Table of Contents Table of Contents
Previous Page  557 / 868 Next Page
Information
Show Menu
Previous Page 557 / 868 Next Page
Page Background

P L U

is Ict to

r.::n,

;.n.:l the exaél: poiat

wncre

il

rcfh

is markcd

with

a ven:

ht; Ihc:o goes

0 0

f" rthef in the line Udl fallen·

eJ, and a. th'!

n c XI

flexure

or

toe adi l he makes a mark

on the lioe

by

a knot or

ot herwir~;

and then lt:tling clown

the di.!.!

a¡;din,

'he there l.kewife

nOtes

down t hat poi nt a!

which Ihe nccJlc It.lnds in this [ecund pofilion.

[o chis

m. nner he proceeds, from turni ng

10 lu rning.

m;ukinc

do",,'" thc:

POil"ltS,

¿nd mai king the li ne,

tiJl

he comes

10

the intl!odcd place :

chis

dune, he

arC~nd5J

and btgins to

wo:k on

th~

furface of the

eilnh

wh~t

he did in Ihe adit,

hri nging che fi rrt knot in the

lioe

10

fuch

a

p)..tce .wl~e re

Ihe ol.lrk of

th~

place of Ihe need le \1,:11 2gain

anr~ver

its

pvint ing. and continues this till he come

10

the defired

p1:tce above

ground,

which is cen ai n

lO

be

perpe~ld!cu~

hrl y

over

the

pan

of

the mine into

which

th~

airJ1Hrt is

' o

be fu roL

PLUMOSE , fJ me,hing formed in ,he m' nner or.. fe . ther,

p

N

E

u

M

T

HIS

fl:ienee

treats of

(he

nature,

weigtlt ,

and prdfure

of the

air,

and

tne effl'tls

arifin g

from

it.

T he

air

is

th.tt

thin

trd.nfpdreot

fluid body in which

we

Jíve

and

breal he ...

lt

encompJffcs

thl! wholc

earth to a conu·

dcrablt!

hei~h t

j

and o

tOgether

wirh

the cloud:; and

vapours

lh t O, . , in it, is ealled ,he .. mofphere. T he .ir is j "íJly

recko.1ed

among lhe number of 8

.ids,

becaufe

it has a1l the

propen ies by which • fl uid is dillinguirn, d . (See HVOR O–

ST AT' CS .)

For i, yiel'ds tO ,he le"(\ force impieffod, its

pans are eafily moved amoog one another,

it

prdf: s ac–

lording

tO

in perpendicular

height,

and

its

prdrure is

every

", .yequal.

11lat

the

air

is

a

fluid,

confifiing of fuch pan iclcs a,

h:\\'e

na

cohdio~

belwixt

Ihem ,

bUl eafily

glidl! over one another,

4ind yieJd to

lhe

Oighteft impreffion ,

appe4.rs

from

th:ll

eafe

and

freedoól with

which aniOlals

breathl!

iD

il. and move

th ro"gh

it

wi,hoUl.• ny diílieulty or fenGble

reGHar.ce

.

Bo, il.d;(fe" frottl . 11 o ,her flo ids in Ihe th ree following

r aniculars . 1t

can

be

eomprelTcrl

¡nlo

a

lefs fpace

lhí\n

what

. ic naluraliy poffeffeth.

~hich

no olher fl uid

call .

2.

h

can~

not

be congeaJed or fiKCd,

as

other

fl uid s

mayo

3. It

is

or

a

difFc:renl

denfi ty

in

every

part,

upwai"d

from lhe

ean h's

Cur~

l¡tce, deerealing

i~

in

weight. bulk

for bulk, the

higher ít

r ifes; and theref" re

m~(l

al lo deere. fe inden fi, y. 4 ..

lt

is of

án

elaClic

or

Cpringy

nature,

and

the force of ilS

Cpríng

is e·

q ual lO

jn

weight.

Th:n air

is

a

b ody,

is evi": ent from

¡ts

exelud¡"'

hg all oTher

)jodies out of ,he fpaee it poff, ffcs ¡ for, if .

gl.fs

· jar be

plcnged

wi th it; mOlHh

tlownward

iuto a

vd fel

of

water,

tliere

will bUI very

little

waler gel iOlO

the

jar: becaufe

the

air of

",hieh

it

is

full

keeps Ihe waler out

. As air is a

bod y, ir

mua

needs

ryOlve

gra \·ity or weight

f

~nd

lhu

it

i,

weighty.

i,

demonflr,lIed

by

expt:riment.

For,

Jet .he air be

ukf!n

om of a veffd

by

means of

the

air-pump ;

, henoha, ing

wei~hcd

the

vecrel, let in

Ihe

:lir

ag~in ;

and

upon

w('i~:h i ng

it,

when

rc-.fi

lJed

Wilh

airo it \ViII be found

¿onfidtíaL.'y

h~.t9ier ,

Th'.ls,

a botde lhat

holds

a wine

qu<t rt,

b~i ng

emptjcd

of

::ir,

and

wcigh ~d.

is f'ou nu lobe a:–

b-;"Ul

1,7

grains

li~h t<.r

lhao

when lhe ai r is I:!l i:lloit 3&1io ;

"...,hit:h Ih,;V/s

tI..

"t

a

cpprt

of

eir

weighs 17 graios.

Dut

a 'lUlrt of W,ler

wc:~hs

14625 s raios ; ,his diviJed by

lo

P L U

wilh

a (l e;n

and libres

ifT'uing

from

ir

on each

{ice

~

fuch

are (he antenoa: of certain

mOlhs, bUHerfiies,

&e,

PLURA

r.,

in brammt\ r, an

epi lhel

;:¡ pplied

to

th;u ncmb<r

"f

nouns

and

verl s

which is uli:d

when

w:

fpeak of more

Ih.lO

une

thing. See

GRAto1MAR.

PLURALI T Y. • difere,e 'Iu.n,i,y, co"r,Oi ng of

,\vo

or a

greatt r

number

o" tbe folme kind

j

Ihus

w t:

fay

a pluralilY

of gods,

&c.

PLUS, in . Igebra,

a

eh.r.n"

mar~ed

,hu.

+,

ufed for the

lign of addi,ion.

PLUSH, in eommeree,

&f . •

kind ¡'f ¡¡ uff

h..

ing

a

for'

of velve, kn.p, or (h' g. on on< fid e, compo(cd regul.r1y

of a woof of a

(jr~le

wooleo

thread, and "

double \V2rp;

the

One

w.)o!, of

l WO

thre:\ds twifted;

lhe other

goals or

cltmcls h3ir;

though there

are fome plllfhes

emir ely

of

worf!ed.

, ñ:l

o,h~rs

eo:npofed wholly of hair.

PLUVfALIS , in zoology. See eH'ARAD RI vs .

A

' l .

e s.

t

7.

quotrs 860

in

round

numbers; whirh

fh ews,

Ihal

water is 860

times as

bea\'y

as

¡ir

oear

lhe

fu rface

of the

earth .

As

lhe ai r rifeS above

the eatth's

fu rfaee.

ir gro\\'S ra·

rer,

.n~

eonf<qllentfy lighter, bulk for bu'k . F or r,nee i, i'

of

a.n e);t[tic

or

fpringy nature, and

¡es

lowe rmo(l part! are

prdTed

with the- weight

ofi all

thJt

is abo\'e them. il is

plain

tirat the

ai r

muH

be

mere

den

fe or comp

\ét

at

<{he earl h's

fu rface, than at any height above

it;

and

graduaJly raler

,he higher up. F or, the denfi,y of ,he . ir is alw. ys "

the

force Ih"t

comprelrelh

it :

and

thercfore ,

lhe

¡ir

te·

wards

the u'pper

pa ru

of

lhe atmo(phere beir.g ters pre(s.

ed

th.m th,il

'w hict\

is

near lhe eanh ,

it

will

expl od ¡Ifelf,

and thereby

become

IhinnN lhao

al

the (uTface of lhe earlh.

Dr

Cotes

h3S demonnrated, tbat

if

altitudes in'

the

Olit

b'!

taken

in arithmc[icdl

propon ion,

~rhe

rarity of tb: air

will be in

geometricd.1 proponion,

For ¡nnance,

r

71

~

(

.

41

I

~ ~'¡:i

l . ..

~~

\

u

28

1

-5

I

.

25 6

1-=

'\ 35

10 2

4

"

4

2

-5"

I

.

4

0

9 6

1

~

t...

49

E

.

r638 tl

-=

:

56 1

u

65 536 1'

t

~

:...

~~_

63

~

I

262 1-1 4

~~

=

70

o

10485i6 ¡:'=:2

77

r

~ ~

4

1

9 43°4

2! .~

-5

84

~

I

167772 16

~ ~

<

9 1 2 ,

.

67 108 864 1

~~

\ 98 1-5 \

268

43545 6

:a

. ' 05

u .

10

7374 182

4 -

l

it

2

:;

I

42 94~67 2'16 1 ~

11 9 \

~

17' 79

86 9,84

·5

126. ::

6 8 7

194i 6 73 6 \

1 3 ~

I '§

2H S 7790 6 9 44

ll 40 )

L

1° 99 5

11 62

777

6 )

Ana

hene\!

it

is eafy

tO

prove

by

calcul.u ion, rh;¡ t a ell"

bic ineh of fu eh air as we brealhe, wOll ld be

fa

much

riHe–

fied

2'

,he alt;tude of 500 miles. th. t il " ould !ill a Ir- her •

t'l"' !

io di. meter to ,he orbit

o~Sa'urn.

Th: