of phosphomolybdic acid was purchased from Aldrich
Chemical Co. It was further diluted to 10% (w/ v), and 5%
quantified in terms of carbon content with a calibrated total
organic carbon analyzer (O.I. Corp. model 700).
(
v/ v) concentrated sulfuric acid was added prior to use. The
Photochem ical Reaction Cell. All irradiations were
performed with an EF-260C UV lamp from Spectronics
Corporation (Westbury, NY). The lamp emits a narrow band
of radiation at 254 nm. The irradiation experiments did not
employ additional filters or monochromators. The light
source contains two 6-W tubes that are 8 cm long. Typical
solvents dichloromethane, ethyl acetate, and hexane were
purchased from EM Science. HPLC-grade methanol and
acetonitrile from EM Science were used for HPLC experi-
ments. All H NMR experiments were conducted in deuter-
ated chloroform purchased from Aldrich Chemical Co. The
1
2
CDCl
3
was supplied with 0.03% tetramethylsilane as an
output is 810 µW/ cm . Samples were irradiated in quartz
tubes (1 mm thick). Tube dimensions were 12.5 mm i.d. and
internal reference. All solvents were used as received.
1
00 mm length. A maximum of seven tubes could be
Collection and Preparation of DOM Sam ples. One soil
sample and one water sample were collected for use in the
photochemical experiments. The organic surface horizon was
collected from a stand of red pine in Orono, ME (November
irradiated at the same time. The distance from the light source
to the middle of the sample tube was 3.8 cm. Irradiation
samples reached a maximum temperature of 28 °C in
approximately 30 min. Solutions were not agitated or mixed
during exposure.
The photochemical reaction cell was characterized using
a potassium ferrioxylate actinometer as described in Photo-
chemistry by Calvert and Pitts (15). The calculated value of
1
995). Soil cores, approximately 8 cm deep and 5 cm in
diameter, were collected from random sites within the stand
of trees. The forest soil, litter, and humus was dark in color
and included fallen pine needles. The subsamples were
combined and stored at 4 °C prior to extraction and filtration.
4
-1
-1
the extinction coefficient was 1.18 × 10 L mol cm , which
An additional sample of organic matter was collected from
Caribou Bog in Orono, ME. This wetland site is described as
a sphagnum bog. To collect water from the bog, the vegetation
was pushed aside and the void was allowed to fill with water.
Cleaned and sterilized 1-L nalgene bottles were submerged
in the water and allowed to fill. The water was dark in color
and turbid. A total of 2 L was collected and stored at 4 °C
prior to filtration.
4
is in good agreement with the published value of 1.10 × 10
-
1
-1
L mol cm . Lamp flux was determined by irradiating the
potassium ferrioxylate reactant for 12 s and determining the
number of Fe2 molecules produced. The average value of
+
1
6
16
the flux is 2.664 × 10 photons/ s, with a range of 2.77 × 10
1
6
to 2.58 × 10 photons/ s.
All solutions for the photolysis experiments were prepared
immediately prior to irradiation. Solutions were made in an
appropriately sized volumetric flask and then immediately
transferred to a nalgene bottle. Long periods of storage in
glass were avoided to prevent loss of carbofuran due to
molecules adhering to the glass walls of the flask. Exactly 4
mL of the solution to be irradiated was pipetted into the
reaction tubes. Typically, six reaction tubes were irradiated
simultaneously. At various times, two reaction tubes were
collected for each data point. The contents of the two tubes
were stored in a small (20 mL) nalgene bottle until HPLC
testing could be started. Again, the solution was stored in
nalgene to avoid loss of carbofuran due to adhesion to glass.
Quantification by HPLC was performed as soon as possible
following the completion of the irradiation experiment.
Product Separation. To identify the decomposition
products, a suitable quantity of each compound had to be
generated and isolated. To maintain consistency to the
kinetics experiments, a series of irradiations were conducted
with 30 ppm aqueous solutions of carbofuran. Following
irradiation, the aqueous solution was saturated with sodium
chloride to improve extraction efficiency. The reaction
products were extracted with five 15-mL portions of ethyl
acetate. Ethyl acetate was removed by rotary evaporation
until the sample volume was approximately 1 mL.
A humic acid and a fulvic acid sample used in the
photochemical experiments were purchased from Aldrich
Chemical Co. and provided by Dr. Christopher Cronan from
the Program in Ecology and Environmental Science, Uni-
versity of Maine, respectively. The Aldrich humic acid sample
was determined to be 40.7% C. The fulvic acid sample was
isolated from a southern hardwood forest soil, and carbon
content of this sample was 47.2% C. Both the humic and
fulvic acids were received as brown solid material that was
stored in a desiccator prior to use in the photolysis experi-
ments.
To separate the organic matter from the pine forest soil
sample, approximately 1.5 kg of soil was placed in a 2-L
nalgene bottle and 1500 mL of distilled, deionized water was
added. The sample was extracted for 24 h at room temper-
ature with periodic shaking. Following the extraction, the
liquid from the pine forest soil extract was darkly colored
and turbid.
The remaining steps of sample processing apply to both
the pine forest soil sample and the water sample collected
from the bog. The soil extract and the water sample were
passed through a series of filters to remove clay particles,
plant debris, and other unwanted particulates. First, the
samples were passed without vacuum through Whatman 41
ashless filter paper. The resulting filtrant was passed through
a Gelman A/ E glass fiber filter with a pore size of 1 µm with
the aid of vacuum. The final filtration was conducted with
a Gelman A/ E glass fiber filter with a pore size of 0.45 µm,
again, using vacuum filtration. At this point the samples were
no longer turbid. The bog sample and the coniferous sample
were both deep amber in color.
The product mixture was analyzed with HPLC and GC-
MS. Both techniques indicated that the mixture contained
seven compounds. These products were separated via
preparative thin-layer chromatography (TLC) using plates
purchased from VWR Scientific (Merck, Item 13894). The
stationary phase was 0.50 mm layer of 60 mesh silica,
containing no fluorescent indicator, and coated onto a 20 ×
2
0 cm glass plate. The mobile phase consisted of 3:1 hexane:
Following filtration, the samples were passed through a
cation exchange column. Columns with inside diameters of
ethyl acetate. As many as three developments of the TLC
plate were required to achieve adequate separation. Products
were visualized with an alcoholic phosphomolybdic acid
solution. The indicator was applied to both vertical edges of
the TLC plate and dried with a heat gun.
Upon visualization, the silica from the appropriate region
of the plate was removed with a razor blade. The compound
was resolvated by placing the silica in 100 mL of ethyl acetate
and stirring for 10 min. The silica was removed with vacuum
filtration. Again, the excess solvent was removed via rotary
evaporation.
4
.5 mm were packed with Rexyn 101H beads. The packing
material had previously been Soxhlet extracted with methanol
to remove residual carbon. The pumping sequence through
the column was as follows: 1 M HCl for 15 min to condition
the packing material, distilled/ deionized (dd) H O for 30 min,
2
DOM sample. Approximately 200 mL of DOM sample was
collected at a time. Following sample collection, the columns
were flushed with water (10-15 min) and the HCl/ H
2
O
conditioning step was repeated. Finally, the samples were
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