GEO Brasil - UNEP
GEO Brasil - UNEP
GEO Brasil - UNEP
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Barreiras Group, sandy re-covering<br />
which exists along the Brazilian coast<br />
from Amapá to the State of Espírito<br />
Santo<br />
In this hydro-geologic context, the<br />
shallow water level (WL) from<br />
excavated depth in the plateau might<br />
be temporary, which means it dries out<br />
along the period when there are no<br />
rains or it disappears when a deep well<br />
is perforated in its surroundings<br />
Thus, the deep or tubular well crossed<br />
the hydro -geologic substratum which<br />
supported the accumulation of<br />
shallow underground water, the<br />
suspended aquifer (Figure 2b)<br />
24<br />
Contamination Agents<br />
Underground water is “hidden” under<br />
a layer of non saturated filtrating<br />
material of high purifying power Due<br />
to local and occasional geological<br />
characteristics, the deepening of the<br />
well could be the solution for<br />
obtaining a larger flow and better<br />
which affect the waters stocked in<br />
dams (Santiago, 1984) Thus, based<br />
on the results of 500 analyzed samples,<br />
it is observed that only 37 percent<br />
present total dissolved solid content<br />
(STD) similar or inferior to 2000 mg/L<br />
(Cruz & Melo, 1968; Rebouças, 1973)<br />
However, the studies developed by<br />
EMBRAPA-CPTSA (2000) show that<br />
there are several alternatives for using<br />
brine generated by mineral processes<br />
of well-drawn waters, which draw the<br />
fractured rocky areas under the<br />
crystalline substratum water in the<br />
semi-arid Northeast Among viable<br />
alternatives, the irrigation of forrage,<br />
which are of great economical and<br />
social reach in the development of<br />
caprine-raising, stands out<br />
Consequently, the use of water<br />
desalinisation agents in inverse<br />
osmosis processes has been growing<br />
in the last decade In this case, the<br />
collection or inadequate deposits of<br />
garbage, which is produced in the<br />
cities mainly, the disordered<br />
implementation of service posts,<br />
cemeteries, the installation of buried<br />
or semi-buried tanks of dangerous<br />
products without proper<br />
consideration regarding corrosion<br />
risks-specially in a country where there<br />
is a great amount of rain and hot<br />
weather for most of the year are<br />
frequent agents which affect the good<br />
natural quality of underground water<br />
(Hassuda, 1997, Hirata, 1994, Hirata et<br />
al, 1997)<br />
Among the agents of underground<br />
water contamination in Brazil, the<br />
nitrogen series (NH4, NO2 and NO3)<br />
stands out and is brought about by<br />
the chaotic dominant sanitation<br />
situation of our cities (Parissot, 1983,<br />
Pacheco, 1984, Mello, 1995,<br />
Cavalcante, 1998, Santos, 2000)<br />
the state of the environment in Brazil<br />
quality of drawn water, while in other<br />
places this alternative may result in<br />
substantial reduction of obtained<br />
flows and worsening of its quality<br />
Also, due to lack of appropriate<br />
foundation to the ringed space,<br />
sanitation stamp and other technical<br />
deficiencies such as constructive,<br />
operational, maintenance and<br />
abandonment of wells, there may be<br />
processes of crossed contamination<br />
caused by polluted waters from<br />
main problems faced result in:<br />
a) lack of monitoring of the quality<br />
of water extracted from wells and<br />
which tends to improve after 2 - 3<br />
years use as the intensive well<br />
pumping engenders greater<br />
renewal dynamics to the water<br />
drawn from the underground;<br />
b) lack of equipment maintenance;<br />
and<br />
In addition, among the risks of binomial<br />
underground soil-water contamination<br />
in Brazil, the growing industrialization<br />
and development of agricultural<br />
activities with intensive use of chemical<br />
inputs-fertilizers, herbicides, pesticides<br />
results in, the existence of inorganic and<br />
organic synthetic chemical micro<br />
pollutants (Hirata, 1994) Among the<br />
most frequent, we emphasize the<br />
following:<br />
neighbouring or shallower layers<br />
In the areas of fractured aquifer rocks<br />
c) lack of rational use of brine<br />
generated this way<br />
a) inorganic non metallic<br />
chemicals, such as phosphorus,<br />
selenium, nitrogen, sulphur and<br />
and alluvial patches of geological<br />
basis from the Pre-Cambrian Age in<br />
the semi-arid Northeast there are<br />
processes of climatic underground<br />
water salinisation similar to those<br />
The construction, operation and<br />
disordered abandonment of wells, the<br />
chaotic forms of occupation of urban<br />
and rural environment, the non<br />
fluorine;<br />
b) poisonous metals, such as<br />
mercury, chrome, cadmium, lead<br />
and zinc;<br />
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