Undergraduate Lecture Notes in Physics
Series Editors Neil Ashby William Brantley Michael Fowler Elena Sassi Helmy S. SherifFor further volumes:
Undergraduate Lecture Notes in Physics (ULNP) publishes authoritative texts covering topics throughout pure and applied physics. Each title in the series is suitable as a basis for undergraduate instruction, typically containing practice problems, worked examples, chapter summaries, and suggestions for further reading.
ULNP titles must provide at least one of the following:
• An exceptionally clear and concise treatment of a standard undergraduate subject.
• A solid undergraduate-level introduction to a graduate, advanced, or non-standard subject.
• A novel perspective or an unusual approach to teaching a subject.
ULNP especially encourages new, original, and idiosyncratic approaches to physics teaching at the undergraduate level.
The purpose of ULNP is to provide intriguing, absorbing books that will continue to be the reader’s preferred reference throughout their academic career.
Hafez A. Radi
•John O. Rasmussen
Principles of Physics
For Scientists and Engineers
October University for Modern Sciences and Arts (MSA) 6th of October City
Egypt
John O. Rasmussen
University of California at Berkeley and Lawrence Berkeley Lab Berkeley, CA
USA
ISSN 2192-4791 ISSN 2192-4805 (electronic) ISBN 978-3-642-23025-7 ISBN 978-3-642-23026-4 (eBook) DOI 10.1007/978-3-642-23026-4
Springer Heidelberg New York Dordrecht London
Library of Congress Control Number: 2012947066 Springer-Verlag Berlin Heidelberg 2013
This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. Exempted from this legal reservation are brief excerpts in connection with reviews or scholarly analysis or material supplied specifically for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Duplication of this publication or parts thereof is permitted only under the provisions of the Copyright Law of the Publisher’s location, in its current version, and permission for use must always be obtained from Springer. Permissions for use may be obtained through RightsLink at the Copyright Clearance Center. Violations are liable to prosecution under the respective Copyright Law.
The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use.
While the advice and information in this book are believed to be true and accurate at the date of publication, neither the authors nor the editors nor the publisher can accept any legal responsibility for any errors or omissions that may be made. The publisher makes no warranty, express or implied, with respect to the material contained herein.
Printed on acid-free paper
Springer is part of Springer Science+Business Media (www.springer.com)
Solutions to the exercises are accessible to qualified instructors at springer.com on this book’s product page. Instructors may click on the link additional information and register to obtain their restricted access.
Preface
This book on Principles of Physics is intended to serve fundamental college courses in scientific curricula.
Physics is one of the most important tools to aid undergraduates, graduates, and researchers in their technical fields of study. Without it many phenomena cannot be described, studied, or understood. The topics covered here will help students interpret such phenomena, ultimately allowing them to advance in the applied aspects of their fields.
The goal of this text is to present many key concepts in a clear and concise, yet interesting way, making use of practical examples and attractively colored illustrations whenever appropriate to satisfy the needs of today’s science and engineering students. Some of the examples, proofs, and subsections in this textbook have been identified as optional and are preceded with an asterisk *. For less intensive courses these optional portions may be omitted without significantly impacting the objectives of the chapter. Additional material may also be omitted depending on the course’s requirements.
The first author taught the material of this book in many universities in the Middle East for almost four decades. Depending on the university, he leveraged different international textbooks, resources, and references. These used different approaches, but were mainly written in an expansive manner delivering a plethora of topics while targeting students who wanted to dive deeply into the subject matter. In this textbook, however, the authors introduce a large subset of these topics but in a more simplified manner, with the intent of delivering these topics and their key facts to students all over the world and in particular to students in the Middle East and neighboring regions where English may not be the native lan-guage. The second author went over the entire text with the background of study and/or teaching at Caltech, UC Berkeley, and Yale.
Instructors teaching from this textbook will be able to gain online access from the publisher to the solutions manual, which provides step-by-step solutions to all exercises contained in the book. The solutions manual also contains many tips, colored illustrations, and explanations on how the solutions were derived.
Acknowledgments from Prof. Hafez A. Radi
I owe special thanks to my wife and two sons Tarek and Rami for their ongoing support and encouragement. I also owe special thanks to my colleague and friend Prof. Rasmussen for his invaluable contributions to this book, and for everything that I learned from him over the years while carrying out scientific research at Lawrence Berkeley Lab. Additionally, I would like to express my gratitude to Prof. Ali Helmy Moussa, Prof. of Physics at Ain Shams University in Egypt, for his assistance, support, and guidance over the years. I also thank all my fellow professors and colleagues who provided me with valuable feedback pertaining to many aspects of this book, especially Dr. Sana’a Ismail, from Dar El Tarbiah School, IGCSE section and Dr. Hesham Othman from the Faculty of Engineering at Cairo University. I would also like to thank Professor Mike Guidry, Professor of Physics and Astronomy at the University of Tennessee Knoxville, for his valuable recommendations. I am also grateful to the CD Odessa LLC for their Concept-Draw software suite which was used to create almost all the figures in this book. I finally extend my thanks and appreciation to Professor Nawal El-Degwi, Professor Khayri Abdel-Hamid, Professor Said Ashour, and the staff members and teaching assistants at the faculty of Engineering at MSA University, Egypt, for all their support and input.
Hafez A. Radi hafez.radi@gmail.com Acknowledgments from Prof. John O. Rasmussen
I would like to thank Prof. Radi for the opportunity to join him as coauthor. I am grateful to the many teachers, students, and colleagues from whom I learned various aspects of the fascinating world of the physical sciences, notably the late Drs. Linus Pauling, Isadore Perlman, Stanley Thompson, Glenn Seaborg, Earl Hyde, Hilding Slätis, Aage Bohr, Gaja Alaga, and Hans-Järg Mang. There are many others, still living, too numerous to list here. I would also like to extend my special thanks to my wife for her support and encouragement.
John O. Rasmussen oxras@berkeley.edu
Contents
Part I Fundamental Basics
1 Dimensions and Units. . . 3
1.1 The International System of Units . . . 3
1.2 Standards of Length, Time, and Mass . . . 5
1.3 Dimensional Analysis . . . 9
1.4 Exercises . . . 12
2 Vectors . . . 17
2.1 Vectors and Scalars . . . 17
2.2 Properties of Vectors. . . 19
2.3 Vector Components and Unit Vectors . . . 22
2.4 Multiplying Vectors . . . 27
2.5 Exercises . . . 33
Part II Mechanics 3 Motion in One Dimension. . . 41
3.1 Position and Displacement . . . 41
3.2 Average Velocity and Average Speed . . . 42
3.3 Instantaneous Velocity and Speed . . . 44
3.4 Acceleration . . . 48
3.5 Constant Acceleration . . . 52
3.6 Free Fall . . . 57
3.7 Exercises . . . 62
4 Motion in Two Dimensions. . . 71
4.1 Position, Displacement, Velocity, and Acceleration Vectors . . . 71
4.2 Projectile Motion . . . 79
4.3 Uniform Circular Motion . . . 87
4.4 Tangential and Radial Acceleration. . . 90
4.5 Non-uniform Circular Motion. . . 91
4.6 Exercises . . . 93
5 Force and Motion. . . 103
5.1 The Cause of Acceleration and Newton’s Laws . . . 103
5.2 Some Particular Forces . . . 106
5.3 Applications to Newton’s Laws . . . 113
5.4 Exercises . . . 124
6 Work, Energy, and Power . . . 137
6.1 Work Done by a Constant Force . . . 137
6.2 Work Done by a Variable Force . . . 142
6.3 Work-Energy Theorem . . . 148
6.4 Conservative Forces and Potential Energy . . . 151
6.5 Conservation of Mechanical Energy . . . 157
6.6 Work Done by Non-conservative Forces . . . 159
6.7 Conservation of Energy . . . 162
6.8 Power . . . 166
6.9 Exercises . . . 170
7 Linear Momentum, Collisions, and Center of Mass. . . 181
7.1 Linear Momentum and Impulse . . . 181
7.2 Conservation of Linear Momentum. . . 184
7.3 Conservation of Momentum and Energy in Collisions . . . 187
7.3.1 Elastic Collisions in One and Two Dimensions . . . . 187
7.3.2 Inelastic Collisions . . . 194
7.4 Center of Mass (CM) . . . 195
7.5 Dynamics of the Center of Mass . . . 199
7.6 Systems of Variable Mass . . . 203
7.6.1 Systems of Increasing Mass . . . 204
7.6.2 Systems of Decreasing Mass; Rocket Propulsion . . . 205
7.7 Exercises . . . 209
8 Rotational Motion . . . 227
8.1 Radian Measures . . . 227
8.2 Rotational Kinematics; Angular Quantities. . . 228
8.3 Constant Angular Acceleration . . . 232
8.4 Angular Vectors . . . 233
8.5 Relating Angular and Linear Quantities . . . 233
8.6 Rotational Dynamics; Torque . . . 238
8.7 Newton’s Second Law for Rotation . . . 240
8.9 Rolling Motion . . . 252
8.10 Exercises . . . 259
9 Angular Momentum. . . 269
9.1 Angular Momentum of Rotating Systems . . . 269
9.1.1 Angular Momentum of a Particle . . . 269
9.1.2 Angular Momentum of a System of Particles . . . 271
9.1.3 Angular Momentum of a Rotating Rigid Body . . . 271
9.2 Conservation of Angular Momentum. . . 277
9.3 The Spinning Top and Gyroscope. . . 285
9.4 Exercises . . . 289
10 Mechanical Properties of Matter. . . 303
10.1 Density and Relative Density . . . 304
10.2 Elastic Properties of Solids . . . 306
10.2.1 Young’s Modulus: Elasticity in Length . . . 307
10.2.2 Shear Modulus: Elasticity of Shape . . . 310
10.2.3 Bulk Modulus: Volume Elasticity . . . 312
10.3 Fluids . . . 314
10.4 Fluid Statics . . . 316
10.5 Fluid Dynamics . . . 328
10.6 Exercises . . . 345
Part III Introductory Thermodynamics 11 Thermal Properties of Matter. . . 357
11.1 Temperature . . . 357
11.2 Thermal Expansion of Solids and Liquids . . . 360
11.2.1 Linear Expansion . . . 361
11.2.2 Volume Expansion . . . 362
11.3 The Ideal Gas . . . 365
11.4 Exercises . . . 371
12 Heat and the First Law of Thermodynamics. . . 379
12.1 Heat and Thermal Energy . . . 379
12.1.1 Units of Heat, The Mechanical Equivalent of Heat . . . 379
12.1.2 Heat Capacity and Specific Heat . . . 380
12.1.3 Latent Heat . . . 384
12.2 Heat and Work . . . 390
12.3 The First Law of Thermodynamics . . . 395
12.4 Applications of the First Law of Thermodynamics . . . 396
12.5 Heat Transfer . . . 406
12.6 Exercises . . . 416
13 Kinetic Theory of Gases. . . 427
13.1 Microscopic Model of an Ideal Gas . . . 427
13.2 Molar Specific Heat Capacity of an Ideal Gas . . . 434
13.2.1 Molar Specific Heat at Constant Volume . . . 435
13.2.2 Molar Specific Heat at Constant Pressure . . . 436
13.3 Distribution of Molecular Speeds . . . 441
13.4 Non-ideal Gases and Phases of Matter . . . 442
13.5 Exercises . . . 444
Part IV Sound and Light Waves 14 Oscillations and Wave Motion . . . 451
14.1 Simple Harmonic Motion . . . 451
14.1.1 Velocity and Acceleration of SHM . . . 452
14.1.2 The Force Law for SHM . . . 455
14.1.3 Energy of the Simple Harmonic Oscillator. . . 459
14.2 Damped Simple Harmonic Motion . . . 462
14.3 Sinusoidal Waves . . . 463
14.3.1 Transverse and Longitudinal Waves . . . 463
14.3.2 Wavelength and Frequency . . . 465
14.3.3 Harmonic Waves: Simple Harmonic Motion . . . 466
14.4 The Speed of Waves on Strings . . . 470
14.5 Energy Transfer by Sinusoidal Waves on Strings . . . 472
14.6 The Linear Wave Equation . . . 476
14.7 Standing Waves . . . 477
14.7.1 Reflection at a Boundary . . . 481
14.7.2 Standing Waves and Resonance . . . 482
14.8 Exercises . . . 486
15 Sound Waves. . . 499
15.1 Speed of Sound Waves . . . 499
15.2 Periodic Sound Waves. . . 502
15.3 Energy, Power, and Intensity of Sound Waves . . . 505
15.4 The Decibel Scale . . . 510
15.5 Hearing Response to Intensity and Frequency . . . 514
15.6 The Doppler Effect . . . 514
15.7 Supersonic Speeds and Shock Waves . . . 521
15.8 Exercises . . . 523
16 Superposition of Sound Waves . . . 531
16.1 Superposition and Interference . . . 531
16.2 Spatial Interference of Sound Waves . . . 533
16.3 Standing Sound Waves . . . 537
16.5 Temporal Interference of Sound Waves: Beats . . . 549
16.6 Exercises . . . 554
17 Light Waves and Optics. . . 561
17.1 Light Rays . . . 561
17.2 Reflection and Refraction of Light . . . 563
17.3 Total Internal Reflection and Optical Fibers. . . 568
17.4 Chromatic Dispersion and Prisms . . . 571
17.5 Formation of Images by Reflection . . . 575
17.5.1 Plane Mirrors . . . 575
17.5.2 Spherical Mirrors . . . 576
17.6 Formation of Images by Refraction. . . 583
17.6.1 Spherical Refracting Surfaces . . . 583
17.6.2 Flat Refracting Surfaces . . . 584
17.6.3 Thin Lenses . . . 586
17.7 Exercises . . . 595
18 Interference, Diffraction and Polarization of Light. . . 603
18.1 Interference of Light Waves . . . 603
18.2 Young’s Double Slit Experiment . . . 604
18.3 Thin Films—Change of Phase Due to Reflection . . . 611
18.4 Diffraction of Light Waves . . . 615
18.5 Diffraction Gratings . . . 620
18.6 Polarization of Light Waves . . . 624
18.7 Exercises . . . 627
Part V Electricity 19 Electric Force . . . 637
19.1 Electric Charge. . . 637
19.2 Charging Conductors and Insulators . . . 639
19.3 Coulomb’s Law . . . 642
19.4 Exercises . . . 651
20 Electric Fields . . . 659
20.1 The Electric Field . . . 659
20.2 The Electric Field of a Point Charge . . . 660
20.3 The Electric Field of an Electric Dipole . . . 666
20.4 Electric Field of a Continuous Charge Distribution . . . 670
20.4.1 The Electric Field Due to a Charged Rod . . . 672
20.4.2 The Electric Field of a Uniformly Charged Arc . . . . 679
20.4.3 The Electric Field of a Uniformly Charged Ring . . . 681
20.4.4 The Electric Field of a Uniformly Charged Disk . . . 682
20.5 Electric Field Lines. . . 684
20.6 Motion of Charged Particles in a Uniform Electric Field . . . . 686
20.7 Exercises . . . 691
21 Gauss’s Law. . . 701
21.1 Electric Flux . . . 701
21.2 Gauss’s Law . . . 705
21.3 Applications of Gauss’s Law . . . 707
21.4 Conductors in Electrostatic Equilibrium. . . 717
21.5 Exercises . . . 720
22 Electric Potential. . . 731
22.1 Electric Potential Energy . . . 731
22.2 Electric Potential . . . 733
22.3 Electric Potential in a Uniform Electric Field. . . 735
22.4 Electric Potential Due to a Point Charge . . . 741
22.5 Electric Potential Due to a Dipole . . . 745
22.6 Electric Dipole in an External Electric Field . . . 747
22.7 Electric Potential Due to a Charged Rod . . . 749
22.8 Electric Potential Due to a Uniformly Charged Arc . . . 752
22.9 Electric Potential Due to a Uniformly Charged Ring. . . 753
22.10 Electric Potential Due to a Uniformly Charged Disk . . . 754
22.11 Electric Potential Due to a Uniformly Charged Sphere . . . 756
22.12 Electric Potential Due to a Charged Conductor . . . 757
22.13 Potential Gradient . . . 758
22.14 The Electrostatic Precipitator . . . 761
22.15 The Van de Graaff Generator . . . 762
22.16 Exercises . . . 763
23 Capacitors and Capacitance. . . 773
23.1 Capacitor and Capacitance . . . 773
23.2 Calculating Capacitance. . . 775
23.3 Capacitors with Dielectrics . . . 781
23.4 Capacitors in Parallel and Series. . . 790
23.5 Energy Stored in a Charged Capacitor. . . 795
23.6 Exercises . . . 797
24 Electric Circuits. . . 809
24.1 Electric Current and Electric Current Density. . . 809
24.2 Ohm’s Law and Electric Resistance . . . 814
24.3 Electric Power . . . 823
24.4 Electromotive Force . . . 825
24.5 Resistors in Series and Parallel. . . 829
24.7 The RC Circuit . . . 838
24.8 Exercises . . . 844
Part VI Magnetism 25 Magnetic Fields . . . 859
25.1 Magnetic Force on a Moving Charge . . . 859
25.2 Motion of a Charged Particle in a Uniform Magnetic Field . . 863
25.3 Charged Particles in an Electric and Magnetic Fields . . . 865
25.3.1 Velocity Selector . . . 866
25.3.2 The Mass Spectrometer . . . 866
25.3.3 The Hall Effect . . . 867
25.4 Magnetic Force on a Current-Carrying Conductor. . . 869
25.5 Torque on a Current Loop . . . 874
25.5.1 Electric Motors. . . 876
25.5.2 Galvanometers . . . 877
25.6 Non-Uniform Magnetic Fields . . . 878
25.7 Exercises . . . 879
26 Sources of Magnetic Field. . . 889
26.1 The Biot-Savart Law . . . 889
26.2 The Magnetic Force Between Two Parallel Currents. . . 895
26.3 Ampere’s Law . . . 897
26.4 Displacement Current and the Ampere-Maxwell Law . . . 901
26.5 Gauss’s Law for Magnetism. . . 903
26.6 The Origin of Magnetism . . . 904
26.7 Magnetic Materials . . . 908
26.8 Diamagnetism and Paramagnetism . . . 910
26.9 Ferromagnetism . . . 914
26.10 Some Applications of Magnetism . . . 919
26.11 Exercises . . . 921
27 Faraday’s Law, Alternating Current, and Maxwell’s Equations. . 933
27.1 Faraday’s Law of Induction . . . 933
27.2 Motional emf . . . 936
27.3 Electric Generators . . . 940
27.4 Alternating Current . . . 942
27.5 Transformers . . . 943
27.6 Induced Electric Fields . . . 945
27.7 Maxwell’s Equations of Electromagnetism . . . 947
27.8 Exercises . . . 950
28 Inductance, Oscillating Circuits, and AC Circuits. . . 961
28.1 Self-Inductance. . . 961
28.2 Mutual Inductance . . . 964
28.3 Energy Stored in an Inductor . . . 966
28.4 The L–R Circuit . . . 967
28.5 The Oscillating L–C Circuit . . . 971
28.6 The L–R–C Circuit . . . 974
28.7 Circuits with an ac Source . . . 977
28.8 L–R–C Series in an ac Circuit . . . 984
28.9 Resonance in L–R–C Series Circuit . . . 988
28.10 Exercises . . . 988
Appendix A Conversion Factors . . . 999
Appendix B Basic Rules and Formulas. . . 1003
Appendix C The Periodic Table of Elements . . . 1013
Answers to All Exercises. . . 1015
Fundamental Physical Constants
Quantity Symbol Approximate value
Speed of light in vacuum c 3:00 108m/s
Avogadro’s number NA 6:02 1023mol1¼ 6:02 1026kmol1
Gas constant R 8:314 J/molK ¼ 8 314J/kmol K
Boltzmann’s constant k 1:38 1023J/K
Gravitational constant G 6:67 1011N m2=kg2
Planck’s constant h 6:63 1034J s
Permittivity of free space 0 8:85 1012C2=N m2
Permeability of free space l0¼ 1=ðc20Þ 4p 107T m/A
Atomic mass unit 1u 1:6605 1027kg¼ 931:49 MeV/c2
Electron charge -e 1:60 1019C
Electron rest mass me 9:11 1031kg¼ 0:000549 u
¼ 0:511 MeV/c2
Proton rest mass mp 1:6726 1027kg¼ 1:00728 u
¼ 938:27 MeV/c2
Neutron rest mass mn 1:6749 1027kg¼ 1:008665 u
¼ 939:57 MeV/c2
The greek alphabet Alpha A a Nu M m Beta B b Xi N n Gamma C c Omicron O o Delta D d Pi P p Epsilon E e Rho Q q Zeta F f Sigma R r Eta H g Tau S s Theta H h Upsilon T t Iota I i Phi U / Kappa J j Chi V v Lambda K k Psi W w Mu L l Omega X x
Acceleration due to gravity at the Earth’s surface (av.) g¼ 9:8 m/s2
Absolute zero (0 K) 273:15C
Joule equivalent (1 kcal) 4; 186 J
Speed of sound in air (20C) 343 m/s
Density of air (dry) 1:29 kg/m3
Standard atmosphere 1:01 105Pa
Electric breakdown strength 3 106V/m
Earth: Mass Radius (av.) 5:98 1024kg 6:38 103km Moon: Mass Radius (av.) 7:35 1022kg 1:74 103km Sun: Mass Radius (av.) 1:99 1030kg 6:96 105km
Earth–Moon distance (av.) 3:84 105km
Earth–Sun distance (av.) 1:5 108km
Some SI base units and derived units
Quantity Unit name Unit symbol In terms of base units
Mass kilogram kg
Length meter m
Time second s
Electric current ampere A
Force newton N kgm=s2
Energy and work joule J kgm2=s2
Power watt W kgm2=s3
Pressure pascal Pa kg=ðms2Þ
Frequency hertz Hz s-1
Electric charge coulomb C As
Electric potential volt V kgm2=ðAs3Þ
Electric resistance ohm X kgm2=ðA2s3Þ
Capacitance farad F A2s4=ðkgm2Þ
Magnetic field tesla T kg=ðAs2Þ
Magnetic flux weber Wb kgm2=ðAs2Þ
Inductance henry H kgm2=ðs2A2Þ
{
Base SI unitsyotta Y 1024 zeta Z 1021 exa E 1018 peta P 1015 tera T 1012 giga G 109 mega M 106 kilo k 103 hecto h 102 deka da 101 deci d 10-1 centi c 10-2 milli m 10-3 micro l 10-6 nano n 10-9 pico p 10-12 femto f 10-15 atto a 10-18 zepto z 10-21 yocto y 10-24 xviii
Part I
Dimensions and Units
1
The laws of physics are expressed in terms of basic quantities that require a clear definition for the purpose of measurements. Among these measured quantities are length, time, mass, temperature, etc.
In order to describe any physical quantity, we first have to define a unit of measurement (which was among the earliest tools invented by humans), i.e. a mea-sure that is defined to be exactly 1.0. After that, we define a standard for this quantity, i.e. a reference to compare all other examples of the same physical quantity.
1.1
The International System of Units
Seven physical quantities have been selected as base quantities in the 14th General Conference on Weights and Measurements, held in France in 1971. These quantities form the basis of the International System of Units, abbreviated SI (from its French name Système International) and popularly known as the metric system. Table1.1
depicts these quantities, their unit names, and their unit symbols.
Many SI derived units are defined in terms of the first three quantities of Table1.1. For example, the SI unit for force, called the newton (abbreviated N), is defined in terms of the base units of mass, length, and time. Thus, as we will see from the study of Newton’s second law, the unit of force is given by:
1 N= 1 kg.m/s2 (1.1)
When dealing with very large or very small numbers in physics, we use the so-called scientific notation which employs powers of 10, such as:
H. A. Radi and J. O. Rasmussen, Principles of Physics, 3 Undergraduate Lecture Notes in Physics, DOI: 10.1007/978-3-642-23026-4_1,
4 1 Dimensions and Units
3 210 000 000 m= 3.21 × 109m (1.2)
0.000 000 789 s = 7.89 × 10−7s (1.3)
Table 1.1 The seven independent SI base units
Quantity Unit name Unit symbol
Length Meter m
Time Second s
Mass Kilogram kg
Temperature Kelvin K
Electric current Ampere A
Amount of substance Mole mol
Luminous intensity Candela cd
An additional convenient way to deal with very large or very small numbers in physics is to use the prefixes listed in Table1.2. Each one of these prefixes represents a certain power of 10.
Table 1.2 Prefixes for SI unitsa
Factor Prefix Symbol Factor Prefix Symbol
1024 yotta- Y 10−24 yocto- y 1021 zeta- Z 10−21 zepto- z 1018 exa- E 10−18 atto- a 1015 peta- P 10−15 femto- f 1012 tera- T 10−12 pico- p 109 giga- G 10−9 nano- n 106 mega- M 10−6 micro- µ 103 kilo- k 10−3 milli- m 102 hecta- h 10−2 centi- c 101 deca- da 10−1 deci- d
aThe most commonly used prefixes are shown in bold face type
Accordingly, we can express a particular magnitude of force as:
1.23 × 106N= 1.23 mega newtons
or a particular time interval as:
1.23 × 10−9s= 1.23 nano seconds
= 1.23 ns (1.5)
We often need to change units in which a physical quantity is expressed. We do that by using a method called chain-link conversion, in which we multiply by a conversion factor that equals unity. For example, because 1 minute and 60 seconds are identical time intervals, then we can write:
1 min
60 s = 1 and 60 s
1 min = 1 (1.6)
This does not mean that 601 = 1 or 60 = 1, because the number and its unit must be treated together.
Example 1.1
Convert the following: (a) 1 kilometer per hour to meter per second, (b) 1 mile per hour to meter per second, and (c) 1 mile per hour to kilometer per hour [to a good approximation 1mi = 1.609 km].
Solution: (a) To convert the speed from the kilometers per hour unit to meters per second unit, we write:
1 km/h= 1 km h × 103m 1 km × 1 h 60× 60 s = 0.2777...m s = 0.278 m/s (b) To convert from miles per hour to meters per second, we write:
1 mi/h= 1 mi h × 1609 m 1 mi × 1 h 60× 60 s = 0.447 m s = 0.447 m/s (c) To convert from miles per hour to kilometers per hour, we write:
1mi/h= 1 mi h × 1.609 km 1 mi = 1.609 km h = 1.609 km/h
1.2
Standards of Length, Time, and Mass
Definitions of the units of length, time, and mass are under constant review and are changed from time to time. We only present in this section the latest definitions of those quantities.
6 1 Dimensions and Units
Length (L)
In 1983, the precision of the meter was redefined as the distance traveled by a light wave in vacuum in a specified time interval. The reason is that the measurement of the speed of light has become extremely precise, so it made sense to adopt the speed of light as a defined quantity and to use it to redefine the meter. In the words of the 17th General Conference on Weights and Measurements:
One Meter
One meter is the distance traveled by light in vacuum during the time interval of 1/299 792 458 of a second.
This time interval number was chosen so that the speed of light in vacuum c will be exactly given by:
c= 299 792 458 m/s (1.7)
For educational purposes we usually consider the value c= 3 × 108m/s. Table1.3lists some approximate interesting lengths.
Table 1.3 Some approximate lengths
Length Meters
Distance to farthest known galaxy 4× 1025 Distance to nearest star 4× 1016 Distance from Earth to Sun 1.5 × 1011 Distance from Earth to Moon 4× 108
Mean radius of Earth 6× 106
Wave length of light 5× 10−7
Radius of hydrogen atom 5× 10−11
Radius of proton 1× 10−15
Time (T)
Recently, the standard of time was redefined to take advantage of the high-precision measurements that could be obtained by using a device known as an atomic clock. Cesium is most common element that is typically used in the construction of atomic clocks because it allows us to attain high accuracy.
Since 1967, the International System of Measurements has been basing its unit of time, the second, on the properties of the isotope cesium-133(13355Cs). One of the transitions between two energy levels of the ground state of 13355Cs has an oscil-lation frequency of 9 192 631 770 Hz, which is used to define the second in SI units. Using this characteristic frequency, Fig.1.1shows the cesium clock at the National Institute of Standards and Technology. The uncertainty is about 5× 10−16 (as of 2005). Or about 1 part in 2× 1015. This means that it would neither gain nor lose a second in 64 million years.
One Second
One second is the time taken for the cesium atom 13355Cs to perform 9 192 631 770 oscillations to emit radiation of a specific wavelength
Fig. 1.1 The cesium atomic clock at the National Institute of Standards and Technology (NIST) in Boulder, Colorado (photo with permission)
Table1.4lists some approximate interesting time intervals.
Table 1.4 Some approximate time intervals
Time intervals Seconds
Lifetime of proton (predicted) 1× 1039
Age of the universe 5× 1017
Age of the Earth 1.3 × 1017
Period of one year 3.2 × 107
Time between human heartbeats 8× 10−1 Period of audible sound waves 1× 10−3 Period of visible light waves 2× 10−15 Time for light to cross a proton 3.3 × 10−24
8 1 Dimensions and Units
Mass (M)
The Standard Kilogram
A cylindrical mass of 3.9 cm in diameter and of 3.9 cm in height and made of an unusu-ally stable platinum-iridium alloy is kept at the International Bureau of Weights and Measures near Paris and assigned in the SI units a mass of 1 kilogram by international agreement, see Fig.1.2.
One Kilogram
The SI unit of mass, 1 kilogram, is defined as the mass of a platinum-iridium alloy cylinder kept at the International Bureau of Weights and Measures in France.
Fig. 1.2 The standard 1 kilogram of mass is a platinum-iridium cylinder 3.9 cm in height and diameter and kept under a double bell jar at the International Bureau of Weights and Measures in France
Accurate copies of this standard 1 kilogram have been sent to standardizing lab-oratories in other countries. Table1.5lists some approximate mass values of various interesting objects.
A Second Standard Mass
Atomic masses can be compared with each other more precisely than the kilogram. By international agreement, the carbon-12 atom,126C, has been assigned a mass of 12 atomic mass units (u), where:
1 u= (1.660 540 2 ± 0.000 001 0) × 10−27 kg (1.8) Experimentally, with reasonable precision, all masses of other atoms can be measured relative to the mass of carbon-12.
Table 1.5 Mass of various objects (approximate values)
Object Kilogram
Known universe (predicted) 1× 1053 Our galaxy the milky way (predicted) 2× 1041
Sun 2× 1030 Earth 6× 1024 Moon 7× 1022 Small mountain 1× 1012 Elephant 5× 103 Human 7× 101 Mosquito 1× 10−5 Bacterium 1× 10−15 Uranium atom 4× 10−25 Proton 2× 10−27 Electron 9× 10−31
1.3
Dimensional Analysis
Throughout your experience, you have been exposed to a variety of units of length; the SI meter, kilometer, and millimeter; the English units of inches, feet, yards, and miles, etc. All of these derived units are said to have dimensions of length, symbolized by L. Likewise, all time units, such as seconds, minutes, hours, days, years, and centuries are said to have dimensions of time, symbolized by T. The kilogram and all other mass units have dimensions of mass, symbolized by M. In general, we may take the dimension (length, time, and mass) as the concept of the physical quantity.
From the three fundamental physical quantities of length L, time T, and mass M, we can derive a variety of useful quantities. Derived quantities have different dimen-sions from the fundamental quantities. For example, the area obtained by multiplying one length by another has the dimension L2. Volume has the dimension L3. Mass density is defined as mass per unit volume and has the dimension M/L3. The SI unit of speed is meters per second (m/s) with the dimension L/T.
The concept of dimensionality is important in understanding physics and in solv-ing physics problems. For example, the addition or subtraction of quantities with different dimensions makes no sense, i.e. 2 kg plus 8 s is meaningless. Actually, phys-ical equations must be dimensionally consistent. For example, the equation giving the position of a freely falling body (seeChap. 3) is giving by:
10 1 Dimensions and Units
x= v◦t+1
2g t 2
(1.9)
where x is the position (length),v◦the initial speed (length/time), g is the acceleration due to gravity (length/time2), and t is time. If we analyze the equation dimensionally, we have: L= L T× T + L T2× T 2= L + L (Dimensional analysis)
Note that every term of this equation has the dimension of length L. Also note that numerical factors, such as 12 in Eq.1.9, are ignored in dimensional analysis because they have no dimension. Dimensional analysis is useful since it can be used to catch careless errors in any physical equation. On the other hand, Eq.1.9may be correct with respect to dimensional analysis, but could still be wrong with respect to dimensionless numerical factors.
If we had incorrectly written Eq.1.9as follows:
x= v◦t2+1
2g t (1.10)
Then, by analyzing this equation dimensionally, we have:
L= L T× T 2+ L T2 × T (Dimensional analysis) = L T × T × T + L T× T× T
and finally we get: L= LT+L
T (Dimensional analysis)
Dimensionally, Eq1.10is meaningless, and thus cannot be correct.
Example 1.2
Use dimensional analysis to show that the expressionv = v◦+ at is dimensionally correct, where v and v◦ represent velocities, a is acceleration, and t is a time interval.
Solution: Since L/T is the dimension of v and v◦, and the dimension of a is L/T2, then when we analyze the equation v = v◦+ at dimensionally, we have:
L T = L T + L T2× T (Dimensional analysis) =L T + L T× T× T
and finally we get: L T = L T+ L T (Dimensional analysis)
Thus, the expressionv = v◦+ at is dimensionally correct.
Example 1.3
A particle moves with a constant speedv in a circular orbit of radius r, see the figure below. Given that the magnitude of the acceleration a is proportional to some power of r, say rm, and some power of v,say vn, then determine the powers of r andv.
v a
r
Solution: Assume that the variables of the problem can be expressed mathemat-ically by the following relation:
a= k rmvn,
where k is a dimensionless proportionality constant. With the known dimensions of r,v, and a we analyze the dimensions of the above relation as follows:
L T2 = L m× L T n =Lm+n Tn (Dimensional analysis)
This dimensional equation would be balanced, i.e. the dimensions of the right hand side equal the dimensions of the left hand side only when the following two conditions are satisfied:
m+ n = 1,
and n= 2.
12 1 Dimensions and Units Therefore, we can rewrite the acceleration as follows:
a= k r−1v2= k v
2
r
When we later introduce uniform circular motion inChap. 4, we shall see that
k= 1 if SI units are used. However, if for example we choose a to be in m/s2and
v to be in km/h, then k would not be equal to one.
1.4
Exercises
Section 1.1 The International System of Units
(1) Use the prefixes introduced in Table1.2to express the following: (a) 103lambs, (b) 106 bytes, (c) 109 cars, (d) 1012 stars, (e) 10−1Kelvin, (f) 10−2 meter, (g) 10−3ampere, (h) 10−6newton, (i) 10−9kilogram, (j) 10−15second.
Section 1.2 Standards of Length, Time, and Mass
Length(2) The original definition of the meter was based on distance from the North pole to the Earth’s equator (measures along the surface) and was taken to be 107m. (a) What is the circumference of the Earth in meters? (b) What is the radius of the Earth in meters, (c) Give your answer to part (a) and part (b) in miles. (d) What is the circumference of the Earth in meters assuming it to be a sphere of radius 6.4 × 106m? Compare your answer to part (a)
(3) The time of flight of a laser pulse sent from the Earth to the Moon was measured in order to calculate the Earth-Moon distance, and it was found to be 3.8 × 105km. (a) Express this distance in miles, meters, centimeters, and millimeters. (4) A unit of area, often used in measuring land areas, is the hectare, defined as 104m2. An open-pit coal mine excavates 75 hectares of land, down to a depth of 26 m, each year. What volume of Earth, in cubic kilometers, is removed during this time?
(5) The units used by astronomers are appropriate for the quantities they usually measure. As an example, for planetary distances they use the astronomical
unit (AU), which is equal to the mean Earth-Sun distance(1.5 × 1011m). For stellar distances they use the light-year(1 ly = 9.461 × 1012km), which is the distance that light travels in 1 yr(1 yr = 365.25 days = 3.156 × 107s) with a speed of 299 792 458 m/s. They use also the parsec (pc), which is equal to 3.26 light-years. Intergalactic distances might be described with a more appropriate unit called the megaparsec. Convert the following to meters and express each with an appropriate metric prefix: (a) The astronomical unit, (b) The light-year, (c) The parsec, and (d) The megaparsecs.
(6) When you observe a total solar eclipse, your view of the Sun is obstructed by the Moon. Assume the distance from you to the Sun(ds) is about 400 times the distance from you to the Moon(dm). (a) Find the ratio of the Sun’s radius to the Moon’s radius. (b) What is the ratio of their volumes? (c) Hold up a small coin so that it would just eclipse the full Moon, and measure the distance between the coin and your eye. From this experimental result and the given distance between the Moon and the Earth(3.8 × 105km), estimate the diameter of the Moon.
(7) Assume a spherical atom with a spherical nucleus where the ratio of the radii is about 105. The Earth’s radius is 6.4 × 106m. Suppose the ratio of the radius of the Moon’s orbit to the Earth’s radius(3.8 × 105km) were also 105. (a) How far would the Moon be from the Earth’s surface? (b) How does this distance compare with the actual Earth-Moon distance given in exercise 6?
Time
(8) Using the day as a unit, express the following: (a) The predicted life time of proton, (b) The age of universe, (c) The age of the Earth, (d) The age of a 50-year-old tree.
(9) Compare the duration of the following: (a) A microyear and a 1-minute TV commercial, and (b) A microcentury and a 60-min TV program.
(10) Convert the following approximate maximum speeds from km/h to mi/h: (a) snail(5 × 10−2km/h), (b) spider (2 km/h), (c) human (37 km/h),(d) car
(220 km/h), and (e) airplane (1,000 km/h).
(11) A 12-hour-dial clock happens to gain 0.5 min each day. After setting the clock to the correct time at 12:00 noon, how many days must one wait until it again indicates the correct time?
14 1 Dimensions and Units (12) Is a cesium clock sufficiently precise to determine your age (assuming it is
exactly 19 years, not a leap year) within 10−6s ? How about within 10−3s ? (13) The slowing of the Earth’s rotation is measured by observing the occurrences
of solar eclipses during a specific period. Assume that the length of a day is increasing uniformly by 0.001 s per century. (a) Over a span of 10 centuries, compare the length of the last and first days, and find the average difference. (b) Find the cumulative difference on the measure of a day over this period.
Mass
(14) A person on a diet loses 2 kg per week. Find the average rate of mass loss in milligrams every: day, hour, minute, and second.
(15) Density is defined as mass per unit volume. If a crude estimation of the average density of the Earth was 5.5 × 103kg/m3and the Earth is considered to be a sphere of radius 6.37 × 106m, then calculate the mass of the Earth.
(16) A carbon-12 atom(126C) is found to have a mass of 1.992 64 × 10−26kg. How many atoms of126C are there in: (a) 1 kg? (b) 12 kg? (This number is Avogadro’s number in the SI units.)
(17) A water molecule(H2O) contains two atoms of hydrogen (11H), each of which has a mass of 1 u, and one atom of oxygen (168O), that has a mass 16 u, approx-imately. (a) What is the mass of one molecule of water in units of kilograms? (b) Find how many molecules of water are there in the world’s oceans, which have an estimated mass of 1.5 × 1021kg?
(18) Density is defined as mass per unit volume. The density of iron is 7.87 kg/m3, and the mass of an iron atom is 9.27×10−26kg. If atoms are cubical and tightly packed, (a) What is the volume of an iron atom, and (b) What is the distance between the centers of two adjacent atoms.
Section 1.3 Dimensional Analysis
(19) A simple pendulum has periodic time T given by the relation:
T = 2πL/g
where L is the length of the pendulum and g is the acceleration due to gravity in units of length divided by the square of time. Show that this equation is dimensionally correct.
(20) Suppose the displacement s of an object moving in a straight line under uniform acceleration a is giving as a function of time by the relation s= kamtn, where k is a dimensionless constant. Use dimensional analysis to find the values of
the powers m and n.
(21) Using dimensional analysis, determine if the following equations are dimen-sionally correct or incorrect: (a)v2 = v2◦+ 2a s, (b) s = s◦+ v◦t+ 12a t2,
(c) s= s◦cos kt, where k is a constant that has the dimension of the inverse of time.
(22) Newton’s second law states that the acceleration of an object is directly propor-tional to the force applied and inversely proporpropor-tional to the mass of the object. Find the dimensions of force and show that it has units of kg·m/s2in terms of SI units.
(23) Newton’s law of universal gravitation is given by F= Gm1m2/r2, where F is the force of attraction of one mass, m1, upon another mass, m2, at a distance r. Find the SI units of the constant G.
Vectors
2
When a particle moves in a straight line, we can take its motion to be positive in one specific direction and negative in the other. However, when this particle moves in three dimensions, plus or minus signs are no longer enough to specify the direction of motion. Instead, we must use a vector.
2.1
Vectors and Scalars
A vector has magnitude and direction, examples being displacement (change of position), velocity, acceleration, etc. Actually, not all physical quantities involve direction, examples being temperature, mass, pressure, time, etc. These physical quantities are not vectors because they do not point in any direction, and we call them scalars.
A vector, such as a displacement vector, can be represented graphically by an arrow denoting the magnitude and direction of the vector. All arrows of the same direction and magnitude denote the same vector, as in Fig.2.1a for the case of a displacement vector.
The displacement vector in Fig.2.1b tells us nothing about the actual path taken from point A to B. Thus, displacement vectors represent only the overall effect of the motion, not the motion itself.
Another way to specify a vector is to determine its magnitude and the angle it makes with a reference direction, as in Example 2.1.
H. A. Radi and J. O. Rasmussen, Principles of Physics, 17 Undergraduate Lecture Notes in Physics, DOI: 10.1007/978-3-642-23026-4_2,
Fig. 2.1 (a) Three vectors of the same direction and magnitude represent the same displacement. (b) All three paths connecting the two points A and B correspond to the same displacement vector
A1 B1 A B A2 B2 A B (a) (b) Example 2.1
A person walks 3 km due east and then 2 km due north. What is his displacement vector?
Solution: We first make an overhead view of the person’s movement as shown in Fig.2.2. The magnitude of the displacement d is given by the Pythagorean theorem as follows:
d =(3 km)2+ (2 km)2= 3.61 km
The angle that this displacement vector makes relative to east is given by:
tanθ = 2 km
3 km = 0.666... Then:θ = tan−1(0.666...) = 33.69◦
Thus, the person’s displacement vector is 56.31◦east of north.
Fig. 2.2 Start End 3 km 2 km d θ E N W S
2.2 Properties of Vectors 19
2.2
Properties of Vectors
In text books, it is common to use boldface symbols to identify vectors, such as
A, B, etc., but in handwriting it is usual to place an arrow over the symbol, such as,
→
A,B→, etc. Throughout this text we shall use the handwriting style only and use the
italic symbols A, B, etc. to indicate the magnitude of vectors.
Equality of Vectors
The two vectors A→ andB→are said to be equal if they have the same magnitude, i.e. A= B, and point in the same direction; see for example the three equal vectors
AB, A1B1, and A2B2in Fig.2.1a.
Addition of Vectors
Of course, all vectors involved in any addition process must have the same units. The rules for vector sums can be illustrated by using a graphical method. To add vector B→to vector A→, we first draw vector A→on graph paper with its magnitude represented by a convenient scale, and then draw vectorB→to the same scale with its tail coinciding with the arrow head ofA→, see Fig.2.3a. This is known as the triangle method of addition. Thus, the resultant vector R→is the red vector drawn from the tail of A→to the head ofB→and is shown in the vector addition equation:
→
R =→A +B→, (2.1)
which says that the vector R→is the vector sum of vectors A→andB→. The symbol +
in Eq.2.1and the words “sum” and “add” have different meanings for vectors than they do in elementary algebra of scalar numbers.
(a) (b) A A B A B
=
+ R A B=
+ R A B B = + R A BFig. 2.3 (a) In the triangle method of addition, the resultant vector →R is the red vector that runs from the tail of →A to the head of →B. (b) In the parallelogram method of addition, the resultant vec-tor →R is the red diagonal vector that starts from the tails of both →A and →B. This method shows that→A +→B =→B +→A
An alternative graphical method for adding two vectors is the parallelogram rule of addition. In this method, we superpose the tails of the two vectors A→and→B; then
the resultant →R will be the diagonal of the parallelogram that starts from the tail of both →A and→B (which form the sides of that parallelogram), as shown in Fig.2.3b.
Vector addition has two important properties. First, the order of addition does not matter, and this is known as the commutative law of addition, i.e.
→
A +B→=B→+A→ (Commutative law) (2.2)
Second, if there are more than two vectors, their sum is independent of the way in which the individual vectors are grouped together. This is known as the associative law of addition, i.e.
→
A + (→B +C→) = (A→+→B) +C→ (Associative law) (2.3)
The Negative of a Vector
The negative of a vector B→is a vector with the same magnitude which points in the opposite direction, namely−→B, see Fig.2.4a. Therefore, when we add a vector and its negative we will get zero, i.e.
→
B + (−B→) = 0 (2.4)
Adding−B→to A→has the same effect of subtracting B→from →A, see Fig.2.4b, i.e. → S =A→+ (−→B) =A→−B→ (2.5) (a) (b) B -B
=
-B -S A B AFig. 2.4 (a) This part of the figure shows vector→B and its corresponding negative vector−→B, both of which have the same magnitude but are opposite in direction. (b) To subtract vector→B from vector→A, we add the vector−→B to vector→A to get→S =→A −→B
2.2 Properties of Vectors 21
Example 2.2
A car travels 6 km due east and then 4 km in a direction 60◦north of east. Find the magnitude and direction of the car’s displacement vector by using: (a) the graphical method, and (b) the analytical method.
Solution: (a) Let A→ be a vector directed due east with magnitude A= 6 km and B→be a vector directed 60◦north of east with magnitude B= 4 km. Using graph paper with a reasonable scale and a protractor, we draw the two vectors →
A and→B; then we measure the length of the resultant vector R→. The
measure-ments shown in Fig.2.5indicates that R= 8.7 km. Also, the angle φ that the resultant vectorR→makes with respect to the east direction can be measured and will giveφ = 23.4◦. Fig. 2.5 ° Start End 6 km 4k m θ E N W S 60° A B R φ sin 60 B
(b) The analytical solution for the magnitude of →R can be obtained from geom-etry by using the law of cosines R = √A2+ B2− 2AB cos θ as applied to an obtuse triangle with angleθ = 180◦− 60◦= 120◦, see exercise (10b). Thus:
R=A2+ B2− 2 AB cos θ
=(6 km)2+ (4 km)2− 2(6 km)(4 km) cos 120◦ =(36 + 16 + 24) (km)2= 8.72 km
The angle that this displacement vectorR→makes relative to the east direction, see Fig.2.5, is given by:
sinφ = B sin 60 ◦ R = 4 km sin 60◦ 8.72 km = 0.397 Then:φ = sin−1(0.397) = 23.41◦.
2.3
Vector Components and Unit Vectors
Vector Components
Adding vectors graphically is not recommended in situations where high precision is needed or in three-dimensional problems. A better way is to make use of the projections of a vector along the axes of a rectangular coordinate system.
Consider a vector A→ lying in the xy-plane and making an angle θ with the positive x-axis, see Fig.2.6. This vector →A can be expressed as the sum of two vectors→Ax and
→
Aycalled the rectangular vector components of →
A along the x-axis and y-axis, respectively. Thus:
→
A =→Ax+A→y (2.6)
Fig. 2.6 A vector→A in the xy-plane can be presented by its rectangular vector components→Axand→Ay, where →A =→A x+→Ay θ A x y Ay Ax o
From the definitions of sine and cosine, the rectangular components ofA→, namely Axand Ay, will be given by:
Ax = A cos θ and Ay= A sin θ , (2.7) where the sign of the components Axand Aydepends on the angleθ.
The magnitudes Axand Ayform two sides of a right triangle that has a hypotenuse of magnitude A. Thus, from Ax and Aywe get:
A= A2 x + Ay2 and θ = tan−1 Ay Ax (2.8)
The inverse tan obtained from your calculator is from −90◦< θ < 90◦. This may lead to incorrect answer when 90◦< θ ≤ 360◦. A method used to achieve the correct answer is to calculate the angleφ such as:
2.3 Vector Components and Unit Vectors 23
φ = tan−1|A y|/|Ax|
(2.9)
Then, depending on the signs of Axand Ay, we identify the quadrant where the vector →
A lies, as shown in Fig.2.7.
x y |Ax| A o x y o x y o x y o |Ay| |Ax| A |Ay| θ |Ax| A |Ay| |Ax| A |Ay| θ θ Ax positive Ax negative Ay negative Ax positive Ay positive Ax negative Ay negative Ay positive φ φ φ θ Quadrant I Quadrant II
Quadrant III Quadrant IV
θ ≡ φ
Fig. 2.7 The signs of Axand Aydepend on the quadrant where the vector→A is located
Once we determine the quadrant, we calculateθ using Table2.1.
Table 2.1 Calculatingθ from φ according to the signs of Ax and Ay
Sign of Ax Sign of Ay Quadrant Angleθ
+ + I θ = φ
− + II θ = 180◦− φ
− − III θ = 180◦+ φ
+ − IV θ = 360◦− φ
Unit Vectors
A unit vector is a dimensionless vector that has a magnitude of exactly one and points in a particular direction, and has no other physical significance. The unit vectors in
the positive direction of the x, y, and z axes of a right-handed coordinate system are often labeled→i,→j, and→k, respectively; see Fig.2.8. The magnitude of each unit vector equals unity; that is:
|→i | = |→j | = |→k| = 1 (2.10) x y o x y o OR Z Z i k j i j k
Fig. 2.8 Unit vectors→i,→j, and→k define the direction of the commonly-used right-handed coordinate system
Consider a vector →A lying in the xy-plane as shown in Fig.2.9. The product of the component Axand the unit vector→i is the vector→Ax= Ax
→
i, which is paral-lel to the x-axis and has a magnitude Ax. Similarly,A→y= Ay→j is a vector parallel to the y-axis and has a magnitude Ay. Thus, in terms of unit vectors we writeA→
as follows:
→
A = Ax→i + Ay→j (2.11)
Fig. 2.9 A vector→A in the xy-plane can be represented by its rectangular components Ax and Ayand the unit vectors →i and→j, and can be written as→A = Ax→i + Ay→j A x y Axi o Ay j
This method can be generalized to three-dimensional vectors as: → A = Ax → i + Ay → j + Az → k (2.12)
2.3 Vector Components and Unit Vectors 25 We can define a unit vector→n along any vector, say,A→, as follows:
→ n =
→
A
A. (2.13)
Adding Vectors by Components
Suppose we wish to add the two vectors A→= Ax → i + Ay → j andB→= Bx → i + By → j using the components method, such as:
→
R =→A+B→
= (Ax→i + Ay→j ) + (Bx→i + By→j )
= (Ax+ Bx)→i + (Ay+ By)→j (2.14) If the vector sum R→is denoted by→R = Rx
→ i + Ry
→
j, then the components of the resultant vector will be given by:
Rx= Ax+ Bx
Ry= Ay+ By
(2.15)
The magnitude of R→can then be obtained from its components or the components of A→and B→using the following relationships:
R= R2 x+ R2y = (Ax+ Bx)2+ (Ay+ By)2 (2.16)
and the angle that R→makes with the x-axis can also be obtained by using the fol-lowing relationships: θ = tan−1Ry Rx = tan−1Ay+ By Ax+ Bx (2.17)
The components method can be verified using the geometrical method, as shown in Fig.2.10.
IfA→= Ax→i +Ay→j +Az→k and→B = Bx→i +By→j +Bz→k, then we can generalize the previous case to three dimensions as follows:
→ R =A→+→B = (Ax+ Bx) → i + (Ay+ By) → j + (Az+ Bz) → k = Rx → i + Ry → j + Rz → k (2.18)
Fig. 2.10 Geometric representation of the sum of the two vectors→A and→B, showing the relationship between the components of the resultant→R and the
components of→A and→B x y o i j B R Ax Rx Bx By Ay Ry A θ Example 2.3
Find the sum of the following two vectors: →
A = 8→i + 3→j →
B = −5→i − 7→j
For convenience, the units of the two vectors have been omitted, but for instance, you may take them to be kilometers.
Solution: The two vectors lie in the xy-plane, since there is no component in the z-axis. By comparing the two expressions ofA→and→B with the gen-eral relations A→= Ax → i + Ay → j and →B = Bx → i + By → j we see that, Ax= 8,
Ay= 3, Bx= − 5, and By= − 7. Therefore, the resultant vector R is obtained by using Eq.2.14as follows:
→ R =→A +B→= (Ax+ Bx) → i + (Ay+ By) → j = (8 − 5)→i + (3 − 7)→j = 3→i − 4→j That is: Rx= 3 and Ry= −4. The magnitude of
→ R is given according to Eq.2.16as: R= R2 x + Ry2= (3)2+ (−4)2=√9+ 16 =√25= 5
2.3 Vector Components and Unit Vectors 27 while the value of the angle θ that→R makes with the positive x-axis is given according to Eq.2.17as:
θ = tan−1 Ry Rx = tan−1 −4 3 = 360◦− tan−1 4 3 = 360◦− 53◦= 307◦
where we used Table2.1to calculateθ in case of negative Ry(Q IV).
2.4
Multiplying Vectors
Multiplying a Vector by a Scalar
If we multiply vector A→by a scalar a we get a new vector→B, i.e.
→
B = aA→ (2.19)
The vector B→ has the same direction as A→ if a is positive but has the opposite direction if a is negative. The magnitude of B→is the product of the magnitude of A→
and the absolute value of a.
The Scalar Product (or the Dot Product)
The scalar product of the two vectors A→and→B is denoted by A→• B→ and is defined as:
→
A •B→= AB cos θ (2.20)
where A and B are the magnitudes of the two vectorsA→andB→, and θ is the angle
between them, see Fig.2.11. The two anglesθ and 360◦− θ could be used, since their cosines are the same. As we see from Eq.2.20, the result ofA→•B→is a scalar quantity, and is known as the dot product from its notation. Also, we get:
→ A •B→= AB cos θ = ⎧ ⎪ ⎪ ⎨ ⎪ ⎪ ⎩ +AB if θ = 0◦ 0 ifθ = 90◦ −AB if θ = 180◦ (2.21)
According to Fig.2.11, the dot product can be regarded as the product of the magnitude of one of the vectors with the scalar component of the second along the direction of the first. That is:
A B A B A B θ θ θ cos A
θ
cos Bθ
Fig. 2.11 The left part shows two vectors →A and →B, with an angle θ between them. The middle and the right parts show the component of each vector along the other
→
A • B→= (A cos θ)B = A(B cos θ) (2.22) This indicates that scalar products obey the commutative and associative laws, so that:
→
A • →B =B→•A→ (Commutative law) (2.23)
→
A • (B→+C→) =A→• →B +A→•C→ (Associative law) (2.24) By applying the definition of dot product to the unit vectors→i,→j, and→k, we get the following:
→
i • →i =→j • →j =→k • →k = 1 →
i • →j =→i • →k =→j • →k = 0 , (2.25) where the angle between any two identical unit vectors is 0◦and the angle between any two different unit vectors is 90◦.
When two vectors are written in terms of the unit vectors→i,→j, and→k, then to get their dot product, each component of the first vector is to be dotted into each component of the second vector. After that, we use Eq.2.25to get the following:
→
A • →B = (Ax→i + Ay→j + Az→k) • (Bx→i + By→j + Bz→k)
= AxBx+ AyBy+ AzBz (2.26)
Thus, from Eqs.2.20 and 2.26, we can generally write the dot product as follows:
→
2.4 Multiplying Vectors 29
Example 2.4
Find the angle between the vectorA→= 8→i +3→j and the vector B= −5→i −7→j . Solution: Since A= A2 x+ Ay2and B= B2
x+ By2, then using the dot product given by Eq.2.20we get:
→
A • B→= AB cos θ =82+ 32×(−5)2+ (−7)2cosθ = 8.544 × 8.60 cos θ
= 73.5 cos θ
Keeping in mind that there is no component for A→andB→along the z-axis, we can find the dot product from Eq.2.26as follows:
→
A •B→= AxBx+ AyBy+ AzBz
= 8 × (−5) + 3 × (−7) + 0 × 0 = −61
Equating the results of the last two steps to each other, we find:
73.5 cos θ = −61 Thus: θ = cos−1 −61 73.5 = 146.1◦.
The Vector Product (or the Cross Product)
The vector product of the two vectors A→and →B is denoted by A→×B→and defined as a third vector C→whose magnitude is:
C= AB sin θ , (2.28)
whereθ is the smaller angle between A→andB→(hence, 0≤ sin θ ≤ 1). The direction ofC→is perpendicular to the plane that contains both →A and B→, and can be determined
by using the right-hand rule, see Fig.2.12. To apply this rule, we allow the tail of →
A to coincide with the tail of →B, then the four fingers of the right hand are pointed
right thumb is the direction of C→, i.e. the direction of →A ×→B. Also, the direction of
→
C is determined by the direction of advance of a right-handed screw as shown in Fig.2.12. Right-hand rule Direction of Advance A B C =A B θ
Fig. 2.12 The vector product→A×→B is a third vector→C that has a magnitude of AB sinθ and a direction perpendicular to the plane containing the vectors→A and→B. Its sense is determined by the right-hand rule or the direction of advance of a right-handed screw
The vector product definition leads to the following properties:
1. The order of vector product multiplication is important; that is: →
A×B→= −(B→×A→) (2.29)
which is unlike the scalar product and can be easily verified with the right-hand rule.
2. If A→is parallel to →B (that is,θ = 0◦) or →A is antiparallel to →B (that is,θ = 180◦), then:
→
A×→B = 0 (if →A is parallel or antiparallel to B→) (2.30) 3. If A→is perpendicular to B→, then:
|A→×→B| = AB (if A→⊥B→) (2.31) 4. The vector product obeys the distributive law, that is:
→
A × (B→+C→) =A→×→B +A→×C→ (Distributive law) (2.32) 5. The derivative of A→×B→with respect to any variable such as t is:
d dt( → A×B→) =A→×d → B dt + dA→ dt × → B (2.33)
2.4 Multiplying Vectors 31 6. From the definition of the vector product and the unit vectors→i, →j, and→k, we
get the following relationships: →
i ×→i =→j ×→j =→k×→k = 0 (2.34) →
i × →j =→k, →j × →k =→i, →k × →i =→j (2.35) The last relations can be obtained by setting the unit vectors→i ,→j , and →k on a circle, see Fig.2.13, and rotating in a clockwise direction to find the cross product of one unit vector with another. Rotating in a counterclockwise direction will involve a negative sign of the cross product of one unit vector with another, that is:
→
i ×→k = −→j, →k ×→j = −→i, →j ×→i = −→k (2.36)
Fig. 2.13 The clockwise and counterclockwise cyclic order for finding the cross product of the unit vectors→i,→j, and→k
k + + +
-j i7. When two vectors A→andB→are written in terms of the unit vectors→i , →j , and →
k, then the cross product will give the result: → A×→B = (Ax → i + Ay → j + Az → k) × (Bx → i + By → j + Bz → k) = (AyBz− AzBy) → i + (AzBx− AxBz) → j + (AxBy− AyBx) → k (2.37)
This result can be expressed in determinant form as follows:
→ A×B→= → i →j →k AxAy Az BxBy Bz = → i AyAz ByBz − → j Ax Az Bx Bz + → k Ax Ay Bx By (2.38)