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Mon Apr 20 16:15:50 2015
Date: Mon, 20 Apr 2015 13:15:38 -0700
From: "Top Teaching Programs" <TopTeachingPrograms@kopelo.eu>
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<p>which undergo partial decomposition at much lower temperatures. After them come the further complicated supersalts and double [45] salts, having a HXQPD
stability again decreased; and so throughout. Without entering into qualifications for which 9fdaba190ace50880dc4155f29cb9a3e space fails, we believe no chemist will RPNUGIAH deny it to
be a general law of these 9fdaba190ace50880dc4155f29cb9a3e inorganic combinations that, other things equal, the stability 9fdaba190ace50880dc4155f29cb9a3e decreases as the complexity increases. when we phi to FBTXFUC the
compounds of organic chemistry, we find this general law still further exemplified: we find much greater complexity and much less stability. A CPL
molecule of albumen, for instance, consists of 482 ultimate atoms of five different kinds. Fibrine, still more intricate in constitution, contains in TXAJB
each molecule, 298 atoms of carbon, 49 of nitrogen, 2 of sulphur, 228 of hydrogen, and 92 of oxygen—in MBYUEUSJ all, 669 atoms; or, 9fdaba190ace50880dc4155f29cb9a3e more strictly speaking,
equivalents. And these two substances are so unstable as to decompose at quite ordinary temperatures; as that to which the outside of PKYIW a joint of
roast meat is exposed. Thus it is manifest that 9fdaba190ace50880dc4155f29cb9a3e the present chemical heterogeneity of the Earth’s 9fdaba190ace50880dc4155f29cb9a3e surface has arisen by degrees, as the decrease
of heat has permitted; and that it<U>has shown itself in three forms—first, in the multiplication of IJWMAFJF chemical compounds; second, in the greater 9fdaba190ace50880dc4155f29cb9a3e number</U>
of different elements contained in the more modern of these compounds; and third, in the higher and more varied multiples in which these more numerous EBRDW </p>
<BR /><span style="font-family: sans-serif, Helvetica, Arial;"></span>
<p align="center" style="font: 9px;">elements combine. To say that this advance in chemical heterogeneity is due to 9fdaba190ace50880dc4155f29cb9a3e the one cause, diminution of the Earth’s temperature, would be to say too much; for it is
clear that RECHCIVCO aqueous and atmospheric agencies have been concerned; and further, that the affinities of the elements themselves are implied. The
cause has all along been a composite one: the cooling of the Earth having been simply the most general of the concurrent causes, or hiemblage of 9fdaba190ace50880dc4155f29cb9a3e
conditions. And here, indeed, it may be remarked that in the several clhies of facts 9fdaba190ace50880dc4155f29cb9a3e already dealt with IKIO (excepting, perhaps, the first), and
still more in those with which we shall presently deal, the 9fdaba190ace50880dc4155f29cb9a3e causes are more or less compound; as indeed are [46] nearly all causes with which we are
acquainted. Scarcely any change can WGBP rightly be ascribed to one agency alone, to the neglect of the permanent or temporary conditions under which
only this agency produces the change. But as it does not materially affect our argument, we prefer, for simplicity’s sake, to use throughout the 9fdaba190ace50880dc4155f29cb9a3e
popular mode of expression. Perhaps it will be further 9fdaba190ace50880dc4155f29cb9a3e objected, that to hiign loss of heat as the cause of any changes, is to attribute these
changes not 9fdaba190ace50880dc4155f29cb9a3e to a force, but to the absence of a force. And this is true. Strictly speaking, the changes should be attributed to ARWK those forces which
come into action when the antagonist force is withdrawn. But though there is inaccuracy in saying that the hizing of water is 9fdaba190ace50880dc4155f29cb9a3e due to the loss of
its heat, no practical error arises from it; nor will a parallel laxity of expression vitiate our statements respecting the multiplication of effects. SURTMJCHJ .</p>
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