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An alternative way of computation of amplitudes and intensities in time-dependent Mössbauer spectroscopy (TDMS)

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HAL Id: jpa-00212379

https://hal.archives-ouvertes.fr/jpa-00212379

Submitted on 1 Jan 1990

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An alternative way of computation of amplitudes and

intensities in time-dependent Mössbauer spectroscopy

(TDMS)

I.D. Christoskov, E.I. Vapirev

To cite this version:

(2)

An

alternative

way

of

computation

of

amplitudes

and

intensities

in

time-dependent

Mössbauer

spectroscopy

(TDMS)

I. D. Christoskov and E. I.

Vapirev

Department

of

Physics, University

of Sofia,

Sofia-1126, Bulgarie

(Reçu

le 24

juillet

1989,

accepté

sous

forme

définitive

le 13 novembre

1989)

Résumé. 2014

Nous exposons une autre

façon

de

présenter

la

dépendance temporelle

des

amplitudes

et intensités de radiation obtenues dans des

expériences

de diffusion et

d’absorption

résonnante. Des suites infinies de fonctions de Bessel avec des coefficients

complexes

sont

remplacées

par des

intégrales

définies

simplement

calculables avec une seule fonction de Bessel par

point

de tabulation. Il s’ensuit une réduction du temps de calcul pour

l’ analyse

des résultats

expérimentaux.

Abstract. 2014 An

alternative way of

presenting

the

time-dependent amplitudes

and intensities of

radiation,

corresponding

to resonant

absorption

and

scattering experiments,

is

developed.

Infinite series of Bessel functions with

complex

coefficients are

replaced by

simple

for calculation definite

integrals

and the number of Bessel function calls is reduced to one per a tabulation

point.

Thus the calculational effort for

experimental

data

processing

becomes smaller. Classification

Physics

Abstracts 24.30

Classical

electromagnetic theory

-

damped

oscillators,

dispersive

media,

and the

correspondence

between the

frequency

and the time domain - has been used to describe the

phenomenon

of « time filtration » both for transmission

[1]

and resonant

scattering

[2, 3].

Since then many similar

experiments

have been

performed,

the interest

arising

from the fact that those

experiments

are the

only

ones in which

quantum

effects in the time domain within the natural linewidth

(or

the excited state

lifetime)

could be observed.

In the

present

work an alternative

technique

(again

in terms of the

electromagnetic

approach)

is

proposed

for

presenting

the

time-dependent amplitude

and

intensity

of

radiation, corresponding

to resonant

absorption

and

scattering experiments.

1. Resonant

absorption.

Let the source

(S)

linewidth be denoted

by

Fs,

and the resonant level lifetime be

,r, = 1 IF,

(h = 2 ir ).

The central

frequency

of S is lds. The filter

(F)

linewidth is

T f,

its central

frequency - w f,

and the effective resonant

thickness - B = no- 0 fa.

(3)

444

n is the number of resonant absorber nuclei per

cm2,

o-o - the resonant cross-section and

f a

- the recoilless fraction of

absorption.

The

frequency amplitude

of S is

and the

frequency

amplitude

of F is

Hence the

time-dependent amplitude

of transmitted

gamma-quanta

will be the Fourier

image

of the

product

S(,w).

F(w ) [1] :

The factor

F,lFf

is introduced in the

exponent,

thus

preserving

the

absorption

line area. If we introduce the

following designations

- relative shift V

=

CI) s - CI) f,

relative

broadening

rs

s

R =

r f/rs

[u

=

(R - 1 )/2],

and time in source lifetime units T =

Fs t ;

the

following

expression

for

A,, (T,

B, R,

V )

can be obtained :

J,,

are Bessel functions of order n. In TDMS transmission

experiments

the time distribution of

counts of transmitted

gamma-quanta

(t

= 0

corresponds

to the moment of formation of the

Môssbauer state in the

source)

can be described

by

the

squared amplitude

Expressions (2)

and

(3)

for the

amplitude

and the

intensity

are

usually applied

for numerical simulation of

experiments

or for

experimental

data

processing

(least

square

fitting

for

parameter

search,

etc.).

Nevertheless, they

are not very convenient because the series

(2)

converges with reasonable accuracy

only

after order 5-7 and therefore for the calculation of

(2)

at a

single

time

point

several calls of the Bessel function are necessary. Here it should be

specified

that for the sake of better convergency the series

(2)

must

always

be

absolutely

convergent.

So,

at a fixed set of

parameters

(B,

R,

V ),

if T becomes

large enough

and the modulus of the coefficient in front of the Bessel function exceeds

unity,

the series

(2)

must be transformed

by

means of the

generating

function of

ln (z).

At

that,

the

application

of the recursion formula for calculation of

J,,(z), n:--.

1 leads to an

abrupt

loss of accuracy in the

vicinity

of the critical value of T.

Therefore,

it is reasonable to make use of the reverse recursion formula

[6] [starting

at a

sufficiently big

order of the Bessel function n

(e.g.

7 = 9)].

Furthermore,

the task is

complicated

because for the purpose of

experimental

data

fitting

the transmitted

intensity

Itr(T, B, R, V ),

together

with its derivatives with

respect

to

all

parameters

subject

to

determination,

must be calculated for a

large

sequence of measured

(4)

That is

why

we

suggest

a more convenient

presentation

of

expressions

(2)

and

(3).

Let us introduce the

quantities a

=

(u

+

iV )/B

and z =

ÙÔ.

If we make use of the connection

[4] :

the transmission

amplitude

takes the form :

The

integral

in the RHS of

(4)

can be transformed :

Finally,

for

Atr(T,

B, R, V )

one obtains :

The

intensity

takes the form :

where

In this form the effect of the resonant interaction appears as an addition to the pure

exponential

decay

of the excited state in the source. The

sub-integral

function is smooth

enough

and well

suppressed

with

time,

and for a

reasonably

small

step

of the

argument

(which

is the case in

experimental

data

fitting)

even the

simple

trapezoidal

rule for numerical

quadrature

is sufficient for

calculating

the

integral.

Due to the

additivity

of the

integral only

one call of the Bessel function per tabulation

point

is necessary, instead of several ones in the conventional case.

Moreover,

its derivatives with

respect

of the

parameters

(R,

B,

... )

have a

simple

form.

Therefore,

this method

requires

a

substantially

smaller calculational effort. It has been tested in numerous

applications

and has

proved

to be

fast,

accurate and

simple

for realization. Here the

following

must be

specified :

if the values of the

amplitude

and the

intensity

are needed for a small number of remote moments of

time,

the conventional method is more suitable since the number of calls of the Bessel function does not

depend

on time.

2. Resonant

scattering.

Let

/3

be the resonant thickness of a

layer

of the

scattering

filter.

According

to the

approach

(5)

446

where

The

following generally applicable

relation

[5]

between the

amplitudes

Atr (T,

6,

R,

V )

and

Asc(T, (3,

R,

V )

exists :

Therefore,

all results demonstrated in section 1 can be

applied

in this case. For the final calculation of

1 sc (T, B, R, V)

again

a

simple

numerical

quadrature

can be

applied,

thus

eliminating

the

necessity

to use Bessel function series and all

problems

connected with their convergence. Modifications of this scheme have also been tested in several

applications

and have

proved

to work

effectively.

References

[1]

LYNCH F. J., HOLLAND R. E. and HAMMERMESH M. H.,

Phys.

Rev. 120

(1960)

513.

[2]

THIEBERGER P., MORAGUES J. A. and SUNYAR A. W.,

Phys.

Rev. 171

(1968)

425.

[3]

DROST H., PALOW K. and WEYER G., J.

Phys. Colloq.

France 35

(1974)

C6-679.

[4]

PRUDNIKOV A. P., BRYCHKOV Yu. A., MARICHEV O. I.,

Integraly

i

ryady.

Special’nye

funkcii.

(Integrals

and Series.

Special

Functions),

M. : Nauka

(in Russian)

1983.

[5]

VAPIREV E. I., KAMENOV P. S., DIMITROV V. and BALABANSKI D. L., Nuclear Instrum. Methods 219

(1984)

376.

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