Full text: Révision (Troisième partie)

     
  
  
  
  
  
    
  
  
  
  
  
  
  
= T PROFILTYP 1 T PROF ILTYF 2 
x 100.0 + - 
u = + 
= - ER 
I + 3 
uw 
u 
Zz + = 
T 
B 10.0 t = 
Tr a + 
ac B -— 
uw 
Ei. + + 
À T T 
[= - d 
= + = 
= 1 M Hi SCHRITTWETTE M 
0.1 + rH ee 8 H— HH 
1 10 100 1000 10000 1 10 100 1000 10000 
z T PROFILIYP 3 T PROFILTYP 4 
x 100.0 mu 
ul - M 
i nad + 
u 
Zz + + 
uw 
X 
Ww 10,0 - 3 + 
© P € 
T — —— 
+ + 
x + + 
wi 
x 
ul 1.0 je > 
d — d 
= 1 + 
T + T 
2 + SCHRITIWEITE M + SCHRITINEITE M 
0.1 EA | rb AA HM 
- 1 10 100 1000 10000 1 10 100 1000 10000 
1000.0— PROFILIYP 9 
3 0 
T O 1 là 
h = x a, 1 1b 
Oy « 100.0 + Xi at 8,25 
ofile > t a 1.5 35 
ere T n 
gegeben  , * Ws 
ole z + S 2 
I 
10.0" + 
e = 
| = x 
ge, + ; ; 
ensteieun Fig. 9 - Mittlere Abweichungen 
STE Suns x + der Modellannäherung 
iligen Ww 
teigung = 1.0 + 
> T 1 - in Ebene/Flachland 
be TI 2 - in Flachland/Mittelgebirge 
icht = 3 - in Mittelgebirge 
des + SCHRITTWEITE M 4 - in aridem Mittelgebirge 
4 + L I | EÙ + + LL 4 143 5 - in Hoch ebirge 
0 l PA T T Ju T Wet T1 T 1 T Jt f: Fr T3 g g 
1 10 100 1000 1000C 
= 71 + 
  
 
	        
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