The Kinetic Theory of Gases Elementary Treatise With Mathematical Appendices
The Kinetic Theory of Gases Elementary Treatise With Mathematical Appendices
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In our eReader you can find the full English version of the book. Read The Kinetic Theory of Gases Elementary Treatise With Mathematical Appendices Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book The Kinetic Theory of Gases Elementary Treatise With Mathematical Appendices
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Let a fluid, whose depth is equal to the unit of length, move over a horizontal plane, and let its motion have become stationary and be of such character that all the particles in the same horizontal plane have the same velocity. A necessary consequence of this is that the velocity is given by a linear function of the height above the base. For in this state of motion each layer experiences on its two sides equal and oppositely directed friction, so that no change can occur in the velocity of a... layer. If we further assume that the lowest layer sticks fast to the base, and that, on the contrary, the highest layer has such a velocity that it moves over unit length in unit time, so that the speed in each layer is numerically equal to the height, then the friction on unit area which is exerted between any two neighbouring layers of this fluid is equal to its coefficient of viscosity.
The measurement of the internal friction of a medium consists in the determination of the value of this coefficient ; it is a constant magnitude if Newton's assumption that the friction is proportional to the relative velocity is really true.
What to read after The Kinetic Theory of Gases Elementary Treatise With Mathematical Appendices?
You can find similar books in the "Read Also" column, or choose other free books by Oskar Emil Meyer to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Let a fluid, whose depth is equal to the unit of length, move over a horizontal plane, and let its motion have become stationary and be of such character that all the particles in the same horizontal plane have the same velocity. A necessary consequence of this is that the velocity is given by a linear function of the height above the base. For in this state of motion each layer experiences on its two sides equal and oppositely directed friction, so that no change can occur in the velocity of a... layer. If we further assume that the lowest layer sticks fast to the base, and that, on the contrary, the highest layer has such a velocity that it moves over unit length in unit time, so that the speed in each layer is numerically equal to the height, then the friction on unit area which is exerted between any two neighbouring layers of this fluid is equal to its coefficient of viscosity.
The measurement of the internal friction of a medium consists in the determination of the value of this coefficient ; it is a constant magnitude if Newton's assumption that the friction is proportional to the relative velocity is really true.
What to read after The Kinetic Theory of Gases Elementary Treatise With Mathematical Appendices?
You can find similar books in the "Read Also" column, or choose other free books by Oskar Emil Meyer to read onlineMoreLess
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