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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from ...Show synopsisThis historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1893 Excerpt: ...movements of adjoining particles. Hence, although the path in space of each particle will be hyperbolic, the evidence of movement will indicate relative transfer of adjoining particles in opposite directions along lines of maximum tangential strain. The energy of this relative movement will evidently increase with the excess of the pressure above the limit at which flow begins, sometimes called the limit of solidity. Thus, if one supposes the pressure suddenly to surpass the limit of solidity and then to be kept constant, the mechanical effects of the relative motion (and the chemical effects attending the expenditure of energy) will be very pronounced on the lines on which flow begins." As the process continues and the stress diminishes with the increase of the area of the mass, the lines first affected will make an increasing angle with the line of force, while the new fibers of the material which are forced into the direction of maximum strain will be less and less affected. The result will at least resemble schistose structure and will be marked by the presence of lines of relative movement intersecting one another at very acute angles. In the case of direct uniform pressure there will be four such sets, each set at a large angle to all the others. If the load were to increase in the same proportion as the area of the loaded mass, so that the stress would be kept uniform, an indefinite amount of flow might be produced, provided that the rock is not hardened During flow there is no progressive change of volume. Hence, a point for which at the inception of flow x--1, y =. 1, will be moved to a point x', i/, and x't y' = 1. The curves of this form are sometimes called the lines of flow They would be more aptly called lines of absolute movement. They s...Hide synopsis
Finite Homogeneous Strain, Flow and Rupture of Rocks (1893) (Kessinger Publishing) – Hardcover (2010)
by
George Ferdinand Becker
Hardcover, Kessinger Publishing 2010
English
84 pages
ISBN: 1162087528 ISBN-13: 9781162087528
This scarce antiquarian book is a selection from Kessinger Publishing's Legacy Reprint Series. Due to its age, it may contain imperfections such as marks, notations, marginalia and flawed pages. Because we believe this work is culturally important, we have made it available as part of our commitment to protecting, preserving, and promoting the world's literature. Kessinger Publishing is the place to find hundreds of thousands of rare and hard-to-find books with something of interest for everyone!This scarce antiquarian book is a selection from Kessinger Publishing's Legacy Reprint Series. Due to its age, it may contain imperfections such as marks, notations, marginalia and flawed pages. Because we believe this work is culturally important, we have made it available as part of our commitment to protecting, preserving, and promoting the world's literature. Kessinger Publishing is the place to find hundreds of thousands of rare and hard-to-find books with something of interest for everyone!Hide
Description:New. This item is printed on demand. This scarce antiquarian...New. This item is printed on demand. This scarce antiquarian book is a selection from Kessinger Publishing's Legacy Reprint Series. Due to its age, it may contain imperfections such as marks, notations, marginalia and flawed pages. Because we believe this wor.
Description:BRAND NEW HARDCOVER. 5.98 by 9 inches. This book is printed on...BRAND NEW HARDCOVER. 5.98 by 9 inches. This book is printed on demand [allow 1-2 weeks for printing]. (00084 pages) [this book may have imperfections such as missing or blurred pages, poor pictures, errant marks, etc. that were either part of the original artifact, or were introduced by the scanning process]lang=english accessory: no accessory (Hardcover )