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EBSD and BKD    

Transmission Kikuchi Diffraction TKD

The first Transmission as well as Backscatter Kikuchi Patterns [1, 2] (later named TKP and BKP) were published in the same volume of Proc. Imperial Academy of Japan (Tokyo) 4(1928) pp. 354 resp. pp. 475.  Experimental work has been focused during the first decades preferably on Transmission Kikuchi Diffraction (TKD) because of instrument-based reasons. Since the end of last century Backscatter Kikuchi Diffraction (BKD) in the SEM, then named Electron Backscatter Diffraction (EBSD), is about to prevail thanks to the availability of commercial systems, the ease of operation and sample preparation, and enabling of dynamic experiments. Recently interest in TKD has risen again, in particular as a supplementary facility to an EBSD system, a wishful dream of improving resolution in texture analysis.

In the TEM the diffraction patterns are either acquired with a CCD camera placed on-axis at the bottom of the microscope column or with a retractable CCD camera on the side-entry flange above the viewing screen. A circular continuous density filter in the optical path is of advantage to equalize the steep drop of intensity from the blooming primary beam spot to the dim marginal area. Pattern intensity is of minor concern in TKD with a TEM. The patterns should cover a large angular range and be undistorted. These requirements limit TKD orientation mapping to the use of a TEM with a condenser objective lens and microbeam diffraction facility such as for instance the Philips CM series, respectively FEI TEM. For automated mapping [3] a computer controlled scan of the beam spot is implemented. For details and some applications see http://www.crystaltexture.com/tkd.htm .

In BKD mode the sample surface is steeply inclined by about 60º to 70º out of the horizontal to produce a sufficient backscatter intensity. The EBSD detector is placed horizontally on the side (Fig. 1a). The distance between sample and screen is typically 2 cm, roughly like the diameter of the screen, so that a wide cone of about 45º of backscattered electrons is acquired. As a consequence of strong forward scattering of energetic electrons by matter a steep lobe of intensity is generated. The maximum is close to the direction of optical reflection that a light beam would have from an opaque surface. The height of the EBSD detector is therefore set such that the intensity maximum falls on the center of the phosphor screen.

Figure 1  Kikuchi diffraction in the SEM. The cone sections of the acquired patterns are marked in green.
Fig. 1a shows the setup of BKD. In TKD the detector comes in from the side beneath the horizontal sample.
Either the standard EBSD detector (Fig. 1b) is used, or (as in Fig. 1c) a dedicated detector with the transparent phosphor screen is placed concentrically to the primary beam spot beneath the sample.

TKD in the SEM is applied to a thin foil at least parts of which have to be transparent to electrons. The foil sits horizontally in a special holder.  Diffraction is either carried out with  the EBSD  screen  positioned  vertically beneath the sample so that about half the pattern cone is captured (Fig. 1b) [4]. A standard EBSD detector is placed in the same position as for BKD. An alternative setup (Fig. 1b) [5] uses a dedicated EBSD detector having the transparent phosphor screen horizontally about 1 cm beneath the sample. A mirror at 45° at the backside of the screen reflects the pattern to the CCD camera. The advantage of this setup is the acquisition of the whole cone of the Kikuchi pattern, as in the TEM equipped with a side-entry CCD camera. However, the intense central beam spot might overexpose the camera, as a consequence of limited dynamics, whereas the fringe of the pattern shows an intensity too low for evaluation. A circular continuous density filter in the optical path is recommended, as for TKD in the TEM.

Spatial resolution in EBSD and TKD

A high spatial resolution in orientation measurement is required for the study of fine grain and heavily deformed materials in general, of recrystallization and grain growth, of grain boundary characterization, of nanomaterials and in the study of the impact effects of high-energy particles. But why does spatial resolution in Kikuchi diffraction fall more than one order of magnitude behind spatial resolution in conventional SEM imaging, and still further behind when compared to the spatial resolution of a TEM?

The inherent resolution limit of Kikuchi diffraction is set primarily by the excitation volume rather than by the diameter of the beam spot at the point of impact on the sample surface. The excitation volume is the fraction of the interaction volume of the primaries with the sample from where the pattern forming electrons are diffracted and can leave the crystal with no further scattering. Gray hading in the figure indicates this volume fraction. The footprint of the beam spot is marked in bright green.

Spatial resolution BKD TKD IBP

Fig. 2 Excitation volume and spatial resolution in TKP, BKP and IBP

A further limitation of spatial and depth resolution in Kikuchi diffraction is set by the smallest grain size. To exclude overlapping Kikuchi patterns, grain size should be larger than the excitation volume. Spatial resolution with copper is better than 0.05 μm at 20 kV using a tungsten filament and presently about 0.03 μm with a FE gun.

The pattern is formed on the exit side of the foil in a depth of about the free mean path of the electrons. Patterns generated close to the entrance side are blurred due to inelastic scattering and thus contribute mainly to background. Therefore, a thin (amorphous) layer on the entrance side only widens the beam.

Resolution in depth, δz, simply equals foil thickness. In practical work, the smallest probe size and hence spatial resolution is limited to about 10 nm with TKD, due to the decrease in image brightness as the probe becomes smaller, and due to the spread of the scattered beam on its way through the specimen foil. If neighboring grains are studied, orientation differences down to 0.1° can be measured with TKD in the TEM and about 0.5° in the SEM. While resolution within a grain is of lower significance, it becomes quite critical when the beam spot approaches a grain boundary. A smart pattern indexing software can then improve resolution in TKD and EBSD by taking account of the intensity levels of superimposed patterns, rejecting less likely orientation solutions and comparing orientations in neighboring pixels. Pattern contrast strongly depends on foil thickness, density and accelerating voltage. Resolution in depth, δz, simply equals foil thickness or is less.

A promising alternative to EBSD will be crystal orientation mapping using Ion Blocking Patterns (IBP) [6]. These patterns consist of a bright even background superposed by a regular system of very sharp black lines. An IBP is similar to quasi a negative image of a BKP. A black line is formed by ions which impinge on the surface parallel with a low-indexed lattice plane, channel deep into the crystal, but cannot leave the crystal unless they are backscattered again in the channel of an angular width of less than twice the Bragg angle to the lattice plane. As a consequence of the small deBroglie wavelength of ions the lines are significantly narrower than the corresponding bands in BKP. A thin foreign amorphous layer fans out the incoming beam by scattering, thus suppresses channeling into the crystal and lastly the formation of black lines. The requirements for a gentle sample preparation and a clean vacuum are very high. At present commercial ion scanning microscopes with high current densities in small probes in the nanometer range and a clean vacuum in the specimen chamber are not yet available. Spatial resolution equals the footprint of the ion probe on the surface.

Foil thickness and buckling set limits to TKD

Thin foils are often difficult to prepare from the bulk. It is in many cases questionable whether a thin foil truly represents the structure of the interior of the material. The grains relax on both surfaces when the matrix is removed. Due to different grain orientations in a polycrystal the foil contains local residual stress. Therefore surfaces of freestanding foils are often not really flat but show a grain-specific surface relief and bulging. This foil bending and puckering cannot be easily excluded. The result is a change in local orientations of up to several degrees with respect to the microscope-specific reference directions.

A large grain or a single crystalline foil is bent, but roughly retains its intrinsic orientation. This is visualized in the grain orientation map by color shading for low deviations in orientation. At larger surface slopes pattern indexing may jump to another solution, which is correct for the microscope-specific reference directions (x, y and z) deviating from the local grain-specific reference directions and the local surface normal, but is not correct for the orientation if it could have been measured in the bulk material. Such jumps in orientation are reproduced by distinct color skips in the orientation map. Irregular bending and wrinkles are readily perceived in orientation maps of single crystal foils at large area scans since the resulting damask pattern appears factitious.

The tiling of fine grains in a wrinkled foil, however, follows the local bending. The superposition of the surface topography and the rotated orientations of the individual grains result in a distinct color, presumable without shading, for each grain in the orientation map. If texture is not extremely sharp the map looks like a map of a usual fine grain polycrystal. Foil wrinkling is thus disguised.

The slopes of foil bending are in the range of several degrees. As a consequence measured local orientations scatter by an error of this range about the orientations one would obtain if the sample were flat. The ODF and pole figures are slurred by widening sharp peaks of orientation densities by several degrees as well. Ideal thin samples with bulging inclinations below the angular resolution of a Kikuchi system are very hard to realize [4]. This is true in particular for transmission studies in the SEM where foil thickness has to be much smaller, to be transparent at the lower accelerating voltage, than in the TEM at medium to high accelerating voltages. Dedicated sample preparation techniques are absolutely essential. A compromise between correct measurement on a flat surface and a reduced spatial resolution is to deposit the specimen foil on an amorphous support film. The specimen is then placed upside down in the microscope. The amorphous support widens the incoming beam by scattering, but contributes merely to the background in the pattern.

Foil buckling is nicely displayed in "bend contours", also named "extinct ion contours", in TEM micrographs [7]. They are formed preferably at lower magnifications when a small selector aperture is used. They are dark in bright field images, respectively light in dark field images, for crystal regions where the lattice planes are in Bragg position. Contours of equal intensity represent lines of equal inclination to the electron beam. The angular deviation between contour lines is thus a multiple of the Bragg angle. [see TEM textbooks for details, e.g. [8], Section Bend contours; [9], Chapter 23.4 Bend Contours (Annoying Artifact, Useful Tool, and Invaluable Insight]

Synoptic Overview





Spatial resolution      


0.3 nm
<10 nm diam.

2 nm  (SE)
10 nm diam.

2 nm  (SE)
30 nm x 90 nm

Angular resolution

0.05° ... 0.5°

0.2 - 0.5°

Observable area

small, 50 µm diam.
be aware of foil wrinkling

large, some mm²

grain boundaries
Lattice defects          



tilt experiment

Δg > 0.2°
(FE SEM only)

Burgers vector analysis

yes, tilt experiment

in principle yes

not yet

Main applications

<500 nm      foil thickness     <100 nm
high resolution, misorientations

bulk surfaces
orientation  microscopy

Sample preparation

difficult, laborious

relatively easy

[1] Download  pdf icon S. Kikuchi: Diffraction of cathode rays by mica, Part 1-4.
Proc. Imp. Acad. Japan (Tokyo) 4 (1928) 271 ff.
[2] Download  pdf icon S. Nishikawa and S. Kikuchi: The Diffraction of Cathode Rays by Calcite.
Proc. Imperial Academy (of Japan) 4 (1928) 475-477

[3] Download pdf icon R.A. Schwarzer and J. Sukkau: Automated crystal orientation mapping (ACOM) with a computer-controlled TEM by interpreting transmission Kikuchi patterns. Mat Sci Forum 273-275 (1998) 215-222.
[4]  P.W.  Trimby: Orientation mapping of nanostructured materials using transmission Kikuchi diffraction in the scanning electron microscope. Ultramicroscopy 120 (2012) 16-24.
[5]  Bruker OPTIMUSTM TKD; Technical Note 2015. http://www.bruker.com/
Downloadpdf icon  R.A. Schwarzer: Spatial resolution in ACOM - What will come after EBSD.
Microscopy Today 16 (January 2008) 34-37
Download pdf icon R. Schwarzer: Transmission Kikuchi diagrams and convergent beam diffraction patterns of epitaxially evaporated copper layers (in German).
Beitr. elektronenmikroskop. Direktabb. Oberflächen (BEDO) 10(1977)195-202
[8] J.W. Edington: Interpretation of Transmission Electron Micrographs. Practical Electron Microscopy in Materials Science, Monograph 3. MacMillan Philips Techn. Library, Eindhoven 1975
[9] D.B. Williams and C.B. Carter: Transmission Electron Microscopy. Plenum Press, New York 1996