218
Then the minutes of the La
st
Day meeting were read which gaue
occa
sion w
ch. gaue occa
sion to Di
scour
se further concerning the
nature of the Air and of the vapours Raysd vp into it
by heat.
m
r Henshaw Related the ^ /manner of making the/ Experiment of condensing the
said vapours out of the air, by putting Ice and salt
into a gla
sse
and tapered downwards And ending in a point
and then suspending it in some place where a considerable
currant of the air pa
sses by, for By that meanes the
vaporous parts
out of the air will be conden
sd by
the exceeding great cold of
the ve
ssell and trickling down by
the sides will Drop into a Receiuer placed vnder neath the taper
ing end . a pretty quantity of water in a little time.
This was confirmd by D
r. croon & others.
m
r. Hooke Related an obseruation of the like nature which he
had made in
the year 1665 . in a Deep well of one m
r. Clark
neer Ban
stead Downes of 300 foot Deep. Into w
ch. hauing in
the time of a very great fro
st & exceeding cold wind w
ch. hapned then
about X
tmas. Let Down a bottell w
th Sp
t. of wine soe cooled by the
air aboue, the same - when pulld vp againe - appeard all couerd ouer
w
th Great Dropps of Dew, and besides a great
Deale ^ /many drops of water,/ were ob
serued
to be runn off from the bottell into the scale in w
ch. it stood. w
ch.
by him was attributed wholy to the warm
th. and vapourou
sne
sse
of the air of
the Bottom of
the Well, and the exceeding coldne
sse
of the Bottle Lett down w
ch. conden
sed
the vapours of that air into
water.
m
r. Henshaw and D
r Croon mentiond the Reaking of well water
in fro
sty weather w
ch ^
/the/ /. . ./ /of wch. in cold weather/ wch. was attributed to the warmth of
the water
and coldne
sse of the air.
not . . . that the water -
m
r Hooke
Related conceiued that this was occa
siond partly by the
coldne
sse of the air conden
sing the steames w
ch. Doe continually
ri
se not only from well water but from all other water when
of Such a Degree of Heat. In
soemuch that all water exposed to
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