1C» 
No. 
59 
60 
■6 1 
62 
6 . 3 ' 
64 
65 
66 
6 7 
68 
6g + 
7 °* 
7 i* 
72 
73 * 
74 
75 
76 
77 
7 8 
79 
80 
81 
82 
83 
84 
85 
86 
87 
88 * 
80 
90 
91* 
92 * 
93 * 
94 * 
No. 
283. 
283- 
286 
286 
293 
295 
295 
2 95 
296 
297 
301. 
303 
304 
304 
•321 
32 . I*‘ 
323 
323 
332 
332 
335 
335 
339 
342 
342 
345 
I 345 
347 
347 
349 
I 350 
! 350 
j 352 
j 352 
1 359 
362 
T 
Nordlig Uredde. 
(North Latitude.) 
Længde 
fra 
Greenwich. 
'(/.qriffiluile from 
Orrenwlt/l.) 
Dybde hvorfra Pro- 
ven hentet. 
(J)rpth /ram which the Sam-' 
plrt were collected.) 
Engelske 
Favne. Meter. 
(ICnglilh 1 Metres.) 
0 4- -V 
x;c. 
per Litre. 
’.V 
CC. 
per Litre. 
0 4- iV 
= 100 
0 % 
( U per cent.) 
Tempe- 
ratur. 
Celsius. 
Anmærkninger. 
(Jtemarks.) 
- » ~ 

73° 47 -5 
73 47 5 
72 57 
72 57 
7 1 7 
71 59 
71 55 
71 59 
72 15-5 
72 36.5 
74 1 
75 >2 
75 3 
75 3 
74 56.5 
74 56.5 
72 53-5 
72 53-5 
1 75 56 
75 56 
76 16.5 
76 16,5 
76 30 
76 33 
76 33 
76 42.5 
76 42-5 
76 40.5 
76 40-5 
76 30 
76 26 
76 26 
77 5 6 
77 56 
78 . 2 
79 59 
1 4 0 21 
14 21 
14 32 
14 32 
2 1 11 
1 1 40 
11 30 
1 1 40 
8 9 
5 12 
1 20 
3 2 
4 51 . 
4 ' 5 i 
19 30 
19 30 
21 51 
21 5 1 ' 
1 1 36 
1 1 36 
14 39 
14 39 
15 39 
13 18 
13 18 
10 9 
10 9 
7 47 
7 47 
2 57 
o 29 
o 29 
3 29 
3 29 
9 25 
5 40 
W. 
E. 
W, 
o 
o 
o 
447’ I 
95 ! 
o. 
600 
1 1 10 
100 
1280 
o 
150 
300 
1735 
o 
25 
o 
o 
1149 
1 1 49 
o . 
179 
37 
o 
523 
300 
300 
o 
1429 
1487 
300 
1686 
300 
1686 
o 
o 
o 
o 
817 
174 
o 
1097 
2030 
183 
2341 
o 
274 
549 
3173 
o 
46 
o 
o 
•2IOI 
2 101 
O 
32 7 
68 
o 
956 
549 
549 
o 
2613 
2719 
549 
3083 
. 549 
3083 
o 
o 
19.8 
12.8. 
35-4 ' 
7-2 
19-5 
1 2.6 
35-3 
7-2 
20.6 1 
13.2 
35-8 
7.2 
2 1.8 
14.8 | 
• 3 1 9 
— 0.8 
19.6 1 
13.0 
33-5 
5,1 1 
20.2 
12.8 | 
’ 36.7 
7.0 
2 1 ‘4 
14.6 
3 i -7 
—0.8 1 
2 1-5 I 
14.6 
32.1 
— 1-3 
20.4 1 
13-4 
* 34-2 
*■' 1 
21.3 
13 - 8 '. ! 
35 1 
- 1-4 
21'9 
14.1 j 
35-6 
2.2 
22.6 
t 4-7 
33-1 
— 1- 1 
21-7 
M -7 1 
32.2 
— 0.8 j 
21.6 
14.6 
32.2 
— 1-5 
' 2-3.8 
• 15-4 
35-2 
05 1 
23-7 
15 3 
35-4 
0.2 
i 9-3 
12.3 
36-5 
7.8 
‘ — 
35-8 
7-8 
21.9. 
14.8 
32.2. 
— 1-5 
22.0 ' 
150 
31.8 
— i -5 
20.8 
13-3 
36.2 
5-4 
2 1.0 
14.0 
33-1 
1 .0 
2 1. '6 
142 
34 -i 
0.9 
21.8 
1 4. 1 
35-3 
6.2 
20.8 
13.8 
33-8 
— 1.0 
20.9 
1 13-7 
• 34-4 
1.0 
21.5 
142 
33-9 
1.0 
20.9 
13-4 
35-7 
4-4 
21.4 
13-9 
35-1 
— i -3 
21.7 
14.6 
32-5 
— i -5 
21.9 
14-7 
32-7 
— 1 . 1 
22.9 
i* 5-3 
■ 3 3 -.3 
— i -5 
2 1.9 
14.8 
32-5 
— 0.8 
22.4 
151 
32.8 
— i *5 
— 
-- 
35' 7 
4-3 
20 3 
13.0 
35-8 
5-2 
ke II 
The samples of water 
udtrykkelig er anført, udkogte stvax efter derés Optagels'e. 
Som man ser, ligner denne Tabel overmaade meget 
deh åf Dr. Jacobsen opstillede,. bvad man ogsaa paa For- 
Inuuid kunde vente, da de undersøgto Districter tuldstamdig 
gaa over i hinanden, og naar Differentserne mellom de af Hr. 
Svendsen og mig opforte Tal ere noget storro, da kommer 
dette ligefrem af det af os bearbeidede Felts større Ud- 
strækning og deraf følgende større Uensartethed i de phy- 
verse is .suittu. uum-u ~ -<= 
As will be seen, this Table agrees very closely 
with that prepared by Dr. Jacobsen, which was indeed 
to be expected, since the tracts investigated coalesce; and 
the somewhat greater differences exhibited by Mr. Svend- 
sen’s and my own figures arise Simply lrom tbe region 
explored by the Expedition having been more extensive, 
involving greater 'dissimilarity in the physical conditions. 
sikalske Forholde. 
Hvad dor er most ioinefaldende. er dot paafaldende 
Phænomen,. at der med Hensyn paa den relative Sarnmen- 
sætning af den i OverHadevandet indeholdte Lult paa den 
norske Nordhavsexpedition er fundot betydeligt større Sur- 
stofgehalt end af Dr. Jacobsen for Nordsøen opstillet, sna- 
ledes er Surstofprocenten i Overfiaden i Nordsøen bestemt 
til i Middel 33.93 °/ 0 af den samlede Luftmængde, medens 
den for det af den norske Expedition i 1870 og 77 under- 
søgte Strøg søndenfor den 70 de Breddegrad, beløber sig 
With regard to the relative composition of the air 
in surface-water, the proportion of oxygen was. strange to 
say, on the Norwegian North- Atlantic Expedition lound 
to be considerably greater than that given by Dr. Jacobsen 
for the North Sea. The mean proportion of oxygen in 
the surface-water of the North Sea he determined to be 
33.93 per cent of the total amount of air, whereas the mean 
proportion for the tract of the North- Atlantic stretching 
south of the 70 th parallel of latitude, that investigated by the 
