chlorinated
Choudry into
humic
et
aromatic
compounds
4
5
seems
to
6
' ' ' ,
but
the
al.
reported that polychlorobenzenes were 7 model monomers , but it did not appear from their
paper where the light was absorbed: by the humic model monomers or by the polychlorobenzenes. Therefore,
we
now
report
our
results
disappearance of pentachlorobenzene
on
measurements
and methoxychlor
of
the
rate
of
photo-induced
in various types of purified water
or without added humic acid as a model for aquatic humic material.
t Present adress:
Stork Screens B.V., P.O. Box 67, 5830 AB
395
Boxmeer,
The Netherlands.
with
396
MATERIALS AND METHODS
Humic
acid
was
a
obtained
from
Fluka.
Aqueous humic acid solutions were prepared
according to Zepp . Irradiations were carried out in a Rayonet Photochemical Reactor equiped with eight RUL-3500A lamps and a RMA-400 Merry-Go-Round.
RPR 208
Deionized water was purified
by two series of oxidation with KMnO 4 and distillation. Quantitative analysis of penta-, hexachlorobenzene,
and
methoxychlor
in
water
was
containing trichlorobenzene as internal standard
done
followed
by by
extraction injection
and
with cyclohexane on
a
Carlo
Erba
gaschromatograph equiped with an ECD.
RESULTS
The
irradiation of 12.6 ~g/l of pentachlorobenzene in deionized water resulted in a
decrease of the concentration with a rate constant of 0.032 h -I (Fig.la). Irradiation in
the
presence of humic acid (DOC- I0 mg/l) afforded a rate constant of 0.14 h "I (Fig. ib). In (Co/C) 10
In (Co/C) 1.0
Fig. la
x
xJ
/
Fig.x x
0.5
.S
0.5
jJ x
0
5
10
15
20
25 h
0
1
3
5
7h
Fig.l. Pseudo first-order plot for disappearance of pentachlorobenzene upon A 350 nm ation in (a) deionised water,
The presence of oxygen, KNO s (IM), KCI (IM), or Zn(NOs) ~ (0.5 M) had almost no the
rate
constants:
hexachlorobenzene
irradi-
(b) deionised water containing humic acid at i0 mg C/I.
they were 0.13, 0.17, 0.13, and 0.18 h "I respectively.
influence
on
Disappearance of
(7.8 ~g/l) upon irradiation in the presence of humic acid (i0
mg
C/I)
in
deionised water proceeded with a rate constant of 0.i0 h -I. When the irradiation of pentachlorobenzene was carried water
(without
out
in
purified
process (Fig.2a).The addition of pentachlorobenzene to the irradiated mixture of not,
upon
deionized
humic acid) the kinetic of the disappearance rather suggested a second order
prolonged
irradiation,
result
in
Fig.2a
did
a further decrease of the pentachlorobenzene
concentration. This demonstrates that the disappearance
of
pentachlorobenzene
is
not
the
The effect of humic acid on the aquatic photochemistry of pentachlorobenzene in
the
result of the addition of pentachlorobenzene. purified
water
was
determined
by
measuring
the
decrease
concentration upon irradiation of a solution of pentachlorobenzene
of
the
pentachlorobenzene
(12.6 #g/l) and humic acid
(DOC- 20 mg/l) in purified deionized water containing pentachlorobenzene at 13 ~g/l which was
397
pre-irradiated for 24 h (Fig.2b). Also in this case pentachlorobenzene
the
kinetic
of
decrease
of
the
C/Co 1.0
CICo 1.0 Fig, 2a
Fig. 2b
~
0.8
x x
0.5 -
-f
-
X - - X ~
x
x
x
.
1'o
1's
2'o
o
s
20
Fig.2. The change of the relative concentration of pentachlorobenzene ation
the
concentration was apparently second order.
in
(a) purified deionised water,
with pentachlorobenzene present,
2Sh
upon A 350
nm
irradi-
(b) purified deionised water pre-irradiated for 24 h
followed by humic acid addition prior to the
final
irradi-
ation.
Since methoxychlor was reported by Zepp to disappear very rapidly
on
irradiation
in
humic
s
waters
,
we studied the photochemical behaviour of methoxychlor under the same conditions as
for Fig.2b.
In contrast to Zepp,
we
found
the
concentration
of
methoxychlor
to
remain
constant upon irradiation for 6 h.
DISCUSSION
Our
results
from
the
irradiation in the not-purified deionised water demonstrate
that the addition of humic acid affords an acceleration of the disappearance by a
factor
of
about 4. This acceleration is of the same magnitude as found for the irradiation of 2-chloro3
biphenyl in humic acid containing water
4
, of chlorophenols
in estuarine water
, and of the
2-
5
butoxyethyl
ester of 2,4-D in a natural water
, but is much less than found for methoxychlor
e
in natural waters In expected
the
since
disappearance trace
. purified
prior
impurity
water
pentachlorobenzene
pentachlorobenzene
of
to
does
not
absorb
does at
not disappear. the
This is of course
wavelengths
employed.
Its
the pre-irradiation demonstrates the presence of a photosensitising
unknown
identity
in
the
water
which
is
completely
consumed
upon
irradiation. In the presence of humic acid, pentachlorobenzene water
was
consumed
to some extent.
in
ance, this may also be the result of the presence of (unknown) addition
of
a
concentrated
humic
the
pre-irradiated,
purified
Because of the second order character of the disappear-
acid
solution
impurities introduced
by
the
to the pre-irradiated water. We have no
analytical data on the impurity since we do not know what
to
look
for.
The
stability
of
398
methoxychlor
also
points
to
the
photochemical
irreactivity
of
humic
acid
towards
chloroaromatics. Recently,
the near-surface
steady-state
concentration
of the photoproduced
hydrated
9
electron was determined by us to be i.I×i0 -17 M per mg DOC/I in natural waters
and
by
Zepp
Io
et
al. to be I.2xlO-17M
Zepp, but on different material
may
for the Swiss Greifensee
grounds,
undergo
photoreductions
hydrated electron steady-state steady-state
concentration
the chloroaromatics second
order
conversion of with
at
associated
a
concentrations.
dissolved
organic
aquatic
rate higher than expected on the basis of the Under our
in humic water for 6 h (in other words,
acid,
acceleration
with
conditions
the
hydrated
is 3xI0-17M 9. The pseudo first order rate constant
much less than l~lO'2h-l). humic
We pointed out, and so did
electron
for reaction of
with the hydrated electron can be estimated from literature data for the 1, constants to be about IxlO'3h -I, For methoxychlor we found no
rate
it
pentachlorobenzene
with
that substrates
(DOC= 4 mg/1)
will
some
This demonstrates be
by
less
association
than
any disappearance
a
factor
assisted acceleration
will not be of several orders of magnitude.
humic
acid had no detectable 12 excited humic acid to substrates
would proceed at a
rate
that if there is acceleration by association of
I0
for
methoxychlor.
could have occurred.
Earlier we
found
For
Anyhow,
that
this
association
effect on the rate of triplet energy transfer from photo13
Finally,
our results demonstrate
that on performing
purity of the water should be subject to attention,
tests on photodegradation
especially when the test
the
solution
is
weak light absorber.
REFERENCES
i. M. Malaiyandi,
K. Muzika,and
2. M. Malaiyandi,
S.M. Shah, and P. Lee, J. Environ.
3. D. Dulin, H. Drossman,
and Th. Mill,
4. H.-M. Hwang, R.E. Hodson, 5. R.G. Zepp, N.L. Wolfe,
F.M. Benoit, J. Environ.
Environ.
Sci. Health,
Sci. Health,
Sci. Technol.,
and R.F. Lee, Environ.
AI7, 299 (1982).
AI7, 283 (1982).
20, 72 (1986).
Sci. Technol.,
20, 1002 (1986).
J.A. Gordon,
and G.L. Baughman,
Environ.
J.A. Gordon,
and R.C. Fincher,
J. Agric.
Sci. Technol.,
9, 1144
(1975). 6. R.G. Zepp, N.L. Wolfe,
Food Chem.,
24, 727
(1976). 7. G.G. Choudry,
J.A. van den Broecke,
495 (1987); G.G. Choudry, Environ.
Toxicol.
G.R.B. Webster,
J.A. van den Broecke,
and O. Hutzinger,
G.R.B. Webster,
Chemosphere,
16,
and O. Hutzinger,
Chem., ~, 625 (1986).
8. R.G. Zepp, G.L. Baughman,
and P.F. Schlotzhauer,
9. P. Breugem,
S. Velberg,
P. van Noort,
Chemosphere,
E. Wondergem,
I0, 109 (1981).
and J. Zijlstra,
Chemosphere,
15,
717 (1986). I0. R.G. Zepp, A.M. Braun,
J. Hoign~,
and J.A. Leenheer,
Environ.
Sci. Technol.,
21, 485
(1987). ii. M. Anbar and P. Neta, 12. P. van Noort, 13. J. Lemaire, Wolff, (Received
submitted
Isotopes,
18, 493 (1967).
for publication.
J.A. Guth, O. Klais, J. Leahey, W. Merz, J. Philp, R. Wilmes,
Chemosphere, in
Int. J. Appl. Radiat.
Chemosphere,
Germany
and C.J.M.
14, 53 (1985). 24
September
1987;
accepted
17 N o v e m b e r
1987)
a