Boyle, Robert, New experiments physico-mechanicall, touching the spring of the air and its effects, 1660

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              from pumping) by the bare application
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              of a hand moderately warm to the deſert­
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              ed part of the Tube, the remaining Wa­
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              ter would be ſpeedily and notably de­
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              preſſ'd. </s>
              <s>And having for a while held a
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              kindled Coal to the outſide of the Tube,
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              (the Pump being ſtill unimploy'd, becauſe
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              the Veſſel chanced to hold extraordinarily
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              well) the Air was by the heat ſo far ex­
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              panded, that it quickly drave the Water
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              to the bottom of the Tube, which was
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              divers Inches beneath the ſurface of the
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              ambient Water. </s>
              <s>Whereby it appears (by
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              the ſame way by which we formerly mea­
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              ſur'd the dilatation of the Air) that the
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              Air, even when it is expanded to between
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              90 and 100 times, its extent will yet rea­
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              dily admit of a much further rarifaction
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              by heat. </s>
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              <s>I conſider'd alſo that in caſe the Bub­
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              bles we have been ſpeaking of, were pro­
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              duc'd by the parcels of Air latitant in the
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              Water, that Air being now got together
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              to the top of the Tube, though the Air
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              were again drawn out of the Receiver,
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              the taking off its preſſure would not diſ­
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              cloſe bubbles as before; and accordingly,
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              the Air being again pump'd out, the Wa­
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              ter in the Tube deſcended as formerly: </s>
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