Full text: Resource and environmental monitoring

  
ALLOCATION OF SOIL RECLAIMING MATERIAL BASED ON DIGITAL PROCESSING OF AERIAL 
PHOTOGRAPH 
T. Tóth!, L. Pásztor!, M. Kertész, B. Zágoni! and Zs. Bakacsi' | 
!'research fellows of the Research Institute for Soil Science and Agricultural Chemistry of the Hungarian Academy of Sciences, 
? senior research fellow of the Institute of Ecology and Botany of the Hungarian Academy of Sciences 
Commission VII 
KEY WORDS: aerial photograph, digital processing, 
sampling plan, estimation error, salt-affected soil, soil 
reclamation, gypsum requirement, Hungary 
ABSTRACT 
Precision farming has two requirements, such as i) correct 
dosage of agricultural materials realized at ii) the exact 
location in the plot where these are needed. Our objective was 
to introduce the direct use of remotely sensed images into the 
practice of soil reclamation as a source of information on 1) the 
probable dosage of required amendment and ii) precise 
location of reclaiming materials. 
The remotely sensed image was used in two phases, for the 
selection of optimal soil sampling plan to reclaim the plot and 
for the compilation of actual plan of reclamation. 
The basic material of the study was a panchromatic aerial 
photograph on a sodic plot with patches of higher sodium- 
affection. 
As a first step the relationship between gypsum requierement 
and the intensity of the aerial photograph was established. It 
turned out to be linear and therefore the aerial photograph was 
used directly for the analysis of alternative sampling plans. 
As a test of the utility of sampling plans, a set of potential 
sampling points were used for the interpolation of the original 
aerial photograph and the precision of the interpolation was 
measured by the sum of squares of the differences between the 
original and the interpolated photographs. 
The optimal sampling plan was selected accordingly and the 
field sampling, which was carried out for its test, confirmed the 
previous selection. 
INTRODUCTION 
All over the world large tracts of sodic soils receive gypsum as 
reclaiming material. We do not describe its mechanism here, 
just make reference to that the calcium ions released upon the 
dissolution of gypsum replace the harmful sodium ions and 
create favourable conditions for the soil solute transport and 
plant growth (McBride, 1994) . 
The present status of within-plot reclamation of salt-affected 
soils in Hungary does not follow the technological 
advancements (MSZ 9693/1-77). When there is a special map 
series of the status of salt accumulation, it is perfectly suitable 
for the production. If it is not available, the corresponding 
national standard prescribes the reclamation based on average 
samples. In view of the mosaic pattern of such lands the use of 
average samples easily can result in largé sub- or 
overestimation of the necessary dosage of reclaiming materials. 
This mosaic pattern of the salt-affected soils is manifested in 
several properties of the soil, most importantly its natural 
vegetation (Csillag et al., 1993, Kertész and Toth, 1994, Toth 
and Kertész, 1996, Tóth and Pásztor, 1996, van Meirvenne et 
al., 1996). On croplands, when there is no vegetation cover, 
the areas with different salt accumulation status can often be 
distinguished on remotely sensed images (aerial photograph, 
satellite images) (Metternicht and Zinck, 1996, Tôth et al, 
1991a and b) based on the surface features of the soil. 
Our objective was to improve the reclamation of salt-affected 
soils with the direct use of aerial photographs. 
MATERIALS AND METHODS 
Preliminary sampling and its evaluation 
In order to describe the character of the relationship between 
the intensity of aerial photograph and the gypsum requirement, 
on a sampling route representing the intensity distribution of 
the aerial photograph (Fig 1), we collected soil samples at 13 
points, and measured field bulk electric conductivity in situ at 
another 50 points. The location and elevation of the sampling 
points was recorded with a field station, therefore we could 
find out the intensity from the aerial photograph. 
  
intensity 
sampling track represents the within plot distribution 
  
  
5505288838389 3E 
  
  
   
  
  
Fig 1. Airborne image of the sample plot with the preliminary 
sample sites 
The preliminary sampling showed that there is linear 
relationship between the gypsum requirement (GR) determined 
in the laboratory and the intensity value of the pixels, and these 
results suggested that the aerial photograph could be used 
directly for the realization of the sampling plan. 
178 International Archives of Photogrammetry and Remote Sensing. Vol. XXXII, Part 7, Budapest, 1998 
  
=. 
Ca
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.