REPORT OF COMMISSION VII
GVTI-73
Table II
Comparison of Engineering Soils Types as Classified by Photo Interpretation and
Field Classification, Bangor Quadrangle, Maine
classification by photo interpretation
Soil
Type
R
%
BG
%
B
%
G
%
F
%
S
%
P
%
R
58
79
24
32
9
10
2
2
BG
11
15
47
62
3
3
В
3
4
3
4
64
72
1
4
15
16
2
4
G
1
1
2
3
4
4
20
77
4
4
F
9
10
5
19
72
76
1
2
S
2
2
40
74
5
14
F
11
20
31
86
'total
73
99
76
101
89
99
26
100
95
100
54
100
36
100
Italicized values indicate correct photo interpretations as confirmed by field checking. For
example, of the 73 areas classified by photo interpretation as R, 58, or 79 per cent, were found to
be correct. Of the remainder, 11, or 15 per cent, were found to be erroneously classified as BG;
3, or 4 per cent, were called B; and 1, or 1 per cent, was called G.
ACCURACY OF MAP UNIT DESIGNATION
Ail examination of the engineering soils map indicated that the existing
road grid traversed the map units to such a degree that it would be convenient
to do the sampling in the vicinity of the roads. Although this is a questionable
departure from the concept of random sampling, it was accepted because of the
limitations in time and funds.
If the field check is accepted as the final authority, then the photo interpreta
tion is either correct or incorrect. This makes the data amenable to analysis
employing the binomial theorem. Snedecor (9) discusses this in detail and pro
vides a table on page 4 of Statistical Methods. Within this table the confidence
interval at 19:1 odds or 99:1 odds can be determined without any computations
at all. In chapter 16, Snedecor provides the background information to make
computations leading to a greater degree of refinement than is possible by using
the table.
Accuracy of Boundary Line Location
The accuracy increment, or degree of precision, in map checking is de
pendent on map scale, type of interpretation, whether the study is reconnais
sance or detailed in nature, and other factors peculiar to any given mapping
project. The reconnaissance engineering soils map of the Bangor Quadrangle is
at a scale of 1:31,680. At this scale, the actual width of soil type lines on the
final map represents approximately 50 feet on the ground. For this study the
minimum error, or accuracy increment, to be measured was established as 100
feet. For other types of mapping, the accuracy unit may be a foot or a hundred
yards depending on the scope and purpose of the particular map.
A problem in checking the boundary line accuracy is locating the boundary
in the field. In some instances the boundary is well defined, but in others there
is a transitional band of considerable width between map units. Unless these
bands are extensively sampled, different observers could easily locate the
boundary in different places. For reconnaissance mapping, however, time-con
suming and expensive sampling is not justified. In soils engineering, forestry and
geology there are situations in which boundary delineations by photo interpreta