145
neer the top. then a gla
sse made of the forme of an Inuerted syphon -
like the annexed figure and conteining at the bottom a pretty quan
tity of mercury, this ^ ___ tube being gradually sunk down into the water it
was very obuious how the pre
ssure of the water vpon the

in that part
of the syphon, which was open ^ /to the water/ did depre
sse it and ray
se the same in
theother part w
ch. was open to the air and Excluded the water. And It was
plainly shewed that the cylinder of mercury kept vp by the pre
ssure of
the water
was always about a 14
th part in length of the length of the water cylinder
between the surface of
the Quicksiluer and the top of
the water. It was far
ther Explaind by him and shewd that
that the air and water in this Represented
in all circum
stances materiall in this tryall the aether & air in the com
on
Barometer, that the mercury was common in both. for as twas suppo
sd that
the Barometer at the top of
the cane admitted
the aether & excluded the air
soe in this, it admitted the air & excluded the water -
He further shewd how the alteration of the specifique grauity of the air didalter the pre
ssure though the cylinder or altitude of the pre
ssing atmosphere
were the same, which to make more plaine by An Experiment, the fre
sh wa=
ter w
th. w
ch.
the greater gla
sse was filld was powred out & it was filld w
th. a very
strong solution of salt. care being first taken to obserue the exact
comparatiue height of
the mercuriall cylinder to
the fre
sh water cylinder
and it now appeard very plaine that the same altitude of salt water
kept vp a cylinder of mercury much higher than did the fre
sh water -
Here by the way Al
so m
r. Hooke shewd how
the pre
ssure of
the air Decrea
sd as
by a
ssending a mountaine approach is made neerer to the top, /of the air/ and he men
tiond
aso al
so that he had formerly brought into this Society Diuers Di
scour
ses &
experiments by w
ch. he had manife
sted that the pre
ssure of the air did actually
soe decrea
se in grauity according to the exp
t. was made further from the
center of the earth.
euen after the same manner as the Decrea
se of the
pre
ssure of the water was very visible in this In
strument. And also added that he
was preparing an in
strument for some tryalls to that purpose which he would shortly shew.
These were
an ^ /2/ other In
struments of the like nature w
ch tho
se other he hath for
merly produced since their meeting. w
ch. /are/
was not Designed to shew one ^ /or two/ single Exp
tand noe more but to be
& con
stant & standing In
struments whereby all the
phenomena of Grauitation and pre
ssure may be explaind, by hundreds of
Exp
ts. -
Further when a query was made why the Longer end of the syphon was not seald
vp, but remaind open, which was otherwi
se in the Barometer. m
r. Hooke explaind
the same and shewd that it was by rea
son the spring of the air that was included
would vary its pre
ssure vpon the rising or falling of the cylinder of mercury -
which being left open the weight of the air did not noe more than the aether did in the
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