17
. The use of nuclear methods RBS, ERD / RBS and RBS / NR to determine the depth profile of atoms in the subsurface layers of the solid state Agata Barańska University of Adam Mickiewicz, Poznań, Poland Dagmara Bentryn Nicolaus Copernicus University , Toruń, Poland Dimitar Stoychev University of Plovdiv Paisii Hillndarski ”, Bulgaria Frank Laboratory of Neutron Physics Supervisor: Mirosław Kulik UMCS Lublin Poland

The use of nuclear methods RBS, ERD / RBS and RBS / NR to ...newuc.jinr.ru/img_sections/file/Practice2014/EU... · The use of nuclear methods RBS, ERD / RBS and RBS / NR to determine

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Page 1: The use of nuclear methods RBS, ERD / RBS and RBS / NR to ...newuc.jinr.ru/img_sections/file/Practice2014/EU... · The use of nuclear methods RBS, ERD / RBS and RBS / NR to determine

. The use of nuclear methods RBS, ERD / RBS and RBS / NR to determine the

depth profile of atoms in the subsurface layers of the solid state

Agata Barańska University of Adam Mickiewicz, Poznań, Poland Dagmara Bentryn Nicolaus Copernicus University, Toruń, Poland Dimitar Stoychev University of Plovdiv „Paisii Hillndarski”, Bulgaria

Frank Laboratory of Neutron Physics Supervisor: Mirosław Kulik UMCS Lublin Poland

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Table of contents

1. Physical basics of nuclear methods 2. Experiment and method of the study 2. RBS-Rutherford Backscattering 3. ERD-Elastic Recoil Detection 4. NR-Nuclear Reaction 5. Conclusion

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Physical basics of nuclear methods

Hans Geiger

Ernest Rutherford

Series of experiments (Geiger-Marsden)conducted between 1908 and 1913 led to the discovery of nucleus.

Ernest Marsden

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Experiment and experimental apparatus EG5 – van der Graaf accelerator

Ion source

Dome- collects an electrostatic charge

Experimental apparatus(scheme)

1. Ion beam 2. Magnetic lenses and screen forming ion beam 3. Holder 4. Sample 5. Screen 6. Detector 7. Multichannel analizator 8. Computer

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RBS • Elastic collision between particle with the eneregy

Eo and stationary nucleus, • mirror surface • constant atomic density in layer • Rapid change of the density between two

neigbouring layers (assumption)

Scheme of elastic collision

Simple model of scattering process

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kEE 01

2

21

2

1

2

1

2

211 sincos

MMM MM

k

222

2

22

2

11

2

01 VMVMVM)cos()cos( 22111 VMVMVM o

0)sin()sin( 2211 VMVM

Energy of scattered projectile

Conservation of kineti energy Conservation of momenetum

Kinematical factor

Yield

Y = σ(Ө, E) D Nt dΩ

D- total numer of incydent ions Nt – concentration of atoms in the layer σ(Ө, E)- cross-section dΩ- solid angle

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0

2

4

6

ele

me

nts

Depth [1*1015

Atoms/cm2]

C

O

Al

In

Graph1. The profile depth.

1000 1500 2000 25000

1000

2000

In

Al

ex

pe

rim

en

t [c

ou

nts

]

sim

ula

ted

[c

ou

nts

]

energy [keV]

simulated

experimental

=60

1000 1500 2000

0

2000

ex

perim

en

tal

[co

un

ts]

In

sim

ula

ted

[co

un

ts]

energy [keV]

simulated

experimental

Al =30

0 2 4 6 8 10

Eα= 2028 keV ϴ=170o

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500 1000 15000

1000

2000

3000

ex

pe

rim

en

tal

[co

un

ts]

sim

ula

ted

[c

ou

nts

]

energy [keV]

simulated

experimental

Sisurface

Sisubstrate

Nsurface

30

500 1000 1500 20000

500

1000

1500

2000

ex

pe

rim

en

tal

[co

un

ts]

simulated

experimental

sim

ula

ted

[c

ou

nts

]

energy [keV]

Sisurface

Sisubstrate

Nsurface

500 1000 1500 2000 25000

250

500

750

1000

1250

energy [keV]e

xp

eri

me

nta

l [c

ou

nts

]

sim

ula

ted

[c

ou

nts

]

Sn

Al

simulated

experimental

500 1000 1500 2000 25000

500

1000

1500

2000

2500

3000

Sn

Al

ex

pe

rim

en

tal

[co

un

ts]

sim

ula

ted

[c

ou

nts

]

energy [keV]

simulated

experimental

Spectrum: Agata Barańska

Spectrum: Dimitar Stoychev

Eα= 2028 keV ϴ=170o

Eα= 2028 keV ϴ=170o

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ERD

2

21

2

1

2

1

2

211 sincos

MMM MM

k

Simple model of scattering process

sample

Detector RBS

Detector ERD

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1000 2000 3000

0

5000

10000

15000

2000 2100 2200 2300 2400 2500

0

20

40

60

80

100

120

140

expe

rimen

tal [

coun

ts]

energy [keV]

Bie

xp

eri

me

nta

l [c

ou

nts

]

energy [keV]

experimental

simulated

400 600 800

0

20

40

60

simulated

experimental

yie

ld [

co

un

ts]

Energy [keV]

H

Energy= 2297[keV]

=30o

0 1000 2000 3000 4000 5000

0,0

0,1

0,2

0,3

Co

ncen

tarti

on

[%

]

Thickness 1x1015

[atoms/cm2]

Bi

sample St922

EHe

+=2297 keV

0 1000 2000 3000 4000

0

5

10

15

Co

ncen

tarti

on

[%

]

Thickness 1x1015

[atoms/cm2]

H

sample St922

EHe

+=2297 keV

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600 8000

15000

30000

Yie

ld [

co

un

ts]

Energy [keV]

simulated

experimentalsample 223

The depth distribution of elements in the MOS structure

0 2000 40000

2

4

6

8

Co

ncen

tra

tio

n [

%]

Thickness [1x1015

[atoms/cm2]

H

sample 223

0 2000 4000 6000

0

2

4

6

Co

ncen

tra

tio

n [

%]

Thickness [1x1015

[atoms/cm2]

N

sample 223

0 2000 4000 6000

0

10

20

30

40

50

60

Co

ncen

tra

tio

n [

%]

Thickness [1x1015

[atoms/cm2]

O

sample 223

0 2000 4000 6000

0

10

20

30

40

50

60

Co

ncen

tra

tio

n [

%]

Thickness [1x1015

[atoms/cm2]

Al

sample 223

0 2000 4000 6000

0

20

40

60

80

100

Co

ncen

tra

tio

n [

%]

Thickness [1x1015

[atoms/cm2]

Si

sample 223

Spectrum: Dagmara Bentryn

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0 2000 40000

5

10

co

nc

en

rati

on

[%

]

Thickness [atoms 1x1015

/cm2]

B

500 1000 15000

2000

4000

6000

OSiO

2

SiSiO

2

Ex

pe

rim

en

tal

Yie

ld [

co

un

ts]

Energy [keV]

experimental

simulated

SiSiO

2

EHe

+=2297 keV

=135o

=75o

400 450 500 550 600 650 700 7500

100

200

300

400

500

yie

ld [

co

un

ts]

Energy [keV]

Hydrogen

Spectrum: Agata Barańska

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RBS/NR .

21

2

2

1

2

21

2

2

1

2

2

2

21

sin1

sin1cos

)(sin2

MM

MM

E

eZZ

d

d

Yield depends on: • number of incident particles • atomic density of elements in the target • cross-section • solid angle

Simple model of scattering process

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0 100 200 300 400 500

0

20

40

60

Co

ncen

tra

tio

n [

%]

Thickness [1x1015

[atoms/cm2]

O

Fe

Co

Ag

sample St404

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1000 1500

0

1000

2000

3000sim

ula

ted

energy (keV)

Sisurface

Sisubstrate

Osurface

E=3030keV

30o

170o

Spectra: Dagmara Bentryn

Spectrum: Agata Barańska

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Conclusions Application of the classical description

The ability to identify impurities and their

distributions

Layer thickness

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Thank you for your attention