deraf beregnet Sa.ltgehalten i de øvrige ved Ejælp at' Klbr- 

 mængden og den specifiske "\ ægt. 



I den følgende Tabel har jeg ordnet Bestemmelsefne 

 eftei' Nummeret ai' dr Stationer, hvor Vandprøverne er op- 

 tagne. Bestanddelene er i Tabel l beregnede som Pro- 

 center at' Sovandet. I Tabel II har jeg i Lighed med 

 Forchhammer udregnet Bestanddelenes Forhold til Klor- 

 mængden, naar denne sættes = 100. 



Egenvægten ai Sovandet er i Tabellen udtrykt ved 

 17 .5 C. sammenlignet med Vand af samme Temperatur. 



De Tal. der er satte i Parenthes. er enten fundne 

 ved Beregniug eller udledede af Bestemmelser fra nærlig- 

 gende Yandprøver. 



minations with divers samples ol' sea-water, he computéd 

 from the results obtained the proportion of salt in the 

 others; by means of the amount of chlorine and the spe- 

 cific gravity. 



In the accompanying Table the numbers of the de- 

 terminations are arranged to correspond with those of the 

 Stations at whicb the samples of sea-water were collected. 

 In Table I. the amounts nre computéd as percentages of 

 the sea-water examined. In Table II. I have, in common 

 with Forchhammer, computéd the. amounts as percentages 

 of the proportion of chlorine. taking the latter at 100. 



The specific gravities of the samples are reduced in 

 the Table to 17°.5 C. as compared with pure water of 

 the same temperature. 



The figures parentheticallv enclosed were either found 

 by computation or deduced from determinations with sam- 

 ples drawn in some adjacent locality. 



Den norske Nordhavsexpedition. Schmelck: Chemi. 



