Full text: XVIIIth Congress (Part B7)

  
  
  
  
  
  
  
  
  
  
  
  
  
Fig. 2: Time series of scaled NDVI-values of pine forest biotopes in the surroundings of the opencast mine of Nochten 
which are shown in Fig. 2. The visual impression, accor- 
ding to which the highest values of NDVI have been 
found in 1990 and 1995 while 1992 standed for the lo- 
west ones, could be proved by statistical analyses (Fig. 
3). More comparing investigations between the reference 
biotopes and those ones in the opencast mining impact 
zones are carried out during the vegetation period of 
1996. 
With exception of the low values found in 1992, the mean 
NDVI values from both, single pine forest types and total 
area clearly indicated an increase of vitality for the time 
period considered ( 1988-1995). The main reason for this 
Mean values of NDVI for pine forest 
biotopes 
  
    
  
0,8 
0,6 
B 1988 
0,4 B 1990 
0.2 1992 
01995 
  
  
  
total type5 type6 type7 type 8 
Fig. 3: Monitoring of vegetation for different pine forest bi- 
otopes in the area of Nochten 
was due to the meteorological situation. Owing to great 
precipitation deficits during spring and summer 1992, it 
explains also the lower NDVI values. Because of the 
deindustrialization and reinforced protection measures 
against pollution, extreme declines in dust and sulphur 
dioxid emissions were observed (between 60% and 90%) 
which also proved to be important for the vegetation 
changes. 
3 VEGETATION CHANGES ON SUCCESSION AREAS 
Parallel to the preservation of nearly natural landscapes 
with high biotope and species diversity like, for instance, 
pine-moor forest and nado-callunetea in the surroun- 
dings of opencast mines, it is of interest, to utilize the 
specific site conditions which are characteristic to open 
post mining areas for a natural development. For such 
areas of renaturation which have been abandoned to 
natural succession, 15% of the dump areas are planned 
to get this status after closing of the mining activities. 
Such processes of natural settlement have been obser- 
ved both by high spatial resolution satellite data and by 
field work on vegetation to serve as input for monitoring 
systems. 
The investigation area selected has been the former 
opencast mine of Schlabendorf (see frame 1 in Fig. 1), 
whose northern part was closed in 1977. 1640 hectares 
out of 2490 hectares excavated area were given back to 
agriculture. 717 hectares were reforested and 133 hecta- 
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996 
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