The Theory of Electrons And Its Applications to the Phenomena of Light And Radiant Heat; a Course of Lectures Delivered in Columbia University, New York, in March And April, 1906
The book The Theory of Electrons And Its Applications to the Phenomena of Light And Radiant Heat; a Course of Lectures Delivered in Columbia University, New York, in March And April, 1906 was written by author Lorentz, H. A. (Hendrik Antoon), 1853-1928 Here you can read free online of The Theory of Electrons And Its Applications to the Phenomena of Light And Radiant Heat; a Course of Lectures Delivered in Columbia University, New York, in March And April, 1906 book, rate and share your impressions in comments. If you don't know what to write, just answer the question: Why is The Theory of Electrons And Its Applications to the Phenomena of Light And Radiant Heat; a Course of Lectures Delivered in Columbia University, New York, in March And April, 1906 a good or bad book?
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120. Before coming to solutions of our system of equations, it will be well to go into some details concerning the cause by which the absorption is produced. We have provisionally admitted the existence of a resistance proportional to the velocity of an electron, which is represented by the terms —'J-f., —g-ri, ~9^ in (198) '' cit (it dt and by the terms i/3P^, jj3P,^, ijiP^ in (204). It must be observed, however, that in our fundamental equations there is no question of a resistance of this ki...nd; as we have formerly seen, an electron can move for ever through the ether with undiminished velocity. In our RESISTANCE TO THE MOTION 141 considerations we have come across only one force that may be termed a resistance, namely the force which is proportional to the rate of change of the acceleration. In the case of simple harmonic vibrations, its components can be re- presented in the form (197), with the following value of the coefficient ^=S- (206) Some numerical data which I shall mention later on, show however that this force (205) is much too small to account for the absorption that is really observed in many cases.
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