287
Feb: 20. 1678/9.
m
r. Henshaw the vice Pres
t. tooke the chair
The minutes of February the 13
th. Gaue occa
sion to Di
scour
se
further concerning the Theory of the Barometer from w
tcau
ses the alterations thereof might proceed.
some were of Opinion that the cau
se thereof might proceed fr
othe extraordinary height of the air only ebbing and flowing
as it were like a tyde but w
th vncon
stant motions -
m
r. Hooke was of opinion that together w
th. this was to be ioynd
the Particular & specifique grauity of the body of the air
as being charged sometimes w
th. heauier sometimes w
th. lighter
vapours or Bodys. di
ssolued into It and taken vp by it
He further explained how Differing heights might produce the
same pre
ssure prouided there were the same quantity of
grauitating w
thin the Same Cylinder and In
stanced that
a Cylinder of the same air Rarifyed into greater height.
In Summer could haue noe more pre
ssure then
a much shorterwhen in the winter time it is conden
sed into a much shorter
Further to Elucidate his theory of it he added that he would
the next meeting produce some Experiments -
S
r. Ionas more acquainted the Society that he had by him
some papers of m
r. Townlys obseruations on that subiect
as al
so some Late obseruations of m
r. Flamstead. and
tht.
he would Produce them here the next meeting.
It was De
sired that the Exp
ts. formerly propounded by m
r. Hooke
to be tryed at the Column at Fi
sh
street Hill might be anew
Prepared. And In order therevnto m
r Hooke was desired
to prouide conuenient Gla
sses and other conueniences for
the perfecting that tryall. And that then the tryall might
be againe w
th all the care and Accuratene
sse necce
ssary.
Herevpon It was queryd how this Experiment of the Differing
pre
ssure of the Atmosphere came at first to be thought of
And It was Related that It was first Propounded by S
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