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c 3g 2<br />
denfeit P<tcr may always endcavour to apyroach<br />
the Center of the Particle: So that a<br />
Particle of’ Salt may be compared to a Chaos ;<br />
being denfe, hard, dry, and earthy in the GUIter<br />
;’ and rare, ibft, moift, and watry in. the<br />
Circumference. And hence it feeems to be that<br />
Salts arc of a Ming nature, being fcarce def’~:ro~r’d<br />
5 ~nlef~ by drawing a\Vay their Wacry<br />
Parts by violence, or by letting theill fo& into<br />
the Pores of the central Earth by a gcnrle E-&WI<br />
in Putrcfa&on, until theEarth be dillblved b17<br />
the Water, and i‘eparzated into t&Her Pn~ticlcs,<br />
which by r&on of their fmallnefs make the<br />
.rotten Compound appear of a black Colour:<br />
Hence nlfo it may be that the Parts of Atlinlals<br />
and Vegetables preferve their feveral For~ns,<br />
,and afl-Slate their Nourifllment ; the fof’e and<br />
moiit Nourifhmen t e&p changi !;g its Text cn-e<br />
by a gentle Heat and IiJlotion, till it becomes<br />
like the denie, hard, drv, and durable Earth<br />
in the Center of each Pal~ticle. Rut when the.<br />
Nourifllmcnt grows unfit to be alGmilat4, or<br />
the central Earth grows too feeble to aff imilate<br />
it, the Motion ends in Confuiion; Puerefi&ion<br />
and Death.<br />
If a vesy fmall quantity of any Salt or Vitriol<br />
:be diffolved in a great quantity of Water 3 the<br />
.Particles of the Salt or Vitriol will not filik to<br />
,the bottom, though they be heavier in Specie<br />
‘than the Water, but will evenly diffufe them-<br />
.Ifelves into all the Water, fo as to make it as faline<br />
at the top as at the bottom. And does n&t<br />
.this imply that the Parts of the Salt or Vitriol<br />
recede from one another> and endeavour to expand