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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 />

91

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