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A similar conclusion can be obtained by consideration of the affinity andstability of chemical compounds. Beginning with the complex nitrogenous compoundsof which formed the living creatures and which, in the history of the Earth essencelater and however, the most heterogeneous, we see that both the affinity, the stability of them are extremely small. The particles do not enter into chemicalthe connection with particles of other substances to form a morecomplex compounds and their constituent parts when normal conditions are often notcan stick together. Beneath the composition there is a great numberoxygen-hydrogen-carbon compounds, a large number of whichshow a positive commitment to and connection with ordinarythe temperature steadily. Passing to the inorganic group, we find the saltsand other compounds of greater affinity between the constituent parts andcompound, which in most cases is not easily decomposable. And then, reachingto oxides, acids, and other double compounds, we find that in manycases, the elements of which they consist, being close to each other,under favorable conditions connected with high energy and that many of themcompounds do not decompose through one heat. So, if, returningback from the latest and most complex substances to the most ancient and simplestsubstances that we see in General a great increase in affinity and stability,this means that if the same law applies to the very simplesubstances which are known to us, it can be assumed that the constituent partsthese substances, if they are complex and connected as a result of much moreaffinity than what we know, and that the degree of sustainability of their farbeyond sustainability, which introduces us chemistry. As a resultit is possible to assume the existence of a class of substancesindecomposable and therefore seem simple. The conclusion is that these substancesformed in the early periods of cooling of the Earth with such heat andsuch pressure, the degree of which we currently can't do anythingto compare it to.
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