NORTH-HOLLAND SERIES IN
APPLIED MATHEMATICS
AND MECHANICS
EDITORS:
E. BECKER
Institut fur
Technische
Mechanik
Hochschule,
Darmstadt
B. B U D I A N S K Y
Division
of Applied
Harvard
Sciences
University
W.T. KOITER
Laboratory
of Applied
University
H.A.
Institute
Mechanics
of Technology,
Delft
LAUWERIER
of Applied
University
of
Mathematics
Amsterdam
V O L U M E 21
N O R T H - H O L L A N D PUBLISHING C O M P A N Y - A M S T E R D A M · NEW YORK · O X F O R D
AN INTRODUCTION TO
THERMOMECHANICS
Hans ZIEGLER
Swiss Federal Institute of Technology,
Zurich
and
University of Colorado,
Boulder
Second, revised edition
1983
N O R T H - H O L L A N D P U B L I S H I N G C O M P A N Y - A M S T E R D A M · N E W YORK · O X F O R D
© N O R T H - H O L L A N D PUBLISHING COMPANY—1983
All rights reserved. No part of this publication may be
reproduced,
stored in a retrieval system, or transmitted, in any form or by any means,
electronic, mechanical, photocopying,
recording or otherwise, without the prior
permission of the Copyright
owner.
First printing 1977
Second, revised edition 1983
PUBLISHERS:
N O R T H - H O L L A N D PUBLISHING C O M P A N Y
A M S T E R D A M OXFORD NEW YORK
SOLE DISTRIBUTORS FOR T H E U . S . A . A N D C A N A D A :
ELSEVIER SCIENCE PUBLISHING C O M P A N Y , Inc.
52 VANDERBILT A V E N U E
NEW YORK, N.Y. 10017, U . S . A .
Library of Congress Cataloging in Publication Data
Ziegler, Hans, 1910 - An introduction to
{North-Holland
series in applied mathematics
Bibliography: 2 pp.
Includes index.
1. Thermodynamics.
2. Continuum
I. Title.
thermomechanics.
and mechanics, 21)
mechanics.
QC311.ZE
531
76-973
ISBN 0-444-86503-9
P R I N T E D IN T H E N E T H E R L A N D S
PREFACE
C o n t i n u u m m e c h a n i c s d e a l s w i t h d e f o r m a b l e b o d i e s . I n its e a r l y s t a g e s it
w a s c o n f i n e d t o a few s p e c i a l m a t e r i a l s a n d t o p a r t i c u l a r s i t u a t i o n s , n a m e l y
t o ideal liquids or t o elastic solids u n d e r i s o t h e r m a l or a d i a b a t i c c o n d i t i o n s .
I n t h e s e s p e c i a l c a s e s it is p o s s i b l e t o s o l v e t h e b a s i c p r o b l e m , i . e . , t o
d e t e r m i n e t h e flow a n d p r e s s u r e distributions or the d e f o r m a t i o n a n d stress
fields in p u r e l y m e c h a n i c a l t e r m s . T h i s is d u e t o t h e fact t h a t t h e s o l u t i o n
c a n b e d e v e l o p e d f r o m a set o f d i f f e r e n t i a l e q u a t i o n s w h i c h d o e s n o t
contain the energy balance.
From
the
viewpoint
of
general
continuum
mechanics,
however,
p r o b l e m s o f t h i s t y p e a r e s i n g u l a r . A n y o n e w o r k i n g in t h i s field k n o w s t h a t
s o o n e r o r l a t e r h e g e t s i n v o l v e d in t h e r m o d y n a m i c s . T h e r e a s o n f o r t h i s is
t h a t in g e n e r a l a c o m p l e t e set o f d i f f e r e n t i a l e q u a t i o n s c o n t a i n s t h e e n e r g y
balance. Since p a r t of the energy exchange takes place as heat flow, the
a p p r o p r i a t e f o r m o f t h e e n e r g y b a l a n c e is t h e first f u n d a m e n t a l l a w o f
thermodynamics,
and
it b e c o m e s
clear
therefore
that
it is
impossible to separate the mechanical aspect of a p r o b l e m
generally
from
the
t h e r m o d y n a m i c processes accompanying the motion. T o obtain a solution,
the f u n d a m e n t a l laws of b o t h mechanics a n d t h e r m o d y n a m i c s must be
applied.
In gas dynamics and
in t h e r m o e l a s t i c i t y
this has long
been
recognized.
T h i s s i t u a t i o n h a s its c o u n t e r p a r t in t h e r m o d y n a m i c s . U n t i l r e c e n t l y t h e
i n t e r e s t in t h i s field w a s a l m o s t e x c l u s i v e l y f o c u s e d o n p a r t i c u l a r l y s i m p l e
b o d i e s , mainly o n inviscid gases, characterized by certain state variables as,
e . g . , v o l u m e , p r e s s u r e a n d t e m p e r a t u r e . I n o t h e r b o d i e s , h o w e v e r , o r if
v i s c o s i t y is t o b e t a k e n i n t o a c c o u n t , o n e is c o m p e l l e d t o u s e c o n c e p t s f r o m
continuum mechanics, replacing the volume by the strain tensor and the
p r e s s u r e b y t h e s t r e s s t e n s o r . It m a y e v e n b e n e c e s s a r y t o h a v e r e c o u r s e t o
the m o m e n t u m
theorems,
and
to account
for
the
kinetic energy
in
f o r m u l a t i n g t h e first f u n d a m e n t a l l a w . I n s h o r t , t h e r m o d y n a m i c s c a n n o t
be separated from continuum mechanics.
I n v i e w o f t h e s e s t a t e m e n t s it b e c o m e s c l e a r t h a t c o n t i n u u m m e c h a n i c s
and
thermodynamics
are inseparable: a general theory of
continuum
vi
m e c h a n i c s a l w a y s i n c l u d e s t h e r m o d y n a m i c s a n d vice v e r s a . T h e e n t i r e field
is t r u l y i n t e r d i s c i p l i n a r y a n d r e q u i r e s a u n i f i e d t r e a t m e n t , w h i c h
p r o p e r l y b e d e n o t e d a s thermomechanics.
may
S u c h a u n i f i e d t r e a t m e n t is t h e
topic of this b o o k .
In order to a m a l g a m a t e t w o b r a n c h e s of science, o n e needs a c o m m o n
l a n g u a g e . C o n t i n u u m m e c h a n i c s h a s a l w a y s b e e n a field t h e o r y , e v e n in its
r u d i m e n t a r y f o r m s like h y d r a u l i c s o r s t r e n g t h o f m a t e r i a l s . T o t r e a t e v e n
such a simple p r o b l e m as b e n d i n g of a b e a m , o n e m u s t recognize t h a t the
states of strain a n d stress d e p e n d o n position a n d possibly o n t i m e . T h e
o b j e c t o f t h e r m o d y n a m i c s , o n t h e o t h e r h a n d , h a s a l w a y s b e e n a finite
v o l u m e , e.g., a m o l e , a n d the state within the b o d y has been
tacitly
a s s u m e d t o b e t h e s a m e t h r o u g h o u t t h e e n t i r e v o l u m e . It is s u r p r i s i n g t h a t
this p h i l o s o p h y h a s been m a i n t a i n e d even at t h e age of statistical a n d
quantum
mechanics, although
it is c l e a r l y i n c o n s i s t e n t
with the
first
f u n d a m e n t a l l a w in its c o m m o n f o r m : A t least p a r t o f t h e h e a t s u p p l y
a p p e a r i n g in t h i s l a w is d u e t o h e a t flow t h r o u g h t h e s u r f a c e o f t h e b o d y .
A s long as this process goes o n , t h e t e m p e r a t u r e of t h e elements n e a r t h e
surface differs from the o n e of the elements further inside t h e b o d y ; the
s t a t e o f t h e b o d y is t h e r e f o r e n o t h o m o g e n e o u s .
There are t w o ways out of this dilemma.
T h e h i s t o r i c a l w a y , still d o m i n a t i n g v a s t a r e a s o f t e a c h i n g in t h e r m o d y
n a m i c s , c o n s i s t s in t h e r e s t r i c t i o n t o i n f i n i t e l y s l o w p r o c e s s e s . I n p l a c e o f
actual processes o n e considers sequences of (homogeneous)
equilibrium
s t a t e s . E x c e p t f o r a few s p e c i a l c a s e s , s u c h i d e a l i z e d p r o c e s s e s a r e p r a c t i
cally r e v e r s i b l e , a n d t h i s e x p l a i n s w h y in classical t h e r m o d y n a m i c s
(or
rather thermostatics) the limiting case of reversibility plays such a d o m i
n a n t r o l e . H o w e v e r , t h e e n g i n e e r e n g a g e d in t h e c o n s t r u c t i o n o f t h e r m o m e c h a n i c a l m a c h i n e r y c a n n o t limit h i m s e l f t o i n f i n i t e l y s l o w p r o c e s s e s a n d
hence has never t a k e n this restriction seriously. T h e situation strongly re
s e m b l e s t h e o n e in p r e - N e w t o n i a n m e c h a n i c s w i t h its a t t e m p t s t o d e v e l o p
dynamics from purely static concepts.
T h e m o d e r n w a y o u t o f t h e d i l e m m a is d i f f e r e n t b u t s u r p r i s i n g l y s i m p l e :
instead of infinitely slow processes o n e considers infinitesimal elements of
t h e b o d y in w h i c h a p r o c e s s t a k e s p l a c e , a d m i t t i n g t h a t t h e s t a t e v a r i a b l e s
differ
from
element
to
element.
In
other
words:
one
conceives
t h e r m o d y n a m i c s a s a field t h e o r y in m u c h t h e s a m e w a y a s c o n t i n u u m
m e c h a n i c s h a s b e e n t r e a t e d f o r m o r e t h a n 2 0 0 y e a r s . I n s u c h a field t h e o r y ,
r e a s o n a b l y fast p r o c e s s e s c a n b e t r e a t e d w i t h t h e s a m e e a s e a s s l o w o n e s ,
vii
a n d restriction t o reversible processes b e c o m e s unnecessary. Finally, this
field t h e o r y is t h e p r o p e r f o r m in w h i c h t h e r m o d y n a m i c s a n d c o n t i n u u m
m e c h a n i c s a r e easily a m a l g a m a t e d .
The
strong
interdependence
thermodynamics
was
generally
of
continuum
recognized
about
mechanics
three
and
decades
ago.
V a r i o u s s c h o o l s h a v e s i n c e c o n t r i b u t e d t o t h e r m o m e c h a n i c s , e a c h f r o m its
p o i n t o f v i e w a n d in its o w n l a n g u a g e o r f o r m a l i s m . It is n o t t h e a i m o f t h i s
book to report on the various approaches nor to compare them. The book
is i n t e n d e d a s a n introduction
to this fascinating
field, b a s e d o n
the
simplest possible a p p r o a c h .
E x c e p t f o r a n i n t r o d u c t i o n t o t h e t h e o r y o f c a r t e s i a n t e n s o r s t h e first
three chapters are concerned with the mechanical laws governing
motion
of
a continuum.
They
are based
on
considerations
of
the
mass
geometry, o n the principle of virtual power a n d o n a general form of the
r e a c t i o n p r i n c i p l e . It is well k n o w n t h a t t h e m o s t g e n e r a l a p p r o a c h
to
c o n t i n u u m m e c h a n i c s m a k e s u s e o f t h e d i s p l a c e m e n t field a n d o f m a t e r i a l ,
a n d hence curvilinear, c o o r d i n a t e s . F o r a beginner, however, this a p p r o a c h
presents c o n s i d e r a b l e m a t h e m a t i c a l difficulties t h a t a r e a p t t o o b s c u r e the
p h y s i c a l c o n t e n t s . S i n c e p h y s i c s d e s e r v e s p r i o r i t y in a n i n t r o d u c t i o n o f t h i s
t y p e , a t r e a t m e n t b a s e d o n t h e v e l o c i t y field h a s m a n y a d v a n t a g e s a n d h a s
t h e r e f o r e b e e n p r e f e r r e d . T h i s k i n d o f a p p r o a c h h a s b e e n p r e s e n t e d in a
masterly
fashion
by
Prager
in
his
"Introduction
to
Mechanics
of
C o n t i n u a " , a n d s i n c e t h e r e is n o t m u c h p o i n t in m a k i n g c h a n g e s j u s t f o r
t h e s a k e o f o r i g i n a l i t y , t h e first t h r e e c h a p t e r s a n d c e r t a i n p o r t i o n s o f t h e
subsequent applications are similar to the corresponding parts of P r a g e r ' s
book.
C h a p t e r 4 deals with thermodynamics.
representation,
familiar
from
textbooks
It s t a r t s
from
in t h i s field,
the
classical
introduces
and
discusses the concept of (independent a n d d e p e n d e n t ) state variables, a n d
s h o w s h o w t h e f u n d a m e n t a l l a w s c a n b e f o r m u l a t e d in t e r m s o f a field
t h e o r y . A c h a r a c t e r i s t i c p o i n t o f t h e p r e s e n t t r e a t m e n t is t h e f a c t t h a t t h e
stress a p p e a r s as t h e s u m of a quasiconservative a n d a dissipative stress.
T h e first is a s t a t e f u n c t i o n , d e p e n d e n t o n t h e free e n e r g y , t h e s e c o n d is
c o n n e c t e d with t h e dissipation function. In view of later
developments
( C h a p t e r 14) t h e r o l e o f t h e t w o f u n c t i o n s is e m p h a s i z e d . T h e d e f o r m a t i o n
h i s t o r y is r e p r e s e n t e d in t h e s i m p l e s t p o s s i b l e m a n n e r , n a m e l y b y i n t e r n a l
parameters.
C h a p t e r 5 deals with the characteristic properties of various materials. A
viii
r o u g h c l a s s i f i c a t i o n o f b o d i e s is p r e s e n t e d , a n d t h e c o n s t i t u t i v e e q u a t i o n s
o f s o m e c o n t i n u a a r e d i s c u s s e d . T h e g e n e r a l t h e o r e m s e s t a b l i s h e d in t h e
preceding chapters, supplemented by the proper constitutive
determine
the
thermomechanical
behavior
of
a
given
relations,
body.
This
is
i l l u s t r a t e d in C h a p t e r s 6 t h r o u g h 1 1 , w h i c h d e a l w i t h t h e a p p l i c a t i o n o f t h e
theory to various types of c o n t i n u a .
C h a p t e r s 12 a n d 13 c o n t a i n a s h o r t o u t l i n e o f g e n e r a l t e n s o r s a n d t h e i r
a p p l i c a t i o n in t h e s t u d y o f l a r g e d i s p l a c e m e n t s . T h e r e p r e s e n t a t i o n f o l l o w s
t h e lines o f G r e e n a n d Z e r n a in t h e i r e x c e l l e n t b o o k o n
"Theoretical
E l a s t i c i t y \ T h e i n c l u s i o n o f t h i s m a t e r i a l m a k e s it p o s s i b l e , in p a r t i c u l a r ,
,
t o p o i n t o u t (a) t h e i m p o r t a n c e o f a p r o p e r c h o i c e o f t h e s t r a i n m e a s u r e a n d
o f t h e c o r r e s p o n d i n g s t r e s s , a n d (b) t h e d i f f e r e n c e b e t w e e n c o v a r i a n t a n d
contravariant
c o m p o n e n t s of a tensor, essential for t h e p r o o f of
the
o r t h o g o n a l i t y c o n d i t i o n in C h a p t e r 14.
U p t o a n d i n c l u d i n g C h a p t e r 13 t h e s u b j e c t m a t t e r , in s p i t e o f a p e r s o n a l
t i n g e in t h e p r e s e n t a t i o n ,
remains within confines
that appear to
be
generally accepted by n o w . T h e remainder of the b o o k transgresses these
t r a d i t i o n a l l i m i t s . It m a y b e c o n s i d e r e d , t o g e t h e r w i t h C h a p t e r 4 , a s a
synopsis of the a u t h o r ' s c o n t r i b u t i o n s to t h e r m o m e c h a n i c s ,
published
f r o m 1957 o n w a r d s , o c c a s i o n a l l y w i t h t h e a s s i s t a n c e o f D r . J u r g N a n n i a n d
P r o f e s s o r C h r i s t o p h W e h r l i . It is c l e a r t h a t in a s y n o p s i s o f t h i s t y p e m a n y
p o i n t s w h i c h o n c e s e e m e d e s s e n t i a l b u t h a v e lost t h e i r i m p o r t a n c e c a n b e
dropped,
and
it is e q u a l l y
obvious
that
many
thoughts
which
once
a p p e a r e d v a g u e h a v e s i n c e a s s u m e d a m o r e c o n c i s e f o r m . I n c i d e n t a l l y , in a
field
which
is still in
a
state
of
development
a
certain
amount
of
c o n t r o v e r s y c a n n o t b e a v o i d e d ; in t h i s r e s p e c t I a s s u m e full r e s p o n s i b i l i t y
for t h e final c h a p t e r s .
C h a p t e r 14 r e t u r n s t o t h e b a s i s o f t h e r m o d y n a m i c s . T h e c l a s s i c a l t h e o r y ,
restricted to reversible processes, tacitly excludes gyroscopic forces. W i t h
e x a c t l y t h e s a m e r i g h t t h e y m a y b e e x c l u d e d in t h e i r r e v e r s i b l e c a s e . T h e
o b v i o u s w a y o f d o i n g t h i s is t o a s s u m e t h a t t h e d i s s i p a t i v e s t r e s s e s a r e
d e t e r m i n e d b y t h e d i s s i p a t i o n f u n c t i o n a l o n e m u c h in t h e s a m e w a y a s t h e
q u a s i c o n s e r v a t i v e f o r c e s d e p e n d o n t h e free e n e r g y . F o r c e r t a i n s y s t e m s , t o
be called e l e m e n t a r y ,
the connection
between dissipative stresses
dissipation function then turns out to have the form of a n
condition,
and
orthogonality
a n d it f o l l o w s t h a t t w o s c a l a r f u n c t i o n s , t h e free e n e r g y a n d t h e
dissipation function (or the rate of e n t r o p y p r o d u c t i o n ) completely govern
a n y kind of process.
ix
C h a p t e r 15 s h o w s t h a t t h e o r t h o g o n a l i t y c o n d i t i o n is e q u i v a l e n t t o a
n u m b e r of e x t r e m u m principles, a m o n g t h e m a principle of m a x i m a l rate
of e n t r o p y p r o d u c t i o n . T h i s last principle suggests a generalization of the
o r t h o g o n a l i t y c o n d i t i o n for systems of the so-called c o m p l e x type. This
g e n e r a l i z a t i o n will b e r e f e r r e d t o a s t h e orthogonality
principle,
a n d it is
e a s y t o see t h a t it r e d u c e s t o O n s a g e r ' s s y m m e t r y r e l a t i o n s in t h e l i n e a r
c a s e . F i n a l l y , C h a p t e r s 16 t h r o u g h 18 a r e c o n c e r n e d w i t h a p p l i c a t i o n s o f
the orthogonality condition a n d the orthogonality principle to
various
types of continua.
A s already m e n t i o n e d , I have tried to keep the m a t h e m a t i c a l formalism
a s s i m p l e a s p o s s i b l e . I a s s u m e , h o w e v e r , t h a t t h e r e a d e r is f a m i l i a r w i t h
vector
algebra
and
analysis,
with
the
basic
laws
of
mechanics
and
t h e r m o d y n a m i c s , w i t h t h e e l e m e n t s o f g e o m e t r y in ^ - d i m e n s i o n a l s p a c e
a n d of the theory of functions, a n d with the n o t i o n of convexity.
p r o v i d e t h e r e a d e r w i t h a m e a n s o f t e s t i n g his g r a s p o f t h e
To
matter,
p r o b l e m s have been a d d e d at the end of each section wherever this was
possible.
In
the
second
edition
of
this b o o k
the thermodynamic
aspect
of
c o n t i n u u m m e c h a n i c s h a s been stressed wherever this seemed desirable;
besides, s o m e weak points have been strengthened. In C h a p t e r 1 a section
d e a l i n g m a i n l y w i t h i n v a r i a n t s h a s b e e n a d d e d , a n d in t h i s c o n t e x t t h e b a s i c
i n v a r i a n t s o f s e c o n d - o r d e r t e n s o r s h a v e b e e n r e d e f i n e d . C h a p t e r s 11 a n d
18, d e a l i n g w i t h v i s c o e l a s t i c i t y , h a v e b e e n e x t e n d e d t o i n c l u d e t h e r m a l
e f f e c t s . T h e first o n e a p p e a r s s u p p l e m e n t e d b y a s e c t i o n , t h e s e c o n d o n e
h a s b e e n c o m p l e t e l y r e w r i t t e n . S e c t i o n 14.4 a p p e a r s in a n e w f o r m , a s d o
C h a p t e r 16, o n n o n - N e w t o n i a n l i q u i d s , a n d C h a p t e r 17, o n p l a s t i c i t y . I n
C h a p t e r 15 a s e c t i o n d e a l i n g w i t h t h e d e r i v a t i o n o f t h e s e c o n d f u n d a m e n t a l
law from the orthogonality condition has been a d d e d . O n the whole, the
terminology
has been
simplified,
particularly
in c o n n e c t i o n
with
the
classification of materials (fluids, solids a n d viscoelastic bodies). M a n y
m i n o r c h a n g e s h a v e b e e n m a d e , a n d m i s p r i n t s o f t h e first e d i t i o n h a v e b e e n
e l i m i n a t e d . M o s t o f t h e p r o b l e m s h a v e b e e n r e f o r m u l a t e d in s u c h a w a y
that they n o w show the m a i n results.
I a m greatly indebted to Professors William Prager and W a r n e r
T.
K o i t e r , w h o h a v e b o t h c r i t i c a l l y r e a d t h e m a n u s c r i p t o f t h e first e d i t i o n a n d
p r o v i d e d n u m e r o u s suggestions for i m p r o v e m e n t . I a m also grateful
to
Professors R a l p h C . Koeller a n d William L. W a i n w r i g h t for pointing o u t
t h a t s o m e o f t h e a p p l i c a t i o n s in S e c t i o n 15.3 a n d C h a p t e r
16 l a c k e d
χ
generality.
A
Hansheinrich
special
word
of
thanks
Ziegler,
for
his
valuable
is d u e
to
my
linguistic
son,
Professor
assistance
in
the
p r e p a r a t i o n o f t h e t e x t . I finally e x p r e s s m y g r a t i t u d e t o D r . C a r l o S p i n e d i
for
his h e l p ,
particularly
in p r o o f r e a d i n g ,
and
to the Daniel
Jenny
F o u n d a t i o n for s u p p o r t in t h e p r e p a r a t i o n o f t h e d r a w i n g s .
Z u r i c h , J u l y 1982
H a n s Ziegler
CHAPTER 1
MATHEMATICAL PRELIMINARIES
I n o r d e r t o d e s c r i b e t h e configuration
reference
system,
of a n arbitrary b o d y , we need a
e.g., a rigid b o d y o r f r a m e serving as a basis for the
o b s e r v e r . A n y q u a n t i t a t i v e t r e a t m e n t r e q u i r e s a coordinate
system
fixed t o
t h i s r e f e r e n c e f r a m e . O u r first t a s k is t o d e v e l o p t h e m a t h e m a t i c a l t o o l s
needed for the description of the m o t i o n or, m o r e generally, of a n y process
in
which
framework
the
body
must
in
consideration
be consistent
with
takes
the
fact
part.
that
The
mathematical
the choice
of
the
c o o r d i n a t e s y s t e m is a r b i t r a r y . I n c o n s e q u e n c e , o u r s t a r t i n g p o i n t m u s t b e
the study of coordinate t r a n s f o r m a t i o n s .
R e s t r i c t i n g o u r s e l v e s in
this
c h a p t e r t o c a r t e s i a n c o o r d i n a t e s y s t e m s , w e will d e v e l o p t h e c o n c e p t o f t h e
cartesian tensor.
1 . 1 . Cartesian t e n s o r s
L e t u s r e f e r ( F i g . 1.1) t h e t h r e e - d i m e n s i o n a l p h y s i c a l s p a c e t o a g i v e n
Fig. 1.1. Cartesian coordinate systems.
2
r e f e r e n c e f r a m e a n d h e r e t o a cartesian,
coordinate
system
x x ,x
u
axes. T h e axes X
2
i.e., rectangular a n d rectilinear,
w i t h u n i t v e c t o r s #Ί, ι , 1 3 a l o n g t h e c o o r d i n a t e
3
2
(p= 1 , 2 , 3 ) w i t h u n i t v e c t o r s I
p
define a n o t h e r cartesian
p
coordinate system with the s a m e origin O . Denoting t h e cosines between
the axes X
p
and x by c
t
we have, for arbitrary indices ρ a n d / between 1
p h
and 3,
c
= c o s (X , x ) = I -i .
pi
p
i
Let Ρ be a point with coordinates
p
(1.1)
i
i n t h e first s y s t e m . I t s c o o r d i n a t e s i n
the second system are the projections of the radius vector (or, equivalently,
o f t h e s e q u e n c e o f s t r a i g h t s e g m e n t s r e p r e s e n t i n g t h e xi) o n t o t h e a x e s
X.
p
M a k i n g use of (1.1), we obtain
X\=c x +c x
u
x
n
+ c x ,
2
n
X = c \X\ + c x
2
2
22
3
+ C23X3,
2
^3=^3,^+032^2 +
(1.2)
^ 3
a s c o o r d i n a t e t r a n s f o r m a t i o n s b e t w e e n t h e t w o c o o r d i n a t e s y s t e m s . It is
e a s y t o see t h a t t h e i n v e r s i o n s a r e
x =c X +c \X
l
u
l
2
x = c X\
2
+
2
+ c X
n
22
cX
3l
39
+ c X
>
(1-3)
^ = Σ c X,
(1.4)
2
32
3
3 - \?>X\ + 2 3 - ^ 2 + 3 3 - ^ 3 ·
x
C
c
c
A m o r e c o m p a c t w a y t o w r i t e ( 1 . 2 ) a n d ( 1 . 3 ) is
3
3
Χ =Σ
Cpi*b
Ρ
pi
p
p=\
1=1
w h e r e ρ is free i n t h e first e q u a t i o n , a n d / i n t h e s e c o n d o n e . W e m a y e v e n
dispense of the s u m m a t i o n symbol by a d o p t i n g , once a n d for all, t h e soc a l l e d summation
convention
stipulating that whenever
a letter
index
a p p e a r s t w i c e in a p r o d u c t t h e s u m is t o b e t a k e n o v e r t h i s i n d e x . W e t h u s
w r i t e , in p l a c e o f ( 1 . 4 ) ,
Xp
=
pi i>
c
x
i
x
=
CpiXp ·
(1 · 5)
It is c l e a r t h a t a n i n d e x a p p e a r i n g o n c e i n a t e r m o f a n e q u a t i o n l i k e ( 1 . 5 )
m u s t a p p e a r in every single t e r m . O n t h e o t h e r h a n d , t h e s u m m a t i o n index
is s o m e t i m e s c a l l e d a dummy
index
letter.
may become
Such
a
replacement
s i n c e it m a y b e r e p l a c e d b y a n y o t h e r
necessary
to avoid
indices
3
a p p e a r i n g m o r e t h a n t w i c e . T o i n s e r t ( 1 . 5 ) i n t o ( 1 . 5 ) i , e . g . , it is n e c e s s a r y
2
t o w r i t e ( 1 . 5 ) in t h e f o r m
2
ΛΓ/ —
(1.6)
CqiXq.
Thus,
X
P
= c i CqiXq
a n d similarly
P
*,· =
(1.7)
c c Xj,
pi
pJ
w h e r e t h e r i g h t - h a n d sides a r e d o u b l e s u m s .
I t is o b v i o u s t h a t t h e c o e f f i c i e n t o f X
in ( 1 . 7 ) ! m u s t b e 1 f o r q-p
q
f o r q^p.
and 0
A similar s t a t e m e n t holds for ( 1 . 7 ) . I n t r o d u c i n g the so-called
2
Kronecker
symbol
p q
Π
forp
(0
f o r ρ Φ q,
= q,
(1.8)
we thus have
Cpi^qi ~ 3pq>
pi PJ
C
(1.9)
~ ^U'
C
These equations might be interpreted as o r t h o n o r m a l i t y conditions; they
a r e v a l i d o n l y in o r t h o g o n a l c o o r d i n a t e s y s t e m s .
The c
pi
m a y be written as a m a t r i x ,
C\2
(1.10)
C22
C
J>1\
33.
H e r e t h e first i n d e x i n d i c a t e s t h e l i n e , t h e s e c o n d t h e c o l u m n in w h i c h a
g i v e n e l e m e n t is s i t u a t e d . F o r a n y fixed v a l u e o f ρ t h e c
p h
a p p e a r i n g in t h e
/7-th line of t h e m a t r i x (1.10), a r e , a c c o r d i n g t o (1.1), t h e c o m p o n e n t s of
the unit vector I
p
in t h e c o o r d i n a t e s y s t e m x
h
T h u s , the d e t e r m i n a n t of the
m a t r i x is t h e t r i p l e p r o d u c t
detc
= I
pi
l
(/2X/3).
(1.11)
It f o l l o w s t h a t
det
c
pi
= ±1,
w h e r e t h e positive sign c o r r e s p o n d s t o t h e case w h e r e b o t h
(1.12)
coordinate
systems a r e right- o r l e f t - h a n d e d , t h e n e g a t i v e sign t o t h e case w h e r e o n e of
t h e m is r i g h t - h a n d e d a n d t h e o t h e r o n e l e f t - h a n d e d . I n t h e first c a s e t h e
s e c o n d c o o r d i n a t e s y s t e m is o b t a i n e d f r o m t h e first o n e b y a r o t a t i o n a b o u t
4
Ο , in t h e s e c o n d c a s e a r e f l e c t i o n o n a p l a n e p a s s i n g t h r o u g h Ο m u s t b e
added.
M a k i n g o n c e m o r e use of (1.1), we o b t a i n
I = (I · */)// = c ii,
P
P
// = {irl )l
pi
p
= c I.
p
pi
(1.13)
p
C o m p a r i n g this to (1.5), we n o t e t h a t the base vectors of the t w o cartesian
coordinate
systems
transform
as
the
coordinates
of
e q u i v a l e n t l y , a s t h e c o m p o n e n t s o f its r a d i u s v e c t o r ) . I n
a
point
(or,
non-cartesian
c o o r d i n a t e systems, this w o u l d n o t be true.
O u r p r e s e n t i n t e r p r e t a t i o n o f ( 1 . 2 ) is t h i s : P i s a p o i n t fixed in s p a c e , i . e . ,
in o u r r e f e r e n c e f r a m e , a n d ( 1 . 2 ) c o n n e c t s its c o o r d i n a t e s in
different
cartesian systems. A n o t h e r i n t e r p r e t a t i o n , to be used later, considers (1.2)
as representing a displacement with respect to the reference frame:
c o o r d i n a t e s y s t e m is fixed a n d t h e X
p
the
are the instantaneous positions of the
p o i n t s w i t h o r i g i n a l p o s i t i o n s x , . T h e d i s p l a c e m e n t is o b v i o u s l y a r o t a t i o n
a b o u t O, possibly c o m b i n e d with a reflection o n a plane passing t h r o u g h
O.
A scalar
A is a q u a n t i t y w h i c h is i n d e p e n d e n t o f t h e c o o r d i n a t e s y s t e m .
D e n o t i n g the c o r r e s p o n d i n g q u a n t i t y in t h e system X
p
b y Λ, w e t h u s h a v e
Λ=λ.
A vector
(1.14)
ν h a s a d i r e c t i o n a n d h e n c e t h r e e c o m p o n e n t s υ,·. T h e v e c t o r
itself is i n d e p e n d e n t o f t h e c o o r d i n a t e s y s t e m ; its c o m p o n e n t s t r a n s f o r m a s
t h e c o o r d i n a t e s o f a p o i n t ( t h e e n d p o i n t o f ν w h e n t h e c o o r d i n a t e o r i g i n is
chosen as the starting point), i.e., according to (1.5),
Vp = c iV
P
i9
Vi = c V .
pi
(1.15)
p
T h u s , a vector might be defined as a triplet of c o m p o n e n t s
transforming
according to (1.15), a n d this definition might be used to o b t a i n s o m e of the
r u l e s o f v e c t o r a l g e b r a , s u p p l y i n g , e . g . , t h e p r o d u c t λν o f a s c a l a r a n d a
v e c t o r o r t h e s c a l a r p r o d u c t u*v
of t w o vectors.
G e n e r a l i z i n g ( 1 . 1 5 ) , let u s d e f i n e a cartesian
tensor
o f o r d e r η a s a set o f
3 " c o m p o n e n t s //,.../ t r a n s f o r m i n g a c c o r d i n g t o
Tpq...s
=
Cpi^qj · · · s/lij.../>
c
Uj pi^qj
c
· · · ^sl^pq...s*
0·16)
N o t e t h a t t h e o r d e r o f t h e t e n s o r is g i v e n b y t h e n u m b e r o f its i n d i c e s . I n
a c c o r d a n c e with this definition, a scalar λ m a y be considered as a tensor of
o r d e r z e r o . A v e c t o r is a t e n s o r o f o r d e r o n e , symbolically
denoted by
v.
5
W e will h e n c e f o r t h p r e f e r t h e index
notation,
representing a vector by the
s y m b o l i>; o f its g e n e r a l c o m p o n e n t a n d k e e p i n g in m i n d , o f c o u r s e , t h a t t h e
c o m p o n e n t s t r a n s f o r m if t h e c o o r d i n a t e s y s t e m is c h a n g e d .
W e will b e m o s t o f t e n c o n c e r n e d w i t h t e n s o r s o f t h e s e c o n d
denoted
symbolically
by
t
and
in
index
notation
by
order,
Here
the
t r a n s f o r m a t i o n s (1.16) are
Tpq — Cpi Cqj tjj ,
Uj
pi qjT .
c
c
pq
(1.17)
T h e 9 c o m p o n e n t s of a s e c o n d - o r d e r tensor m a y b e a r r a n g e d in m a t r i x
form:
tn
hi
(1.18)
hi
hi
hi
'33.
F o r o t h e r t e n s o r s t h i s is n o t t r u e ; t h e c o r r e s p o n d i n g a r r a n g e m e n t o f t h e 2 7
c o m p o n e n t s o f a t h i r d - o r d e r t e n s o r , e . g . , is a t h r e e - d i m e n s i o n a l b l o c k .
W r i t i n g t h e K r o n e c k e r s y m b o l (1.8) as a m a t r i x , w e o b t a i n
(1.19)
4/ =
If w e i n t e r p r e t t h e e l e m e n t s o f t h i s d i a g o n a l m a t r i x a s c o m p o n e n t s in a
coordinate system x
if
(1.19) defines a s e c o n d - o r d e r tensor. O n a c c o u n t of
( 1 . 1 7 ) ! a n d ( 1 . 9 ) , its c o m p o n e n t s in a n a r b i t r a r y c o o r d i n a t e s y s t e m X
p
^pq ~~ Cpi^qjdij
— Cpfiqi "pq>
z
are
(1.20)
i . e . , t h e y a r e t h e s a m e in a n y c o o r d i n a t e s y s t e m . A n a r b i t r a r y t e n s o r w i t h
c o m p o n e n t s t h a t a r e i n v a r i a n t is c a l l e d isotropic.
Examples encountered so
far a r e t h e s c a l a r a n d t h e K r o n e c k e r t e n s o r .
Problem
S h o w ( b y m e a n s o f a few s i m p l e c o o r d i n a t e t r a n s f o r m a t i o n s ) t h a t a n y
isotropic tensor of order t w o has the form
λδη.
1 . 2 . T e n s o r algebra
I n t h i s s e c t i o n w e will b r i e f l y d i s c u s s t h e p r i n c i p a l r u l e s o f t e n s o r a l g e b r a .
I n s o m e c a s e s w e will r e s t r i c t o u r s e l v e s t o t y p i c a l e x a m p l e s w h i c h a r e easily
g e n e r a l i z e d , a n d w e will l e a v e p a r t o f t h e p r o o f s t o t h e p r o b l e m s e c t i o n .
6
Let r
i j k
_
and s
m
i j k
_
be t w o tensors of equal but arbitrary
m
order.
A d d i n g corresponding c o m p o n e n t s , we obtain a n o t h e r tensor of the same
order,
i//jfc... = r , Y * . . . + S / / * . . . ,
m
called
m
M
t h e sum
of
the original
tensors
( P r o b l e m 1).
Given two tensors of arbitrary order, e.g., r
and s
iJk
products
or
Ujkim = ijk im,
r
their
components.
c a l l e d t h e product
s
These
products
l m 9
define
let u s f o r m t h e
another
tensor
o f t h e o r i g i n a l t e n s o r s . I t s o r d e r is t h e s u m
of the orders of the given tensors ( P r o b l e m 2). Special cases are the p r o d u c t
o f a s c a l a r a n d a t e n s o r (fy = Afy) a n d t h e t e n s o r o b t a i n e d b y m u l t i p l y i n g
t h e c o m p o n e n t s o f s e v e r a l v e c t o r s (t
=
ijk
Let r
u OjW ).
i
k
b e a n a r b i t r a r y t e n s o r o f o r d e r n. P i c k i n g t h e c o m p o n e n t s in
ijkLmmP
w h i c h t w o g i v e n i n d i c e s a r e e q u a l (r
)
ijnmmmP
and applying the summation
c o n v e n t i o n , w e o b t a i n a n o t h e r t e n s o r (///...^ = ///,/...;?) o f o r d e r η - 2 . T h e
p r o c e s s is c a l l e d contraction
w i t h r e s p e c t t o t h e t w o i n d i c e s in q u e s t i o n
( P r o b l e m 3 ) . A s i m p l e e x a m p l e is t h e t r a c e o f a s e c o n d o r d e r
tensor,
t r ί = ία, w h i c h is itself a s c a l a r .
In particular, the process of c o n t r a c t i o n m a y be applied t o a p r o d u c t
w i t h r e s p e c t t o i n d i c e s t a k e n f r o m e a c h o f t h e t w o f a c t o r s (r sij
= t ).
ijk
An
iki
e x a m p l e is t h e s c a l a r p r o d u c t Μ,υ, o f t w o v e c t o r s . If o n e o f t h e t w o f a c t o r s is
a s e c o n d - o r d e r t e n s o r a n d t h e o t h e r t h e K r o n e c k e r t e n s o r (tijdj
= t ),
k
o p e r a t i o n y i e l d s t h e o r i g i n a l t e n s o r . T h u s , δ„ is a l s o c a l l e d t h e unit
o f o r d e r t w o . O t h e r e x a m p l e s a r e t h e powers
the
ik
tensor
of a s e c o n d - o r d e r t e n s o r / ,
symbolically d e n o t e d by / , f , ... a n d defined as t h e second o r d e r tensors
2
3
Up tpj> Up tpq tqj>
It s o m e t i m e s h a p p e n s t h a t , g i v e n a set o f 3 " q u a n t i t i e s / ( / , y . . . , / ) , t h e
q u e s t i o n a r i s e s w h e t h e r t h e y d e f i n e a t e n s o r . It is c l e a r t h a t t h i s q u e s t i o n
c a n b e a n s w e r e d b y c h e c k i n g w h e t h e r t h e t(ij...,
/) t r a n s f o r m a c c o r d i n g t o
( 1 . 1 6 ) . A n e a s i e r m e a n s is t o u s e t h e s o - c a l l e d quotient
o f t h i s l a w s t a t e s t h a t , e . g . , t(i j
k) a r e t h e c o m p o n e n t s o f a t e n s o r t
9 9
t(i j
9 9
k)UiVjW
k
law. A t y p i c a l f o r m
ijk
is a s c a l a r f o r a n y c h o i c e o f v e c t o r s u
i9
v
j9
w.
k
if
I n f a c t , if t h i s is
the case, (1.15) yields
2
T(p, q, r)U
p
Since U ,
p
V W = t(i,j,
q
r
k)u VjW
t
k
= /(/,y, k)c U c
pi
p
Vc
qj
q
rk
W.
(1.21)
r
V , W a r e a r b i t r a r y , it f o l l o w s f r o m ( 1 . 2 1 ) t h a t
Q
r
T(p,
q, r) = CpiCqjCrkt&j,
k).
(1.22)
T h i s is in f a c t t h e t r a n s f o r m a t i o n (1.16)i f o r η = 3 . A n o t h e r f o r m o f t h e
q u o t i e n t l a w s t a t e s t h a t t h e set t(i j
9 9
k) d e f i n e s a t e n s o r t
ijk
if t(i j
9 9
k)^
is a
7
v e c t o r f o r a n y c h o i c e o f t h e t e n s o r ry ( P r o b l e m 4 ) . O t h e r v e r s i o n s o f t h e
q u o t i e n t l a w a r e easily i n f e r r e d f r o m t h e s e e x a m p l e s .
A t e n s o r is c a l l e d symmetric
w i t h r e s p e c t t o t w o i n d i c e s if t h e e x c h a n g e
o f t h e s e i n d i c e s d o e s n o t a l t e r t h e c o m p o n e n t s . If t h e e x c h a n g e i n v e r t s t h e
s i g n s o f t h e c o m p o n e n t s , t h e t e n s o r is c a l l e d antimetric.
second-order tensor t
ij9
In t h e case of a
t h e o n l y s y m m e t r y r e l a t i o n is (/,· = *(/. T h e m a t r i x
r e p r e s e n t a t i o n ( 1 . 1 8 ) s h o w s t h a t t h e s y m m e t r i c t e n s o r ty h a s o n l y six
independent components. O n the other h a n d , the only antimetry condition
f o r tij is ίβ = -tij.
indicating
cyclic
Since this implies f = ··· = 0 (three d o t s in general
n
permutation),
there
remain
only
three
independent
c o m p o n e n t s . I t is e a s y t o see t h a t t h e s e p r o p e r t i e s a r e i n d e p e n d e n t o f t h e
coordinate system (Problem 6).
By m e a n s of t h e identity
tij^Htij
+ tjd + Uty-tji)
(1.23)
t h e s e c o n d - o r d e r t e n s o r ty a p p e a r s d e c o m p o s e d i n t o its s y m m e t r i c a n d
antimetric parts,
kij) = Wij + /),
t
m
= Wij-
tji\
(1.24)
r e s p e c t i v e l y . I n t h e c a s e o f t w o t e n s o r s , r a n d $/,, it is e a s y t o see t h a t
(J
It i m m e d i a t e l y f o l l o w s t h a t
iJ U = ( W) + [(/]) ( W) +
r
s
r
r
S
w0 = W) W) + m m ·
s
r
s
r
s
ί
1
·
2 6
)
T h r e e a r b i t r a r y n o n - c o m p l a n a r v e c t o r s w, y, w f o r m a r i g h t - o r lefth a n d e d vector system. Since t h e d e t e r m i n a n t
U
U
M
Όχ
V
t>
Wj
W
W
X
D =
is e q u a l t o t h e t r i p l e p r o d u c t u*(oxw),
block
1
2
2
2
3
(1.27)
3
3
it r e p r e s e n t s t h e v o l u m e Κ o f t h e
f o r m e d b y t h e t h r e e v e c t o r s , p r e c e d e d b y t h e p o s i t i v e sign if t h e
vector system a n d t h e coordinate system are b o t h right- or left-handed a n d
b y t h e n e g a t i v e sign if o n e o f t h e m is r i g h t - h a n d e d , t h e o t h e r o n e lefth a n d e d . F o r g i v e n v e c t o r s , Κ is a s c a l a r , w h e r e a s D c h a n g e s sign i n a
1
A shorter word for 'parallelepiped', suggested by Flugge in [1].
8
transformation from a right-handed to a left-handed coordinate system.
W e t h e r e f o r e call D a pseudo-scalar
tensor).
(the simplest version of a
pseudo-
W e will n o t d i s c u s s t h i s c o n c e p t h e r e , b u t r a t h e r a v o i d it b y
restriction to right-handed coordinate systems.
A n y p e r m u t a t i o n of the three digits 1 , 2 , 3 m a y be o b t a i n e d by successive
interchanges of t w o adjacent digits. A c c o r d i n g as the n u m b e r of necessary
s t e p s is e v e n o r o d d , t h e p e r m u t a t i o n itself is c a l l e d a n e v e n o r a n o d d
p e r m u t a t i o n o f 1, 2 , 3 . L e t u s d e f i n e a set o f 27 s y m b o l s e
by stipulating
ijk
t h a t t h e i r v a l u e s a r e 1, - 1 o r 0 a c c o r d i n g a s t h e s e q u e n c e ij
9
k is e i t h e r a n
e v e n p e r m u t a t i o n o f 1, 2 , 3 , a n o d d o n e , o r n o p e r m u t a t i o n a t a l l . I n o t h e r
words, e
m
= ··· = 1 , e
m
= ··· = - 1 a n d e
2 3 3
= ··· =^223=
= *πι = ··· =
0. By m e a n s of these s y m b o l s , t h e d e t e r m i n a n t (1.27) m a y be written as
D = e UiVjW
uk
(1.28)
k
f o r a n y set o f v e c t o r s a n d a n y c h o i c e o f t h e c o o r d i n a t e s y s t e m . I n f a c t , D is
d e f i n e d in m a n y t e x t s b y ( 1 . 2 8 ) . S i n c e w e h a v e r e s t r i c t e d o u r s e l v e s t o r i g h t handed
coordinate
systems, D
is a s c a l a r .
connection with the quotient law that e
ijk
s o m e t i m e s c a l l e d t h e permutation
tensor
From
( 1 . 2 8 ) it f o l l o w s
in
is a n i s o t r o p i c t h i r d - o r d e r t e n s o r ,
o r t h e alternating
t e n s o r . It c a n b e
s h o w n ( P r o b l e m 8) t h a t
Cpij pkl
= $ik fyl ~ ^ilfyk>
e
tpqiepqj = <5ij>
0-29)
2
Cpqr^pqr ~ 6·
L e t Sj b e a n a r b i t r a r y s e c o n d - o r d e r t e n s o r , a n d let u s a s s o c i a t e w i t h it a
k
vector
ti = \e s ,
ijk
c a l l e d its dual
vector.
(1.30)
jk
T h e c o m p o n e n t s o f /, a r e o b v i o u s l y
t\=HS23-S3 )=S ....
2
(1.31)
[23]f
T h e y are identical with the c o m p o n e n t s of the antimetric part of the tensor
Sj
k
a n d h e n c e d o n o t d e p e n d o n its s y m m e t r i c p a r t . O n a c c o u n t o f ( 1 . 3 0 )
and (1.29)!,
^ijk^k
=
i^ijk^kpq^pq
\^kij^kpq pq
=
s
= \ (Sipdjq ~ diqdjp)Spq
= ! ( % ~ ty) = % ] ·
(1.32)
T h u s , the relation
W]
s
=
Uktk
e
(1.33)
9
m a y b e c o n s i d e r e d a s t h e i n v e r s i o n o f ( 1 . 3 0 ) ; it a s s o c i a t e s a n a n t i m e t r i c
tensor
=
w i t h a n y v e c t o r t , c a l l e d its dual
tensor.
k
T h e d u a l v e c t o r o f ujv
k
is
Wi = je UjO .
uk
(1.34)
k
S i n c e its c o m p o n e n t s a r e w =\(u t>3-w i> ),...,
x
2
3
w e h a v e , in
2
symbolic
notation,
w = ±uxv.
(1.35)
O n t h e o t h e r h a n d , ( 1 . 3 4 ) is e q u i v a l e n t t o
w,- = ie UjV
kij
where U
ij9
= \U v
k
ki
= -\UijVj,
k
(1.36)
a c c o r d i n g t o ( 1 . 3 3 ) , is d u a l t o u . T h u s , t h e v e c t o r p r o d u c t
uxv
k
m a y be written as -
UyVj.
Fig. 1.2. Gyro.
If, e . g . , ω is t h e i n s t a n t a n e o u s a n g u l a r v e l o c i t y o f a g y r o ( F i g . 1.2) w i t h
fixed p o i n t O, t h e v e l o c i t y ν o f t h e p o i n t Ρ w i t h r a d i u s v e c t o r r f r o m Ο is
ν = ωΧΓ.
It m a y a l s o b e e x p r e s s e d b y
= e
iJk
where the x
k
a>jx = - QijXj,
(1.37)
k
a r e t h e c o o r d i n a t e s o f Ρ a n d Ω^ = β ^ω/
ί
is d u a l t o a> .
(
k
Problems
1. S h o w t h a t t h e s u m o f t w o t e n s o r s , t j = r j + s j ,
i k
i k
is a t e n s o r .
i k
2 . S h o w t h a t t h e p r o d u c t o f t w o t e n s o r s , tij
= rjj Si
3. Show that contraction of the tensor r
with respect to k and
klm
yields a t h i r d - o r d e r t e n s o r .
i j k l m
k
mi
is a t e n s o r .
m
10
4 . P r o v e t h a t t h e set t(ij, k) d e f i n e s a t e n s o r t
ijk
if t(i,j, k)ry is a v e c t o r
f o r a n y c h o i c e o f t h e t e n s o r ry.
5. P r o v e a n o t h e r f o r m o f t h e q u o t i e n t l a w .
6. S h o w t h a t t h e p r o p e r t i e s o f s y m m e t r y a n d a n t i m e t r y o f t h e t e n s o r t
ijklm
with respect t o j a n d / are independent of t h e coordinate system.
7. L e t D b e t h e d e t e r m i n a n t o f a s e c o n d - o r d e r t e n s o r Sy w r i t t e n a s a
9
m a t r i x . Verify t h e i d e n t i t y e D
=
ijk
e SuSj s .
lmn
m kn
8. P r o v e t h e i d e n t i t i e s ( 1 . 2 9 ) .
9. S h o w t h a t t h e m o m e n t o f i n e r t i a o f a b o d y f o r a n a x i s w i t h d i r e c t i o n
c o s i n e s μ,, p a s s i n g t h r o u g h t h e o r i g i n O , h a s t h e f o r m Ι=Ι μ μ
υ
ί
w h e r e Iy is
]
the symmetric tensor defined b y t h e m o m e n t s of inertia 7 , . . . a n d t h e
n
negative p r o d u c t s of inertia - 7 3 , ··· with respect t o t h e c o o r d i n a t e system
2
Xi. A s s u m e t h a t t h e b o d y is a g y r o w i t h fixed p o i n t Ο a n d a n g u l a r v e l o c i t y
ω , , a n d find its a n g u l a r m o m e n t u m Z), a n d its k i n e t i c e n e r g y Γ .
1 . 3 . Principal a x e s
In this section w e restrict ourselves t o symmetric cartesian s e c o n d - o r d e r
t e n s o r s , a n d w e will b e m a i n l y c o n c e r n e d w i t h f i n d i n g a c o o r d i n a t e s y s t e m
in w h i c h t h e c o m p o n e n t s o f ty a r e p a r t i c u l a r l y s i m p l e .
L e t μ, d e n o t e a u n i t v e c t o r o f a r b i t r a r y d i r e c t i o n . B y m e a n s o f t h e
equation
s^
= tiM
(1.38)
t h e t e n s o r ty a s s o c i a t e s a v e c t o r sj^ w i t h t h e d i r e c t i o n μ,. If, i n p a r t i c u l a r , μ,
h a s t h e d i r e c t i o n o f t h e c o o r d i n a t e a x i s Xj, t h e i-th c o m p o n e n t o f t h e v e c t o r
(1.38) b e c o m e s
^
= ty.
(1.39)
T h e c o m p o n e n t ty o f t h e g i v e n t e n s o r m a y t h e r e f o r e b e i n t e r p r e t e d a s t h e
i-th c o m p o n e n t o f t h e v e c t o r
a s s o c i a t e d w i t h t h e c o o r d i n a t e a x i s Xj.
L e t u s a s k f o r a v e c t o r μ, s u c h t h a t t h e c o r r e s p o n d i n g v e c t o r sj^ is
p a r a l l e l t o i t . I f it e x i s t s , it d e f i n e s w h a t w e call a principal
axis,
a n d it
satisfies t h e r e l a t i o n
sj
M)
=t
ijMj
=t
Mh
(1.40)
w h e r e / is a s c a l a r ( p o s i t i v e , n e g a t i v e o r z e r o ) . T h e s e c o n d e q u a t i o n ( 1 . 4 0 ) is
equivalent t o
(ty-toy^j
= 0.
(1.41)
11
S i n c e y is a s u m m a t i o n i n d e x , w h e r e a s / is a r b i t r a r y , ( 1 . 4 1 ) r e p r e s e n t s t h r e e
h o m o g e n e o u s l i n e a r e q u a t i o n s , c a l l e d t h e characteristic
system,
for
the
u n k n o w n s μ,. F u r t h e r m o r e , s i n c e μ is a u n i t v e c t o r ,
7
a n d t h e t r i v i a l s o l u t i o n μ/ = 0 m u s t b e d i s c a r d e d . A n o n t r i v i a l
however,
only
exists if t h e d e t e r m i n a n t
v a n i s h e s , i . e . , if t h e characteristic
of
the coefficients
solution,
in
(1.41)
equation
det(^-^) = 0
(1.43)
is s a t i s f i e d .
B e f o r e p r o c e e d i n g t o s o l v e ( 1 . 4 3 ) , let u s s h o w t h a t a n a p p a r e n t l y q u i t e
different p r o b l e m yields t h e s a m e characteristic system. O n a c c o u n t of
( 1 . 3 8 ) , t h e p r o j e c t i o n o f t h e v e c t o r sj^ o n t o t h e d i r e c t i o n μ, is t h e s c a l a r
p = sf u
{ i)
= t Mj.
(1.44)
ij
O b v i o u s l y ρ is a f u n c t i o n o f t h e d i r e c t i o n μ,, a n d w e m a y c o n s e q u e n t l y a s k
f o r t h e d i r e c t i o n s f o r w h i c h ρ is s t a t i o n a r y . T h i s q u e s t i o n s t i p u l a t e s a n
e x t r e m u m p r o b l e m , subject t o the side c o n d i t i o n (1.42) a n d solved
by
setting
θ ,
— ( t
u
m
θ
- /μ,μ,) = — [(t - td )Mj]
u
u
= 0,
(1.45)
where M s a Lagrangean multiplier. Carrying out the differentiation
and
m a k i n g u s e o f t h e s y m m e t r y o f ty, w e o b t a i n t h e e q u a t i o n
2(*Ρΐ-* ρΜ
δ
= >
0·
0
4 6
)
w h i c h is in fact e q u i v a l e n t t o ( 1 . 4 1 ) . M u l t i p l i c a t i o n o f b o t h s i d e s o f ( 1 . 4 1 )
b y μ, y i e l d s
^ - 1 0 ^
=0
o r , o n a c c o u n t o f ( 1 . 4 2 ) a n d ( 1 . 4 4 ) , t=p.
(1.47)
It f o l l o w s t h a t t h e L a g r a n g e a n
multiplier belonging t o a solution of (1.41) represents the c o r r e s p o n d i n g
stationary value of the projection (1.44).
Proceeding n o w to the solution of the characteristic equation (1.43), we
w r i t e it in t h e f o r m
I
hi
h -t
hi
hi
2
t
23
hz~t
I =0.
(1.48)
12
Developing t h e left-hand side a n d o r d e r i n g with respect t o p o w e r s of ' , w e
have
-'
+ ' ( ' + -)-'[('22'33 -*23)+ - ] + d e t ^= 0
3
(1.49)
2
π
or
' -7
3
' -7
2
( 1 )
( 2 )
'-7
= 0,
(1.50)
+ ^23 + — ,
(1.51)
( 3 )
where t h e coefficients a r e
J(i)
' n + '">
=
/ ( 2 ) = -^22^33
J(3) = Ί 1 '22'33 - Ί ι /23
+ 2'
2 3
'
3 1
^12 = d e t '//.
A m o r e c o n c i s e f o r m o f ( 1 . 5 1 ) ( P r o b l e m 1) is
Ai)
'//>
=
^(3) \fitijtjktki ~ %jtjihk + '//'//'*:*)·
=
T h e c h a r a c t e r i s t i c e q u a t i o n ( 1 . 5 0 ) is o f t h e t h i r d d e g r e e i n Λ I t h a s t h r e e
r o o t s , c a l l e d t h e principal
values o f t h e t e n s o r ty. A s s t a t i o n a r y v a l u e s o f /?,
they are independent of the coordinate system. According t o the lemma of
Vi6ta, t h e coefficients 7
the
principal
values
( 1 )
,7
( 2 )
and
and 7
( 3 )
hence
in ( 1 . 5 0 ) m a y b e e x p r e s s e d in t e r m s o f
are themselves
independent
of
the
c o o r d i n a t e system. T h e y c a n b e expressed, a c c o r d i n g t o (1.52), in t e r m s of
the traces of /, t
2
and t .
3
O n e o f t h e r o o t s o f ( 1 . 5 0 ) is a l w a y s r e a l . L e t u s d e n o t e it a s t h e first
principal value t . F o r t = t t h e characteristic system (1.41) h a s a t least o n e
x
Y
r e a l s o l u t i o n μ) s a t i s f y i n g ( 1 . 4 2 ) . T h i s s o l u t i o n d e f i n e s t h e first p r i n c i p a l
a x i s o f ty. L e t u s i n t r o d u c e a n e w c o o r d i n a t e s y s t e m x[ t h e first a x i s o f
w h i c h c o i n c i d e s w i t h t h e p r i n c i p a l a x i s μ).
e q u a t i o n (1.40) takes t h e f o r m
=
In this system the second
. W e t h u s h a v e t' = t
n
u
/
2 1
= /
3 1
=0,
a n d t h e c h a r a c t e r i s t i c e q u a t i o n ( 1 . 4 8 ) , w r i t t e n in t h e s y s t e m Λ / , r e d u c e s t o
ti-t
0
0
0
'22->
'23
0
= 0
(1.53)
' 3 3 - '
&
or
( Ί - ' ) [ ' - ('22 + ' 3 3 ) ' + '22'33 - '23 ] = 0 .
2
The remaining
expression
principal values
between
(1.54)
2
' , '
n
m
are obtained
by equating the
square brackets to zero. T h e discriminant
of the
13
c o r r e s p o n d i n g q u a d r a t i c e q u a t i o n is
('22 + ' 3 3 ) - 4 ( & * 3 3 " Φ
S i n c e it is n o n - n e g a t i v e , i
n
and t
(1.55)
= (*22 " *33Ϋ + 4 $ ·
2
a r e r e a l , a n d it f o l l o w s t h a t a s y m m e t r i c
m
tensor of order t w o only a d m i t s real principal values.
Let us characterize t h e principal axes corresponding t o t
and t
u
v e c t o r s μ]
1
a n d μ]
11
by the
m
respectively. T h e y a r e also real, a n d since they a r e
solutions of the characteristic system, we have
(*y ~ hAj )μ} = 0 ,
(tij - ίηιδ^μ}
1
11
= 0.
(1.56)
M u l t i p l y i n g t h e first o f t h e s e e q u a t i o n s b y μ / , t h e s e c o n d o n e b y μ} , a n d
11
1
substracting t h e results, w e obtain
(ήι-ήιι)Λ
? Π
=σ.
(1.57)
It f o l l o w s t h a t t h e p r i n c i p a l a x e s c o r r e s p o n d i n g t o d i f f e r e n t
principal
values a r e o r t h o g o n a l . In consequence, t h e tensor h a s a u n i q u e system of
principal axes p r o v i d e d t h e t h r e e principal values a r e different. If t = t ,
u
t h e d i s c r i m i n a n t ( 1 . 5 5 ) m u s t v a n i s h ; h e n c e t' = 0 a n d t' = t
13
21
33
m
= t = tm. I t
u
f o l l o w s t h a t t h e c o o r d i n a t e s y s t e m xi a n d i n c o n s e q u e n c e a n y c o o r d i n a t e
s y s t e m c o n t a i n i n g t h e a x i s x[ d e f i n e s a p r i n c i p a l s y s t e m . A s l o n g a s t\ is
d i f f e r e n t f r o m t = t , t h e p r i n c i p a l a x i s x[ is u n i q u e ; o t h e r w i s e , i . e . , if
u
h = hi = hn>
a n
m
Y coordinate system defines a system of principal axes.
I n p r i n c i p a l a x e s t h e t e n s o r ty is r e p r e s e n t e d b y a d i a g o n a l m a t r i x ,
0
0
hi
0
0
'in J
It is o b v i o u s t h a t a l s o t h e p o w e r s o f / , d e f i n e d in S e c t i o n 1.2 a s
hptpqtqj*
-
(1.58)
,, a r e represented b y d i a g o n a l matrices
0
0
0
if.
0
0
0
tt
•*P PJ>
ip
g
(1.59)
T h e i r p r i n c i p a l a x e s a r e t h o s e o f t, a n d t h e i r p r i n c i p a l v a l u e s a r e t h e p o w e r s
of
S i n c e t h e p r i n c i p a l v a l u e s t\,... satisfy t h e c h a r a c t e r i s t i c e q u a t i o n ( 1 . 5 0 ) ,
we have
<2)'l + A3)'
(1.60)
14
T h e three e q u a t i o n s (1.60) m a y b e c o n d e n s e d i n t o a single o n e , t h e soc a l l e d Hamilton-Cayley
equation
ΐ=Ι
( 1 )
ί
+Ι ί
2
+ Ι δ,
{2)
(1.61)
0)
w h e r e δ d e n o t e s t h e u n i t t e n s o r . I n p r i n c i p a l a x e s ( 1 . 6 1 ) is i n f a c t e q u i v a l e n t
t o (1.60). A s a t e n s o r e q u a t i o n , (1.61) r e m a i n s valid in t h e f o r m
Uptpqtqj — h^iptpj
+ h^)Uj +
(1.62)
in a n y c a r t e s i a n c o o r d i n a t e s y s t e m .
B y m e a n s o f ( 1 . 6 1 ) it is p o s s i b l e t o e x p r e s s a n y p o w e r o f / in t e r m s o f t , t
2
a n d δ. T h e f o u r t h p o w e r , e . g . , is g i v e n b y
t
= / ( ΐ ) ( / ( ΐ ) / + 7(2)/ + /(3)<*) + I(2)* + / < 3 ) '
4
2
=
2
+ hi))*
2
+ (Ai) (2) + / ( 3 ) ) ' + W ( 3 ) A
(1-63)
7
H e r e t h e coefficients of t , t a n d δ a r e p o l y n o m i a l s in t h e invariants 7
2
a n d 7(3), o f d e g r e e 2 t o 4 i n /,·,· s i n c e , a c c o r d i n g t o ( 1 . 5 2 ) , 7
of
t h e first,
second
a n d third
degree respectively.
( 1 )
,7
( 2 )
( 1 )
and 7
,7
( 2 )
are
( 3 )
In a similar w a y
f , . . . m a y b e r e d u c e d . I t f o l l o w s t h a t a n y p o w e r series i n f,
5
s = AO + Bt + Ct
+ Dt +
2
3
(1.64)
2
(1.65)
can be reduced to three terms
s=fo + gt + ht
w i t h c o e f f i c i e n t s / , g, h t h a t a r e p o w e r series i n t h e i n v a r i a n t s 7
A deviator
( 1 )
,7
( 2 )
,7
( 3 )
.
is a s y m m e t r i c t e n s o r / ' t h e t r a c e o f w h i c h is z e r o . If t j is a n
t
arbitrary symmetric tensor,
t ^ t i j - ^ i j
is a d e v i a t o r s i n c e t' =0.
h
(1.66)
O n the other h a n d , by the inversion of (1.66),
tu = t' + \t d ,
u
kk
u
(1.67)
t h e t e n s o r ty a p p e a r s d e c o m p o s e d i n t o a d e v i a t o r a n d a n i s o t r o p i c t e n s o r .
O n a c c o u n t o f ( 1 . 6 6 ) , t h e p r i n c i p a l a x e s o f t[j c o i n c i d e w i t h t h e o n e s o f t
ij9
a n d t h e p r i n c i p a l v a l u e s o f ty a r e t \ - \ t
k k
, . . . . T h e principal axes of the
i s o t r o p i c p a r t o f ty a r e a r b i t r a r y , a n d t h e t h r e e p r i n c i p a l v a l u e s a r e \ t
Problems
1. V e r i f y t h e e x p r e s s i o n s ( 1 . 5 2 ) .
k k
.
15
2. S h o w t h a t the d e c o m p o s i t i o n (1.67) of a symmetric tensor into a
d e v i a t o r a n d a n i s o t r o p i c t e n s o r is u n i q u e .
1.4. Invariants a n d i s o t r o p i c t e n s o r f u n c t i o n s
Let us consider functions of o n e or m o r e tensors. Provided such a
f u n c t i o n is itself a s c a l a r , w e c a l l it a scalar-valued
t e n s o r s . I n a s i m i l a r m a n n e r , w e d e f i n e vectorfunctions.
function
of the given
o r tensor-valued
tensor
For example, the expansion
X = C+C t j
iJ i
+ C t jt +
iJkl i
.··
kl
(1.68)
w h e r e C , Q , , C ^ / . - . a r e c o n s t a n t t e n s o r s o f o r d e r s 0 , 2 , 4 , . . . , is a s c a l a r valued function of the second-order tensor t
ij9
U
S
+ Gjkltkl
=
whereas
+ Qjklmn hltmn+
(1 · 6 9 )
is a t e n s o r - v a l u e d f u n c t i o n o f o r d e r 2 .
A s a scalar,
λ
in ( 1 . 6 8 ) is i n d e p e n d e n t
H o w e v e r , if t h e n u m e r i c a l v a l u e s o f t h e
of the coordinate
system.
are prescribed independent of
t h e c o o r d i n a t e s y s t e m , t h e t r a n s i t i o n f r o m o n e s y s t e m t o t h e o t h e r r e s u l t s in
d i f f e r e n t v a l u e s f o r λ a n d a l s o f o r t h e c o m p o n e n t s s^ in ( 1 . 6 9 ) s i n c e , w i t h
the components C
ij9
0 , * / , . . . , t h e f u n c t i o n a l f o r m s o f t h e r i g h t - h a n d s i d e s in
( 1 . 6 8 ) a n d ( 1 . 6 9 ) d e p e n d o n t h e c h o i c e o f t h e c o o r d i n a t e s y s t e m . If t h i s is
n o t t h e c a s e , t h e t e n s o r f u n c t i o n is c a l l e d isotropic.
If, e . g . , a s c a l a r - v a l u e d
f u n c t i o n / o f t h e v e c t o r s u„ vv , . . . a n d t h e t e n s o r s t u >
y
kh
...satisfies the
mn
equation
/(V
h
Wj, ...,T U ,...)
kh
mn
= / ( ! * , wj, . . . J
k b
u
m n 9
...\
(1.70)
its f u n c t i o n a l f o r m t h u s b e i n g i n d e p e n d e n t o f t h e c o o r d i n a t e s y s t e m , t h e
f u n c t i o n is i s o t r o p i c . S c a l a r - v a l u e d i s o t r o p i c t e n s o r f u n c t i o n s , a s ( 1 . 7 0 ) ,
a r e a l s o c a l l e d invariants.
T h e properties of invariants a n d of m o r e general
isotropic tensor functions have been studied by Rivlin a n d collaborators.
W e o n l y need a few of their results; for t h e o m i t t e d p r o o f s a n d for m o r e
i n f o r m a t i o n , see t h e c o m p r e h e n s i v e a r t i c l e b y S p e n c e r [ 2 ] .
A n y scalar-valued function
o f a n i n v a r i a n t is itself a n i n v a r i a n t .
It
f o l l o w s t h a t a n y set o f t e n s o r s h a v i n g a t least o n e i n v a r i a n t p o s s e s s e s a n
i n f i n i t y o f t h e m . H o w e v e r , it is a l w a y s p o s s i b l e t o e x p r e s s t h e m in t e r m s o f
a s m a l l n u m b e r o f i n d e p e n d e n t i n v a r i a n t s , r e f e r r e d t o a s basic invariants
a s a n integrity
basis.
or
T h e s i m p l e s t i n t e g r i t y b a s i s o f a s c a l a r , e . g . , is t h e
16
s c a l a r itself. A n y f u n c t i o n o f it a l s o is a n i n v a r i a n t . S i m i l a r l y , t w o o r m o r e
scalars represent their o w n integrity basis. In the case of a vector v
h
it is
o b v i o u s t h a t its m a g n i t u d e o r , p r e f e r a b l y , its s q u a r e
V(i = v v
)
i
(1.71)
i
m a y s e r v e a s a n i n t e g r i t y b a s i s . I n t h e c a s e o f t w o v e c t o r s t>, a n d w,-, t h e
simplest basic invariants are their squares a n d their scalar p r o d u c t ,
»(\) = i>i»i>
w
( 1 )
= W/W/,
l(i = v w .
)
i
i
(1.72)
I n S e c t i o n 1.3 w e h a v e e n c o u n t e r e d t h r e e i n d e p e n d e n t i n v a r i a n t s ( 1 . 5 2 )
o f a s y m m e t r i c t e n s o r o f s e c o n d o r d e r . It is o b v i o u s t h a t t h e y c a n b e
reduced to the simpler invariants
'(1) = '/'/>
i.e., to the traces of /, t
'(2) = ' ( / ( / / >
' ( 3 ) Uj tjktki >
=
(1-73)
a n d / . In fact, a c c o r d i n g t o (1.73) a n d (1.52), we
2
3
have
/ ( l ) = '(1),
hi) = W{2)
/(3) =£(2'(3)
-
-
3'(2)'(1) + '(I))-
(1-74)
In principal axes the invariants (1.73) b e c o m e
Ό) = Ί + - >
'(2) =
tf+
'(3) = * ? +
(1-75)
I n t h e c a s e o f a d e v i a t o r t[j, t h e first o f t h e m is z e r o , a n d t h e o t h e r o n e s m a y
a l s o b e w r i t t e n ( P r o b l e m 1) in t h e f o r m s
'<2) = - 2 ( ί ί ϊ / ί „ + · - ) ,
f<3) = 3 f i / i i / i n .
,
(1.76)
In t e r m s of the invariants (1.73), the H a m i l t o n - C a y l e y e q u a t i o n (1.62)
assumes the form
Uptpqtqj = t \)tipt
{
pj
+ »(2'
+ \(t
~
{1)
( 3 )
-3/
( 2 )
/
( 1 )
t )tij
2
X)
+ '
3
(
1 )
)^.
(1.77)
W i t h its h e l p , a n y p o w e r o f t h e t e n s o r ty a n d h e n c e a l s o t h e p o w e r series
s = Ad
u
u
+ Bt
u
+ Ct t j+Dt t t +
ip P
ip pq qj
-
(1.78)
can be reduced to three terms
Sij=fSij
+ gtij + ht t ,
ik kJ
(1.79)
w h e r e t h e c o e f f i c i e n t s a r e p o l y n o m i a l s o r , i n t h e l a s t c a s e , p o w e r series i n
the invariants (1.73).