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Submitted on 1 Jan 1983

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DISPERSIVE EFFECTS IN RADIATION

TRANSPORT AND RADIATION HYDRODYNAMICS IN MATTER AT HIGH DENSITY

B. Crowley

To cite this version:

B. Crowley. DISPERSIVE EFFECTS IN RADIATION TRANSPORT AND RADIATION HYDRO-

DYNAMICS IN MATTER AT HIGH DENSITY. Journal de Physique Colloques, 1983, 44 (C8),

pp.C8-25-C8-38. �10.1051/jphyscol:1983803�. �jpa-00223310�

(2)

J O U R N A L DE PHYSIQUE

Colloque C8, supplement

au

n O 1 l , Tome 44, novembre 1983 page C8-25

DISPERSIVE EFFECTS IN RADIATION TRANSPORT AND RADIATION HYDRODYNAMICS IN MATTER AT HIGH DENSITY

B.J.B. Crowley

Atomic Weapons Research Establishment, Aldermaston, Reading, U . K .

Rdsumd

Dans un t r a v a i l r e c e n t , j ' a i g 6 n E r a l i s 6 l e s S q u a t i o n s d e l l h y d r o d y n a m i q u e r a d i a t i v e au c a s 06 l e rayonnement 6 l e c t r o m a g n d t i q u e s a t i s f a i t

B

une r e l a t i o n d e d i s p e r s i o n l i n 6 a i r e nw = k c , 06 l ' i n d i c e d e r 6 f r a c t i o n n d6pend d e l a f r 6 q u e n c e U e t / ou du nombre d'onde k. A p p l i q u a n t l a t h g o r i e d e t r a n s p o r t B o l t z m a n n - L i o u v i l l e aux p h o t o n s du domaine i3 c o u r t e l o n g u e u r d ' o n d e , j ' o b t i e n s d e s d q u a t i o n s d ' d n e r g i e e t d e moment, q u i , combindes a u t r a i t e m e n t c l a s s i q u e du m i l i e u f l u i d e e n ETL, donnent une t h d o r i e dynamique complGte d e s i n t e r a c t i o n s l i n e a i r e s (+ p r o c e s s u s s t i m u l d s ) e n t r e l e rayonnement t h e r m i q u e i n c o h d r e n t , e t l a m a t i l r e d e n s e , l o c a l e m e n t i s o t r o p e . Ce f o r m a l i s m e e s t g d n 6 r a l i s a b l e aux i n t e r a c t i o n s n o n - l i n b a i r e s , oh l ' i n d i c e de r 6 f r a c - t i o n depend d e 1 1 i n t e n s i t 6 l o c a l e s p d c i f i q u e du champ d e rayonnement, e t d a n s une c e r t a i n e mesure, g g a l e m e n t , a u t r a i t e m e n t du rayonnement c o h 6 r e n t d e h a u t e f r 6 q u e n c e . La g d n d r a l i s a t i o n d e p l u s i e u r s formes a p p r o e h d e s de t h d o r i e du t r a n s p o r t d e rayon- nement ( d i f f u s i o n ) e s t c o n s i d 6 r d e e n d d t a i l . Parmi l e s problBmes o u v e r t s , mention- nons : l a d i s p e r s i o n a n o r m a l e , l ' a s p e c t p h y s i q u e a t o m i q u e d e s p r o p r i s t d s d l e c t r o m p - g n d t i q u e s e t r a d i a t i v e s d ' u n m i l i e u m a t d r i e l d i s p e r s i f .

A b s t r a c t

I n a r e c e n t r e s e a r c h program ( r e p o r t e d i n AWRE 0 2 0 1 8 2 ) I have i n v e s t i - g a t e d t h e g e n e r a l i s a t i o n o f t h e e q u a t i o n s of r a d i a t i o n hydrodynamics when e l e c t r o - m a g n e t i c r a d i a t i o n i s assumed t o obey a l i n e a r - r e s p o n s e d i s p e r s i o n r e l a t i o n of t h e

form nw = kc where t h e r e f r a c t i v e i n d e x n depends o n t h e f r e q u e n c y

w

a n d / o r wave number k . From t h e a p p l i c a t i o n of t h e B o l t z m a n n - L i o u v i l l e t r a n s p o r t t h e o r y t o pho- t o n s i n t h e s n o r t - w a v e l e n g t h ( g e o m e t r i c a l o p t i c s ) l i m i t , I d e r i v e t h e e n e r g y and momentum e q u a t i o n s which, when combined w i t h a c l a s s i c a l (Euler-Lagrange-Navier-

S t o k e s ) t r e a t m e n t of a f l u i d m a t e r i a l medium i n LTE, y i e l d a c o m p l e t e d y n a m i c a l t h e o r y of l i n e a r i n t e r a c t i o n s ( + s t i m u l a t e d p r o c e s s e s ) between i n c o h e r e n t ( t h e r m a l ) r a d i a t i o n and d e n s e , l o c a l l y i s o t r o p i c m a t t e r . The t h e o r y i n c l u d e s a n a c c o u n t o f pondero-motive f o r c e s and e l e c t r o (magneto) s t r i c t i o n . Moreover, i t i s a p p a r e n t l y c a p a b l e of b e i n g g e n e r a l i s e d t o n o n - l i n e a r i n t e r a c t i o n s i n which t h e r e f r a c t i v e i n d e x depends o n t h e l o c a l s p e c i f i c i n t e n s i t y o f t h e r a d i a t i o n f i e l d , and, t o some e x t e n t , t o t h e t r e a t m e n t o f h i g h - f r e q u e n c y c o h e r e n t r a d i a t i o n . The g e n e r a l i s a t i o n of v a r i o u s a p p r o x i m a t e d forms of r a d i a t i o n - t r a n s p o r t t h e o r y ( e s p . d i f f u s i o n ) h a s been c o n s i d e r e d i n d e t a i l .

Some problems remain however. One s u c h i s t h e t r e a t m e n t o f anomalous d i s p e r s i o n . C u r r e n t r e s e a r c h work i s c o n c e n t r a t i n g o n t h e i n t e r e s t i n g a t o m i c p h y s i c s a s p e c t s o f e l e c t r o m a g n e t i c ( e s p . r a d i a t i v e ) p r o p e r t i e s o f a d i s p e r s i v e m a t e r i a l medium.

The f o l l o w i n g i s e x t r a c t e d from AWRE r e p o r t 0-20182 e n t i t l e d " C l a s s i c a l R a d i a t i o n Hydrodynamics i n Inhomogeneous R e f r a c t i n g Weakly D i s p e r s i v e Media". I n i t i s d e s -

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphyscol:1983803

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C8-26 JOURNAL

DE

PHYSIQUE

c r i b e d a t h e o r e t i c a l s t u d y o f t h e dynamical e f f e c t s of r a d i a t i o n t r a n s p o r t ( e s p e - c i a l l y LTE) i n a moving inhomogeneous l o c a l l y - i s o t r o p i c m a t e r i a l medium when t h e r a d i a t i o n d i s p e r s i o n r e l a t i o n i s g i v e n a s

(U = a n g u l a r f r e q u e n c y ,

k

= wavenumber, c = v e l o c i t y of l i g h t , n = REFRACTIVE INDEX = Re (€U)).

OUTLINE

O b j e c t i v e : t o d e v e l o p a g e n e r a l t h e o r y o f r a d i a t i o n t r a n s p o r t i n h i g h - d e n s i t y b u l k m a t t e r

-

i n LTE i n t h e f i r s t i n s t a n c e

-

t a k i n g f u l l a c c o u n t o f r e f r a c t i o n , d i s p e r s i o n and r e l a t e d m i c r o p h y s i c a l p r o c e s s e s .

S o l u t i o n : from t h e c o n c e p t o f a model p h o t o n d e s c r i b e d by t h e E i n s t e i n - d e B r o g l i e r e l a t i o n s , E

= n u ,

p

-

= .hk

-

and whose o n l y i n t e r a c t i o n s a r e w i t h t h e medium, o n e d e v e l o p s a d y n a m i c a l t h e o r y b a s e d o n a M a s t e r E q u a t i o n t h a t i s a g e n e r a l i s e d Boltzmann e q u a t i o n o f r a d i a t i o n t r a n s p o r t d e r i v e d from t h e L i o u v i l l e theorem.

The i n p u t p a r a m e t e r s o f s u c h a t h e o r y , v i z o p a c i t i e s and r e f r a c t i v e i n d i c e s , a r e i n t e r - r e l a t e d t h r o u g h d e t a i l e d b a l a n c e c o n d i t i o n s a n d , i n t h e l i n e a r r e g i m e , c a u s a l i t y - b a s e d d i s p e r s i o n r e l a t i o n s . These c a n b e shown t o b e e x p r e s s i b l e i n t e r m s of a s i n g l e complex f u n c t i o n of f r e q u e n c y and wave-number t h a t i s a n a l y t i c i n t h e u p p e r h a l f o f t h e complex-frequency p l a n e , and t h r o u g h s u c h a f u n c t i o n , c a n b e r e l a t e d t o a m i c r o p h y s i c a l model. T h i s f u n c t i o n embodies a f u l l d e s c r i p t i o n o f t h e l i n e a r r e s p o n s e of t h e medium t o

3

e l e c t r o m a g c e t i c d i s t u r b a n c e .

Method

(1) S p e c i f y r a d ; a t i o n d i s p e r s i o n r e l a t i o n

T h i s

i s

e x p r e s s e d i n t e r m s o f t h e r e f r a c t i v e i n d e x which

i s

a g i v e n f u n c t i o n o f :

(i)

f r e q u e n c y : n = n(w): FREQUENCY DISPERSIOX - most a p p r o p r i a t e a t h i g h f r e q u e n c i e s

( i i j w a v e - v e c t o r : n = n i k ) :

-

S P A ~ ~ A L D I S I J e K S I O N

-

may be i m p o r t a n t a t l o w e r f r e q u e n c i e s due t o c o l l e c t i v e e f f e c t s and e f f e c t s of medium a n i s o t r o p y

(4)

( i i i ) f r e q u e n c y and w a v e - v e c t o r : n = n ( w , k ) : b o t h FREQIJEXCY and

-

SPATIAL DISPERSION: Over a p e r h a p s l i m i t e d r a n g e o f

w

o r k may b e e q u i v a l e n t t o ( i i ) o r , i n c a s e o f i s o t r o p i c medium, ( i ) i f d i s p e r s i o n r e l a t i o n i m p l i e s a d i f f c o m o r p h i s m between L! and k

s u c h t h a t

o v e r f r e q u e n c y r a n g e o f i n t e r e s t

-

e x c e p t p e r h a p s a t a number of d i s c r e t e f r e q u e n c y p o i n t s ( s h a r p l i n e s ) . The r e f r a c t i v e i n d e x

w i l l

a l s o depend o n v a r i a b l e s p , T,

...

s p e c i f y i n g t h e l o c a l thermodynamic s t a t e of t h e medium. I n g e n e r a l n

i s

i m p l i c i t l y a f u n c t i o n of p o s i t i o n

r -

and t i m e t .

F o r s i m p l i c i t y we c o n s i d e r o n l y i s o t r o p i c media f o r which n i s i n d e p e n d e n t ( i n t h e CO-moving f r a m e ) of t h e d i r e c t i o n

2. -

The f o r m a l i s m a s p r e s e n t e d a l s o assumes n t o b e i n d e p e n d e n t of t h e r a d i a t i o n i n t e n s i t y ( l i n e a r r e s p o n s e r e g i m e ) . Howc?ver, ad hoc f o r n a l

g e n e r a l i s a t i o n t o i n c l u d e dependence o f r e f r a c t i v e i n d e x on i n t e n s i t y I (non- l i n e a r r e s p o n s e ) a p p e a r s s t r a i g h t f o r w a r d .

( 2 ) Apply c l a s s i c a l ( I A i o u v i l l c - B o l t z m a n n ) t r a n s p o r t t h e o r y t o t h e d e r i v a t i o n o f t h e g e n e r a l t r a n s p o r t e q u a t i o n . ( V a l i d when grou;) v e l o c i t y vg i s e n c r g y p r o p a g a t i o n v e l o c i t y . )

(3) E s t a b l i s h d y n a m i c a l p r o p e r t i e s of an i n d i v i d u a l p h o t o n and h e n c e , w i t h a i d o f t h e t r a n s p o r t e q u a t i o n , d e d u c e e q u a t i . o n s of e n c r g y and no:nentum t r c n s p o r t

("Pl" e q ~ a t i o n s ) .

( 4 ) Combine t h e s e w i t h c l a s s i c a l f l u i d dynair~ic (Euler-1,ngrr;nge-Navier- S t o k e s ) t r e a t m e n t o f m a t e r i a l i n c o r p o r a t i n g a t h e r ~ ~ o t l y n a m i c trc.ntmcnt of t h e t o t a l s y s t e m => d e t a i l e d t h e o r y of r a d i a t i o n "hydrodynamics" i n c o r p o r a t i n g

t r e a t m e n t s o f ELECTRO/UGNETOSTRICTION (and r e l a l e d E!,ECTRO/:~~GNET@CALORT(~ EFFECTS) and POl\'DEROMOTIVE FORCES.

(5) Apply a p p r o x i m a t i o n s f o r LTE r a d i a t i o n t r a n s p o r t : c l . o s u r e of 1'1

e q u a t i o n s + f r e q u e c c y a ~ r e r a g i n g (Planck a?" R o s s e l e n d ) =>

Di

f [us; nq a p p r o w i n ~ a t i o n Averaged o p a c i t i e s depend on t h e r e f r a c t i v e i n d e x .

( 6 ) D e t e r m i n e r e f r a c t i v e i n d e x and o p a c i t i e s from m i c r o p h y s i c a l n o d c l . ( i ) M o d i f i c a t i o n of I.TE d e t a i l e d b a l a n c e c o n d i t i o ; ~ when n

# 1

(5)

JOURNAL DE PHYSIQUE

implies modification of opacities for use when n P 1 in place of those which apply when n

=

1.

(ii) Standard calculations (XSNB) yield a so called reduced opacity

KO

from which refractive index can be deduced by applying a Kramers-Kronig dispersion relation (refractive index and opacity being related to real and imaginary parts of the dielectric

function

€(W)

or, more generally, €(w)p(w)). "True" opacity is then K O / ~ . (iii) Need to consider effects of dispersion on treatment of

microphysical processes (collective effects, modified spectroscopy, multi-atom coherence, recoil corrections ...

) =>

development of more general microphysical models.

(7)

Other problems include treatment of anomalous dispersion (particularly when a(n~))/aw

<

1 over a finite range of frequencies)

=>

breakdown of Hamiltonian description embodied in the transport equation, and phase-space representation.

Group velocity is not in (O,c), and therefore is not energy propagation velocity.

1 .

THERMODYNAMIC EQUILIBRIUM

Application of Bose-Einstein statistics in the continuum approximation yields the equilibrium phase-space distribution as

" 3

in which f(k)d k is the mean equilibrium density of photons with wave vectors in

"

the range d k about

3

- k. - In frequency space the corresponding distribution is

"

2

dk cnL -

N(w)dw

=

4nk f (k) - dw dw

=

- NB (w)dw

g

-

'U

where N

(U) =

- 2 3 e ~ / ; A ~ 1 is the BLACK BODY distribution which applies

B

s c

when n

f

1. The EQUILIBRIUM SPECIFIC IliTENSITY is therefore

(6)

i s

t h e PLANCK FlJNCTION o r BLACK BODY SPECIFIC INTENSITY.

2. CLASSICAL RADIATION TRANSPORT

2 . 1 G e o m e t r i c o p t i c s l i m i t i s v a l i d i f

( i ) P h o t o n w a v e l e n g t h i s s m a l l o n a l l o t h e r r e l e v a n t s c a l e s . ( i i ) I n p a r t i c u l a r

h

<< mean f r e e p a t h f o r a l ) s o r p t i o r ~ ancl

scattering => v a l i d i t y of TFXCSPARIXCY CONDITIO:;

l m E << R e E

e.g. I n a c o l l i s i o n do!ninated n o n - d e g e n e r a t e n e u t r a l c l a s s i c a l plasma f o r w h i c h

2

2

c o n d u c t i v i t y , 0 = E V . / ( U 2 + V . )

p o e l e~

( r a d i a t i o n p r o p a g a t i n g above plasma f r e q u e n c y ) ,

( n o n - d e g e n e r a t e ) , t h e t r a n s p a r e n c y c o n d i t i o n i s

w h i c h

i s

s u f f i c i e n t . I n t h e above formulae, Z = mean i o n i z a t i o n s t a t e (Ne = %Ni), ye = S p i t z e r c o r r e c t i o n , N . = i o n d e n s i t y (cm

-3

) ,

v

= e f f e c t i v e e l e c t r o n - i o n c o l l i . s i o n frequency.

e i

2.2 B o l t z n a n n e q u a t i o n of r a d i a t i c n t r a c s p o r t :

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JOURNAL DE PHYSIQUE

a H a f all a f P o i s s o n b r a c k e t E

- . - - - -

ak a r a r ' ak S o u r c e l ~ u n c t i o n a l T h i s e q u a t i o n i s obeyed ( e x a c t l y ) by s y s t e m o f n o n - s e l f i n t e r a c t i n g c l a s s i c a l p a r t i . c l e s ("photons") moving i n a sniootli I l a r n i l t o n i a n f i e l d H ( k ; r ; t )

- -

= w ( k ; r ; t ) and

- -

o t h ~ _ r ! . ~ i s e r n h j e c t o n l y t n d i s c r e t e ( s ~ ? ( _ ( . e r i n g s , a h s r \ r ; t i n n r , E ) T ~ ~ S ~ _ ~ O I I C ) i c t e r - a c t i o n s r e p r e s e n t e d by t h e s o u r c e f u n c t i o n a l S ( { f } ; k ; r ; t ) . k

- -

I n t h i s e q u a t i o n , f ( k ; r ; t ) i s t h e p h a s e - s p a c e d i s t r i b u t i o n w h i l e s k i s t h e n e t r a t e o f p r o d u c t i o n of

-

p h o t o n s p e r u n i t "volume" o f p h a s e s p a c e .

The r e s u l t i n g t r a n s p o r t e q u a t i o n t h a t one e v e n t u a l l y o b t a i n s f o r t h e s p e c i f i c i n t e n s i t y i s o f t h e form

i n which a s u b s c r i p t d e ~ o t e s t h e CO-moving f r a m e

-

o t h e r w i s e i n e r t i a l f r a m e ( c o - o r d i n a t e s

r , t -

a r e a l w a y s r e f e r r e d t o t h e i n e r t i a l f r a m e )

-

and

U = medium v e l o c i t y i n i n e r t i a l f r a m e

-

v = g r o u p v e l o c i t y i n CO-moving f r a m e (v = g r o u p v e l o c i t y i n

-g

-

inertial f r a m e ) .

Note how t h e t r a n s p o r t e q u a t i o n g e n e r a l l y i n v o l v e s 1 / n 2 i n p l a c e o f

I .

The q u a n t i t y 1 / n 2 u 3 i s a LORENTZ INVARIANT.

I n t h e a b o v e e q u a t i o n s , t h e s o u r c e f u n c t i o n a l s a r e s p e c i f i e d a s b e i n g g i v e n i n o n e of t h e f o l l o w i n g f o r m s :

a b s o r p t i o n

d i r e c t s c a t t e r ? ng

(8)

i n d u c e d s c a t t e r i n g ;

3 4 4

+

is l [ ( 5 )

e x p f i ( w 1

-

U ) / ~ T ) I ( U '

,g') -

I ( u , ~ ) z ( U , u ' ; k , k ' ) d w ' d 2 i '

I - -

W d i r e c t s c a t t e r i n g

i n d u c e d s c a t t e r i n g i n which K ~ ( w ) i s t h e a b s o r p t i o n o p a c i t y , N t h e mean d e n s i t y o f s c a t t e r e r s and

a

t h e therrna1.ly-averaged s c a t t e r i n g c r o s s - s e c t i o n . 2 . 3 C o n d i t i o n s a t b o u n d a r i e s and i n t e r f a c e s .

T h e s e a r e p r o v i d e d by S n e l l ' s Laws, which imply

n 2 c o s eldQl

1

= n2 c o s 0 dQ 2 2 and t h e F r e s n e l f o r m u l a e w h i c h y i e l d

PF

= 2n n c o s

e1

c o s 8

1 1

1 2 2 2 +

(nl COS

O1 +

n 2 COS 02) ( n 2 COS

O1

+ n1 COS e 2 ) i n t e r m s o f which

R12 =

1 -

P = f ( A / h ) ( l

-

PF)

c o s dQl n 2

T12 = P - 2

cos

e 2

d n 2

- ( T )

1

P

where

A

i s t h e s u r f a c e d i f f u s e n e s s and f ( x ) i s a f u n c t i o n f : ( 0 , ~ ) + ( 0 , l ) s u c h t h a t f ( 0 ) = 1 and f (m) = 0 ( f % e - * ) . R e f l e c t i o n i s s t r o n g l y damped a t i n t e r f a c e s where

A

>> h.

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JOURNAL DE PHYSIQUE

Note t h a t t h e above p e r m i t a d i s c o n t i r i u i t y i n I where n i s d i s c o n t i n u o t t s , e v e n i n e q u i l i b r i u m :

< => I

d i s c o n t i n u o u s .

I n LTE, t h e f u n c t i o n 1 / n 2 i s a c o n t i n u o u s f u n c t i o n o f p o s i t i o n . 2.4 Energy t r a n s p o r t

D e f i n i n g t h e r a d i a t i v e e n e r g y d e n s i t y

and t h e e n e r g y f l u x

t h e e n e r g y t r a n s p o r t e q u a t i o n t h a t f o l 1 o r . r ~ by t a k i n g t h e a p p r o p r i a t e z e r o t h moment o f t h e t r a n s p o r t e q u a t i o n i s :

au

1 2,-

~ 0 1 1

- + v . F + - j + d , k + Q

= o

a t - - C a t -

----..-A

?'

Ponderomotive c o n t r i b u t i o n where

c o l 1 c o l 1

=

Q, +

u.fo

( G a l i l e a n t r a n s f o r m a t i o n v a l i d i f u / c << 1 )

where

f c o l l

-0 ( G a l i l e a n t r a n s f o r m a t i o n v a l i d i f u / c

<<

1).

Momentum t r a n s p o r t

I n

t e r m s o f t h e r a d i a t i v e (Minkowski) momentum d e n s i t y

(10)

and t h e c o r r e s p o n d i n g s t r e s s t e n s o r

t h e momentum t r a n s p o r t e q u a t i o n , which i s a f i r s t moment of t h e t r a n s p o r t e q u a t i o n ,

p o n d e n n o t i v e c o n t r i b u t i o n i n which T~ - - d e n o t e s t h e t r a n s p o s e of C - .

3 .

RADIATION HYDKODYNA'IICS

To c o m p l e t e t h e p i c t u r e , t h e above e q u a t i o n s must b e c o u p l c d t o t h e a p p r o p r i a t e e q u a t i o n s f o r t h e e n e r g y and momentum a s s o c i a t e d w i t h t h e m a t e r i a l . T h i s r e q u i r e s a r e s o l u t i o n of t h e i s s u e s sometimes r e f e r r e d t o a s " t h e mosentum of l i g h t problem". E a s i c a l l y , t h e problem i s how t o decompose t h e t o t a l s t r e s s t e n s o r of t h e s y s t e m p r o p e r l y i n t o a r a d i a t i v e ( o r e l e c t r o m a g n e t i c ) component and a t h e r m o k i n e t i c ( o r m a t e r i a l ) component. P e i e r l s d e n o n s t r a t e s t h a t t h e s e a r c , i n g e n e r a l , two d i f f e r e n t d e c o m p o s i t i o n s , a s p a r t of

a p h o t o n ' s momentum a s g i v e n

by nfik i s a c t u a l l y a s s o c i a t e d w i t h mechanical motion of t h e medium under t h e -

i n f l u e n c e o f t h e p h o t o n e l e c t r o m a g n e t i c f i e l d . The b a r e e l e c t r o m a g n e t i c momentum i s t h a t p r o p o s e d by Abraham: g = 4 w v / c L from which we c a n d e f i n e a n e l e c t r o -

-g m a g n e t i c momentum d e n s i t y

G

- by:

G

=

f g d k

3

- - -

The f i n a l r e s u l t i s t h a t t h e e n e r g y and momentum e q u a t i o n s r e p r e s e n t i n g t h e m a t e r i a l c a n b e e x p r e s s e d

as

f o l l o w s

DE

p - =

Dt (!U)

:

- +

Q

- £.U .-. .-. +

r . .

i n w h i c h E i s t h e m a t e r i a l i n t e r n a l e n e r g y d e n s i t y , p t h e mass d e n s i t y , and

G

- t h e

t h e r m o k i n e t i c s t r e s s t e n s o r . The q u a n t i t i e s f and

Q

r e p r e s e n t t h e p r i m a r y

c o u p l i n g t o t h e r a d i a t i o n f i e l d :

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JOURNAL DE PHYSIQUE

The radiation field also gives rise to photocaloric and photostrictive

(=

magnetostrictive + electrostrictive) contributions to E and

0 .

The relevant

... -

relations, which apply in the co-moving frame in LTE, are

where E") and

a(')

are the internal energy and stress-tensor which apply under

..

the prevailing conditions of temperature and density in the absence of radiation;

F is the total free-energy

=

F(') - Pr; Pr is the radiation pressure

=

- 3

1

trace L ) ; ( '

O H

is the so-called Helmholtr Stress-Tensor which contains the

-0

=

photos trictive pressure,

which reduces, in the case of unpolarised, high-frequency, monochromatic radiation, to

Consequently, the relations which apply to a general unpolarised high-frequency radiation field are found to be:

an

2..

E - = L I 3 dud k

pc aT

The time-derivative terms involving M - - G in the expressions for f and ...

.-.

Q arise

in respect of the mec':ianical momentum component of the radiation.

(12)

Thc non-collisional part of the radiatively induced force on a material is the ponderomotive force fPmf which, according to the above, is given -

(u/c

<<

1) by:

special case of which are:

(i)

A

beam of monochromatic radiation in a stationary stezdy-state medium:

2 2

(ii) Monocl~romatic radiation in a plasma (nz

=

1 - w /w

)

P

which is independent of the plasma's state of motion (at least to first order in u/c) .

4 .

DIFFUSION APPROXIMATION

I n a quasi-equilibrium state of an optically thick system, the limiting diffusion-approximation solutions of the transport equation are

W s a T

4

in which

with

and

where

8

is the radiation temperature.

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JOURNAL

D€

PHYSIQUE

In terms of the solution W the radiation pressure P and the enthalpjr-

0'

density U + P are given by:

where

and

Note that, in general, the radiation pressure is no-longer given by P

=

U/3.

Finally, rcrrembering that -P is the Helmholtz Zree energy U - TS, one also finds the entropy associated with the radiation to be given by

5.

ABSORPTION COEFFICIENT

Neglecting scattering, the absorption coefficient

K

is found to be

related to the imaginary part of the product of the electromagnetic susceptibilities

by

L W

K,

=

( ; ) I~(EP)

in which €(w)U(w) is analytic in upper half U-plane and satisfies the Kramers-Kronig dispersion relations. (These permit expression of Re(cp), and hence n, in terms of

K ~ . )

Note the factor of l/n in the above expression.

6. ANOMALOUS DISPERSION

A problem with the above theory is that it does not yield a correct description in regions of anomalous dispersion where the energy propagation velocity vE is not the group-velocity v . Indeed, in such a region, v may not

g be in (0,c) and cannot therefore represent the propagation velocity.

A realistic calculation of the energy-trznsport velocity v

=

E

X

H/U

E -. -

in a region of anomalous dispersion (Sommerfeld and Brillouin) yields the result

(14)

in place of

for n

=

Re

F

1 . Writing

E =

l + xl + ix2

=

(n + ig12, we have, at the centre of an isoiated resonance wnere

axl - - - X, ax2

- -

x l = o , - -

a~ y

S

aw - 0 , that

while

Away from resources where x2

2

<< lxl l

;

IX2 I

<<

1, lx2 l <<

W

2 , 2

>

0 both

formulae yield:

It is not clear how the foregoing theory can be improved to take account of the above. It is not sufficient to simply replace v throughout by vE, es v often

g

g

arises as a Jacobian in transformations between

W

and k.

SELECTED BIBLIOGRAPHY General

CROWLEY, B J B: Op. cit. (to be published, with revisions, in physics Reports).

POMRANING, G C: The Equations of Radiation Hydrodynamics (Pergamon, 1973).

COX, J P and GUILI, R T: Principles of Stellar Structure (Gordon and Breach,

W ,

1968) v01 I.

Radiation pressure and ponderomotive forces in plasmas

LANDAU, L D and LIFSHITZ, E M: Electrodynamics of Continuous Media (Pcrgamon 1960).

PENFIELD, P and HAUS, H A: Electrodynamics of Moving Media (MIT Press,

Camb., Mass., 1967).

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C8-38 JOURNAL DE PHYSIQUE

BOOT,

H

A

H,

SELF, S A a n d SHERSBY-IWIE,

R B K: J .

E l e c t r o n i c s a n d C o n t r o l 5

(1958) 434-453.

I h W N , C L: A s t r o p h y s .

J .

142 (1965) 201.

MORE, R M:

J.

P h y s . A: Math. Gen. 2 (1976) 1979-1985.

Momentum o f l i g h t p r o b l e m

BURT, M G a n d PEIERLS, R: P r o c . R. S o c . Lond. A, 333 (1973) 149-156.

PEIERLS, R: P r o c . R . Soc. Lond. A, 347 (1976) 475-491.

JONES, R V a n d LESLIE,

B:

P r o c . R. S o c . Lond. A, 360 (1978) 347-363.

BREVIK, I: P h y s . Rep. 52 (1979) 1 3 4 .

LAX, H M, SUEN, W

M a n d YOUNG, K: P h y s . Rev. A 2 (1982) 1755-1763.

Anomalous d i s p e r s i o n

BRILLOUIN, L: Wave P r o p a g a t i o n a n d Group V e l o c i t y (Academic P r e s s ,

hY,

1 9 6 0 ) .

C o p y r i g h t @ C o n t r o l l e r HMSO, London, 1 9 8 3

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