by
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dy
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in
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of
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dy
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o
20
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AVERAGE:77
h90i 4» 01O - 0000 C —
OOOOOOOOOO
0 400 800 (ha)
T 0O T A 1 A R E. A
(1) Score destribution in londslide area
Fig.3 Result. of getting
SCORE
110
100
90
80 1305
70 AVERAGE:70
60
50
40
30
20
1000 2000 (ha)
T. 0 T A L A R E A
(2) Score destribution in total study areo
score of overlaid polygon.
ut
0
EXTRACTED AREA
100%
80%
60%
40%
20%
0%
Fig.5 Rote of extracted
1
F R E O0 U E N
0
150
0
CY
area in each landslides.
3.2 Attempt to extract landslide areas
The factor information used for the analysis of
3.1 was organized into one :layer ‘by polygon
overlay. The polygon created as a result of polygon
overlay was added with the score worked out for
each factor from its relationship with the
landslide, The extraction of landslide areas is
carried out basing on these score. The extracted
results are discussed from the viewpoint of
coordination with the already-occurred landslide
areas.
3.2.1 Establishment of threshold: It is necessary
to give a score for each category and add weight to
the factor information organized into one layer. At
present, however, there is no effective method to
do so which is both objective and quantitative. In
this study, therefore, we worked out the ratio of
area occupied by each category within the landslide
area and discussed thereon the relationship between
the factor and landslide. Namely, the difference of
area ratio within the landslide area can be
considered as the difference of weight among the
categories. For example, lithologic character at
the total area of landslide Shows that
approximately 11% of "colluvial and debris" and
approximately 2% of. "gravel, sand and silt" are
distributed on the already occurred landslide
areas, Within the total study area, on the other
hand, the share of "colluvial and debris" is
approximately 5% and that of "gravel, sand and
silt" is approximately 6%. Thus, if the area ratio
of categories related to the landslide, the area
ratio changed between the landslide area and the
total study area. Therefore, the value of percent
of each category at the landslide area can be used
as the weight. This way of weighting is considered
to be more coinciding with the actual state.
Also, it is impossible to ignore the relation
between landslide and ponds/paddy fields. However,
the database of ponds and paddy fields was not the
one created as the result of classification made to
653
the total study area, but it is a result of
extraction the land information. Therefore, as the
method to add weight to the ponds and paddy fields,
we decide to calculate. the ratio of area occupied
by each factor within the landslide area against
the area of each factor within the total study
area, and to add the percent value as a score.
Also, these scores are used as the threshold
value in extracting the landslide areas. The
information to which the weight addition was
completed is overlaid with the landslide
distribution information. Fig. 3 shows the
distribution of scores within the total study area
and at the landslide areas. The average score in
the already occurred landslide areas is 77 points,
while the average score of total study area was 70.
Now, the difference of score distribution between
the total study area and landslide area is that the
score distribution at the landslide area is lower
than that in the total study area below the
average. Namely, the landslide areas are
distributing at the high score areas within the
total study" area. Basing on this result, we
extracted the polygons which have the score of 77
or higher, which is shown in Fig. 4.
3.2.2 Analysis result: Here, we will evaluate the
information extracted through the above-mentioned
process. Fig. 5 shows the ratio of region with the
score 77 or higher against each landslide area.
There are 672 landslide points in the study area.
Out of which, the landslide points which are
located within the extracted area are 599
(including the point only a part of which is
included in the extracted area). Namely, the
landslide points in the extracted area is 88% of
all the landslide points in the total study area.
Also, the landslide points 60% or more of which is
occupied by the score 77 or higher are 366. Namely,
the landslide points 60% or more of which is
occupied by the score 77 or higher is 54% of all
the landslide points within the total study area.