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POSITRON AND ELECTRON INTERACTION WITH MATTER DISSERTATION SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE AWARD OF THE DEGREE OF iWasiter of ^fjilosopljp "^ * IN PHYSICS \yn ^n. ni BY ARUN PAWAR ••i*.; m A^ UNDER THE SUPERVISION OF jx f ~ l, DR. T. S. GILL *• * - DEPARTMENT OF PHYSICS ALIGARH MUSLIM UNIVERSITY ALIGARH (INDIA) 2003

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Page 1: POSITRON AND ELECTRON INTERACTION · electron scattering from atoms can carry out calculation. There are several important differences between electron and positron scattering. However

POSITRON AND ELECTRON INTERACTION WITH MATTER

DISSERTATION SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS

FOR THE AWARD OF THE DEGREE OF

iWasiter of ^fjilosopljp

"^ *

IN

PHYSICS \yn ^n. ni

BY

A R U N PAWAR

• • i * . ;

m A^

UNDER THE SUPERVISION OF jx f ~ l ,

DR. T. S. GILL *• * -

DEPARTMENT OF PHYSICS ALIGARH MUSLIM UNIVERSITY

ALIGARH (INDIA)

2003

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/v' v ' "' «-,

I % s .

/ '7 li ;v"-'=\3ri^

1 7 JAN 2011

DS3801

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Dr, T. S. Gill

DEPARTMENT OF PHYSICS ALIGARH MUSLIM UNIVERSITY ALIGARH- 202002 (U. P.), INDIA Phone: +9] 571 2701001 (Off.)

+91 571 2601768 (Res.)

CERTIFICATE

This is 10 certify that the work reported in this dissertation entitled

"POSITRON AND ELECTRON INTERACTION WITH MATTER" is

original work of Mr. Aran Pawar, carried out under my supervision.

(Dr. T. S. Gill)

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^^©oe^ir/j^

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Ackno wledgemen ts

I am deeply indebted to Dr. T. S. Gill, Reader, Physics Department

Aligarh Muslim University, Aligarh, whose encouragement and guidance

has been a constant source of inspiration to me throughout this work.

I express my gratitude to Prof. A. K. Chaubey, Chairman, Physics

Department A.M.U. Aligarh, for their interest, and extending

departmental facilities during the period of this work.

I am thankful to all teachers, staff members and non-teaching staff of this

department.

I wish to express my thanks to Dr. Manoj Sharma (Young scientist) at the

same department and Dr. Pankaj Kumar Sharma with Dr. Avinash

Agrawal for their active help and cooperation.

I also wish to thanks to my younger brother Anuj and Mr. Sumit Pal Gill

for their help to make computer program for calculation.

I wish to special thanks to Mr. Nisar Ahmad to provide necessary help

and suggestion during the calculation,

I wish to thanks various of my colleagues, Ms. Unnati, Mr yatendra, Mr.

BK Sharma, Ms. Anjna Maheshwari, Mr. Ramprakash, Arafat Firdos,

and Mr. D. Singh for their cooperation during this work.

Finally I want to express my very special thanks to my parents with all

family members and intimate friends Dr. Sarita Verma and Ms. Nootan

for their support and constant encouragement and inspiration during the

period of work.

(ARUIV PAWAR)

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CONTENTS

CHAPTER - ONE Introduction to different approaches in Positron and

Electron Penetration

1.1 Introduction 1

1.2 Range definition 4

1.3 Experimental Work 7

1.4 Theoretical developments 8

> C. S. D. A. Ranges 8 > Average penetration depth 9 > Projected Ranges. 11

References 15

CHAPTER- TWO Penetration of Positron and Electron Through different

materials

2.1 Introduction

2.2 lonisation and Excitation loss

2.3 Bremsstrahlung

> Classical theory of Bremsstrahlung > Quantum mechanical theory of

Bremsstrahlung > Comparison with classical theory

2.4 Empirical relations of total stopping power

of Electron and Positron

2.5 Multiple scattering theories

2.6 Straggling.

References

17

18

19

20

21 22

23

24

29

30

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CHAPTER- THREE Theoretical approach for buildins transmission curves

3.1 Introduction

3.2 The present methods of calculation

3.3 Present methods for calculating

Ranges and Absorption coefficients.

References

31

32

36

39

CHAPTER- FOUR Results and Discussion of present theoretical approach

4.1 Introduction 40

4.2 Absorption coefficients 40

4.3 Comparison of present theoretical

and experimental Ranges. 41

References 44

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T:L^Cr(RP^(FEJ^i:(RA'TlO!N'

y Introduction y (Rfluge {fefinition ^ ^JCperimentaCwor^ ^ lUeofeticaCdeveCopments

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1.1 Introduction

The information about the interaction of electrons and positrons through

different materials is frequently required for the experimental methods

in nuclear, atomic and solid state physics.

The transmission and penetration of charged particles tlirough matter

has a great importance for experimental as well as theoretical Physics. In

the experimental study of the energy levels and transition of nuclei,

there are many cases, which require the measurement of the kinetic

energy of a charged particle by method, which depend upon absorption

and scattering phenomena.

The study of the passage of electrons and positrons through matter has

very useful applications in nuclear physics, semi conductor physics,

health physics and several other related fields. It is also useful for the

study of radiation damage, biological effect, and energy distribution at

different depth in matter.

The mechanism by which a charged particle loses its kinetic energy, or

is deflected from its original path, involve two principal types of

interaction,

(1) Inelastic interaction

(2) Elastic interaction

Further we can divide these two into following

(a) Inelastic collision with atomic electrons.

(b) Inelastic collision with a nucleus.

(c) Elastic collision with atomic electrons.

(d) Elastics collision with a nucleus.

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In an absorbing material, a moving particle is slowed down and finally

brought to rest by the combined action of all four of these elastic and

inelastic processes. A particle whose initial kinetic energy is say 1 MeV

may have more than lO'* individual collision of each type.

Which type of interaction, if any will occur when a swift

particle passes a particular atom is described only by the laws of chance.

From collision theory, one can obtained the probabilities of any

particular type of collision, of any particular energy loss, and of any

particular change of direction of the motion of the incident particle.

After the first collision, these probabilities can be applied to a second

collision, then to a third, etc. This method is very complicated, but some

reasonable results have been obtained, notably at Los Alamos, using

electronic computing devices.

Electron bombardment of a sample is unique to microprobe analysis and

produces a large number of effects from the target materials. It is critical

to understand the volume of material from which these are produced and

the effects themselves that includes: X-rays (both continuum and

characteristic), backscattered and transmitted electrons, secondary

electrons Auger electrons etc. (fig. 1.1).

lonisation, bremsstrahlung radiation and annihilation are the three

mechanisms by which electron loses energy in medium.

Coulomb interactions between fast moving electrons and molecular

electrons excite and ionise the molecule producing ion pairs.

When a fast moving electron is accelerated or decelerated, a photon is

emitted, and such photons are called bremsstrahlung radiation (braking

radiation).

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IiKideitf Ele( ti oil beam

.vecoiidJUT Elecliou

Aiigei' Elecri'Oii

back scartered Ekclioii;^

Tliiii s'peciineii

cliviiacreiisfic X - l a v s

Tiaiisinifed ElfCflOILS

bi-cin.sti'aldmt;s:

visible ligltr

If

absorbed ciuieiif

diffeiecfed election

Fig. 1.1 Effects produced by electron bombardment of a material

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Although the positron is an anti particle of the electron, the cross section

(probability) for direct annihilation is much smaller than that for elastic

or inelastic scattering. For these latter processes, treating the positron as

a positive electron and using the usual theoretical methods developed for

electron scattering from atoms can carry out calculation. There are

several important differences between electron and positron scattering.

However since the positron is a distinct particle from the electron,

exchange interactions with the bound atomic electrons do not occur.

More interestingly, the formation of positronium (the bound state of an

electron and a positron) can and dose occur in positron-atom scattering.

In addition, the fact that the sign of the interaction between the positron

and the atom is the opposite of that for electrons leads to rather different

behaviour of the cross section.

As the electron passes through matter it loses its energy in ionising and

radiative collision. In each of these it may suffer significant deflections.

In addition there is a large number of deflection due to elastic scattering.

The net result is that the electron's path as it passes through the absorber

is very tortuous. In practice, one finds the path length to be from 1.2 to 4

times the thickness of the absorber traversed, the ratio being largest for

slow electrons in high Z materials.

The range R of a particle is an experimental concept, relating to the

thickness of an absorber, which the particle can just penetrate. Several

distinct definitions of range, which depend upon the method employed

to determine them, are in common uses.

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1.2 Range Definitions

If a curve is plotted between the fraction of the incident Positrons and

electrons which pass through a given thickness and those thickness, It is

obtained that for high thickness of the absorber the curve passes into the

back-ground, which is due to cosmic and gamma rays. Schonland ' and

Flammersfield^ ', define the point at which the extension of the linear

portion of the transmission curve meets the background as the practical

range, the point where the tail of the transmission curve meets the back

ground is called the maximum range. The maximum range of electrons

and positrons is a very important quantity but it is very difficult to

explain theoretically, because the diffusion is a complicated

phenomenon, which sets in at the end of transmission curve. The

extrapolation of the linear portion of the transmission curve of the

monoenergetic electrons to the thickness axis known as practical

maximum range. A similar definition of range has given by some

workers like Ebert et al ^^\ Tabata et al ^'^\ They define the extrapolation

range Rex, as the point where the tangent at the steepest point on the

almost straight descending portion of the transmission curve meets the

thickness axis.

The practical range, the practical maximum range, and the extrapolation

range are very useful experimental quantity, including the straggling

effects hence can not be compared with theoretical straggling free range.

The range of electrons theoretically, can be given as the limiting

thickness of the absorber beyond which essentially none of the

originally incident electrons emerge. But due to the straggling effects

such a thickness practically dose not exist.

It is not possible to compare the experimental measurements with the

theoretical ranges.

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c

o o

a.

CO c

6 z M

CO

UJ

00 u

H

\J

C3

* # "^ t> CO c C3 L_

0

fS

• »"

eJD

1

oi V CO 2 i— ^ c ^ E CO

E (U

x : • - 1

T3

§

^

.

o

o 31VU DNIlNnOO

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The straggling free practical range Rfj-^ for electrons and positrons can

be define as the point where the extrapolation of the linear portion of the

transmission curve meets the straggling portion of the curve, when it is

extrapolated in the backward direction. All the ranges, which have

defined here, are shown in fig. (1.2) But extrapolated range R x is not

shown because it cannot be shown on semi log graph.

It has been proved experimentally that the range/J^^ is not sensitive to

the strength of the used source. But extrapolated range R x is very much

sensitive of the source strength and percentage of transmission reached.

For light and medium atomic number absorbers the tail of transmission

curve can be shown by a straight line this tail corresponds to straggling,

and error involved in its extrapolation in the backward direction is very

small. For high atomic number absorbers straggling part of the

transmission curve cannot be represented by a straight line because

some error is possible in its extrapolation in backward direction to find

R^fp. In the measurement that has been done by Gill ^^^ et al. this error is

found of the order of 2% for gold and lead.

Electron's total path length is a quantity, which is completely different

from its range. The distinction can be visualized from fig. (1.3) Where R

is the range.

The total path length has been observed in a few experiments, using

cloud chambers or photographic emulsions. Among these, one by E.J.

Williams ^^ provides a direct comparison of total path length S to range

R. In this experiment, monoenergetic electrons were produced in a cloud

chamber by the photoelectric absorption of monochromadc X-rays. The

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Incident electron

End of path

6 ray or branch

Absorber

Fig, 1.3 _ ^ ^ ^

Tlie thickness of absorber is R + dR.

If the absorber had been of thickness R, the electron would have just

penetrated it and would be said to have a range R. The total path length S is

measured along the actual path of the electron and is always considerably

p-cater than R.

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total path length and the maximum distance reached in the initial

direction were than measured.

Fig. (1.4) presents Williams observations on distribution of path length

S and range R in oxygen for 145 individual electrons whose kinetic

energy was 19.6 Kev. Several fundamental feature of the interaction of

electrons with matter can be visualised from a study of these curves in

this energy domain, radiative losses are negligible and curves represent

the effects of ionisation losses, elastic scattering, and straggling of

energy losses.

The curve S shows the fraction f of the electrons whose path length

exceeds the distance D cm. The slope of the curve ds/dD is the fraction

of electrons whose path lengths lie between D and D+dD. These slope

are sufficiently symmetric about f = 0.5, so that the mean path length S

can be taken as the path length at f = 0.5, when one half the electrons

have been stopped.

The broad distribution of path length is noteworthy and is due to the

statistical distribution of energy losses, or straggling for each electron.

Some have large losses, including one or more "branches" due to hard

collision, and have short path lengths. Other suffers smaller and fewer

losses per millimetre of path and have much longer path lengths. The

theoretical value of (dT/ds)ion relates to the average energy losses, and

thus its integral is S, corresponding to the average path length, or mean

path length.

The average path length of an electron of K.E. T will be

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<n c o i -

oQ ^ A < co

^ Q G A ' - ' c c : «^^ O W) ^ . E c >

4 »

1.0

O.b

0

Distance D, cm of oxygen

Fig. (1.4)

The distribution of path lengths (S) and of range (R) for 19.6 Kev electrons

in O2 at 0° C and 1 - atm pressure:

R = 0.32 cm (mean range)

Ro =0.52 cm (extrapolated range)

S = 0.64 cm (mean free path length)

So = 0.82 cm (extrapolated path length)

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^ = I * = l 7 : ^ "- ^ n

{dTldS)

where dS •

+ \(i^)ion \d^)rad

equation (1) will not be valid as the lower limit of T approach zero (Ti

1.3 Experimental Work

Some experimental work with electrons and positrons had been

reviewed by Katz and penfold ^ in Aluminium. They did experiment

only for electron interaction. Due to lack of positron sources no

attempt was made for positron transmission.

Seliger ^"^ and Gubemator ^ °-' ^ did some work on the transmission of

positron in the energy range of 180 Kev to 960 Kev, and 50 Kev to

160 Kev. Gubemater's experiment concludes that the ranges of

positron in Al are less than those of the electron in the energy region

below 160 Kev. These results are in qualitative agreements with the

similar measurements of Seliger. In 1959, Gubemator and

Flamammerfeld " mearured the ranges of 40 to 160 Kev electrons

and positrons in Cu, Ag and Au. They reported that in Cu the range of

positrons is less than that of electrons of the same energy while in Ag

and Au positron has large ranges than electrons.

Some work of on transmission of electrons and positrons has been

done by Gill ^^ et al. They studied experimentally the penetration of

electrons of energy E ax = 0.25 Mev, 0.77 Mev, 1.53 Mev, and 1.71

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Mev through a large number of materials including some rare earth

materials. Also they experimentally investigated the penetration of

1.88 Mev positrons in various materials including rare earth materials

then they compared the results of electron and positron transmission.

1.4 Theoretical Developments

(a.) C.S.D.A. Ranges

The rate of energy loss of electrons and positrons is always subject

to statistical fluctuations. For the simplified evaluation it is assume

that during slowing down process, the rate of energy loss along the

entire path is always equal to the mean rate of energy loss. This is

called C.S.D.A. ranges, (CSDA means, continuous - slowing - down

- approximation.). The CSDA range is the path length, which a

particle travels in the course of slowing down, in a homogenous

medium. Berger and Seltzer ' ^ calculated these CSDA ranges with

energy loss due to ionisation and excitation ^^^\ and also

bremsstrahlung process ''*l

CSDA ranges are calculated by integrating the reciprocal of total

stopping power: -

T\

1 fdE^' dT + R'-iT,) (1.3)

where Ti is some lower limit of energy below which the calculation can

not be possible

Normally T,= 1 KeV

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For intermediate and high-energy electrons R (Ti) is considered

negligible. And we know:-

UE^"-

p V dx ;,„,„/ p

dE_

\dxy

1 ^dE^ +

coll P

±

(1.4)

where + ve and - ve signs are for positron and electron respectively

and p is the density of materials.

If we compare the CSDA ranges of electron and positron in any material

with the conesponding experimental values, it is observed that CSDA

range are always greater than the measured values.

(b.) Average penetration depth

Rohrlich and Carlson ' ^ calculated average penetration depth, Zj*.

Which is define as the amount of absorber thickness which when placed

in the path of the beam of positrons and electrons, such that particles

lose completely their initial orientation.

Mathematically the average penetration depth is given by the condition

< C o s e )average = l /c (1.5)

where 6 is the angle of multiple scattering.

This is the condition when the particle losses its memory of initial

direction at average energy

Ed = Ydmc' (1.6)

The average penetration depth corresponding to yd" is given by,

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10

2 * = j ^ *(/«,/; dy

where ^M/o'7) = (Co5^>',, = G{r),

And G*(/) = 7 + 1

7^ Y

y-ip

(1.7)

(1.8)

(1.9)

The constants a~ and b* were considered to be approximately of the

same order of magnitude for small and large values of atomic numbers.

Using this expression Rohrlich and Carlson obtained the average

penetration depths of positrons and electrons for energy ranges 0.1 to

2.04 MeV for Aluminium and lead. They found that the valueZj/z;

first increase with energy upto 1.0 MeV and there after decrease with

energy. While in the case of lead, this value of Zljl'^ first increase

with energy upto 1 MeV and then becomes constant. But they did not

explain the reason of this behaviour.

Some other limitations of this method are as follows:

1. The constant a" and b* had been designed forZ^/z; in almunium

and lead only. It is very difficult to give seprate constant for every

element.

2. There is no indication has been given for the percentage error, in

the final result.

3. In the expression for ( CosO ) and Zd^ the rate the energy loss that

is dT/ds is found. They used energy loss due to collision only; the

energy loss due to radiation has been not taken into account. The

estimated contribution due to radiation loss of 2 MeV electron in

the case of lead is about 21% of total energy loss. And for energy

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more than 2 MeV the radiation loss increase and it should be

taken into account.

Actually the average penetration depth given by the equation (1.5) is

not experimental quantity. There is no known evidence, which could

support some kind of relationship between the estimated average

penetration depth and the measured ranges. Tomlin ' ^ have

reinvestigated the problem of electron penetration using lewis theory ' ^

of multiple scattering and reported relatively simple expression for the

first and second moments of the electron distribution in depth.

(c.) Projected ranges

Rohrlich and Carlson ''' considered only the elastic scattering of

electrons and positrons to calculate the value of Z / .

While the CSDA ranges ' ^ were based on purely inelastic

consideration. Both the approaches do not interpret the measured ranges.

When electrons and positron passing through an absorber both elastic

and inelastic interaction are possible.

Both the process have been taken into account for calculating the

projected range Rp* for positrons and electrons, by Batra and Sehgal. ' " 20]

The mean projected range can be define as the mean projection of the

path of these particles on the direction of incident in the absorber. They

considered that the inelastic scattering is statistically independent of

energy loss fluctuations. Near the end of the range multiple scattering is

large due to the small energy. At the large multiple scattering angle the

electrons diffuse randomly this is called straggling. They assumed that

the electrons first undergo a straight motion and their interaction with

matter is only through inelastic process.

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12

When electrons traverse a small thickness x of the absorber the mean

square angle of multiple scattering ( 0 >x~ is required. The total stopping

is needed as input for calculating < 0 >, power — P dx • - '" V ^ Jiolal

A simple empirical relation of total stopping power found by Batra and

Sehgal ' ' ° this expression can easily be integrable.

In order to take into account the random motion of electrons and

positrons by multiple scattering they given a definition of transport

mean free path tr, this transport mean free path can be define as the

average distance a particle traverse before being scattered through an

angle > n/2. L 9 - 1 .

If Tr' is the energy and ( 0 >x~ is the mean square projected angle

corresponding to the instant when the motion of the particle become

random, the projected range is given by:

Ki^)=RL{T)-R!jT^^) • (1.10)

These values of projected ranges ' " ° are comparable with the

experimental values given by Gill et al ^^\ For 6 < Z > 13 materials the

agreement is good. For intermediate and heavy elements the calculations

by Batra and sehgal ' " ° give lower values of range as compared to the

experimental values by Dr. Gill ^^\ For intermediate Z values the

difference is small but goes on increasing with increasing value of Z. At

Z = 82, the theoretical values are off by about 25% for particle energies

of 1 MeV.

The difference in the theoretical and experimental values may be due to

following reasons:

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13

1. Batra and Sehgal ' ' ^ had used Mott's expression ^ ' for elastic

scattering cross section, tliis expression is in the form of a power

series in aZ, where a = 1/137. They used only the first term of

this series and leaved the higher order terms. For small value of Z

the term {aZf and (aZ)^ and so on can be ignored but for high Z

values these term can not be ignored.

2. In these calculations ' "^°\ the range coming from the diffusion

part was not taken into account.

It is found from their reference 20, figs 5-6, that as the incident kinetic

energy of electrons and positrons decreases and also with the increase of

atomic number Z of the absorber, the fraction of energy left with these

particle increases.

If the diffusion part of the ranges is taken into account, the calculated

values of straggling free practical ranges in very good agreement with

experimental values.

Gill et al ^^ have developed a theoretical model for obtaining

transmission curves of different energies electrons and positrons using

the energy loss expression '''" ^ and Mott's scattering ^ ' cross section

for the scattering of these particles. The values of ranges and absorption

coefficients thus obtained have been compared with the experimental

data.

If a comparison is made between the experimental values of Dr. Gill

and the theoretical values of Batra and Sehgal, ' "' ° the values are in

good agreement for low Z- materials except the case of carbon. For the

intermediate Z the difference is about 16% and is about 30% in high Z

materials. If higher order term is taken into account in Mott's

expression, or if the correction factor is used the values of range is

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14

improved by about 6 to 12% in low Z and 10 to 18% in high Z

materials.

If the contribution of diffusion part is also taken into account with

correction factor or higher order term, the difference in experimental

and theoretical values are - 0.01 % to 6% in low Z for low energy and

about 6 to 9.5%) for high Z at low energy. Similarly this difference is

about - 0.50%) to 5.3%) in low Z for the energy 1.53 MeV and it is upto

8.4% in high Z, at 1.53 MeV energy.

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References

1. B. F. Schonland, Proc. Roy Soc. (London) A135, 429-58 (1925).

2. A. Flammersfield, Z. Nature-forsch 2a, 370 (1947).

3. P. J. Elbert, A. F. Lauzon E. M. Lent, Phys. Rev. 183, 422-30

(1969).

4. T. Tabata, R. Ito, S. Okabe and Y. Fujita, J. Appl. Phys. 42, 3361

(1971).

5. Dr. T. S. Gill, Ph.D. Thesis 1988, A. M. U. Aligarh

6. E. J. Williams Proc. Roy. Soc. (London) ABO, 310 (1931).

7. L. Katz and A.S. Penfold, Rev. of Mod. Phys. 24, 28-44 (1952).

8. H. H. Seliger, Phys. Rev. 88, 408 (1952).

9. H. H. Seliger, Phys. Rev. 100, 1029 (1955).

lO.K. Gubemator, Zeit Fur Physik, 152, 183 (1958).

U.K. Gubemator and A. Flammerfeld, Z. Phys. Vol 156, No.2, 179

(1959).

12.M. J. Berger And S. M. Seltzer, Studies in penetration of charged

Particles Through matter. National Research council publication

No. 1133, P. 205-268(1964).

13.F. Rohrilish and B. C. Corlson, Phys, Rev. 93, 38 (1954).

14. W. Heither, the quantum theory of radiation (Oxford Univ. press

London, 1954) third edition, P. 242.

15.S. G. Tomlin, Proc. Phys. Soc. 99, 805 (1966).

16.H. W. Lewis, Phys. Rev. 78, 526 (1950).

17.R. K. Batra and M. L. Sehgal, Nuclear Physics A156, 314- 20

(1970).

18.R. K. Batra, Penetration of electrons and positrons in matter,

Ph.D. thesis (1971).

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19.R. K. Batra and M. L. Sehgal, Phys. Rev. B, 23, No. 9, 4448

(1981).

20.R. K. Batra and M. L. Sehgal, Nucl. Inst. Methods 109, 565

(1973).

21.N. F. Mott. Proc. Roy. Soc. (London) A124, 425, (1929),and

A135, 429 (1932).

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^ Introduction y Ionization andej(citation foss y (BremsstrafiCung y Empirical reCations of totaCstopping power of electron and

positrons y MuCtipCe scattering tfieories > StraggCing

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17

2.1 Introduction

When a beam of electrons or positrons of some kinetic energy interact

on a target foil, they penetrate through the foil by undergoing two major

kinds of interaction: the slowing down process and the elastic scattering.

These processes depend upon the energy of the particle and atomic

number of materials traversed. A moving electron by virtue of its

moving electric field creates disturbances in the electronic structure of

the atoms and molecules of the medium through which it moves. These

disturbances is due to transfer of energy from the moving electron to the

surrounding atoms and molecules, raising them to excited states and

frequently producing ionisation and the rapture of the molecular bonds.

Most of the energy of the incident electrons or positrons is dissipated by

the collisions between the incident electrons and orbital electrons of

material. The energy loss due to collisions between the incident

electrons and the nuclei is negligible small because of the large

difference in their masses.

Fast electrons or positrons also lose energy due to the emission of

electromagnetic radiation in the coulomb fields of nuclei and the orbital

electrons. This is known as Bremsstrahlung loss. This loss is very small

due to the coulomb field of orbital electrons in comparison to that of

nuclear coulomb field.

The total energy loss per unit path length is given by:

\ dE^' ( j_^Y f_i^Y p dx J lolal

+ P'^-'') colli V Pdx)

(2.1) rud.

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2.2 lonisation and excitation loss

Bathe and Bloch ' gave the expression for the average energy loss due

to the coHisions between the incident electrons and atomic electrons,

using Moeller's differential cross section ^^\ But the expression given by

Bathe and Bloch cannot distinguish between the energy loss of electrons

and positrons. Rohrlich and Carlson ^^ had given the formula of average

energy loss due to the collisions between positrons and electrons with

orbital electrons.

The Bathe Bloch formula "' of average energy loss by collision is

obtained for electrons under the assumption that above a certain

fractional energy transfer E, the atomic electrons are treated as free.

Under this assumption, Moller's cross section ^ •' for scattering of free

electrons by free electrons at rest in Bom's approximation is applicable.

For low energy transfers i.e. 0< E < Ei, an explicit summation over the

various excitation probabilities can be carried out. The average energy

loss per unit path length in a medium for electrons and positrons is given

by

^ 1 ^ p dx

\ ±

/colli

Ine'NZ

Am^c^j^'

^ r y + O I' 2

+r{/)-^ (2.2)

where /"(/) = i-/?

and /"( /)-21n2-4

2 2 / - 1

r in 2 + -

8 r J for electrons

12

^^ 14 10 4 23 + + ^ + • cr + 1) ir+if (r+i)'

(2.3)

(2.4)

for positrons

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Where

e = electronic charge

iTioC = rest mass energy of electron

Z = atomic number of the absorber

P = v/c

T = Kineticenergyofelectron in units of its rest mass energy

y = total energy of electron expressed in units of rest mass

energy

I = average ionisation potential

A = atomic weight

p = Density of medium

5 = Density effect con-ection factor

it is clear by this equation that the difference in the average energy loss

of positrons and electrons is due to the function f * (y). Rohrlich and

Carlson ^^^ plotted these functions versus y. They conclude that slow

positrons lose energy at a faster rate than slow electrons and vice-versa

occurs in the case of fast electrons and positrons. At energy of about 350

Kev the rate of energy loss positrons is the same as that of electrons ^^\

2.3 Bremsstrahlung

Besides the energy loss due to excitation and ionization the energy loss

is also possible due to emission of bremsstrahlung. This loss occurs

when the electrons accelerated in coulomb field of nucleus.

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20

Bremsstrahlung is the continuous spectra associated with the deflection

of incident charged particle by the coulomb field of nuclei.

(a) Classical theory of Bremsstrahlung

According to classical theory whenever an incident charged particle is

deflected from its path or has its velocity changed it should emit

electromagnetic radiation whose amplitude is proportional to the

acceleration. The acceleration produced by a nucleus of charge Ze on a

particle of charge ze and mass M, is proportional to Zze / M. (M is the

mass of the incident particle).

We know by coulomb force F oc qi q2 / r

Or M.a oc Ze.ze

Or a oc Zze^/M (2.5)

Thus the intensity, which is proportional to the square of the product of

the amplitude and the charge ze, will very as

Amplitude oc acceleration

Intensity oc (amplitude x ze)

oc Zze

•ze

Or intensity oc (Z^z''e^)/M^ (2.6)

Thus the total bremsstrahlung per atom varies as the square of the

atomic number of the absorbing material. We also see that the total

bremsstrahlung varies inversely with the square of the mass of incident

particle.

Therefore Proton and alpha particle will produce about one millionth of

bremsstrahlung of an electron of same velocity. Because of this strong

mass dependence bremsstrahlung is almost completely negligible for all

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21

swift particles otlier than electrons. The incident particle can radiate any

amount of energy from zero to its kinetic energy 'T'.

Thus the maximum quantum energy (hvmax) at the short wavelength of

the continuous X- rays spectrum is

hVmax = T. This relation is called Duane and Hunt's law. *^

(b) Quantum Mechanical Theory of Bremsstrahlung

The deflection of a swift electron of velocity v = pc, rest mass mo, by a

nucleus of charge Ze fall in the domain of Z/137 p « 1, if Z is not too

large.

In a quantum mechanical treatment we know that the first approximation

of Bom's method calls for neglecting Z/137 p compared with unity.

Born's first approximation is therefore applicable to the problem of

bremsstrahlung, except for initial or final electrons of very low velocity.

Bethe and Heitler and others, using Dirac's relativistic theory of the

electron and the first approximation of Bom, have developed the

quamtum mechanical theory for the bremsstrahlung of relativistic

electrons. The non-relativistic theory has been developed by

Sommerfield. Using exact wave functions.

The total bremsstrahlung energy (in MeV per incident electron of kinefic

energy Eg in MeV) is given by

I = KZ Ee^ for E, > 2.5 MeV, where K ~ 7 x lO"""

In quantum mechanical theory a plane wave representing the electron

enters the nuclear field, is scattered and has a small finite chance of

emitting a photon. The electron is acted on by the electromagnetic field

of the emitted photon as well as by the coulomb field of nucleus. The

intermediate states of the system involve the negadve energy state,

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22

which characterized the Dirac electron theory. The theory of

bremsstrahlung is intimately related to the theory of electron pair

production by energetic photons in the field of a nucleus. Because the

radioactive process involves the coupling of the electron with the

electromagnetic field of the emitted photon the cross sections for

radiation are the order of 1/137 times the cross sections for elastic

scattering.

(c) Comparison with Classical Theory

The classical theory of bremsstrahlung gives incorrectly the emission of

radiation in every collision in which an electron is deflected. Yet for the

averages over-all collisions, the classical and the quantum- mechanical

cross section are of the same order of magnitude,

Z 2 f ^2 \

rad J 3 ^ K'^hc' J

cm^ I nucleus (2.7)

In the quantum mechanical model there is a small but finite probability

that a photon will be emitted each time a particle suffers a deflection

however this probability is so small that usually no photon is emitted. In

the few collisions, which are accompanied by photon emission, a

relatively large amount of energy is radiated. In this way the quantum

theory replaces the multiple of small classical energy losses by a much

smaller number of large energy losses the average being about the same

in the two theories. Of course, the spectral distributions are very

different in the two models. All experimental are in agreement with the

quantum mechanical model.

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23

2.4 Empirical relations of total stopping power of electrons

and positrons

The expression of the total stopping power of electrons and positrons

has been given by Batra and Sehgal ^'^\

For the energy range T < 500 Kev, total stopping power is given by

' 1 dE^'

p dx = {mz^c)r[r) (2.8)

/ iiiiul

.2.4

where ^(Y) = — — for positrons (2.9)

,2.56

and f (y) = —J— for electrons (2.10)

and Y = 1— (2.11)

and for the energy between 0.5 Mev to 5.0 Mev the expression is given

by

^ 1 dEY v' =imz + c)^— (2.12)

The value of constant a , b , m, z, are given in table

Table-1 forT<500Kev

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24

S.No.

1.

2.

3.

Z- values

1 < Z < 1 0

10<Z<38

3 8 < Z < 9 2

—• - 2

m (Mev.cm /gm)

- 0.0300

- 0.00595

- 0.00285

C (Mev.cm /gm)

1.1700

0.9282

0.8100

Table -2 for T lying between 0.5 to 5.0 Mev

S.No.

1.

2.

3.

Z- values

1 < Z < 10

10<Z<36

3 6 < Z < 9 2

m (Mev.cm /gm)

- 0.0330

- 0.0097

- 0.0048

C (Mev.cm^/gm)

1.3230

1.0911

0.9156

= -0.0038 = - 0.0040

= 1.8402 = 1.8160

2.5 Multiple scattering theories

If the thickness of absorbing materials or foil is such that a single

particle can suffer a large number of scattering collisions, then statistical

method become applicable for the estimation of mean deflections. These

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25

phenomena are called multiple scattering. The determination of the

ranges from the electron transmission curve is very difficult due to the

statistical fluctuations of path lengths of the electrons in the material

traversed. So many attempts have been made to develop the theory of

multiple scattering. Several review papers on small angle multiple

scattering of fast charged particle are available in the literature ^ ' l

The single scattering of charged particle by the coulomb field of a

nucleus was first given by Rutherford. The differential cross section of

elastic scattering of a non-relativistic particle of charged ze by a nucleus

of charged Ze within the angle 9 to 0 + d9 is given by:

cT[e)i7T%\\\ed0^—~Y^,—-.inimede (2.13) 16£' sin [OH]

where E is the K.E. of the particle .

Mott ' ^ derived an exact expression for the scattering of fast electrons

by a bare nucleus. He used the second order wave equation for Dirac

electrons thus the spin and the relativistic effects were taken into

account. Mott's formula is valid when Ze /hv « 1.

This formula is in the form of a series in Legendre polynomials and its

expansion in power of aZ is equivalent to the solution in Bom

approximation. Here a = Z/137, fine structure constant. The resulting

expression contains only first order tenn of the series in aZ is given by:

^'^^'^^ = ^ | " S : 1 —JrZiT\ [l->^'sin^^/2 + H^^sin^/2(l-sin^/2)] ( Y 1

_sii/(^/2)_

(2.14)

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26

0 T 9 9

where YO "= eVmoC" and y = (T + nioC )/moC

P= v/c, nio = rest mass of electron.

The upper sign stand for positrons and lower for electrons,

The difference between the cross section of electrons and positrons is

that the sign of the last term is reversed. This is because the last term

proportional to the first power of the interaction potential. It is also clear

from the equation (2.14) positron scattering is always less than the

electron scattering under identical conditions. The last term gives the

difference between positrons and electrons scattering and is very

important for heavy nuclei. For heavy element the power series in aZ

converge too slowly. The theory of multiple scattering of fast electrons

given by Willams ^ "'° is based on the assumption that the small angle

multiple scattering will yield a Gaussian distribution. The projection of

the angular distribution of the scattering on a plane containing the

incident beam was also considered. The effects of the shielding of the

nucleus by its orbital electrons and the finite size of the nucleus on the

scattering probability were also included. The effects of the finite size of

the nucleus and its shielding by orbital electrons were also considered.

In order to derive the expression for scattering cross section ' "" ^ he used

the potential

V{r) = —e'''" (2.15) / •

where a = —^ and ao = radius of the first bohr orbit of the Hydrogen

atom. The expression of the scattering cross section is written as

4 sm' 012 ( l - ^ 1 l + t \

2asm0l2 (2.16)

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27

the scattering for 9 » 9min the shielding thus little affects,

where Qm\n ~ ^/a, and it reduces for 8 « Qm\n •

the scattering through an angle 0 depends on the field at distances from

the nucleus of the order of %/Q, this the consequence of bom

approximation.

If the finite size of nucleus is not considered William ^ " ^ used the

potential:

V{r). (Ze'^

V ^ J

[\-e-'"') (2.17)

where b = nuclear dimensions,

and the scattering cross section is given by,

a\ {0). zV (l-/?^ sin'012

1 + ^bsm0l2^''

-2

(2.18)

It can be seen that the nucleus size correction reduces the scattering,

for 9 > ?C/b, but the shielding reduces it for 9 < ^/a, where a = atomic

dimension.

Thus the correction apply to regions which do not overlap, hence the

general solution of a(9) is given by:

Am'V \s\n 012)1 4a ' \ \ / /

(2.19)

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28

Elton " reported on the effect of the finite size of the nucleus on the

elastic scattering cross section. In 1948, Moliere ' ^ proposed a useful fit

to the Thomson- Fermi function for heavy atoms. Later, Bethe ' ^

proved that multiple scattering of electrons given by Moilere^ ' can be

obtained from the exact theory of Goudsmith and Saundersons. The

problem of scattering through the angles for which sin0 cannot be

replaces by 0 was studied by Goudsmith and saunderson ^^"^K Lawis ' ^

gave an approximate solution of the integro -differential diffusion

equation of the multiple scattering problem in an infinite, homogeneous

medium without using small angle approximation. He also included the

energy loss by considering the energy of a particle as a function of its

residual range, the effect of straggling in energy loss assumed to be

small. On the other side so many workers ^^^'^^^ have obtained the r.m.s.

angle of multiple scattering experimentally by measuring the tracks of

scattered electrons and positrons by cloud chamber technique or nuclear

emulsions. It was reported that the experimental curve between r.m.s.

angle of the normal part of multiple scattering distribution versus energy

agrees well with the theory of Willams^ '' ^ and Molier' ^ l

The systematic calculations of the penetration of electrons and positrons

through matter require the correct and convenient form of multiple

scattering cross sections as input data. The results from experiments ' "

^'K indicate that at energies greater than 1 MeV, for electron there is

some agreement with Moilier's ' ^ theory. Below 1 MeV the

comparison between the Moilier's theory and the various experiments

on multiple scattering shows disagreement with decreasing energy. The

experimental evidence for difference in multiple scattering of electron

and positrons is contradictory.

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29

2.6 Straggling

Identical charged particles all having the same initial velocity do not all

have the same range. It is found that the ranges are distributed over a

small interval about a mean range. This phenomenon is called range

straggling and is due to several effects, Since the No. of collision is

large and are independent to each other, hence the distribution may be

expected roughly to be Gaussian.

We have discussed in last article of multiple scattering that the

effects of multiple scattering preclude exact calculations of the range of

electrons. Such calculations are further complicated by the statistical

fluctuations, or straggling of energy losses. Straggling like scattering is

much more pronounced in the case of electrons than for heavy particles.

This is because heavy particles lose most of their energy in ionizing

collisions with atomic electrons, where conservation of momentum

permits fractional energy transfers of the order of the ratio of the masses

(~ mo /m), therefore each collision results in the transfer of only a small

fraction of the energy of a heavy particle. On the other hand, electron

can lose up to one half of their energy in an ionizing collision. In

addition to this, the electron may also lose any fraction of its energy in a

radiative collision.

Among the most instructive observations on electron absorption

are the classic straggling and absorption measurements, made by white

and Millington ''' ^ with the aid of a beta ray magnetic spectrograph, on

seven conversion electron groups from Ra (B + C), covering an energy

range from 0.155 to 1.33 Mev.

Fig. 2.1 shows the effect on a homogeneous number- energy

distribution of 0.2065 - MeV electrons after passing through thin

mica foils of varying thickness.

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0.18 0.19 0.20 Electron energy, Mev

0.21

Fig. 2.1

Transmission through mica of monoenergelic electrons The position of peaks gives the most probable energ>' loss.

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30

References

1. H. A. Bethe, and buch fur Physik ( Julius Springer, Berline 1933),

Vol 24/2, P. 273.

2. C. Moller, Ann. Physik, 14, 531 (1932).

3. E. Rohrlich and B. C. Carlson, Phys. Rev. 93, 38 (1954).

4. R. K. Batra and M. L. Sehgal, Nucl. Inst. Meth. 109, 565 (1973).

5. R. D. Birkoff, passage of fast electrons Through Matter, Hand

buch Der, Physik Vol. 34,115 (1958).

6. M. I. Berger, Monte carlo Calculation of the penetration and

diffusion of fast charged particles, "methods of computational

physics", Vol. 1, 135 (1963), academic press.

7. T. Scott Willams, Rev. Mod. Phys. Vol. 35/2, 231 (1963).

8. N. F. Mott and H. S. W. Massey, The theory of atomic collisions,

Oxford University presses. London (1949).

9. E. J. Williams, Proc. Roy. Soc. (London) A169, 531 (1957).

lO.E. J. Williams, Phys. Rev. 58, 292 (1940).

1 l.L. R. B. Elton, Proc. Phy. Soc. A63,115 (1950).

12.G. Moliere, Z. Naturforch 24, 133 (1947) and 34, 78 (1948).

13.H. A. Bethe, Phys. Rev, 89, 1256 (1953).

M.S. Goundersmith and J. L. Saunderson, Phys. Rev. 57, 24 (1940)

andPhys. Rev. 58, 36(1940).

15.H. W. Lewis, Phys. Rev. 78, 526 (1950).

16.G. Groetzinger, M. J. Berger and F. L. Ribe, Phys. Rev. 77, 584

(1950).

17.F. F. Heymann and, W. F. Williams, Phil. Mag. 1, 212 (1956).

18.W. Duane and F. L. Hunt, Phy, Rev. 6, 166 (1915).

19.P. White and G. Millington, Proc. Roy. Soc. (London) A 120, 701

(1928).

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^ Introduction ^ Hie present methods of caCcuCation y Tfie present methods for calcuCating ranges andaSsorption coefficient

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31

3.1 Introduction With the help of theoretical developments, ^ '" which has already been

discussed in chapter 1, it is not possible to get any useful information

about the absorption coefficients, ranges, etc of electrons and positrons.

Because it is very difficult to make transmission curves of these

particles by these theories. '"

If the initial energies of electrons and positrons are same no difference

can be found out in the characteristics of transmission with the help of

these theories, because by these theories no transmission curve can be

constructed. ^ ""

The transmission curves for electron and positron to get information

about the ranges and absorption coefficient have been made

theoretically by Dr, Gill ^^^ in large number of materials for Z numbers

between 6 to 82, including some rare earth materials like Neodymium,

Yttrium, Ytterbium, and Holmium.

It is of great interest to study the penetration of electrons and positrons^

through rare earth materials, since no information is available for the

electron positron penetration through these materials. The properties of

these materials have been a subject of many latest investigations. ^^'^'^^\

The theoretical approach given by Dr. Gill ^^ was the first such attempt

to reproduced transmission curves of positrons and electrons almost in

the same way as the experimental transmission curves. In this method

the absorber was considered to consist of a large number of extremely

thin slices and Mott's "'^ quantum mechanical expression for the

scattering cross section had been used for computing the scattered flux

at each individual slice of absorber. Inelastic scattering and nuclear

screening had also been taken into account.

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32

The calculation done by Dr. Gill ^^ has the agreement with experimental

values of ranges and absorption coefficients, when they used single

scattering formula ''' ^ multiplied by an empirically determined

correction factor. The energy and Z- dependence of that correction

factor is also calculated.

3.2 The present methods of calculation

The absorber has been considered to consist of a large numbers of thin

slices. The electrons and positrons of same energy were allowed to fall

perpendicularly on the plane of the absorbers. Both elastics and inelastic

scattering of electrons and positrons occur in each slice. It is also

considered that the numbers of particles, which get scattered through an

angle > 90° are supposed to be removed from incident beam.

For the energies between 0.5 to 5.0 MeV the following expression is

used to find out the energy dissipation in each slice.

UdE^

P dx \UX J luial / ^

Where upper + ve sign is for positrons and lower - ve sign is for

electrons

Y is the total energy of electrons and positrons in the unit of rest mass of

electron.

a~ and b~ are the constants and their values are given by

a = -0.0038, b^ = 1.8402 ,

a" = -0.0040, b" = 1.8160

the values of constants m and c for different Z are shown in table.

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33

Atomic Nos.

1 < Z < 1 0

11 < Z < 3 6

3 7 < Z < 9 2

m (Mev-cm^-g"')

- 0.0330

- 0.0097

- 0.0048

c (Mev-cm^-g"')

1.3230

1.0911

0.9156

for the energies less than 0.5 Mev following expression is used

P {mz\c)F^{y)

total

(3.2)

where F" (y)

and F"(Y)

r 2.4

/"-I

7 2.56

f-\

for positrons

for electrons

(3.3)

(3.4)

Since the particles loose their energy in each slice, so that it is clear that

the incident energy on the next slice is less than the energy lost in

previous slice. So we can say as the number of slices increase, the

percentage transmission goes on falling.

The following Mott's scattering formula was used by Dr. Gill et al. ^^^

{ 2 \ 2

d(/ --NTZ^Z^-X) V^c J

Z+lYl-/ • -4

sm (^^

^2J - sin(<^/2)cos^/2)

[1 - / sin'(5^/2) ± a/ll-sm6>/2)sm6^/2]d0 (3.5)

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34

Where -ve sign stands for electrons and +ve sign for positrons

N

Z

e =

a =

P Where y is

7

number of atoms/cm

atomic numtjer of absorber

charge on electron

Z/137

(y'-i)/y'

given in term of the incident kinetic energy T by 9 9

(T + moC ) / nioC

Where moc^ is the rest mass energy of the electron

In the above expression the term Z (Z+1) replaces ^^ the term Z in the

original Mott's ""'^ formula, and is a satisfactory approximation to

account for screening of the nucleus by the orbital electrons. Also for

the inelastic deflection ^^ another term (Z+1) / Z is used. But for the

present calculations we used the Mott's scattering formula "'^ up to fifth

order of aZ, the final expression is given below:

da =N72.{Z+X)- • ^ —^' yin^c^ J

sin- l - |sin(<9/2)cos^/2)

[\-/fsm\0l2)±7raJl\-sm0l2)sm0l2+(/R^+(//^R^Mc^ I /^R

{a' I0')R, +a'R,+a'^R\^a' I/f)R, + ( ^ lj3)R,+(^/^\ ]d0

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35

Where symbols has their usual meanings, and 'R' are the complicated

expression and involve gamma function of complex nature. In the

present calculations all the higher order terms in the Mott's scattering

expression are used, that is the expression given by R. M. Curr ^^ up to

fifth power of aZ, has been used for calculating the transmission of

electrons and positrons.

The values of R's for the angle 90° has been used, the values are given

below,

Ri

0.650

R:

1.477

^ 2

0.259

R3

0.744

K

0.789

R4

0.955

^ 4

2.658

K

0.151

Rs

0.891

R's

0.958

K

l . l f

For the present calculations the values of R's has been used for the angle

9 = n/2, because for computing the transmission of electrons and

positrons through a slice, the numbers of particles scattered through an

angle > 90° have been considered to be removed from the incident beam

for the successive slice. In the calculation done by Dr. Gill ^^ the

scattering formula '"'" ^ multiplied by an empirically determined

correction factor was used, but no correction factor is used for the

present calculations.

To calculate the transmission by the final expression (equation 3.6) it is

considered that all the incident particles scattered through an angle > 90°

have been removed or absorbed from the incident beam while traversing

an individual slice of the absorber. The choice of thickness of slices is

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36

arbitrary and it is taken to be extremely small. The thickness of each

slice is taken to be 22 x 10' x p gm/cm^ and 11 x 10" x p gm / cm^

where p is the density of the material. The fraction of incident particles

removed from the beam or the removed flux is given by:

]dJ]da (3.7) !rll I 0

In the Mott's expression (equation 3.6) the term p = (y - 1)/ Y goes on

changing at each subsequent slice. For the first slice the total incident

energy of the incident particles is measured by y = (T + moC^) / moC^,

where T is the incident kinetic energy and moC" is the rest mass energy

of electron or positron. The beam looses its energy in each slice, the

energy loss of the particles in each slice is computed by using the

formula "'^ for stopping power (equations. 3.1, 3.2) for different Z

values and energy ranges. For every slice the incident energy will be

equal to the incident energy of previous slice less the energy lost in it.

3.3 Present methods for calculating Ranges and Absorption

coefficients

When positrons and electrons pass through the matter elastic and

inelastic collision with the atoms of absorber take place. Due to the

multiple scattering the path of the incident particles gets distorted and

the kinetic energy of incident particle goes on decreasing the distortion

process become more rapid. At the low energy the multiple scattering is

enhanced. After a level at low energy the motion of these particles

become random. This random motion is the diffusion of these particles.

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37

The lower energy below, which the diffusion starts, depends upon the

kinetic energy of incident particle and the nature of the absorber.

The incident positrons and electrons can travel an average distance even

after the diffusion process starts. This average distance is a substantial

fraction of the practical range in the absorber. By using this fact the

straggling free practical ranges of electrons and positrons can be

calculated. Both parts that is before and after diffusion process must be

taken into account.

In the theory of electron penetration, by Bethe ' ^ et al the diffusion of

electrons is taken into account. The assumption of this theory '"' make

the present approach of calculations of the straggling free practical

ranges simpler, and bring close to experimental values.

In the beginning of the journey in absorbing material electrons and

positrons travel along a straight path due to very little multiple

scattering. As the energy goes on decreasing the multiple scattering

starts and when the motion of these particles become random the

diffusion sets in. For the calculation of critical energy Tr~, at which the

diffusion process starts the multiple scattering during their slowing

down in target material is taken into account. However, both multiple

scattering and slowing down cannot be easily treated simultaneously. So

this situation can be simplified by assuming a direct transition from a

straight motion into diffusion. On the basis of transport mean free path

Bethe ' ^ studied this transition

That is

< C o s 0 ) average = l / e ( 3 . 8 )

Where, 0 is the angle between the direction of motion of the particle in

absorber and direction of initial beam.

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38

By knowing ( Cos 0 ) average, the desired range can be calculated. Batra

and Sehgal ^^'^^ calculated the critical kinetic energy Tr~ for electrons and

positrons and plotted against incident kinetic energy T for different

materials. If the critical kinetic energy Tr" for any particular initial

kinetic energy and absorber is calculated, the parts of range before and

after diffusion process starts can also be calculated. The straight path

covered by electrons and positrons or the projected range ^ ' ^ is given in

continuous slowing down approximation as

Rp-(T) = R'cSDA (T) - R'cSDA(Tr-) (3.9)

Where R"CSDA (T) = CSDA range of positrons and electrons for kinetic

energy T,

And R CSDA (Tr) - CSDA ranges of electron and positron at kinetic

energy Tr" (or at critical energy)

And can be obtained by using Berger and Saltzer ^^ table.

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39

References

1. E. J. Williams, phy. Rev. 58, 292 (1940).

2. L. V. Spencer, phys. Rev. 98, 1597 (1955).

3. Dr. T. S. Gill, PhD thesis, A. M. U. Aligarh (1988).

4. N. F. Mott, Proc Roy Soc. (London) A124, 425 (1929) and A135, 429

(1932).

5. N. F. Mott and H. S. W. Massey, The theory of atomic collision

Oxford University press, London (1949).

6. R. K. Batra & M. L. Sehgal, Nuclear Physics A156, 314-320, (1970).

7. R. K. Batra & M. L. Sehgal, Nucl. Inst. Methods (109), 565 (1973)

8. R. K. Batra & M. L. Sehgal, Phys. Rev. B23, No.9, 4448 (1981).

9. M. J. Berger and S. M. Seltzer, NAS - NRC, Publ. No. 1133 (1964)

and NASA SP-3012 (1964).

10. F. Rohrlich and B. C. Carlson, Phys. Rev. 93, 38(1954).

11. P.S. Takhar and M. L. Sehgal, Nuovo Cimento (Italy) 47B, 31

(1978).

12. R. M. Curr, Proc Roy Soc. A68, 156 (1955).

13. H. A. Bethe, M. E. Rose, Proc Am. Phil. Soc. 78, 573 (1938).

14. F. H. Spedding and A. H. Danne, the rare earths (John Wiley and

sons, Inc.) New York (1961).

15. K. A. Gschneider, Jr. Rare Earths, the Fraternal fifteen, published by

united states Atomic energy commission, Division of technical

information (1966).

Page 55: POSITRON AND ELECTRON INTERACTION · electron scattering from atoms can carry out calculation. There are several important differences between electron and positron scattering. However

y IntrocCuction y Jl6soTption coefficients y Comparison of present tfieoreticaCamf^ExperimentaC (Ranges y transmission curves plbtteif 6y present theory y Curves for JiBsorption coefficients y Curves for ^n^es

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40

4.1 Introduction

In this chapter the transmission curves are build to view the

percentage of transmitted beam intensity theoretically as a flmction of

the thickness of the absorber, through which the incident beam is

passing. Tlie transmission curves for rare earth materials and a large

number of absorber is plotted. The shape of these curves is the same as

that of experimental curves. Some curves are shown from figs. 4.1 to

4.12. By using these curves the values of Rsfp and the absorption

coefficients are determined. The shape of these curves for other

absorber is the same.

Figs. 4.13 to 4.16 shows that how we have measured the values of Rsfp

the extrapolation on the curves for measurement of Rs^ is shown.

4.2 Absorption coefficients

For measuring the absorption coefficients we have measured the slope

of curves between 33% to 67% of transmission. These absorption

coefficients are plotted against the Z number of the absorber. Figs 4.17

to 4.20 shows the comparison of absorption coefficients obtained from

present theoretical approach with experimental values of Dr. Gill. '^

The con^arison of the absorption coefficient of positrons and

electrons at the equal energy Emax is the right way of comparison, this

type of comparison is shown in fig. 4.21.

Rohrlich and Carlson * studied the differences in positrons and

electrons scattering. They determined the energy loss and multiple

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4)

scattering of positrons and electrons in AJuminum and Lead. The

energy loss of positrons is greater than that of electrons at very low

energy and for low Z region, the multiple scattering of electrons is

slightly greater than that of positrons. Hence the transmission of

electrons is to be higher than that of positrons at very low energy and

for low Z region. Fig 4,20 shows dependence of absorption coefficient

for positrons and electrons at energy 1.88 MeV. It shows that as Z

increases the absorption also increases. It is clear from these figs. That

there is a difference between the transmission behavior of positrons

and electrons of the same initial kinetic energy.

4.3 Comparison of present theoretical and experimental

Ranges

In the figs 4.22 to 4.24, the values of ranges obtained by present

theoretical approach with experimental values of Dr. Gill '^ are

shown. It is clear from these figures. There is a very small difference

between the present theoretical curves and experimental curves. Or we

can say the values obtained by present theoretical approach are very

close to the experimental values.

The good agreement is because in the present calculation we used the

Mott's scattering expression ^^ including with higher order terms. The

total expression up to fifth order term in ocZ has already given in

chapter 3 (equation 3.6).

This expression is given by R. M Curr ^^ and can be written in the

following simplest form.

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42

<y{e,r) = z' e \2m^c'^ 2 o2

1 - / 3 2 ^

ysin'e 2

1 - ^ ^ i n ^ ^ / + a /3 /? ,+a^ /?^+a^^^ /? ,+^ + a^ /?3 +

Where a = Z/137, p = v/c, G = angle of scattering,

for electrons and positrons only the appropriate sign is to be changed.

'R' is the complicated expression and involves gamma fiinction of

complex nature, which has already discussed in third chapter.

ITie values of theoretically calculated ranges by Batra and Sehgal ^ ' ^

and experimental values '"^ agree for lower Z materials with the

exception of carbon. This difference is of the order of 16% in

intermediate Z values and is the order of 30% in high Z region.

But the difference between the experimental ranges and the ranges

obtained by present theoretical approach after including the higher

order terms in Mott ^^ and Massay ' ^ expression is improved by about

6 to 12% in intermediate Z region and 10 to 18 % in the high Z region.

If the contribution due to diffusion part is also taken into account the

difference in experimental and theoretical values becomes only 0.01 %

to 6 % in low and intermediate Z region at energy 0.77 MeV and only

6 to 9% for high Z region. Similarly at energy 1.53 Mev this

difference becomes only 0.5% to 5.3% in low and intermediate Z and

up to 8.4% in high Z materials. This difference is shown in figs 4.25 to

4.27.

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43

At low energies and for high Z materials the difference between

experimental and present theoretical values is larger than the

difference at high energy and low Z materials.

This difference in experimental values and the values given by present

theoretical approach may be due to the errors in the total stopping

power expression ' " l These expressions are used as input data for the

present calculation. There can be an error of about 4 % in the input

data for stopping power. Also the experimental data has some errors.

Hence the net effects of these errors produce the difference in

experimental and present theoretical values.

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References ""

1. R. K. Batra & M. L. Sehgal, Nuclear Physic

(1970).

2. R. K. Batra & M. L. Sehgal, Nucl. Inst. Methods (109), 565

(1973)

3. R. K. Batra & M. L. Sehgal, Phys. Rev. B23, No.9, 4448

(1981).

4. Dr. T. S. Gill, PhD thesis, A. M. U. Aligarh (1988).

5. N. F. Mott, Proc Roy Soc. (London) A124, 425 (1929) and

A135,429 (1932).

6. N. F. Mott and H. S. W. Massey, The theory of atomic collision

Oxford University press, London (1949).

7. R. M. Curr, Proc Roy Soc. A68, 156 (1955).

8. F. Rohrlich and B. C. Carlson,Phys. Rev. 93, 38(1954).

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Transmission curves for different materials at different energies plotted by present theoretical

approach

Page 62: POSITRON AND ELECTRON INTERACTION · electron scattering from atoms can carry out calculation. There are several important differences between electron and positron scattering. However

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Curves for Absorption coefficients

Page 79: POSITRON AND ELECTRON INTERACTION · electron scattering from atoms can carry out calculation. There are several important differences between electron and positron scattering. However

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Page 83: POSITRON AND ELECTRON INTERACTION · electron scattering from atoms can carry out calculation. There are several important differences between electron and positron scattering. However

Curves, which shows Comparison of present theoretical and

experimental values of ranges

Page 84: POSITRON AND ELECTRON INTERACTION · electron scattering from atoms can carry out calculation. There are several important differences between electron and positron scattering. However

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