For the evaluation of chemical form of particulate matter in the atmosphere,
thin films were prepared as shown below (Mamane and Pena, 1978 and 1980;
Pueschel, 1980, Bigg et al., 1974; Ayers, 1978; Ono et al., 1981; Shimohara
and Murano, 1997, Yamato and Ono, 1989).
4.1. Preparation of thin films and sampling procedures
(1) Pre-treatment of thin films
A nitrocellulose filter, 47 mm in diameter, was
put on a glass plate (50*50*4 mm). The filter was slightly dissolved
and was stuck on the glass plate by exposure to acetone vapor for
30 min. The filter was then strengthened by adding a thin film of
vacuum-evaporated carbon. This pre-treated film was cut into pieces
of about 3*3 mm with a scalpel. A flat polyurethane sponge was dipped
about a half in depth in an acetone solution in a glass vessel.
Then, 200-mesh grids of 3-mm in diameter for transmission electron
microscope were placed on the sponge. The pieces of film were promptly
laid on each grid. The thin film on the grid was then exposed to
acetone vapor for 1-h.Since only the nitrocellulose was dissolved
by the acetone vapor, the carbon thin film remained on the grid
(hereafter referred to as "carbon film") (Shimohara and
Murano, 1997).After drying the carbon films, metal calcium (6 mg)
was vapor-deposited onto some carbon films under vacuum. The calcium
thin film was covered on the carbon film (hereafter referred to
as "calcium film").
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(2) Sampling procedures of particulate matter onto thin films
The calcium film and carbon film were used for the identification
of chemical forms of the particles. The calcium film or carbon film
was placed inside an impactor (see Figs. 4 and 5). A tube of 8 mm
inside diameter and 35 cm in length run into a tube of 8 cm in diameter
and 30 cm in length.Dry silica-gel was filled up to vacancy between
the tubes. When calcium film was used, the tube was equipped onto
the inlet of the impactor. The ambient air is dried by passing through
the tube, and the relative humidity of air decreases to below 5-10%
at the inlet of impactor(Yamato and Ono, 1989).Minute water droplets
and particulate matter having a water-absorbability are dried. On
the other hand, there is no need to use the tube for the sampling
on carbon film. Sampling was performed simultaneously at two sites
in fine days. Air samples were sucked and particulate matter was attached
onto each film at a flow rate of 1.3 l/min for 10 minutes. After sucking
ambient air, each film was stored in a glass tube of 1 ml, and shielded
against outside air. |
(3) After-treatment of thin films
Calcium film after sampling was observed immediately by a transmission
electron microscope. Carbon film after sampling was prepared as follows.
Nitron (8mg, 1,4-diphenyl-endoanilino-dihydrotriazol) and sodium tetraphenylborate
(4mg, C24H20BNa) was sequentially
vapor-deposited onto sampled carbon films under vacuum. Then, the
carbon films were covered with nitron and sodium tetraphenylborate
(see Fig. 6; hereafter referred to as "Ni-Tet film"). On
the other hand, silver nitrate (AgNO3)
was vapor-deposited onto the other sampled carbon films under vacuum.
The carbon film was covered with silver nitrate (hereafter referred
to as "AgNO3 film") was prepared.
Each film after evaporation was then exposed to n-octyl alcohol vapor
for 24-h at 25ºC. The films were observed to identify the chemical
forms of particulate matter by transmission electron microscope. |
4.2. Evaluation of chemical forms of particulate matter
(1) Distinction of particulate NH4HSO4
and H2SO4
Particulate NH4HSO4
and H2SO4
such as hygroscopic particles in the atmosphere will have moisture
even after passing through the silica gel tube. By the contact of
moisture containing in the particulate NH4HSO4
and H2SO4,
calcium reagent is dissolved and non-perfect and perfect homocentric
spots are caused on the film (see Fig. 7). The particulate H2SO4
in the atmosphere has higher water-absorbability than NH4HSO4.
The perfect homocentric and non-perfect homocentric spots are formed
on the film by attaching of H2SO4 and NH4HSO4,
respectively. Therefore, homocentric spots caused by particulate H2SO4
and NH4HSO4
can be differentiated based on morphology by transmission electron
microscope (Yamato and Ono, 1989). |
(2) Distinction of NH4NO3 and the
other NaNO3 and Ca(NO3)2
Figure 6 showsa reaction scheme of particles
collected onto the thin films and reagents. After capturing the
particles onto carbon film, the carbon film was covered with nitron
and sodium tetraphenylborate vapor-deposited. Therefore, particles
and reagents are slightly dissolved with each other under the atmosphere
of n-octyl alcohol vapor, and form coagulated compounds. For example,
nitron reagent reacts with NO3-
corrected onto the carbon film. Needle-like and/or roundly coagulated
insoluble compounds are caused on the film. Sodium tetraphenylborate
reagent reacts with NH4+
corrected onto the carbon film, and an observable homocentric spots
consisted an ultra-minute coagulation are caused on the film (Mamane
and Pena, 1978; Mamane and Pueschel, 1980).In the case of collection
of NH4NO3
onto the film, the needle and/or roundly coagulated insoluble compounds
are appeared within the homocentric spots. The particulate NaNO3
and/or Ca(NO3)2
without NH4+
cause only the needle and/or roundly coagulated insoluble compounds
on Nt-Tet film. Ammonium sulfate, NH4HSO4
and NH4Cl without NO3-
caused only the homocentric spots on Nt-Tet film. Therefore, the
characteristic spots caused by the collection of NH4NO3
can be differentiated from the other NO3-
such as NaNO3 and/or Ca(NO3)2
etc. (Ayers, 1978; Mamane et al., 1980; Bigg et al. 1974).
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(3) Distinction of NH4Cl and the other NaCl and CaCl2
After capturing the particles onto carbon
film, the carbon film was covered with AgNO3 vapor-deposited.
NH4Cl collected on carbon film is dissolved under n-octyl
alcohol vapor for 24-h. NaCl and CaCl2 are hardly dissolved
under same environment. Therefore, Cl- of only NH4Cl
reacts with AgNO3 reagent and roundly coagulated insoluble
compounds of AgCl are formed on the film (Ayers, 1978; Mamane and
Pueschel, 1980). |
Results
Tables 1, 2 and 3 show the average concentrations
of gases and particulate matter at two sampling sites in the periods
of January 1997, December 1997 and February 1999.Figures 8(1), 8(2),
9(1), 9(2), 10(1) and 10(2) show the variations of gaseous and particulate
matter through out the periods. Figure 11 shows the variations of
nss-SO42- concentrations at Goto Island and
Dazaifu-city in the period of January 1997.The variation of nss-SO42-
concentrations at Goto Island was well corresponded to at Dazaifu-city.
Figure 12 shows the mean nano-equivalent concentrations of each
component at two sampling sites in the period of January 1997. Presence
of free nss-SO42- without combined NH4+
is confirmed.
Tables 4- 6 show the size distribution of each
component of particulate matter at Goto sampling site and Tables
7-9 show the size distribution at Dazaifu sampling site in the periods
of January 1997, December 1997 and February 1999, respectively.
Figures 13-18 show the size distributions of individual ion components
in particulate matter, observation at Goto Island and Dazaifu-city.
Acidic components were found in fine size mode (below 2.1um) in
both sites.
Figures 19-21 show the size distribution of H+
in the particulate matter at two sampling site. Figures 22-24 show
the transmission electron microphotographs of three types of Nt-Tet,
calcium and AgNO3 films. The microphotographs show the
sampling results performed at 1500 JST on 13 January 1997 at two
sampling sites. The needle-like particles (see Fig. 22) formed by
the reaction between NO3-
particles and nitron reagent were observed around the rounded particles
at two sampling sites. In contrast, a number of mixing spots with
homocentric spots involving the needle-like insoluble compounds
were observed only at Dazaifu-city. Homocentric spots are the results
of reaction between NH4+ and sodium tetraphenylborate
reagent.It was concluded that the NO3-
at Goto Island hardly contains NH4+, and NO3-
at Dazaifu-city was combined with NH4+, and
present as NH4NO3.
The non-perfect homocentric spots on thin calcium
film were observed at Goto Island as a result of the reaction between
the moisture of hygroscopic particles and calcium reagent (see Fig.
23).The spots caused on calcium film reflect the presence of highly
hygroscopic particles in the atmosphere. The spots observed on the
film sampled at Goto Island were not homocentric form but infinite
form. On the other hand, there was no spot at all at Dazaifu-city.
The characteristic spots of AgCl component formed
by the reaction between nss-Cl- and AgNO3
were observed at Dazaifu-city (see Fig. 24). Although such a spot
was present in Dazaifu-city sample, it was not observed at all at
Goto Island.
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1227-1230.
Bigg F.K., Ono A. and Williams J.A. (1974) Chemical
tests for individual submicron aerosol particles, Atmos. Environ.,
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Mamane Y. and Pena R.G. (1978) A quantitative
method for the detection of individual submicrometer size sulfate
particles. Atmos. Environ., 12, 69-82.
Mamane Y. and Pueschel R.F. (1980) A method for
the detection of individual nitrate particles, Atmos. Environ.,
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Murano, K. (1986) Inorganic Composition (NO3-,
SO42-)
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Shimohara T. and Murano K. (1997) Evaluation
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J. Meteor. Soc. Japan, 67, 147-166.
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