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respostas do volume 1 da 8ª edição do Halliday em inglês
Tipologia: Exercícios
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Lawrence Livermore National Laboratory
to accompany
EIGHTH EDITION
David Halliday University of Pittsburgh
Robert Resnick Rensselaer Polytechnic Institute
Jearl Walker Cleveland State University
Copyright 2007 John Wiley & Sons, Inc. All rights reserved.
Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the 1976 United States Copyright Act without the permission of the copyright owner is unlawful. Requests for permission or further information should be addressed to the Permissions Department, John Wiley & Sons, Inc., 111 River Street, Hoboken, NJ 07030-5774.
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ISBN-10 0-470-11404-
Printed in the United States of America.
1 0 9 8 7 6 5 4 3 2 1
Printed and bound by Odyssey Press, Inc.
( ) ( )
The given measurement is 1.0 km (two significant figures), which implies our result
(b) We calculate the number of microns in 1 centimeter. Since 1 cm = 10−^2 m,
( ) ( )
(c) Since 1 yd = (3 ft)(0.3048 m/ft) = 0.9144 m,
1.0 yd = (^) ( 0.91m (^) ) (^) ( 10 6 μm m (^) )= 9.1 × 105 μm.
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(b) and that distance in chains to be
( 4.0 furlongs^ ) ( 201.168 m furlong^ ) 40 chains. 20.117 m chain
d = =
(a) the distance d in rods to be
( 4.0 furlongs^ ) ( 201.168 m furlong) 4.0 furlongs = 160 rods, 5.0292 m rod
d = =
imply that
1 gry = (1/10)(1/12)(72 points) = 0.60 point.
Thus, 1 gry^2 = (0.60 point)^2 = 0.36 point^2 , which means that 0.50 gry = 0.18 point.^2
(a) In units of W, we have
( )
(b) In units of Z, we have
( )
2 2
V r z π =
where z is the ice thickness. Since there are 10^3 m in 1 km and 10^2 cm in 1 m, we have
( )
3 2 2000 km 10 m^ 10 cm 2000 105 cm. 1km 1m
r
In these units, the thickness becomes
( )
2 3000 m 3000 m 10 cm 3000 102 cm 1m
z
which yields (^) ( ) ( ) 5 2 2 22 3 2000 10 cm 3000 10 cm 1.9 10 cm. 2
π = × × = ×
1 acre ft = (43,560 ft ) ft = 43,560 ft⋅ 2 ⋅^3
Since 2 in. = (1/6) ft, the volume of water that fell during the storm is
V = (26 km )(1/6 ft)^2 = (26 km )(3281ft/km) (1/6 ft)^2 2 = 4.66 × 10 7 ft.^3
Thus,
V =
7 4
ft ft acre ft
acre ft.
3 3
3 7 10 14 86400
m m m day s day
m s
b gc h b gb g
μ = μ
(a) (^) ( 6 ) 100 y 365 day 24 h 60 min 1 century 10 century 52.6 min. 1 century 1 y 1 day 1 h
μ −^
(b) The percent difference is therefore
52.6 min 50 min 4.9%. 52.6 min
(b) In a regular day, there are 86400 seconds, but in the French system described in the problem, there would be 10^5 seconds. The ratio is therefore 0.864.
2 594 33 662 ,. C (^) 7 B (^) 7 B (^) 40 A 5 t = t + t = t −
These are used in obtaining the following results.
(a) We find
( )
495 s B B (^) 40 A A t ′^ − t = t ′ − t =
when t ' A − tA = 600 s.
(b) We obtain t (^) C ′ − t (^) C = t ′ − B tB = =
b g b^495 g 141 s.
(c) Clock B reads tB = (33/40)(400) − (662/5) ≈ 198 s when clock A reads tA = 400 s.
(d) From tC = 15 = (2/7) tB + (594/7), we get tB ≈ −245 s.