e
H E
s
T
R
Y.
~I
,hey nre rario"ny altercd by ,heunior.s ,he)' havc coo·
,'a,qed lI'i,h rer,aio priociples of ,'egetables
anu
aoiOlals,
01'
",hich oo,hin" has becn ye,
f~io,
i, is proper 'o
def~r
~cing
panieuhrbeonceroing ,hem, ,il!
\Ve
hal'e explained
,hofe principies.
O/ L
1M,:.
Ihe lime
10
form wi,h il a while liquor, Ihis liquor il
called
lae ca/cil;
which, beiog left fome lime' lOfeltle,
grows ele., aod traofpareol, ,he lime whichwas fo fpend.
ed thereio and occafioned iu opacity fubfidiog
ro
rhe
botlom of ,he velrel. Then Ihere forms on Ihe forfaee
of Ihe liquor a erynallioe pelliele, fomevÍhat opaque and
dark eoloured, whieh being Otimmed off is reprbdoceJ
from ,ime 'o ,ime. This mamr is calleJ
cr,mor ca/eh .
.fINY
f"bnaneewhatevrr. ,hat has beeo roanea a con.
fi,lnablc ti:ne io
a
flrong fire witlw", melting, is eom'
OIonll' ealled
~
ca"-
Stones aoe! merals
are
,he princi·
p,1
fuhj cas th" have the properry of being converted io'
t"
calca.
We
0".11
treat of metalline
calm
in a fubfe·
quent ehapter, and in ,his eoofine ourfelfes to the
co /x
of
jlo".,
knowo by the name of
lime.
In treating of emhs in geoeral, we obferved thal ,hey
mal' be divieled inlo tWOpriocipal kiods ; ooe of which
aélually aoo proped)' flows wheo
expof~d
to ,heaélion of
lire, aod turos tOglafs; wheoce it is called
a
(/ljihle
or
vi/rifah/,
earrh; the olher refins ,he mmor, force of
fi re, aod is Iherefore faid lObe ao
unjujihle
or
tlnvi/rif·
abl:
earrh The Imer is alfo
001
uncammonly called
calcinable
emh; Ihough fundryfofts of onfufible earths
aTe incapable of acquiring by· ,he aaioo of fire all the
qUlli,ics of
ealeit",1
emh, or
lim,
properly fo called :
¡l,,:h ear,hs are parricularly dininguilhed by the
deo~mi·
o. tion
01'
,,(raflor)
eanhs.
. As
rl!~
d.ffm ot fons of nones are oothing more ,han
rum~nunds
of Jiffereot earrhs, ,hey have ,he fame pro·
pe.
[i,s with ,he e:mhs of whieh they are compofed, .od
mIl', like ,h,m, bedivided ioto fufible or .i"ifiable; and
unfu!ible orcalcinable. The fufib!e flones
are
generally
¿, outed by the name of
Jlin/I ;
the cakioable nones, ••
gai n, are the fel'erol Cons of marbles" cretaceous flones,
thoCe commooly called free.nones,
&c.
fome of whieh,
'as ,hey mJke ,he ben lime.
are,
by '\Vay of emioeoce,
callcd
lim:jl1neJ.
Sea·Olells alCo, and nooes th.. , .
bound ",ith foflile Ihells,
are
capable of being burot tO
lime.
AII
Ihefe {ubnaRces beiog expofed for a looger or
(horrer time 'o ,he , ioleot aNion of fire, are fai d lO be
""tcirud.
By calrio..ion [hey lofe a eoofiderable part of
their weighr, acquirea whireeolour, and becomefriable,
Ihough ever fo folid before : as, for ionaoce, the very
harden marbles. TheCe fubllances, wheo thus calcioed,
tak~
,heoame of
quid·lim,.
Water peoetrates quick.lime, and ruOles into il wilh
vall aélivi,y . If
a
lump of newly ealcioed li\De be ,hrowo
i"to water, it io!laody exciles almon as great a ooife, e·
bullirioo, and fm6ke, as would be produeed .by a piece
of red·hot iron; with fuch a degree of heat lOO, ,hat, ir
Ihe limebe in due proportioo 'o the wa,er, i, will fel fi re
tO combuflible booics; as hath uoforrilOa,e1y happeoed
tO vdTds ladeo wilh quick lime, on their fpringiug a
fmalll<ak.
As foon as quick·lime is pu,
iO.lowater, i, fIVells, aod
falls ,funder intu ao infioite number
01"
m:oute partides :
io • \Vord , it is in a manner dilrolv.d by the water,
which forml therewith a fort of \Vhile palie called
jlaeJ..
d' limt .
If the qu, o,ilYof Water be confiderable eoough fot
Slacked lime gradually grows dry, aod takes ,he form
of a folid body, bot foil of craeks and
den"ot~
of
h~m.
oefs. The eveot is diffcrenl wheo you mix,il up, while
yel a palie, with a cenaio quaoti,y of uoe,lcined flony
mamr, fuch as faod for example: ,hen il takes ,heoame
of
mor/ar,
and gradually . cquires, as il grows drier aod
older, a hardnefs equal to Ihat of the bell nones. This
is a very fiogular property of lime, oor is i, eafy lO ac·
COIlOI for il; but il is a beneficial ooe, for every body
koows the ufeof mortar io buildiog.
~ick.lime
amaéls ,he moiflure of ',he air io Ihe fame
manner as conceotrm d aeiels aod
~ry
fixed alkalis, bUI
001
io fuch qllanti[ies as 'o render it fluid: it ooly faJls
ioto extremely fmall partieles, takes ,he form of
a
filie
powder, aod ,he titleof
IiM
jlacJ.,d in
~he
airo
Lime once flaeked, however dryil may afterIVardsap'
pear. allVays
retai~s.
large portioo of
rh~ wat~r
il h,ld
imbibed; whiehcanOOI be fe paraled from
11
agalO bUI by
meansof aviulcnl cafeioarioo. Being fo reeakined il re·
iuros
10
be quid· lime, recoveriog all i,s properties.
Refides this grw aflioity of quick.lirue wilh water,
whieh difcovers a falioe charaélcr, it has (everal other
faline properries, 'o be afterwards examined, much re·
fembliog ,hofe of nxed alb lis. lochenllflry il aéls Tery
oearly
~s
thofe (al" do, aod mal' be eooliJered as hold·
ing the midole ronk betweeo apure abforbenl
ear~h
and
a fixeo alkali ; aod this hath indoced many chemlns tO
Ihink ,hat lime eontains atrue fah, tOwhich all thepro·
penies it polrelrcs io common wirh (ahs ml y be ami·
bUlcd.
But as the
chcmic~1
ex.minariou of ,his (ubjeél halh
loog been
oegl~éled,
,he exiflence of a faline fubllaoee io
lime harh been loog doublful. Mr du Fay was ooe of
the firn who obtained a falt fr"m lime, by lixivi..iog il
wilh
a
great deal of water, which he afterwards evapo..
rated. But the quami,y of (. h he obtaiord by thar
meaos was verv fmal! ; nor was il of ao alkalioe oature,
as one would thiok it OlOuld have beeo, coofideriog ,he
propenies of li·me. Mr du Fay did OOt carry his expe·
rimeots
00
this fubjeél any futl her, probably for want
of time; oor did he determioe of what oatUre the falt
was.
Mr Malouio hád ,he curiofity tOexamine Ihis (al, of
lime. aod foon found ,hat it was nothiog elfe bu, what
was above ca\led
cmllor c," ciJ.
He found moreover,
tha" by mixiog a fixed alkali lVith lime·water, a vitriol·
md tartar IVas formed; Ih.., by mixiog therewith ao
alkali !ike Ihe bafis of fea·falt. a Glauber's f,h
W3S
pro·
rloced; aod, hntv. by combioing lime wirh a fubflance
abouodiog in phloginoo, he oblaiocd atrtle fulphur. The(e
"ery
io~eoious
experimeots prote ro ademoonratioo, rhar
Ihe vitriolie acid connitutes rhe f. lt of lime; for; as hath
beea lhewD, no olher acid
i.!
capable of forming lu,b
CODlbl'