Full text: XVIIth ISPRS Congress (Part B4)

| im- 
tility 
king 
land 
mon- 
p ter- 
on of 
hills 
sand- 
, the 
com- 
uired 
pho- 
ed in 
veral 
pe at 
tation 
s and 
ireas, 
)Ogra- 
968). 
on the 
ids of 
ion of 
photomorphic characteristics, especially colour tones. In 
other words, each kind of region has own notable photo- 
morphic features, in particular colours and their combina- 
tion. Region A is characteristic of long and very narrow 
white stripe accompanied with wide brown-red stripes on 
both flanks, sometimes on one flank. Region B appears to 
be dark green broad stripes as well as light brown or light 
yellow patches. Region C is dominanted by redish yellow 
colour together with light green narrow stripes. In region 
D, the major colours are brown-red and green, or brown- 
yellow, brown-red and greyish white. In region E, grey- 
ish white is the dominant colour, along with patched 
brown-yellow, light yellow or brown-red colours. 
By consulting the land cover/use map and other ancillary 
data and through reconnaissance surveys an integrated 
analysis on the relationship between photomorphic charac- 
teristics of each region and its probable land system was 
conducted. As a result, each of these regions was assigned 
to a given land system with some indispensable modifica- 
tions in its boundary. The resultant land system map was 
shown in Figure 2, and the main characteristics of each 
land system were briefly described in Table 1. 
Table 1 The Main Characteristics of Land Systmes 
Land system Characteristics Total area 
symbol (sq. km) 
A River beds in greyish white colour; and river terraces cultivated and in brown-red 161. 5 
colour. with patches of woodland in dark brown colour or grassland in light yel- 
low colour. 
B Loess hillside, cultivated and in light brown colour or grass-covered and in light 443. 9 
yellow colour; and sandstone gullies, mostly bared and in dark green colour. 
C Sandstone hillside, mostly grass-covered and in reddish yellow colour, and part- 390. 4 
ly cultivated and in light brown colour: and sandstone gullies, mostly bared and 
in light green colour, and large gully bottoms in brownish red colour. 
D Sand-mantled loess hillside, forested and in brown-yellow colour, or cultivated 679.5 
and in brownish red colour, or bared and in greyish white colour: and grass-cov- 
ered loess gullies in yellow green colour or cultivated and in brown-red colour. 
E Sand-mantled and nearly level to gently undulating ground, mostly bared and in 171.2 
white colour and partly forested and in reddish yellow colour, or cultivated and 
in brownish red colour; and sand-mantled shallower gullies, mostly cultivated 
and in red colour, or forested and in brown-red colour. 
3.2 Interpretation and Mapping of Land Units 
  
Land units are the broader components of a land system. 
Each land unit formed on a basic topographic unit has its 
corresponding soil and vegetation. In order to delineate 
land units in a land system, a number of sub-region with 
relatively homogeneous photomorphic characteristics were 
distinguished on the TM image. In addition, one sampling 
area was selected in each sub-region and its boundary was 
as accurately as possible depicted on 1:50, 000 scale aerial 
photographs. As a result, land units were interpreted 
through analysis on the relationship between photomor- 
phic characteristics and physiographic features combined 
with the consulting of the thematic maps and field obser- 
vation. 
In the interpretation of land units such information as 
landform readily to interprete was extracted in the first 
and could be taken as the starting for further interpreta- 
179 
tion. Land cover/use types are distinguishable based 
mainly on colour variation on the photographs. For exam- 
ple, cultivated farmland, fallow, pasture, woodland and 
settlement cold be distinguished by colours of red, green- 
ish grey. yellowish green, brownish red. and greyish 
white, respectively. Besides, size, texture and shadow of 
ground features on the photographs also were used, for in- 
stance, to make a differentiation between tree, shrub and 
grass. Shadows are particularly useful for the estimation 
of dissection intensity of gullies. Nevertheless, there are 
still a certain amount of information related to land unit 
which are not readily to interprete directly on the pho- 
tographs. Consequently, the deductive inferences added 
some advantages, for instance, to the differentiation of 
such ground features as irrigated farmland and dry-farm- 
ing land based on irrigation canals or special large wells. 
Through these stages all land units in the sampling area 
were recognized and mapped on the 1:50, 000 scale base 
map. 
 
	        
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.