Electronic Material Properties - und Geowissenschaften ...
Electronic Material Properties - und Geowissenschaften ...
Electronic Material Properties - und Geowissenschaften ...
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nearly half a century has been performed, concentrating on the impact of sand and<br />
gravel mining and the recuperation of abandoned mining areas as well as on the<br />
proceeding urbanisation. Fig. 4 shows the dynamic of the urbanisation of the alluvial<br />
plains from 1977 until 1990. These analyses were accompanied by field observations<br />
including geological, pedological and environmental aspects such as the state of the<br />
recuperation of abandoned extraction areas as well as sedimentological structures. The<br />
total area of 6,68 km² of the alluvium between the road MG 424 and the road MG 010,<br />
have been subject to many drastic transformations during the last decades. Frequent<br />
changes of the riverbed, erosion at its margins, siltation and the augmentation of<br />
exposed soil in the alluvial plain could be observed.<br />
Fig.4: Proceeding urbanisation of the alluvial plain of the Riberâo da Mata<br />
between 1977 and 1990.<br />
The peak of the sand mining activities was in the decades of 1970 to 1980, when the<br />
city of Belo Horizonte was growing very rapidly and environment legislation was less<br />
strict. Still, even today, active sand and clay mines can be fo<strong>und</strong> in the area, showing<br />
the importance of these resources for the city. During the last decades, approximately<br />
30% of the study area has been subject to mining (1.5 km² during the 1977 and only 0,5<br />
km² in 1990). In some abandoned mining areas, industrial plants breaking carbonate<br />
rocks for gravel substitution have been constructed, as the alluvium offers plain<br />
construction sites. The gravel mining has stopped since, as the natural gravel resources<br />
are scarce and deep seated. The natural recuperation of abandoned mining areas is<br />
slow and exposed soil and active erosion carries away fertile soil and increases the<br />
sediment load of the river. In the 1970s, 0,4 km² of the area could be classified as<br />
exposed soil showing signs of erosion. The multi-temporal analysis of the land use in<br />
this area together with a comparison with other source areas showed that certain georesources<br />
like sand and gravel for construction purposes are heavily needed in close<br />
distance to the growing city, but competing for space with other uses and with<br />
environmental legislation.<br />
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