SEC. VII1.I OF NATURAL PHILOSOPHY. 367 with which the lincola EG is urged in the places P and S is to the weight of that lineola as HK X A to V X EG ; or as PO X A to VV; because HK was to EG as PO to V. Therefore since the times in which equal bodies are impelled through equal spaces are reciprocally in the subduplicate ratio of the forces, the time of one vibration, produced by the action of that elastic force, will be to the time of a vi bration, produced by. the impulse of the weight in a subdu plicate ratio of VV to PO X A, and therefore to the time of the oscillation of a pendulum whose length is A in the subduplicate ratio of VV to PO X A, and the subdupli cate ratio of PO to A conjunctly ; that is, in the entire ra tio of V to A. But in the time of one vibration composed of the going and re turning of the pendulum, the pulse will be propagated right onward through a space equal to its breadth BC. There fore the time in which a pulse runs over the space BC is to the time of one oscillation composed of the going and returning of the pendulum as V to A, that is, as BC to the circumference of a circle whose radius is A. But the time in which the pulse will run over the space BC is to the time in which it will run over a length equal to that circumference in the same ratio; and therefore in the time of such an oscillation the pulse will run over a length equal to that circumference. G,.E.D. COR. 1. The velocity of the pulses is equal to that which heavy bodies acquire by falling with an equally accele rated motion, and in their fall describing half the alti tude A. For the pulse will, in the time of this fall, sup posing it to move with the velocity acquired by that fall, run over a space that will be equal to the whole altitude A ; and therefore in the time of one oscillation composed of one going and return, will go over a space equal to the circumference of a circle described with the radius A ; for the time of the fall is to the time of oscillation as the radius of a circle to its circumference. COR. 2. Therefore since that altitude A is as the elastic force of the fluid directly, and the density of the same inversely, the velocity of the pulses will be in a ratio compounded of the subduplicate ratio of the den sity inversely, and the subduplicate ratio of the clastic force directly.