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Version 3 186 Part 4 High-Resolution Transmission Electron Microscopy
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High-Resolution Transmission Electron Microscopyfe-b.emse.cwru.edu/~fernst/EMSE-512-S15/Pages/...Version 3 187 Significance • high-resolution transmission electron microscopy (HRTEM):

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Page 1: High-Resolution Transmission Electron Microscopyfe-b.emse.cwru.edu/~fernst/EMSE-512-S15/Pages/...Version 3 187 Significance • high-resolution transmission electron microscopy (HRTEM):

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Part 4

High-Resolution

Transmission

Electron Microscopy

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Significance

• high-resolution transmission electron microscopy (HRTEM):

resolve object details smaller than 1nm (10−9 m)

• image the interior of the specimen

– compare, e. g., scanning tunneling microscopy: atomic resolution, however only at the surface

• local

– compare, e. g., X-ray diffraction: averaging, “statistical” information

• direct imaging

– HRTEM images can be »intuitively« interpretable (however, severe restrictions apply – see below)

• direct imaging of atom arrangements (in projection)

– crystals (and quasi-crystals )

– in particular: structural defects · interfaces (grain boundaries, interphase interfaces) · stacking faults, anti-phase boundaries, inversion domain boundaries, … · crystals dislocations, disclinations, misfit dislocations, …

– however: projection ⇒ no (individual) point defects ⇒ defects need to be parallel to the viewing direction

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• techniques

– HRTEM (high-resolution transmission electron microscopy) · since 1980ies · »steady« improvement of conventional TEM · widespread application · focus of interest in this course

– holography · high-resolution electron holography is relatively new · record amplitude and phase (not just intensity) of the electron wave in

the image plane

– HAADF (high-angle angular dark-field) imaging (“z-contrast”) · new method · scanning transmission electron microscopy · requires annular (HAADF) detector

HRTEM versus CTEM (conventional TEM)

• contrast formation in CTEM

– sometimes absorption contrast, mostly diffraction contrast: · crystallites (grains) of different structure (different phases) or orientation · distortions induced by particles, dislocations, … · variation of the scattering amplitude by stacking faults, grain boundaries,

• CTEM bright-field imaging

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• CTEM dark-field imaging

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• example: Co precipitates in CuCo

– bright-field image

– distortion field introduced by the particles (plane bending) changes diffrac-tion conditions in the matrix ⇒»coffee bean« contrast

• principle of CTEM:

– different specimen regions generate Bragg reflections of different intensity

– contrast: either Bragg reflections or transmitted beam do not contribute to the image

⇒ consequence: interatomic spacings cannot be resolved

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Abbe Theory of Resolution

• ideal object (↔ crystal): lattice with period d

• coherent illumination: plane waves, wavelength λ

d

z=2

z=1

• diffraction:

– path difference between waves emitted from neighboring slits must equal an integer number of wavelengths, z · λ

– diffracted beams make angles ϕz, with the plane of the lattice, and

Sin !z[ ] =

z" #

d

• Abbe: only the diffracted beams carry information about the spacing d

⇒ to image the lattice, the optical system must at least include one diffracted beam (z = 1)

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⇒ generalization: to resolve an object under coherent illumination, the image formation must include at least the first diffraction maximum of the object

⇒ the aperture semi-angle α introduces a limit for the spatial resolution:

! Sin "1[ ] =

#

d < Sin $[ ]

⇒ resolution limit δ: smallest distance d that can be resolved

Sin[!1]= Sin["] # $ =

%

Sin "[ ]

⇒ resolving interatomic distances requires larger aperture than CTEM imaging and interference of (at least two) different Bragg reflections

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⇒ transition from CTEM to HRTEM:

– instrumental pre-requisites for interference images · illumination with a high degree of coherence

(small source, small spread of the wavelength) · mechanics and electronics sufficiently stable · electron lenses with small aberrations

(spherical and chromatic aberration, astigmatism)

– remove objective aperture

– ultra-thin specimen to avoid absorption and inelastic electron scattering (de-stroys coherence)

– orient the specimen to generate suitable Bragg reflections

• “ideal” HRTEM imaging (neglecting lens aberrations)

⇒ high resolution, but no contrast!

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Phase Contrast

• consider thin specimen, plane electron wave ψ0, no absorption

⇒ specimen just introduces small, locally varying phase shift (refractive index ↔ electrostatic potential)

• express exit wave ψe[ x ] as sum of incident wave ψ0 and scattered wave ψs[ x ]

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• phase of ψs[ x ] is shifted by −90° versus ψ0 :

! e x[ ] =!0 " i! s x[ ]

⇒ intensity:

! i x[ ]

2= !e x[ ]

2" ! 0 x[ ]

2

⇒ no contrast!

• must convert locally different phase shifts to locally different intensities (contrast ⇔ intensity variation)

→ if the optics introduces an additional phase shift of the scattered wave by −90°,

! i x[ ]

2= !0 x[ ] "!s x[ ]

2< ! 0 x[ ]

2

• problems:

– � � � � −90° phase shift cannot be realized in an ideal manner

– for TEM there exists no “λ/4 plate” as for light-optical microscopy

– in HRTEM, the required phase shift is introduced by · the spherical aberration of the objective lens · defocusing of the objective lens

– the image, which is obtained by interference of coherent electron waves, of-ten has a complex relationship with ψe, the electron wave function at the exit surface of the specimen

• consequence:

Correct interpretation of HRTEM images requires a quantitative un-derstanding of image formation.

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• example: Al/MgAl2O4 interface

– HRTEM in <110> projection

– microscope: JEM-ARM 1250 (Stuttgart)

• where are which atoms?!

– Al, Mg, O atom columns: “white” or “black”?

– relative visibility of the ions in the spinel?

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Electron Optics

• HRTEM:

– interference → wave properties

→ “wave model” of electron mandatory

• exact treatment of electron interference: quantum mechanics

• however: simpler wave optics also yields correct results – apart from image ro-tation and adjustments of the wave length λ

Properties of Fast Electrons

Physical Constants

rest mass m0 = 9,1091·10−31 kg

charge Q = −e = −1,602·10−19 C

kinetic energy E = e U 1 eV = 1,602·10−19 Nm

velocity of light c = 2,9979·108 m s−1

energy at rest E0 = m0 c2 = 511 keV = 0,511 MeV

Planck constant h = 6,6256·10−34 N m s

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Electrons in Motion

property non-relativistic relativistic

Newton’s law F =

d p

dt= m0

d v

dt

F =

d p

dt=

d

dtmv( )

mass m= m0

m=m0

1! v2/ c

2

energy E = eU = 1

2mv

2 mc2= E0 +E = m0c

2+ eU

velocity

v =2e

m0

v = c 1!1

1+ E/ E0( )2

momentum p = m0v= 2m0E p = mv=

1

c2EE0 + E2

de Broglie wavelength

! =h

p=

h

2m0E

! =hc

2EE0 + E2( )

• de Broglie wavelength as a function of the accelerating voltage:

200 400 600 800 1000 1200

0,5

1,0

1,5

2,0

2,5

3,0

! [pm]

U [kV]

classical

relativistic

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• velocity as a function of the accelerating voltage:

200 400 600 800 10001200

0,2

0,4

0,6

0,8

1,0 velocity of lightv/c

U [kV]

• kinetic and potential energy of the electrons on their way through the micro-scope

.

kin

etic

energ

y

cameracathode anode specimen

pote

nti

al energ

y

– specimen: · electrostatic potential varies ⇒ diffraction · free surfaces → average positive → “inner potential” Ui, attractive for electrons → acceleration, increase of the average velocity → wave length λ becomes smaller

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Fraunhofer Diffraction

• Fresnel diffraction → Fraunhofer diffraction:

– plane incident wave, diffraction pattern at “infinite” distance

– alternatively: diffraction pattern at back-focal plane of a lens

f

b

g

1

f=

1

b+

1

g

! e

! f

! i

focal plane

! 0

object

"

• wave at the exit surface of the specimen: ψe

• focal plane: rays that leave the specimen under the same diffraction angle θ in-tersect in the same point of the focal plane

• note:

– path difference between neighboring rays

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→ phase shift, to be taken into account when calculating the amplitude in the back focal plane

• path difference for scattering of a plane incident wave at two scattering centers P and Q:

– ray through P has longer path than ray through Q

– path difference:

!sg = u0 " !r # u " !r = #$ k # k0( ) " !r = #$q" !r

u0, u: unit vectors; q: scattering vector.

⇔ phase ϕP of the ray through P lags behind compared to phase ϕQ of the beam through Q

– phase difference:

!"g #"P $"Q = $

2%

&!sg = 2%q' !r

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• ray path for HRTEM (see above):

– for a given diffraction angle θ consider phase difference ϕg between ray through r and ray through origin of the object plane (r = 0):

!r = r = x,y,0( )

!"g ="g r[ ] := " r[ ] # " 0[ ]

ϕ[0]: focal-plane phase of the ray emitted at r = 0 with angle θ; ϕ[r]: focal-plane phase of the ray emitted at r with angle θ.

– TEM: small wavelength, small diffraction angles

⇒ q is approximately parallel to the focal plane

q= k ! k0 = 2kSin

"

2

#

$ % &

' ( )

"

*

• in the focal plane all rays with the same scattering vector q intersect in a point, which is displaced from the origin in the direction of q

• distance of the intersection point from the focus (origin of focal plane):

f! = f"q

→ use q as coordinate vector in the focal plane (a vector of length ||r|| in the focal plane corresponds to q = ||r||/fλ)

⇒ amplitude at location q in the focal plane:

! f q[ ] = !e r[ ]Exp i"g r[ ][ ]dS

Se

#

= !e r[ ]Exp 2$i q% r[ ]d2r

Se

#

Se: object plane.

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→ “weighed sum”

– plane waves with the same scattering vector q (and the same wave vector k) but different phases 2πi q·r

– contribution of each wave is proportional to the amplitude of the wave func-tion a the exit surface of the specimen

→ Fourier transformation!

The wave function ψf in the (back-) focal plane corresponds to the Fourier transform of the object wave function ψe (at the exit surface of the specimen):

! f = F ! e[ ]

• however: this is strictly correct only for a perfect, ideal lens

• real lenses: see below …

• wave function in the image plane:

– consider point r = (x, y) of the object

→ conjugate point in the image plane (image):

r '= !Mr

M: magnification.

– this implies:

! i r[ ] =! e "1

Mr

#

$ %

&

' (

• amplitude ψi[r’] at point r’ in the image:

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– since the image of an area is M2 larger than the area itself, the image inten-sity must decrease as M2

⇒ amplitude decreases as M−1

– sum over contributions from all points of the focal plane, taking into account the respective phases

• phase difference of neighboring rays that intersect at image point r’:

– consider ray intersecting with the focal plane at fλ·q away from the focus (q = 0):

– path difference to the ray through the focus:

! s g = f"q#$ '= f"q#

r

f= "qr

– since q || r, the path difference can be expressed by the scalar product q r: ! s g = "q r = #sg

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⇒ the phase shift introduced between the focal plane and the image plane ex-actly compensates the phase shift introduced between the object plane and the focal plane:

! " g = #

2$

%& ! s g = #2$q 'r

(ideal lens: different rays emerging from the same point of the object arrive at the image point without relative phase shifts)

⇒ amplitude at r’ in the image plane:

! i r '[ ] =1

M! f q[ ] Exp "2#i q $r[ ] d2q

Sf

%

=1

M! f q[ ] Exp "2#i q $ "

& r

M

'

( )

*

+ ,

-

. / 0

1 2 d2q

Sf

%

Sf: focal plane.

• often one neglects the magnification and the inversion of the image, and ex-presses the image with respect to the coordinate system of the object (let M = 1, r’ = r):

! i r[ ] = ! f q[ ]Exp "2#i q$ r[ ]d2q

Sf

%

→ inverse Fourier transformation!

The wave function ψi in image plane corresponds to the inverse Fourier transform of the wave function ψf:

! i = F

-1! f[ ]

→ result for the complete imaging process (ideal lens, M = 1, r’ = r):

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The wave function ψi in the image plane corresponds to the inverse Fourier transform of the Fourier transform of the object wave func-tion ψe:

! i = F

"1F ! e[ ][ ]

• ideal lens, M = 1, r’ = r: perfect restoration of the object wave function in the image

• “real” imaging:

– finite aperture → truncates the Fourier spectrum in the focal plane

– lens aberrations introduce additional phase shifts → the objective lens shifts the phases of the plane waves of which ψe is

composed in a complex way versus each other ⇒ ψi does not exactly correspond to ψe

– limited coherence → attenuation of the interference, diffuse background

⇒ interpretation of “real” images requires in-depth understanding of Fourier transformation

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Fourier Transformation

General Properties

• definition of the Fourier transform

F f x[ ][ ] ! F u[ ] := f r[ ]Exp 2"i ux[ ]dx

#$

$

%

• inverse Fourier transform:

F !1 F u[ ][ ] " f x[ ] := F u[ ]Exp !2#i ux[ ]du

!$

$

%

• extension to n dimensions:

F f x[ ][ ] ! F u[ ] := f x[ ]Exp 2"i u x[ ]dnx

Rn#

F $1 F u[ ][ ] ! f x[ ] := F u[ ]Exp $2"i u x[ ]dnu

Rn#

• convention

– factor 2π in the exponent

– sometimes neglected (in quantum mechanics, for example), but this requires to multiply · either F[] or F−1[] by factor (2π)−1, or · each, F[] and F−1[], by (2π)−1/2

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• properties of the Fourier transform

real space Fourier space

f x[ ] F u[ ]

af x[ ] + bgx[ ] aF u[ ] + bG u[ ]

f*

x[ ] F*!u[ ]

f x ! a[ ] F u[ ]Exp 2!i au[ ]

f ax[ ]

1

aF

u

a

!

" # $

% &

d

dxf x[ ]

!2"i u( ) F u[ ]

dn

dxn

f x[ ] !2"i u( )

nF u[ ]

Exp !2"i ax[ ] ! u " a[ ]

! x " a[ ] Exp 2!i au[ ]

f x[ ] ! g x[ ]

F u'[ ] !G u " u'[ ]"#

#

$ d u'% F &G( ) u[ ]

f x'[ ] ! g x " x'[ ]d x'

"#

#

$ % f & g( ) x[ ] F u[ ] !G u[ ]

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Delta Function

• definition of the delta “function” (actually a “distribution,” since it is not defined for every argument)

! x " a[ ] :=0 x # a

$ x = a

% & ' (

! x " a[ ]"#

#

$ =1

• visualization:

• delta function correspond to a normal distribution in the limit of vanishing stan-dard deviation:

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! x[ ] := lim"#0

1

" 2$Exp %

1

2

x

"

& ' (

) * +

2,

- . .

/

0 1 1

&

' ( (

)

* + +

• under an integral the delta function “selects” a value of the integrand function:

! x " a[ ] g x[ ]d x = g a[ ]"#

#

$ ! x " a[ ]d x

"#

#

$ = g a[ ]

• concerning Fourier transforms, the following relation is particularly important:

Exp 2!i ux[ ]d x

"#

#

$ = % u[ ]

Convolution

• definition of the convolution integral of two functions f[x] and g[x]:

f ! g( ) x[ ] := f x'[ ] "g x # x'[ ]d x'

#$

$

%

• substitution y’ = x − x’, dx’ = −dy reveals that the convolution is symmetric with respect to exchanging the argument functions:

!

f " g( ) x[ ] # $ f x $ y[ ] % g y[ ] d y&

$&

' = g y[ ] % f x $ y[ ] d y$&

&

' = g " f( ) x[ ]

• interpretation: spread function f with the function obtained by inverting function g

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Example of a Convolution

f ! g( ) x[ ] " f x'[ ] # g x $ x'[ ]d x'

$%

%

&