Full text: Révision (Troisième partie)

  
  
   
  
  
    
  
  
= T PROFILTYP 1 + PROFILTYP 2 
© 100.0 + + 
= — — 
=) + + 
ac 
a M + 
U) 
Z j d 
w 10.0 + + 
co m a 
= + + 
E. 
1 d 
az = 
Lui T 
ac ur 
eig 1 vat + 
; | =a 1 
+ 4d. [ 
5 
+ SCHRITTWEITE M 3 SCHRITTWEITE M 
0.1 ed - +H 
1 10 100 1000 10000 1 10 100 1000 1000 
E 1 PROFILTYP = T PROFILTYP d 
c 100.0 4 + 
= 1 T 
x + T 
0 
= E + 
LJ 
x 
Li 10:0. 7 Tr 
c —— al 
T + + 
+ + ck 
x - je 
Li 
E i-is ; + | 
-— = + 
pe = = 
= 1 T 
= j SCHRITTHETITE + SCHRITTWEITE N 
0.1 - = 
1 10 : 100 1000 10000 1 10 100 1000 1000 
1000 Or .."ROFILTYP 5 
T 6. 
x + Ins | ge: 
1 Fr 
© 100.0 4d 9.8 an 
z s Aui s D : 
= + die 
a. + x 1-5 25 Un 
e T Li 1 S 35 des 
i ; Eir 
ui 10.0 "T inj 
X À De: 
NE ; : T : ein 
Fig. 11 - Mittlere Unstetigkeiten PC 
oe + der Modellannäherung £ 
= da 
ul 1.0 wt Hol 
as I 1 - in aridem Mittelgebirge gan 
= + 2 - in Ebene/Flachland Er 
x 3 - in Flachland/Mittelgebirge sin 
+ SCHRITTWEITE M din Mittelgebirge Die 
0-1 -L—À—ÀH93-H—I——FH-H—-—9H|P-H-—4——-H 5 - in Hochgebirge 
1 10 100 1000 10000 
„74 
 
	        
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