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9
deraf beregnet Saltgehalten i de øvrige ved Hjælp af
Klor-mængden og den specifiske Vægt.
I den følgeude Tabel har jeg ordnet Bestemmelserne
efter Nummeret af de Stationer, hvor Vandprøverne er
optagne. Bestanddelene er i Tabel I beregnede som
Procenter af Søvandet. 1 Tabel II har jeg i Lighed med
Forchhammer udregnet Bestanddelenes Forhold til
Klormængden. naar denne sættes = 100.
Egenvægten af Søvandet er i Tabellen udtrykt ved
17 °.5 C., sammenlignet med A and af samme Temperatur.
De Tal. der er satte i Parenthes. er enten fundne
ved Beregniug eller udledede af Bestemmelser fra
nærliggende Vandprøver.
minations with divers samples of sea-water, he computed
from the results obtained the proportion of salt in the
others; by means of the amount of chlorine and the
specific gravity.
In the accompanying Table the numbers of the
determinations are arranged to correspond with those of the
Stations at which the samples of sea-water were collected.
In Table I. the amounts are computed as percentages of
the sea-water examined. In Table II. I have, in common
with Forchhammer, computed 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 parenthetically enclosed were either found
by computation or deduced from determinations with
samples drawn in some adjacent locality.
Den norske Nordhavsexpedition. Schmelck: Chemi.
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