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its compounds were the only known source of these new radiations, but many other substances were examined and two years later thorium and its compounds were added to the list. In general the discharging action seemed about the same. Other elements and ordinary substances show a minute activity. Only potassium and rubidium have a greater activity than this, and theirs is only about one-thousandth that of uranium. An Atomic Property In the examination of uranium and thorium compounds it was found that the activity was determined by the uranium and thorium present; it was proportto the amount ofional these elements present and independent of the nature of the other elements composing the compound. The conclusion was, therefore, that the activity was an inherent property of the atoms of uranium and thorium, that is, an atomic property. This was a long step forward and introduced into science the conception of a new property of matter, or at least of certain forms of matter. Discovery of New Radio-active Bodies In examining a large number of minerals containing uranium and thorium, Mme. Curie made the important observation that many of these were more active than the elements themselves. In measuring the activity she made use of the electrical method which will be described later. In the following table giving her results for uranium minerals the numbers under _i_ give the maximum current in amperes. They serve simply for comparison. _i_ Pitchblende from Joachimsthal 7.0 x 10^{-11} Clevite 1.4 x 10^{-11} Chalcolite 5.2 x 10^{-11} Autunite 2.7 x 10^{-11} Carnotite 6.2 x 10^{-11} Uranium 2.3 x 10^{-11} Uranium and potassium sulphate 0.7 x 10^{-11} Uranium and copper phosphate 0.9 x 10^{-11} The last three are pure uranium and compounds of that element given for comparison with the first five, which are naturally occurring minerals. The last compound has the same composition as chalcolite and is simply the artificially prepared mineral. It has the activity which would be calculated from the proportion of uranium present, the copper and phosphoric acid contributing no activity. Since the activity is not dependent upon the composition but upon the amount of uranium present, the activity in all of the minerals
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