Full text: Proceedings of the international symposium on remote sensing for observation and inventory of earth resources and the endangered environment (Volume 2)

       
   
    
    
  
  
   
   
    
   
    
  
   
    
  
  
   
    
    
   
   
   
   
   
   
   
   
   
   
     
   
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speed. Under alkaline and oxidizing conditions prevailing in 
the sea water in this area, chemical reactions between the 
substances introduced and the water occur. These are char- 
acterized by conspicuous colors: the green divalent iron is 
oxidized to reddish brown trivalent iron, which then rapidly 
precipitates as colorful red-brown oxide hydrate, whereas 
dissolved titanium forms similar white colored oxide hydrate. 
These processes seemed to offer a simple pathway for testing 
the suitability of presently available remote sensing tech- 
niques for determining chemical parameters from the sea sur- 
face. Any possibilities for future regular monitoring of this 
dumping area by means of remote sensing were also to be in- 
vestigated. 
Flight Camp a ign and Ground Trout 
The flight campaign for this experiment was conducted on 25 
August 1976, at very favorable weather conditions. During the 
dumping activities, the acid waste tanker was repeatedly and 
at different altitudes passed and surveyed by the research 
airplane. The aircraft was a DO 28 "Skyservant" operated by 
Deutsche Forschungs- und Versuchsanstalt fir Luft- und Raum- 
fahrt (DFVLR, German Research and Testing Institution for 
Aeronautics and Spaceflight) from its Oberpfaffenhofen re- 
search center. The aircraft was equipped with a number of 
multispectral cameras recording on black-and-white and false 
color film, a photogrammetric camera loaded with color nega- 
tive film, and particularly with an eleven-channel-scanner. 
At the same time, the Inorganic Chemistry Group of DHI was, 
together with other scientists, on board of Research Vessel 
"Gauss" of DHI working in the investigation area to obtain 
the necessary "ground truth" data, i.e. to perform chemical 
and physical measurements in and near the sea water surface. 
Parameters determined were mainly dissolved and freshly pre- 
cipitated iron, acidity (pH value), temperature and salinity. 
These parameters were measured continuously from the moving 
ship by & method for Fe and pH developed by WEICHART (2). 
For calibration, some water samples from the surface were
	        
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