p
N
E
u
The w";ght or prclru re of the air is
,,,,31,
dctcrmind by
'the fo!Jowing
expcriRlenr.
T he
TO R IC Ii t.LIAN
EXl' E RIMENT..
T ake a\
gla~~ tub~
t¡hout [hree.: f( et long. and apeo at one
tnd : fill
It
wllh
qUI\:kfJI ...er ; and puu ing your
linga
upon
the ope'n
toJ,
tUI
n [hat end d-,>wllward and
il1lml.!rfe
It
¡nw d
fm .d l
vdrel
of ql1icklilvcr,
WlthOUI
Jt:tting in any ¡ir: (hen
t
ke
aw~y
your
IInga,
and the quickGlver wdl I'emain fuf.
pended io the tube
~
9t
¡nches aboye
in
furf.lcc in the
;vt'f!d; fometimei more, ami
'2t
otbe,r
times J((s, as
lhe
welgh t of Ihe:
¡Ir
15
v.ried
by
winds and other
cauCes.
That
~he ~uickr.lvú
is kept up in ,he
tu~e
by ,he prdfure of ,he
atm~rphere
upon
lh.l\
¡.,
lhe bafon. is cVJd<nt ; (ur,
ir
the
baf~n
and rube be
P~[
unJc r a glafs, and (be air be chen
raken out of [he glals. all dle
qUlckfilver in lhe tU'>e w,1I
:fell! d own in,ta l he hafon ; and
If
{he air be lel
in
agel;n, the
.qlllckfilver \ViII rife
10
(he f04me heigh{ tl's befCJre. There–
(ar~
lile
~i~'s
·prd fure. an lhe
fu rfclc~
of
(he c¡rth, is
t:quJI
to
tnc welgnt
or
29!
Inches uepth af quickfilvl!r
aH
oYer tbe
nnh',
fu rfelce ,
al
a mean
rat~.
A
.fqu4re .c·olumn ,
of
~uickG lver. '9~
¡nches high, and
,~~e
,"ch thlCk,
\~l!lghs JU~~
1)
paunds, which
is
equal lO
,tn.!
pre[furc af alr
~ pan
cyery
r
~u.Heinch of lhe
¿..
nh's
furface
i
an,1
14
~
times as much. a r 2160 paunds,
UpC.lO~very
fq uare
rO~t;
bec.lufe :. fquare foat contain,
144
fquOire
Inches.
Al
\lus
ral!!.
a
midJle-Gzed m",", whort fur(ace
",ay b. abou,
'4
f9u~re
f<et, furt",",
a, prelfu~e;'f
; .0240
pllunds,
w~en
rhe alr
IS
of a ml!an
g~avily
I a pre{fure whlcp
:wculd be It)fopponable, and even tatal
to
us , w:re it not
t9ual one very part ,
.u~d
ccc rilerbalanced by lhe fpring <.tf the
alr within
us'.
which is
dlfFur~d , l~rough
Ihe
whole
,body,
and re.aéls ,\VHh an equal,ForceagOt,nft lhe ou(ward prclfure
Now fince (,he eillrlh's furface contains '(in round
n~m ·
bers)
:200.000,000' fquare miles, and c.very, fquare miJe
27,878,4°°
fquare feet,
ther~
",uH
~e
5,575
,680000,000,
000 fquare
(eel
on the eanh 's furfrlce
i
which
multiplied.by2160
pound, (the p'elrure on eaeh fqua re foot) gi vcs
12,
043,;68,800 o" o,000,000
pound, for the prelrure or
w<i~ht'
of tue whole
a~mo!vhere.
~
\ Vheo thSend of
J
pipe is immerfed in
~'ater,
and the air
as tak..:o OUt of the pip: . lhc' \'1.1tc r ,\ViII rife in it
tO
the
height of
33
feet abo"e ,he furia" of the wat'er in which it
¡,
irnmerfcd ; but will go no highcr : for it is round . IhM a
,common pump will draw w.uer no higher than
33
reet a_
b~\·c.
the
rurf~ce
of , he \\'ell : .Ind unlefs the
bu~ket
goes
\V1I~1O
lhat
ólfidn.~e
from , he weJl . lhe w:uer wi lJ nLvcr cet
ab~ve
it , N o,,', as it is lhe prd fure of lhe atmorpbere, on
(he furface of lhe U'ñter in the \Vell, th;:at caure, (he water
to a(cend i.n lhe
p~,mr,
ann follo'.V lhe pifion or bucket,
.whcn lhe alr abov!!
It
is lirceú up ; it is cvident• •hOlt a
ca·
J~mn .of walt~r ~3
reet high , isequJI in weigh t tO a columo
or qU.lckfih·er of the fame' dilnletCr
291'
incht. s high ; and to
~s
tlllck a column of air, reaehing from the eanb', furface
lO the top ofthe atmoípbere, S1..e
J-IY.DROSTATIC,.
O,
THE
BAP.Ol'vll::TER.
IN
(erene c:llm
w(,3t~er.
lhe .ir
n~s
weigh r
~nongh
to
(upPOrt a column o( qu,ckr.lver
31
in::hcs hil::h : bur in tem–
p.cfiutlus (lormy we:n her, cm :"ul)ve 28 ¡nches. The C]u¡c!c'
filvn. lhu5 rnpported ·in a J!lars
'ub~.
it;;
founn to be a n:cc
count: rbal~ne(' .
to tllt
w ...
:gHt
or prdTure of Ihe A;r, and lO
Jh~\V
'"
aherltlO" a' diJf" ,nt time.,
Acd
bein¡; ncw ge.
A
T
e
s.
4 RS
nC'T'iJJy uft d to denote the chilngc! in lhe weight óf 'lhc Air,
and
of
l :)C
weather eonlcquent upon lhem, it i5 called
[he
6urom~((I',
or wealher· glar,.
Ti·, 11/u cury
'1·;/1
/ll1nd
al
Jh,[ame
ht!Íghl
eitlur
in
QII
in.
c/rned
6arouu/~r
"
in an
er~él on~,
. Ifthc mcrcury at any ,ime lland.., the height of 30 inche'
'~the
b.rom<ter D , . (Plate CXLV. c,g . 6 .) thenby. incli.
OI~g
thlS baromeler
lnr~
the po(jtion
E,
the
pc: rp~nd
¡cul.lrh"ght ofthe mereury wdl no, be ahered;' for it will IIdl lIand
~~
the height of
30
inches: fo th;, if the 'e"e1 AH i,
30.
IO :hes f'om ,he furface
FG,
the mercury will fland at thi.
leve', t ither in the erel'l tube
O
~ or
in lhe!
inclin~d
one
E~.
N ow here it is
e.,ide~r,
Ih u if
NL
i5 the height oflhe'Oler:
eu ry
wh~n
th('
rube
IS
ereél, aod
NM
is the height of.the
m~rcury
In ·
the f"Ole tube or an equal one when ¡t. is in–
chrred , (here: mufi be:. more mercury io the incliDed tube
than (here is in the ercét one, F or we may conf,der
NL
as
the Gde, and NM.s the diagonal , of a
ri~h,· angJ.d
paralldo.
gramo
Bm
,he diagonal of a righl angled
parallel~gram
is·
Jonger Ihan
the.
(ide. Thert'fore,-Ihotlgh elthtr
L
or
M
are
at
t~e
f,me perpendicular
~ltrr,n,"
froO!
FG,
yet
NM will
be
long~r
llt. n
N~.
Since ¡hen {he columo of mercury
is
longer
10
the I.nclmed
tU
be
Ihan in the creél one, lhere will
b.e
mort mer::urylo lhejoclinedlhan in Ihe'ered one. The q ue'–
fiion therefore i" How thc prdfu e of (he atmurphere ca.Q
fuppon a greattr qU3mity of maUer in one Gtuarion of the
~ub~
rhao
in
lhe olher. W e e.lonot fa y,
¡hat
though in Ihe
lnehoed IUI)e there i5 a gre';:aler q uaolity of mercury Ihan
in
the crea one,
~et
a
pa.reof this greater weight
will
be fup_
poned by tl'e (,de o( the tube as
I,y
.n iucllOed pl,ne. The
lrue anfwcr
¡St
tha! the eoJumn of a:r which rupporu the
me~cury
in lhe inclioed tl.lbe,
is
greater lhao Ihe coJumo
wl)1ch ftlpporu it in lhe eretl one
The heigh, of 1he ca·
lum of air is i,ndeed lhe
(~nle
in bOlh cafes · (or in eithe-r
caf,
it
i, <qua l t<, the h<ight of the ¡ imofpher:. B ut , he baf.
ofthe columo of air, and confeq uendy i1S weigh!,
is~reale.r
when {he tube is incl'ned lb",n when il is crerl. For the
bare o.f '
I.hé:..:olulOn 'of air which fupports lhe mercury in lhe
tube,
IS
equ<l1 to as mueh of 111(' llagn2n't mc rcury's
fUI
face
a.s
rhe bJfe of the lul:-e covers ,
No\V,
if lhe di"melers of the
,ube, D aod E 3re equa' ; ,he bare of the inchned ,ube E
will cover a greélter pan of the fur(ace FG· th",n Ihe ereCt
tube
D
covers, or the barc of the t"ube
E
\ViII be grea ter
th, n ,he b,fe of the tube D . For th< contents of the in–
cJioed cubc are gre;u er thim lhofe of Ihe ereét one, as has
beeo
"lhe,vn
a'lrea~y-:.
But Ihe colurrin' of mercury in e;:ach
of the ,ubes are cyhndea of the fal1'o height .. Therefore
.he" baf., are
u
their eontentS . F.u• .
~ :
XI!. prop.
J
r.
Since (hen Ihe COOlents or lhe: weighls af n¡ercury in each
tube H e as their
b¡¡[fS,
wh~n.
Ihci r heighls are equoll; anti
the hafe of lhe column oral r, which....fuprorts Ihe mercury ,
aod conrequently the wt"il!ht of Ih is column
l •
is prc portion..l
t?
th~ b~fe
of the tube; it follo\\'s, that the
~eight
of lhe
;ur wIll aJways be proportion",1 tO_ lhe wt:ight of lhe nler·
cury when
it
ftaDds at a ¡;iven height, whtthcr lbe,lube
Is
';nclincd or erctl·.
Thou~h
we have here (h'ewo, th:lt the Contenu of lile in·
cJincd tube are gre:uer than Ihofe of the ere{t one, Rnd con- ·
f<qu~ntly
th•.t their bafe, muJl be unc·qu. l, Gnc< ,hcir per–
pendIcular hClghls are lhe f.une
~
yM
it will not be impro.
per
10
nlew wh;:at we me;¡ n
by
the bil re of Ihe ,indined tube.
or' ra1he-r of
th~
inclined columo " f 1'¡1ercurYt anJ'
~·hy·
,h;s
Ibculd be grc.ter than tbe ba:e of tbe ere(\ on,. N olV
by
tIu: ,