The Norwegian North Polar Expedition, 1893-1896: Scientific Results, Volume 5

ISBN 10: 1286436028 / ISBN 13: 9781286436028
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Sinopsis: This is a reproduction of a book published before 1923. This book may have occasional 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. We believe this work is culturally important, and despite the imperfections,
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The Norwegian North Polar Expedition, 1893-1896: Scientific Results, Volume 5; The Norwegian North Polar Expedition, 1893-1896: Scientific Results; Fridtjof Nansen

Fridtjof Nansen

Longmans, Green and co., 1906

Arctic regions; Fram" Expedition; Fram" Expedition/ 1893-1896); Scientific expeditions

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Título: The Norwegian North Polar Expedition, 1893-...



Condición del libro: Good

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1.

Nansen, Fridtjof,
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Descripción 2016. Softcover. Estado de conservación: New. 342 Lang:- eng, Vol:- Volume 5, Pages 342, Print on Demand. Reprinted in 2016 with the help of original edition published long back[1906]. This book is Printed in black & white, sewing binding for longer life with Matt laminated multi-Colour Soft Cover {HARDCOVER EDITION IS ALSO AVAILABLE}, Printed on high quality Paper, re-sized as per Current standards, professionally processed without changing its contents. As these are old books, there may be some pages which are blur or missing or black spots. We expect that you will understand our compulsion in these books. We found this book important for the readers who want to know more about our old treasure so we brought it back to the shelves. (Customisation is possible). Hope you will like it and give your comments and suggestions. Volume 5 Language: eng. Nº de ref. de la librería PB1111001131453

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Nansen, Fridtjof,
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Descripción 2016. Hardcover. Estado de conservación: New. 342 Lang:- eng, Vol:- Volume 5, Pages 342, Print on Demand. Reprinted in 2016 with the help of original edition published long back[1906]. This book is in black & white, Hardcover, sewing binding for longer life with Matt laminated multi-Colour Dust Cover, Printed on high quality Paper, re-sized as per Current standards, professionally processed without changing its contents. As these are old books, there may be some pages which are blur or missing or black spots. We expect that you will understand our compulsion in these books. We found this book important for the readers who want to know more about our old treasure so we brought it back to the shelves. (Customisation is possible). Hope you will like it and give your comments and suggestions. Volume 5 Language: eng. Nº de ref. de la librería 1111001131453

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3.

Fridtjof 1861-1930 Nansen
Editorial: Wentworth Press, United States (2016)
ISBN 10: 1363592696 ISBN 13: 9781363592692
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Descripción Wentworth Press, United States, 2016. Paperback. Estado de conservación: New. 234 x 156 mm. Language: English . Brand New Book ***** Print on Demand *****. Nº de ref. de la librería AAV9781363592692

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Fridtjof 1861-1930 Nansen
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ISBN 10: 1363592696 ISBN 13: 9781363592692
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Descripción Wentworth Press, United States, 2016. Paperback. Estado de conservación: New. 234 x 156 mm. Language: N/A. Brand New Book ***** Print on Demand *****. Nº de ref. de la librería AAV9781363592692

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5.

Fridtjof Nansen
Editorial: RareBooksClub
ISBN 10: 1236493621 ISBN 13: 9781236493620
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Descripción RareBooksClub. Paperback. Estado de conservación: New. This item is printed on demand. Paperback. 94 pages. Dimensions: 9.7in. x 7.4in. x 0.2in.This 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. 1906 edition. Excerpt: . . . resistance and the frictional resistance cannot be quite independent of each other, and the method should consequently not be allowed; but the experiments seem to show--as might be expected a priori--that it is practically correct. 1 This artifice may often be of use in solving problems concerning the motion of the water-layers in the sea. See Whites Manual, p. 479 seq. It may be pointed out that the two rules above, hold approximately even if the whole resistance be considered. For the frictional resistance varies approximately as the wetted area of the vessel and as the square of the velocity, so that it is obvious it will vary approximately according to the two rules given. The eddy-making resistance is of smaller importance; the same rules hold true for it, provided the motions are really similar, because it is a resultant of pressure. It could not, however, be taken into account when deducing the rules, because it should not exist at all in a frictionless fluid. Besides the viscosity, we must also take account of the capillary forces, which influence the small scale experiments more strongly than those on a full scale, and thus disturb the similarity. On the one hand, these forces prevent the creation of ordinary surface waves in the experiments; on account of capillarity these waves cannot move with a velocity slower than 20 or 23 cm. per second, and the boat-models were towed at still smaller velocities. This effect of capillarity is, however, of no importance, because, at the slow speeds at which dead-water occurs, even full-sized ships do not produce any appreciable surface-waves. The secondary waves in the surface which are produced by the boundary-waves, are--on account of their greater length--not appreciably influenced. . . This item ships from La Vergne,TN. Paperback. Nº de ref. de la librería 9781236493620

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6.

Fridtjof Nansen
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ISBN 10: 1130663086 ISBN 13: 9781130663082
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Descripción RareBooksClub. Paperback. Estado de conservación: New. This item is printed on demand. Paperback. 92 pages. Dimensions: 9.7in. x 7.4in. x 0.2in.This 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. 1906 Excerpt: . . . be geometrically similar in the two cases, and the ratio of the resultants of pressure upon corresponding surfaces is then p X7t--XWd (d) In the case specially interesting us, the boundary-conditions are then practically satisfied if: (1) the linear dimensions of the two vessels are in the constant ratio X; (2) the linear dimensions of the basins, in which they move, are in the same ratio X; or the basins are so wide and deep that their boundaries have no influence upon the motion of the vessel; (3) the velocities of the two vessels are in the ratio v to oneanother. It is not necessary, that the condition concerning the pressure on the free surfaces be satisfied. For, as the water is practically incompressible, the motion is, in both cases, unaltered, if the pressure in the water be diminished by a constant quantity (for instance, the atmospheric pressure), so that the pressure be nil in the free surface. It is then obviously necessary to leave the air-pressure consistently out of account. Equations (b) and (c) give As the possible variations of the density, of the gravity, and of the coefficient of friction, are very limited, the right hand side of this equation cannot be made many times greater or smaller than unity; and it is consequently impossible to reproduce exactly similar motions on very different scales, if gravity and viscosity have both to be taken into account. The gravity is of essential importance, in cases where there is wave-motion. We must therefore at first neglect the viscosity, and afterwards consider its influence as best we can; equation (c) is consequently left out of consideration for the present. Gravity is furthermore practically constant, and so y 1. If the densities of the water-layers are also the same in the two cases, 6 . . . This item ships from La Vergne,TN. Paperback. Nº de ref. de la librería 9781130663082

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7.

Dr Fridtjof Nansen
Editorial: Rarebooksclub.com, United States (2012)
ISBN 10: 1236493621 ISBN 13: 9781236493620
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Descripción Rarebooksclub.com, United States, 2012. Paperback. Estado de conservación: New. 246 x 189 mm. Language: English . Brand New Book ***** Print on Demand *****. This 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. 1906 edition. Excerpt: .resistance and the frictional resistance cannot be quite independent of each other, and the method should consequently not be allowed; but the experiments seem to show--as might be expected a priori--that it is practically correct. 1 This artifice may often be of use in solving problems concerning the motion of the water-layers in the sea. See White s Manual , p. 479 seq. It may be pointed out that the two rules above, hold approximately even if the whole resistance be considered. For the frictional resistance varies approximately as the wetted area of the vessel and as the square of the velocity, so that it is obvious it will vary approximately according to the two rules given. The eddy-making resistance is of smaller importance; the same rules hold true for it, provided the motions are really similar, because it is a resultant of pressure. It could not, however, be taken into account when deducing the rules, because it should not exist at all in a frictionless fluid. Besides the viscosity, we must also take account of the capillary forces, which influence the small scale experiments more strongly than those on a full scale, and thus disturb the similarity. On the one hand, these forces prevent the creation of ordinary surface waves in the experiments; on account of capillarity these waves cannot move with a velocity slower than 20 or 23 cm. per second, and the boat-models were towed at still smaller velocities. This effect of capillarity is, however, of no importance, because, at the slow speeds at which dead-water occurs, even full-sized ships do not produce any appreciable surface-waves. The secondary waves in the surface which are produced by the boundary-waves, are--on account of their greater length--not appreciably influenced. Nº de ref. de la librería APC9781236493620

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Dr Fridtjof Nansen
Editorial: Rarebooksclub.com, United States (2012)
ISBN 10: 1130663086 ISBN 13: 9781130663082
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Descripción Rarebooksclub.com, United States, 2012. Paperback. Estado de conservación: New. 246 x 189 mm. Language: English . Brand New Book ***** Print on Demand *****. This 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. 1906 Excerpt: .be geometrically similar in the two cases, and the ratio of the resultants of pressure upon corresponding surfaces is then p = X7t--XWd (d) In the case specially interesting us, the boundary-conditions are then practically satisfied if: (1) the linear dimensions of the two vessels are in the constant ratio X; (2) the linear dimensions of the basins, in which they move, are in the same ratio X; or the basins are so wide and deep that their boundaries have no influence upon the motion of the vessel; (3) the velocities of the two vessels are in the ratio v to oneanother. It is not necessary, that the condition concerning the pressure on the free surfaces be satisfied. For, as the water is practically incompressible, the motion is, in both cases, unaltered, if the pressure in the water be diminished by a constant quantity (for instance, the atmospheric pressure), so that the pressure be nil in the free surface. It is then obviously necessary to leave the air-pressure consistently out of account. Equations (b) and (c) give As the possible variations of the density, of the gravity, and of the coefficient of friction, are very limited, the right hand side of this equation cannot be made many times greater or smaller than unity; and it is consequently impossible to reproduce exactly similar motions on very different scales, if gravity and viscosity have both to be taken into account. The gravity is of essential importance, in cases where there is wave-motion. We must therefore at first neglect the viscosity, and afterwards consider its influence as best we can; equation (c) is consequently left out of consideration for the present. Gravity is furthermore practically constant, and so y = 1. If the densities of the water-layers are also the same in the two cases, 6 =. Nº de ref. de la librería APC9781130663082

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ISBN 10: 1354931149 ISBN 13: 9781354931141
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Descripción Palala Press, United States, 2016. Hardback. Estado de conservación: New. 234 x 156 mm. Language: N/A. Brand New Book ***** Print on Demand *****. Nº de ref. de la librería APC9781354931141

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Editorial: Palala Press, United States (2016)
ISBN 10: 1354931149 ISBN 13: 9781354931141
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Descripción Palala Press, United States, 2016. Hardback. Estado de conservación: New. 234 x 156 mm. Language: N/A. Brand New Book ***** Print on Demand *****. Nº de ref. de la librería APC9781354931141

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