EVALUATION OF MERCURY
ATMOSPHERIC CONTAMINATION IN A DENTAL OFFICE USING TRANSPLANTED SPANISH MOSS (Tillandsia usneoides, L.): ESTABLISHING
ENVIRONMENTAL BACK GROUND LEVELS.
Calasans,C.V.C.; Carvalho,
C.E.V.; Primo,W.S., Cavalcante, M.P.O.; Souza, C.M.M. (Laboratório de
Ciências Ambientais, Universidade Estadual do Norte Fluminense, Campos dos
Goytacazes, Rio de Janeiro, 28015-620, Brazil, Tel: +55 24 726-3909, Fax: +55
24 726-3720); Castanheira, C. (Prefeitura Municipal de Campos dos Goytacazes,
Campos, R.J., Brazil). carvalho@cbb.uenf.br
.
The
aim of the present study was to monitoring the air quality in a dental office
by the use of transplanted Spanish moss (Tillandsia
usneoides). Transplant technique consists of transferring plants from
unpolluted sites to the area that will be monitored and it was successfully
employed at some industries (chlor-alkali, zinc smelter) to evaluate
atmospheric heavy metals contamination. Mercury background concentrations were
determined by analysis of 10 plant samples collected at rural areas. Samples
(dried at < 40oC) were wet digested using a H2SO4:HNO3
mixture (1:1 v/v), H2O2 and KMnO4. Mercury
determinations were performed by ICP-AES (Varian Liberty II). Analytical method
reliability was evaluated by digesting a Standard Reference Material (SRM 1515
Apple Leaves) and Hg concentration obtained (41.9 ± 3.6 ng.g-1) was in accordance to
the certified value (44.0 ± 4.0 ng.g-1). The Spanish moss had
a mean Hg value of 82.5 ± 21.0 ng.g-1. Since Hg background
level was established, the next step will be the exposure of the plant in the
dental office.
Dental offices are among the main sources of amalgam to
the environment. Dental amalgam is a mixture of silver-tin particles, liquid
mercury, copper and zinc. Silver amalgam consists of 43 to 50 % Hg and during
its preparation some losses of Hg to the atmosphere may occur due to the high
vapor pressure of elemental mercury (Hg0). The studied dental office
is a small, hot and not well ventilated room where the amalgam is prepared in a
mortar and Hg in excess is removed by squeezing the amalgam in a cloth. This
procedure yields some Hg droplets in the working bench.
The use of lichens and mosses to monitoring air quality
had been proposed by several authors (Steines & Krog, 1977; Rühling and
Tyler 1968, 1969, Goodman and Roberts, 1971; Hawksworth & Rose, 1970).
These organisms have an exceptional capacity to retain inorganic ions. As
minerals enters these plants almost entirely through the air they are useful
indicators of atmospheric pollutants (Steines & Krog, 1977).
Plant
samples were collected by hand in the north of Rio de Janeiro State at the
Municipality of São Fidélis in Barro Branco locality. Ten sub-samples were
collected in different trees in the surroundings. Each of these sub-samples
were packed in distinct plastic bags during transport to the laboratory. In the
laboratory, the plants were separately oven-dried (40ºC), powered in porcelain
mortar and wet digested in triplicate, using the procedure described by Bastos
(1998).
Analytical
method reliability was evaluated by digesting a Standard Reference Material
(SRM 1515 Apple Leaves) and Hg concentration obtained (41.9 ± 3.6 ng.g-1) was in accordance to
the certified value (44.0 ± 4.0 ng.g-1). Mercury was measured
in an ICP/AES (Varian, model Liberty II) with vapor generating accessory. The
detection limit of the method used was 0.5 ng/g-1.

Figure 1. Sampling site
location is indicated by dashed arrow.
All mercury data obtained in the sampling station is
presented in Table 1 with the respective variation coefficient and standard
deviation.
Mercury concentration in all samples varied from 55.4 to
127.1 ng.g-1, with an average concentration of 82.5 ng.g-1. The standard
deviation for each sub-samples was low with and average of 6.2. The variation
coefficient between duplicates was also low with an average of 7%. (Table 1).
Although the coefficient of variation and the standard deviation between each
sub-samples duplicate was low, the standard deviation among all 10 analyzed
samples was very high (21%).
Comparing our results to the study develop by Calasans
and Malm (1997) with the same species, it is possible to observe similar values
(100 ng.g-1) described as the background from a rural area.
Comparing our results to other values described by the literature as background
for lichen and moss: 70 to 480 ng.g-1 for the lichen H. physodes (Lodenius, 1981); 60 to 90
ng.g-1 for the feather moss P.
schreberi (Rinne & Estrup, 1980), it was possible to observe that they
are also similar to our results, and also presented high standard deviation.
Although mercury contamination in the North of Rio de
Janeiro region had already been reported by some authors (Primo et al., 1999; Souza, 1994; Lacerda, et al. 1993; Câmara, 1986), mainly due
to past gold mining activities and the large use of mercury fungicides on the
sugar cane plantations (banished in the beginning of the eighties), the
observed Hg concentrations in T.
usneoides did not showed any high values.
According to Primo et
al. (1999) the old harvesting methodologies used at the sugar plane cane
plantations, like burning the sugar cane fields before harvest increase the Hg
atmospheric transport to remote areas. This hypothesis developed by Primo et al. (1999) is not confirmed by the
concentrations found in Tillandsia
usneoides at the region. These hypothesis was probably valid in the past
when Hg fungicides were widely used but in the present our results showed that
atmospheric Hg deposition is low.
Table
1. Mercury concentration in Tillandsia
usneoides and respective standard deviation and variation coefficient from
the ten sampling sites.
|
Sample
number |
Hg (ng.g-1) |
Standard deviation |
Variation coefficient (%) |
|
1 |
71.8 |
2.4 |
3 |
|
2 |
89.3 |
9.2 |
10 |
|
3 |
67.4 |
3.9 |
6 |
|
4 |
59.9 |
0.1 |
0 |
|
5 |
92.1 |
4.8 |
5 |
|
6 |
55.4 |
0.9 |
2 |
|
7 |
76.1 |
1.6 |
2 |
|
8 |
127 |
15.2 |
12 |
|
9 |
94.5 |
13.3 |
14 |
|
10 |
91.5 |
10.8 |
12 |
|
Average |
82.5 |
6.2 |
7 |
Based on the above arguments it was possible to assume
that, although high variation on the Hg concentrations in samples collected in
the same areas was observed, this variations are probably due to natural
factors. The environmental contamination of the samples was rejected based on
the background concentrations described by other studies, carried out with the
same plant or with other species, that presented similar concentrations.
Although, the sampling area was very restricted it was possible to establish an
average Hg background levels for Tillandsia
usneoides for the region (82.5 ± 21.0 ng.g-1).
However, we reinforce the necessity of extending the sampling area.
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The authors would like to thanks the technicians Denise Nogueira de Souza and Cristina B. Siqueira for helping in the laboratory procedures..