Top Banner
Quasimosaic crystals Yu.M.Ivanov
48

Quasimosaic crystals

Jan 05, 2016

Download

Documents

sahara

Quasimosaic crystals. Yu.M.Ivanov. Elastic quasimosaic (Sumbaev) effect. Studied by Sumbaev in 1957 Resulted in broadening of gamma-ray diffraction peaks from bent quartz plates - PowerPoint PPT Presentation
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: Quasimosaic crystals

Quasimosaic crystals

Yu.M.Ivanov

Page 2: Quasimosaic crystals

Elastic quasimosaic (Sumbaev) effect

• Studied by Sumbaev in 1957

• Resulted in broadening of gamma-ray diffraction peaks from bent quartz plates

• Caused by bending of the reflecting atomic planes (initially flat and normal to large faces of plate) due to crystal anisotropy

• Depends on choice of

crystallographic plane and orientation angle of plate cutting relative to a normal to the chosen crystallographic plane

Figure from article: O.I.Sumbaev, Reflection of gamma-rays from bent quartz plates, Sov. JETP 32(1957)1276

Page 3: Quasimosaic crystals

Quasimosaic effect in silicon

• Calculations of deformed crystal plate done by V.M.Samsonov (Preprint No. 278, LIYaF AN SSSR, 1976).

– Resulted in predictions of elastic quasimosaic effect for some other quartz and silicon plate orientations

– Large elastic quasimosaicity for (011) plane of silicon predicted

• Zero result in the first experiments in 1999

• New calculations using Samsonov approach and new measurements:

- (111) plane, not (011) - published in JETP Letters 81, 99, 2005

Figure from article: V.M.Samsonov and E.G.Lapin, On some possibilities and pequliarities of a curved crystal use in crystal diffraction instruments, Preprint No. 587, LIYaF AN SSSR, 1980

Page 4: Quasimosaic crystals

Elastic quasimosaic in dependence on cut angle for Si

(111) plane

T – thickness of plate

k9 – deformation coefficient

= 2k9 T , where

Plate bending radius R = 1 m

( formula taken from V.M.Samsonov, E.G.Lapin, Preprint No. 587, LIYaF AN SSSR, 1980 )

Page 5: Quasimosaic crystals

Silicon cuts

Cut without quasimosaic

Cut with quasimosaic

Oriented ingot

φ

Page 6: Quasimosaic crystals

Rocking curves for Si plate with quasimosaic

before and after bending.

Quasimosaic effect in Si with X-rays

Rocking curves for Si plate without

quasimosaic before and after bending.

Page 7: Quasimosaic crystals

Shape of bent Si plate with elastic quasimosaic

Page 8: Quasimosaic crystals

Bending device

Page 9: Quasimosaic crystals

First quasimosaic silicon crystal prepared in 2002 for channeling experiment with 70 GeV protons

Page 10: Quasimosaic crystals

Layout of experiment at IHEP in April, 2002

Crystal 1Magnets

Crystal 2

Emulsion 1

S1

S2 S3

Background

Channeled_1

30 m

35 m 4.6 m

Collimator

1.3 m

Emulsion 2

Channeled_2

70 GeVp-beam

5 m

R=3 m

Page 11: Quasimosaic crystals

Profile of 70 GeV proton beam passed through the crystal measured with emulsion: superposition of channeling and volume reflection effects

Page 12: Quasimosaic crystals

Explanation of the observed picture on emulsions

Proton trajectories crossing the crystal and emulsions in horizontal plane (top view)

Page 13: Quasimosaic crystals

Samples 0.3 mm and 2.7 mm with ~0.4 mrad bending angle

Page 14: Quasimosaic crystals

Sample 10 mm with ~100 μrad bending angle

Page 15: Quasimosaic crystals

Crystals for experiment on extraction of high entensive proton

beam at IHEP

Plane (111)

Length along beam 2.65 mm

Bending angle 400 μrad

Page 16: Quasimosaic crystals

Crystal station at IHEP ring

Page 17: Quasimosaic crystals

Crystal mounted on station

Page 18: Quasimosaic crystals

Result

Beam in the U-70 ring 5.5∙1012 p

Intensity of extracted beam 4.0∙1012 p

Efficiency 70%

Page 19: Quasimosaic crystals

Experiment on observation of volume reflection effect with 1 GeV protons

at PNPI, Gatchina

Beam divergence ~ 160 μrad

Beam size ~ 0.8 mm

Critical angle for channeling ~ 170 μrad

Crystal length along beam ~ 30 μm

Bend angle of (111) planes ~ 380 μrad

Page 20: Quasimosaic crystals

One of unsuccessful attempts to bend a 30 μm crystal on 20 mm

radius

Page 21: Quasimosaic crystals

Bent crystals in bending devices

Page 22: Quasimosaic crystals

Check of crystal shape with laser

~1

m

Page 23: Quasimosaic crystals

Measurement of bending angle with X-rays

Page 24: Quasimosaic crystals

Collimator

Crystal mounted on goniometer

Page 25: Quasimosaic crystals

Horizontal profiles of the p-beam vs. crystal angle measured with

PPC

p-beam

reflection

channeling

p-beamCry

sta

l an

gle

, ste

p 6

2.5

μra

d

Channel number, step 200m

Page 26: Quasimosaic crystals

Channeling experiment with 400 GeV protons

H8 beam line

FAR_DETECTOR areaCRYSTAL area

Page 27: Quasimosaic crystals

QM2

Page 28: Quasimosaic crystals

QM2

2 4 6 8 10 120

50

100

150

200

250

300

350

400

Position, mm

Cry

stal

ang

le, m

krad

Crystal QM2

Page 29: Quasimosaic crystals

QM2

Channeling angle (68.2 0.4) μrad

Volume reflection deflection (12.7 0.6) μrad

Volume capture ε (1.8 0.7) %

Page 30: Quasimosaic crystals

QM1

Page 31: Quasimosaic crystals

QM1

2 4 6 8 10 120

20

40

60

80

100

120

140

160

180

200

Position, mm

Cry

stal

ang

le, m

krad

Crystal QM1

Page 32: Quasimosaic crystals

QM1

Channeling angle (77.0 0.4) μrad

Volume reflection deflection (11.6 0.8) μrad

Volume capture ε (2.6 0.8) %

Page 33: Quasimosaic crystals

QM2+QM1

Page 34: Quasimosaic crystals

QM2+QM1

2 4 6 8 10 120

50

100

150

Position, mm

Cry

stal

ang

le, m

krad

Crystal QM1-QM2

Page 35: Quasimosaic crystals

QM2+QM1

Channeling angle

Volume reflection deflection (23.4 0.7) μrad

Volume capture ε (5 1) %

Page 36: Quasimosaic crystals

QM3

Page 37: Quasimosaic crystals

QM3

2 4 6 8 10 120

20

40

60

80

100

120

140

160

180

Position, mm

Cry

stal

ang

le, m

krad

Crystal QM3

Page 38: Quasimosaic crystals

QM3

Channeling angle (72.7 0.8) μrad

Volume reflection deflection (11.9 0.7) μrad

Volume capture ε (5 1) %

Page 39: Quasimosaic crystals

QM4

Page 40: Quasimosaic crystals

QM4

2 4 6 8 10 120

20

40

60

80

100

120

140

160

180

Position, mm

Cry

stal

ang

le, m

krad

Crystal QM4

Page 41: Quasimosaic crystals

QM4

Channeling angle (120.0 0.4) μrad

Volume reflection deflection (12.7 0.5) μrad

Volume capture ε (4.4 0.7) %

Page 42: Quasimosaic crystals

Design: sequence of quasimosaic crystals cut from a

single initial plate

p

1 Si plate 0.3 x 30 x 60 mm3

12 Si plates 0.3 x 8 x 14 mm3

Page 43: Quasimosaic crystals

Check of plate wedging with optical goniometer

Page 44: Quasimosaic crystals

Prototype assembly from 5 plates

Page 45: Quasimosaic crystals

0

1000

2000

3000

4000

5000

6000

7000

14,85 14,90 14,95 15,00 15,05 15,10 15,15 15,20 15,25

Check with narrow X-ray beam

ΔN

Δθ≈0.017x ΔN μrad

Δθ < 40 μrad

X, mm

N,

coun

ts

ΔX

N1

N2

Δθ

ΔN=N2-N1

ΔX

Page 46: Quasimosaic crystals

Need to provide or to compensate plate wedging

Page 47: Quasimosaic crystals

Realization with evaporation technique

Al-layer of 0.14 μm thickness

Δθ = 0.14 μm / 12 mm = 12 μrad

Page 48: Quasimosaic crystals

Further steps

• to improve prototype assemly for experimental run in May’07 at CERN

• to prepare larger plates and assemble them for experiments at CERN and IHEP in the Fall’07