Full text: Nivellement zwischen Swinemünde und Berlin

III. §. 18. Theorie der Höhemnessang. 
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5. Als Beispiel zur Berechnung der x\ufgabe 5. wollen wir folgende 
Data annelimen: 
In B. In C. 
gegeben: li ... — 180 T //' — 300 T 
BÄ — s — 3500 T CA — 4’ — 4200 T 
BÄ — s — 5000 T CÄ— s" ~ 5600 T 
beobachtet: Elev. von A — e — 0° 10' 30" c — 1° 29' 59''8 
- von Ä — e — 0° 35' 45" e" — — 0° 42' 10','7 
gesucht wird: k die Strahlenbrechung in B\ k' die Strahlenbrechung in C; 
h die Höhe von A; h die Höhe von Ä. 
1. 
Berechnung von h t 
nach Formel ... 1. 
unter 5. 
logi 
= 3,54407 
log s = 3,69897 
log / = 3,623249 
i /// 
log s 
log e 
= 2,79934 
löge = 3,33143 
log e — 3,732378„ 
log e" 
log — 
° CO 
— 4,68557 
log - = 4,68557 
log — = 4,685575 
log — 
° CO 
• se 
los — 
° CO 
= 1,02898 
log — = 1,71597 
log = 2,041202,, 
J"J» 
| o 6 
log 
° CO 
+ 10?690 
+ 51,996 
— 109,952 
4,68557 
68,707 
■190,048.. log=2,278863 
log 4^=9,940074 
S S 
2,218937 
+ 165,553 
231,293 
231,996 
— 0,703.. log = 9,84696« 
log Ti — 9,69020 
s 
lsler Theil // + — = +190,690 
9,53716, t 
- 0,344 
2ter Theil 
3ter Theil 
= —165,553 
= — 0,344 
+ 24,799 .. log = 1,394434 
lo- / K~-\ = 0,889787 
log h — 2,284221. .Die Höhe von A od. h ~ 192*407
	        
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