Introduction
Scanning electron microscopy (SEM) has become as fundamental to metallurgical analysis as the optical microscope. Where optical microscopy is limited by the wavelength of light (resolution limit ~200 nm at best), the SEM uses a focused electron beam with wavelength 10⁻¹⁰⁰ pm — three orders of magnitude smaller — enabling resolution of 1–5 nm in modern instruments. Combined with X-ray energy-dispersive spectroscopy (EDS) for compositional mapping and electron backscatter diffraction (EBSD) for crystallographic orientation mapping, the SEM platform provides more microstructural information per experiment than any other technique available to the practising metallurgist.
SEM Working Principles
The SEM works by rastering a focused electron beam (probe) across the specimen surface in a raster pattern. Various signals generated by the electron-specimen interaction are detected synchronously:
| Signal | Origin | Information Provided | Typical Resolution | |
|---|---|---|---|---|
| Secondary electrons (SE) | Low-energy electrons emitted from near-surface (<5nm) | Topography; surface morphology | 1–5 nm | |
| Backscattered electrons (BSE) | High-energy electrons elastically scattered from specimen | Atomic number contrast (Z-contrast); phase identification | 5–20 nm | #f9f6f0 |
| Characteristic X-rays | Inner shell electron excitation → relaxation | Elemental composition (EDS/WDS) | 500nm–2µm | |
| Electron backscatter diffraction (EBSD) | Diffracted electrons from crystalline planes | Crystal orientation; phase; grain boundaries | 50–200 nm | #f9f6f0 |
| Cathodoluminescence (CL) | Photon emission from electron-excited states | Defect mapping in semiconductors; rarely used in metals | 50–500 nm |
Secondary Electron Imaging: Fractography
Secondary electron (SE) imaging reveals topographic contrast with high depth of field — typically 100–300× greater than an optical microscope at equivalent magnification. This makes SEM the definitive tool for fractographic analysis: examination of fracture surfaces to determine failure mechanism.
Key fractographic features visible in SEM:
- Fatigue striations: Parallel ridges perpendicular to crack propagation direction; spacing reflects crack growth rate per cycle
- Dimples (microvoid coalescence): Hemispherical depressions indicating ductile fracture; equiaxed dimples = normal stress fracture; elongated dimples = shear fracture
- Cleavage facets: Flat, reflective crystallographic planes with “river marks” converging to crack origin; characteristic of brittle transgranular fracture in BCC steels
- Intergranular fracture: Smooth grain surfaces exposed; no striations or dimples; indicates grain boundary embrittlement (temper embrittlement, hydrogen embrittlement, liquid metal embrittlement)
Backscattered Electron Imaging and Phase Contrast
BSE yield increases with mean atomic number (Z). In BSE imaging, heavy phases appear bright (high Z) while light phases appear dark. This provides immediate phase identification without etching:
- In steel: WC particles in tool steel binder phase (bright W vs darker Fe matrix); cementite vs ferrite contrast
- In aluminium alloys: CuAl₂ precipitates (bright Cu) vs Al matrix (dark)
- In duplex stainless steel: ferrite and austenite have similar Z (both Fe-based) — BSE cannot distinguish them reliably; EBSD is needed
EDS: Elemental Mapping and Quantitative Analysis
Energy-dispersive X-ray spectroscopy (EDS) detects characteristic X-rays emitted when the electron beam excites inner-shell electrons. Each element produces characteristic X-rays of defined energy (keV), allowing simultaneous multi-element detection. Capabilities:
- Spot analysis: Quantitative or semi-quantitative composition of a phase or particle (typically ±1–2 wt% accuracy without standards; ±0.1–0.5% with standards and ZAF/φρZ correction)
- Line scan: Composition profile across a microstructural feature — segregation at grain boundaries, carbide depletion zones, coating thickness
- Element map: 2D distribution map of each element across the SEM field — reveals segregation patterns, coating uniformity, inclusion chemistry
Detection limits: ~0.1–0.3 wt% for most elements in a metallic matrix. Light elements (B, C, N, O) are detectable but accuracy is limited by absorption correction and carbon contamination. WDS (wavelength-dispersive spectroscopy, as in EPMA) provides better detection limits (20–100 ppm) and accuracy for light elements.
EBSD: Crystallographic Orientation and Phase Mapping
EBSD captures diffraction patterns (Kikuchi patterns) from the near-surface crystal lattice when the specimen is tilted to 70° relative to the electron beam. Automated indexing of thousands to millions of patterns per map produces:
- Inverse pole figure (IPF) maps: Grain orientation shown by colour — each grain appears a different colour based on its crystallographic orientation relative to the specimen normal. Immediately reveals grain size, shape, and texture.
- Phase maps: Distinguishes phases with different crystal structures (FCC austenite vs. BCC ferrite in duplex stainless; austenite vs. martensite in TRIP steel)
- Grain boundary maps: Identifies low-angle boundaries (sub-grain structure), high-angle boundaries, and coincidence site lattice (CSL) boundaries (Σ3 twin boundaries in austenite)
- Kernel average misorientation (KAM): Local misorientation distribution maps plastic strain accumulation — used to quantify deformation around cracks, HAZ, or forming operations
Specimen Preparation for SEM
Specimen preparation requirements are more demanding than for optical microscopy — the sub-nanometre scale of interest means even a thin deformed surface layer will mask true microstructure in EBSD:
- Final mechanical polish with 0.05µm colloidal silica (OPS) for 10–20 minutes
- Electropolishing (for metals amenable): provides deformation-free surface ideal for EBSD but may not reveal all phases equally
- Focused ion beam (FIB) milling: site-specific preparation for transmission electron microscopy lamellae or cross-sections through specific microstructural features
- Non-conductive specimens must be coated with thin conductive film (5–10nm carbon or Ir) to prevent charging — this absorbs some SE signal but is necessary for insulating phases
Frequently Asked Questions
Q: What is the difference between SEM and TEM?
A: SEM images the specimen surface using reflected/emitted signals; TEM transmits the electron beam through a very thin foil (<100nm) to image crystal defects, precipitates, and interfaces at atomic resolution. SEM is better for 3D surface information and large areas; TEM for atomic-scale structural information. STEM (scanning TEM) combines both capabilities with atomic-column resolution EDS mapping.
Q: Can SEM identify hydrogen embrittlement fracture?
A: SEM fractography can strongly suggest hydrogen embrittlement: the combination of intergranular fracture mode (smooth grain surfaces) at stress levels below yield, absence of dimples or striations, and specific crack morphology (branching, flat facets) is characteristic. However, hydrogen itself cannot be directly detected by EDS (Z=1, too light). Confirmation requires correlation with processing history (plating, welding) and sometimes thermal desorption spectroscopy.
Conclusion
The SEM platform — combining SE/BSE imaging, EDS elemental analysis, and EBSD crystallographic mapping — is the most powerful and versatile tool for microstructural characterisation in metallurgy. Understanding which signal to use for which question, combined with proper specimen preparation, allows definitive identification of phases, fracture modes, compositional gradients, and crystallographic textures that underpin materials performance in service. See also: Optical Metallography Guide and Fatigue Testing and S-N Curves.
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