H Y D R
o
S T A T
e
S.
they do in open ai ro To prove lhis by experimento let
as muen OIOt be put illto a poial, as, wheo eorked. \ViII
make it fiok io water : aod beiog tnus enarged, let it
ue
weigned, lidl io air, aod lnen in \lam, ano Ine weiglils
in botn hoth ea[es wrote uown. Tneo, as the phi,l
hangs fufpended io
wat~r,
and eounterpoifed, pull oUllhe
eork, that water may run inlo il, and il wd l defeeod,
and pull dowo Ihal end01" Ihe
be~m.
1
his done, pUl as
much weight into the 6ppofile
1~.lc ~s
"ill reaore Ihe e·
quipoife; "'hien
wei~ht
\Vdl be fouod 10 l"flVer exatllyto
Ihe additional wei;:hl of Ine phial wheo II is agaio wClgh–
ed in air, wilh Ihe lValer io it.
The vdocity "ith \Vhlch walcr fpouls out at a hole in
Ihcfid~
or bonom ofa vell'd, isas Ihe fquale root of lhe
dcpln or diaaoee of lhe hole below Ihe furfaee of Ihe wa–
ler. For, io order 10
m.kedoubl~
lhe qu.otilY of a
fluid ruo lhrough one nole as lhroogh .oodler of IOC fame
fize, it will require four times Ihe pren'ule of lhe olher,
aod therefore roul! be ¡our limes Ihe d' pÚI 01' lhe olher
bdow lhefurface of lhe water: aod for lhe fame reafoo,
time limes Ihe quaolily ruooiog iodO equal lime lhrougn
tne fame fon of hole, mul! ruo wiln lhree limes lhe ve–
locily, which will require oioe li",es lhe prell'ure; aod
coofequeody mufl be ilioe limes as dtep uelow the furface
oflhefluid: and fo on.- fo prove lhis by ao expenmerot,
let tIVO pipes, as
C
andg (Iig 9.) 01' equal fi zed bures,
be fixed ioto lhe fide oJ lne v, lI't1 A13 ; lhe pipe
g
bcing
four limes as deep belolV lhe lurfaee of Ihe "'alel' al
h
io
lhe vell'd as lhe pipe
C
is: ami .·hill\ lhefe pipes ruo, 1. 1
waler ue con(!lody poured iOlO lhe vcll'e1, 10 kcep Ihe
fu,faee aill al Ihe fame neignt. Theu, if a
COI'
dut
holds a piat be fo plaeed as 10 r:eeive Ihe water Ihat
fpoul! from the pipe
C,
aod al Ihe fame momeol a eop
tlUI holds a quart be fo plaeed as 10 reeeivé the \I/'Iér
Ibu
fpou~s
fromlhe pipeg, uOlhcops " ill be filkdallhe
fame linle byIheir refpetlave pipes.
The herizo",1di(!aoee,
10
whieh a fluid \ViII fpoul
froma norizonlal pipe, io aoy pan of Ihefide of ao"P–
righl "lI'tI belolV Ihe fu,faee of Ihe fluid, is equallO
I.·ice Ihe leoglh of a perpeodieular 10 Ihe lide of Ihevef·
fel, dra.·o from Ine moulh of Ihe pipe 10 a femi eircle
deferibed upoo the altilude of Ihe fluid : aon Ihercforr,
Ihe fluid will fpout 10 the greaten dlaanee poflible from a
Fipe wnafe mOUln ismhe eenlre of Ihe feolleircle; beeaufe
a perpeodieular to in diameler (fuppofed paralld 10 Ihe
fide of Ihe veOel) drawo from Ihal poiot, i! Ihe longel!
lhal eao poffibly be drawo from aoy par! of Ihe di. mtlCr
10lhe eireumfereoee of Ihe fe;nieircle. ThllS, if Ihe
..lI'd
AB
(fig. 9.) be full of waler, Ihe horizoolal pipe
D
be io the middle of its fide, aod Ihe femicirde
N.
:,'h
be deferibcd upoo
O
as a eeOlre, wilh Ihe r.dius or f<–
midiamel~r
OgN,
or
Dr.,
Ihe perpeodieular
Dd
10
ti"
diammr
NO.
i! the loogen Ihal eao be drown from ar,y
part of lile diameler 10 Ihe eireumference
N,deb.
Aod
if Ihe ' ell'd be kept full, Ihe jel
G
will fpOll1from Ihe
pipe
O,
10 Ihe horizontal dinanee
M,
whieh is dOllble
Ihe I,oglh of the perdeodieular
Dd.
lf IWOOlhtr pipes
al
e
alid
E,
be fixeo ioto Ihe fid. of Ihe veOd al equal
dialoces above aod be/olV Ihe pipe
O.
the pcrpendieulats
Ce
aod
F.c,
frolO Ihefé pipe 10 Ihe fcmicirclc, will be c–
Iiu¡l.¡ aoo Ihe jm
F
aod
H
fpoution from IheOl
wi!l
eaeh go 10 tlle hcrizonlal di(boee
NK;
whieh i! double
Ihe leoglh of Il:e equal perpeodieulars
Ce
or
Od.
Floids by Iheir prell'ore :Ildy be eooveycd over hills aod
.alleys io beoded pipes, 10 aoy heighl oot grealer Ihao
Ihe level of Ihe fpriogs from wheoee Ihey /lo
IV •
But
\VheoIhey are dcligoed 10 be rúf"dhigher IhaoIhc fprings,
forGiog eogines mUI! be ufed; whieh Olall be deferibed
wheo we come
10
treat of pomps.
A
jjphor.,
geoerally ufed for deeaoling liquors, is a
beodt4 piFe, whofe legs are of uoequal leoglhs; and Ihe
!horten leg muO allVays be put iOlo Ihe liquor ioteodcd
to be deeaoted, Ihal Ihe perpendieolar al lilude of Ilre
eolumnof liquor io Iheother leg may be looger Ihao Ihe
eolumn io Ihe immerfed Ieg. ef'pecially aboye Ihe fil r–
faee of Ihe water. For, if bOln columos were eqllally
high in Ihat refpeél, Ihe almofphere, whieh prell'es as
mueh up\Vard as dowoward. aod tlterefore aéls as mueh
npward agaioa Ihe eolumo io Ine leg Ihat haogs wilnoul
lhe .rll'd, as il aéls downward upon Ihe furfaee of the 11-
quor io Ihe ,ell'e1, \Vould hioder Iheruooiog of the liquor
Ihrough lhe fyphoo, eveo Iho"gh il were broughl ovcr
the beoded par! byfuélioo. So Ihat lhere is oOlhing lefl
10 eaufe Ihe mOliol\ of Ihe liquor, but Ihefoperior IVeiglrl
of Ihe eolumo io the looger leg, 00
aeev~OI
of ¡IS having
the greater perpeodielllar height.
Let
D
(Iig. 10.) be a eup fillcd lVirh walerto
e,
and
ABC
a fyphoo, \l/hofe OIOrlCr leg
BCF
is immerfed iD
the water from
C
to F. lf Ihe
e~d
.of Ihe olh,r leg
were no lower Ihao Ihe hoe
AC,
I'/ll\eh
IS
level lI'ilh 1m:
furfaee of Ihe waler, Ihe fyphoa woulJ OOt
filO ,
,.en.
Ihough Ihe
.i.r
(hould be dllll OOUI of it al Ihe momh
A. For allhough Ihefuétioo \\'ould dralV fome w' ler al
fidl,
)'el Ihe wm r would aop
al
Ihe momeot Ih, futlioo
e..red; becaufe
Ih~
air woulr! aél as muehuplVard againll
Ihe wareral
A••
! it .éled dO'voward for il
by
prelr.og00
lhe fu rface
at
C.
BUI if Ihe leg
I\B
come; dO\l/o to
G
aod Ihe air be d"IVo OUI al
G
by fllélioo, lile IVat';
will immecl:.Ilc1y follo\V, aon eontiooe 10 ruo, until Ihe
rorfaee of
I~e
waler io Ihe eup comes dewo10 F; beeaufe,
ulllhtn, Ihe rerper.dieul" hei&hl of Ihe eolumn
!:lAG
\ViII be grc:uer Ih"o Ihal of 1:,. .olllmo
en;
aod eoole–
queody. ilS \V1ighl IVi!! be grwrr,
uOlillhefurf.ceeom~
dOIVa 10
F;
and Iheo Ihe fyphoo willlfo p, thougn the
leg
CF
Ihould releh 10 Ihe bOIlOIll of Ihe cup.
FOI"
~vhich
rc"feo, Ihe leg Ih' l h.lngs IVilhoul Ihe CI'Pis , l.
W.IYS made long eoollgh 10 rcaó brlo'v Ihe lerel
01' liS
bOIlO,II ; as from
.t
10
E :
and I:.( n, wheo Ihe,Iyphoo i!
emplied of ,ir by ("élioo al
r,
Ihe W.llCr
imOl~c1iately
f"lIoll's, and by ils
eO"liouill br;n~s
a.·ay .he wholefrom
Ihe eup ; jllll as pu:lingooe eod of a Ih!Cld IVill ma"eIhe
,\hol ~
c1\;e
(O!i:l\'I ,
~
lf
Ih. perr,odielll" heighl of a fn ·hon. f, om Ihe fur–
f.liC of Ihe
\\al~r
10 ils beoded 10p 31 B. be OIore Ihan
33
leel, it will draw 00 wm r, eveo Iho"gl1 Ihe olher
Icg
wele l¡l:1Ch looger, aod
I ~e
fyrhoo
q~¡lc
cmpli(d of
air, uccallle Ihe wcight of a eolurnn of waler
33
fw
high is equ.,1
10
Ihe lI.ighl of
al
Ihick a COI"010 of
a:r, re.-hlog from :he ;,11 Íace of Ihe earth 10 Ih, 10p of
Ih~
alnlo(phm; fo Ihal locre willlheoh. aoequilibriom ;
a01 coo(e(l'lently, Ihour.h Ihere wOllld be w, ighl eoough
of air opon lhe furface
C
to
tu.k.e
Ihe W.\I:r alc<:od 10Ihe
leg