Full text: XVIIth ISPRS Congress (Part B4)

  
Figure 3 shows the sampling area in a sub-region of land 
system B (loess-covered sandstone hill). The sampling 
area consists chiefly of two kinds of land unit, namely, 
cultivated and gently sloping hillside and rocky gully 
slope. They together account for approximately 85 per 
cent of the total sampling area, indicating a close correla- 
tion between the sampling area depicted by photomorphic 
characteristics on the TM image and the real distribution 
of the land units. Using this approach, not only all land u- 
nits in the sampling area were recognized and mapped, but 
also all land units in the land system were deduced based 
on the area proportion and real distribution of the land u- 
nits in the sampling area, and the area proportion of the 
sampling areas in the sub-region or even in the land sys- 
tem. 
3.3 Interpretation and Mapping of Land Sites 
  
A land site as part of the land unit is, for all practical pur- 
poses, uniform throughout its extent in landform, soil and 
vegetation. In general, the interpretation and mapping of 
land sites in a land unit followed the approach similar to 
that for land unit. First, the land unit was divided into a 
number of small areas with more homogeneous photomor- 
phic characteristics on 1: 50, 000 scale photograph. Sec- 
ond, a sampling plot was chosen for each of small areas 
and its boundary was as accurately as possible located on 
1:10, 000 scale photograph. Third, elementary relief units 
and the associated soils and land cover/use types in the 
plot were identified. Final, all land sites in the sampling 
plot were interpreted and delimited based on comprehen- 
sive analysis on photomorphic characteristics and consult- 
ing thematic maps as well as field studies. 
Figure 4 illustrates a rocky gully slope plot. In this plot, 
the land site of gully slope (581) accounts for approxi- 
mately 68 per cent in area, indicating a good correlation 
between the sampling plot depicted by photomorphic char- 
acteristics on 1:50, 000 scale for land site interpretation 
and mapping. Based on the area proportion and spatial 
distribution of land sites in the sampling plot as well as the 
area proportion of the sampling plot in the land unit, all 
land sites in the unit could be deduced and mapped. 
4. CONCLUSSIONS 
The multi-level sampling interpretation of remotely sensed 
imagery in terrain survey and mapping conducts the inter- 
pretation successively from entirety to part and from high- 
er level to lower level of land type. This stage-by-stage 
approach is much beneficial to improving quality of the in- 
180 
terpretation. In addition, time and costs in the survey and 
mapping can be substantially reduced as the approach is 
based on the statistical sampling theory and land type in- 
formation is extracted step-by-step from sampling areas 
with relatively homogeneous photomorphic characteristics 
on imagery. However, it should be noted that the accura- 
cy of resultant land type maps produced based on the ap- 
proach is largely dependent on appropriate selection of 
Therefore, 
much attention should be paid to field survey and inves- 
sampling areas. while using this approach 
tigation to ensure the accuracy of the interpretation and 
mapping. 
5. REFERENCES 
Christian, C. S. and Stewart, G. A.. 1968. Methodology 
of Integrated Surveys. In: Unesco Conference on Princi- 
  
ples and Methods of Integrating Aerial Survey Studies of 
  
Natural Resources for Potential Development. Thoulouse, 
Unesco, Paris, pp. 233-280. 
  
Townshend, John, R.G., 1981. Regionalization of Ter- 
rain and Remotely Sensed Data. In: Terrain Analysis and 
Remote Sensing edited by John, R. G. Townshend. 
George Allen & Unwin, London, pp. 109-132.
	        
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