Slip Systems in Metals — BCC, FCC and HCP Compared
Slip is the dominant mechanism of plastic deformation in crystalline metals — the process by which dislocations translate through the lattice along specific slip planes in specific slip directions, producing permanent macroscopic shape change. A slip system is the combination of one slip plane and one slip direction lying within it. The number, geometry, symmetry, and activation energy of available slip systems directly govern a metal’s ductility, formability, work-hardening behaviour, and susceptibility to cleavage fracture — making slip system analysis the quantitative foundation of all crystal plasticity.
- FCC metals have 12 slip systems {111}⟨110⟩ on 4 close-packed planes — satisfying the Von Mises criterion (5 independent systems) with large margin, producing excellent ductility at all temperatures.
- BCC metals have up to 48 possible slip systems but no true close-packed plane; screw dislocations undergo pencil glide and CRSS increases sharply below the ductile-to-brittle transition temperature (DBTT).
- HCP metals have only 3 independent basal slip systems {0001}⟨11̅20⟩ — insufficient for polycrystalline ductility; non-basal slip and mechanical twinning are essential to reach the Von Mises threshold.
- Schmid’s Law: the slip system with the highest resolved shear stress activates first. Schmid factor m = cos(φ)·cos(λ); theoretical maximum m = 0.5 at 45° orientation.
- Stacking fault energy (SFE) controls cross-slip: high SFE (Al, ~140 mJ/m²) enables easy cross-slip and low work hardening; low SFE (Cu, austenitic SS) produces planar dislocation arrays and rapid work hardening.
- The Taylor factor M (typically 2.5–3.5 for polycrystals) relates the single-crystal CRSS to the macroscopic polycrystal yield stress: σy = M × τCRSS.
1. Crystallographic Fundamentals of Slip
Plastic deformation by slip requires dislocations to traverse the crystal lattice. The energetic preference for specific slip planes and directions arises from two crystallographic principles. First, slip occurs on the most densely packed planes — those with the greatest interplanar spacing and weakest interlayer bonding, minimising the lattice friction (Peierls-Nabarro stress) that must be overcome to move a dislocation. Second, slip propagates in the closest-packed direction within those planes, because this minimises the Burgers vector magnitude and therefore the elastic strain energy of the dislocation, which scales as Gb²/2 where G is the shear modulus and b is the Burgers vector length.
The Peierls-Nabarro stress provides a quantitative measure of lattice friction:
τ_PN = (2G / (1-ν)) × exp(-2πw / b)
where:
G = shear modulus (Pa)
ν = Poisson's ratio
w = dislocation core width ∝ d (interplanar spacing)
b = Burgers vector magnitude
Consequence: wider planes (large d) and smaller Burgers vectors (small b)
give exponentially lower slip resistance.
FCC {111}: highest atom density → largest d → lowest τ_PN
BCC {110}: intermediate density → higher τ_PN, more T-sensitive
1.1 Miller Indices and Slip System Notation
Slip planes are identified by Miller indices {hkl} — braces denoting the family of symmetry-equivalent planes. Slip directions are identified by ⟨uvw⟩ angle-bracket notation — denoting all symmetry-equivalent directions. A complete slip system is written {hkl}⟨uvw⟩. The number of distinct systems is the product of the number of equivalent planes and the number of permissible directions per plane, accounting for the constraint that the direction must lie within the plane (confirmed by the condition hu + kv + lw = 0). For a deeper treatment of crystallographic notation, see the iron-carbon phase diagram article, which applies these conventions to describe phase boundaries in the Fe-C system.
2. FCC Slip Systems: {111}⟨110⟩
The face-centred cubic structure has four equivalent {111} planes (the octahedral planes): (111), (1̅11), (11̅1), and (111̅). Each plane contains three ⟨110⟩ directions — six directions lie in each {111} plane, but only three are crystallographically distinct due to the ± symmetry of slip (a dislocation moving in +[̅110] is the reverse of one moving in [1̅10]). This gives 4 planes × 3 directions = 12 slip systems.
Of these 12, exactly 5 are linearly independent — satisfying the Von Mises criterion for polycrystalline ductility. The consequence is that any grain in a polycrystalline FCC metal can deform to accommodate an arbitrary imposed strain without cracking at boundaries. This geometric fact, combined with the low Peierls stress on close-packed {111} planes, explains why FCC metals (copper, aluminium, nickel, austenitic stainless steel, gold) achieve elongations of 20–60% in tensile testing and are readily cold-rolled, deep-drawn, and wire-drawn.
2.1 Stacking Fault Energy and FCC Work Hardening
In FCC metals, a perfect dislocation with Burgers vector b = ½⟨110⟩ spontaneously dissociates into two Shockley partial dislocations with vectors of type ⟨112⟩/6, separated by a ribbon of stacking fault. The equilibrium ribbon width d is:
d = Gb² / (8π × SFE) where SFE = stacking fault energy (J/m²) Typical SFE values: Aluminium (Al) : ~140 mJ/m² → narrow ribbon, easy cross-slip Copper (Cu) : ~45 mJ/m² → wide ribbon, restricted cross-slip Nickel (Ni) : ~120 mJ/m² → moderate, some cross-slip Austenitic SS : 15–50 mJ/m² → very wide ribbon, planar slip, high WH Silver (Ag) : ~22 mJ/m² → wide, strong stacking fault texture
Metals with high SFE (aluminium) have narrow extended dislocations that recombine readily, enabling cross-slip — the transfer of a screw dislocation from its primary {111} plane to a secondary intersecting {111} plane. Cross-slip allows dislocations to bypass obstacles, promoting recovery and annealing of work-hardened structure at modest temperatures. Low-SFE metals (copper, austenitic stainless steel) cannot cross-slip; dislocations are pinned in planar tangles, cell walls, and Lomer-Cottrell locks, producing rapid work hardening. This is why type 316 austenitic stainless steel (SFE ~25 mJ/m²) achieves a work hardening exponent n of ~0.5 and UTS/YS ratios above 2, compared to n ~0.15 for aluminium alloys.
3. BCC Slip Systems and Pencil Glide
The body-centred cubic structure has no truly close-packed plane — the {110} planes are the most densely packed but fall short of the FCC {111} packing density. Slip nevertheless occurs on {110}, {112}, and {123} planes, all sharing the ⟨111⟩ close-packed direction as the unique Burgers vector b = ½⟨111⟩. This gives:
Primary BCC systems:
{110}⟨111⟩ : 6 planes × 2 directions = 12 systems
{112}⟨111⟩ : 12 planes × 1 direction = 12 systems
{123}⟨111⟩ : 24 planes × 1 direction = 24 systems
Total possible: up to 48 slip systems
The defining feature of BCC plasticity is pencil glide: screw dislocations with b = ½⟨111⟩ have a non-planar, spread-out core structure distributed simultaneously across {110}, {112}, and {123} planes. There is no preferred glide plane — the screw dislocation selects whichever plane currently presents the highest resolved shear stress, switching between planes as the stress state evolves. The result is wavy, irregular slip traces on polished surfaces (resembling pencil strokes) rather than the sharp parallel traces of FCC octahedral slip. While the number of available systems is large, the non-planar core architecture means that dislocation mobility is not simply determined by resolved shear stress — the non-Schmid behaviour of BCC screws (dependence on stress components beyond the resolved shear stress) adds complexity to crystal plasticity modelling of ferritic steels and refractory metals.
3.1 The Ductile-to-Brittle Transition in BCC Metals
The most consequential engineering difference between BCC and FCC plasticity is the ductile-to-brittle transition temperature (DBTT). In BCC metals, the CRSS for screw dislocation motion increases steeply as temperature decreases — the Peierls stress for the non-planar core scales approximately as:
τ_CRSS(T) ∝ exp(+Q_kink / kT) [approximation for thermally activated kink-pair]
For α-iron:
CRSS at 300 K : ~50–80 MPa
CRSS at 150 K : ~200–400 MPa
CRSS at 77 K : >600 MPa (approaching cleavage stress)
When τ_CRSS > σ_cleavage (fracture stress on {100} planes):
→ brittle cleavage fracture replaces ductile slip
→ this crossover temperature = DBTT
For mild (ferritic) steel with a DBTT of approximately −20°C to +10°C, this explains failures such as the Liberty ship fractures of World War II — steel performing adequately in temperate workshops became brittle at North Atlantic service temperatures. DBTT is not an intrinsic material constant but depends strongly on grain size (Hall-Petch: finer grain = lower DBTT), carbon and nitrogen interstitial content (raise DBTT by locking dislocations), radiation damage (displacement cascades raise DBTT by creating dislocation obstacles), and strain rate (higher rate raises effective DBTT). See the grain boundaries article for how grain refinement mechanisms reduce DBTT in structural steels.
4. HCP Slip Systems: Basal, Prismatic, and Pyramidal
HCP metals have three distinct families of slip plane with different crystallographic characters. The c/a ratio of the HCP unit cell (ratio of lattice parameters) is the primary determinant of which family is active at lowest stress:
| Slip Mode | Slip Plane | Slip Direction | No. Systems | Independent | Active in |
|---|---|---|---|---|---|
| Basal | {0001} | ⟨11̅20⟩ | 3 | 2 | Mg, Zn, Cd (c/a > ideal) |
| Prismatic | {10̅10} | ⟨11̅20⟩ | 3 | 2 | Ti, Zr (c/a < ideal) |
| 1st-order pyramidal ⟨a⟩ | {10̅11} | ⟨11̅20⟩ | 6 | 4 | Most HCP at elevated T |
| 2nd-order pyramidal ⟨c+a⟩ | {11̅22} | ⟨11̅23⟩ | 6 | 5 (cumulative) | Ti, Zr above ~600 K |
The critical point is the independent system count. Basal slip alone provides only 2 independent systems — incapable of accommodating strain along the c-axis. Prismatic slip adds 2 more independent systems (total 4). Only pyramidal ⟨c+a⟩ slip — which has a Burgers vector with a component parallel to the c-axis — provides the fifth independent system required by the Von Mises criterion. Without ⟨c+a⟩ slip (or mechanical twinning as a substitute), polycrystalline HCP metals fracture prematurely because grains oriented with the c-axis parallel to the tensile axis cannot deform and must shed load to adjacent grains until a boundary crack initiates.
4.1 Magnesium vs. Titanium: c/a Ratio Effects
The ideal c/a ratio for HCP (assuming hard-sphere close packing) is 1.633. Metals with c/a above this value have {0001} as the most densely packed plane and activate basal slip most easily. Metals below ideal c/a have relatively more closely packed prismatic planes. Alpha-titanium (c/a = 1.587, below ideal) exhibits primary prismatic slip {10̅10}⟨11̅20⟩ with CRSS ~50–100 MPa at room temperature, contrasting with magnesium (c/a = 1.624, near ideal) which activates basal slip at CRSS ~0.5–1.0 MPa. The practical consequence: commercially pure titanium (Grade 2) achieves 20–25% elongation in tensile testing through prismatic + pyramidal slip, while pure magnesium polycrystals fracture at 2–8% elongation unless fine grain size, alloying (RE additions), or elevated temperature (activating non-basal systems) is employed. For microstructural effects on titanium’s mechanical properties, see the discussion in the martensite formation article on diffusionless transformation comparisons.
4.2 Mechanical Twinning as a Supplement to Slip
When the available slip systems cannot accommodate an imposed strain direction — particularly compression along the c-axis in hexagonal metals — mechanical twinning activates as a supplementary deformation mode. Twinning produces a mirror-image lattice reorientation across the twin boundary by a homogeneous shear, reorienting the crystal into a more slip-friendly orientation for subsequent dislocation glide. In magnesium, {10̅12}⟨10̅11⟩ extension twinning reorients the c-axis by 86.3°, converting a hard orientation into one where basal slip is favoured. In titanium, {10̅12} extension twinning and {11̅22} contraction twinning both activate, the latter at higher stresses. Understanding twin activation is critical for modelling texture evolution during rolling and extrusion of Mg alloy sheet and Ti forging billets.
5. Schmid’s Law and the Critical Resolved Shear Stress
Schmid’s Law provides the quantitative link between the macroscopic applied stress and the driving force for dislocation glide on any specific slip system. It applies rigorously to single crystals in the early stages of deformation (single slip); with modifications, it extends to polycrystals through the Taylor model.
The critical resolved shear stress (CRSS) is a material parameter representing the minimum resolved shear stress required to move dislocations on a given slip system at a given temperature and strain rate. It varies with temperature, purity, alloying, and prior deformation (work hardening). The table below summarises room-temperature CRSS values for representative metals:
| Metal | Structure | Primary Slip System | CRSS (MPa) RT | Temperature Sensitivity |
|---|---|---|---|---|
| Aluminium (pure) | FCC | {111}⟨110⟩ | ~0.5–1.0 | Very low — ductile at −196°C |
| Copper (pure) | FCC | {111}⟨110⟩ | ~0.6–1.5 | Very low — low SFE, high work hardening |
| Nickel (pure) | FCC | {111}⟨110⟩ | ~6–12 | Low — ductile to cryogenic T |
| Alpha-iron (pure) | BCC | {110}⟨111⟩ | ~50–150 | Strong — DBTT ~−10 to +20°C (purity-dependent) |
| Tungsten (pure) | BCC | {110}⟨111⟩ | ~500–1000 | Very strong — DBTT above +200°C |
| Magnesium (pure) | HCP | {0001}⟨11̅20⟩ (basal) | ~0.5–1.0 | Basal easy; prismatic activates above ~250°C |
| Alpha-titanium | HCP | {10̅10}⟨11̅20⟩ (prismatic) | ~50–100 | Moderate — prismatic dominant to 600 K |
| Zinc (pure) | HCP | {0001}⟨11̅20⟩ (basal) | ~0.2 | Very strongly basal; high anisotropy |
5.1 Single Crystal Deformation Stages
A single-crystal tensile test reveals three distinct work-hardening stages controlled by slip system geometry. In Stage I (easy glide), a single slip system dominates — dislocation density rises slowly, dislocations escape to the surface, and the hardening rate dτ/dγ is very low (~10−4G). In Stage II (linear hardening), a secondary slip system activates; dislocations on intersecting systems interact, forming Lomer-Cottrell locks and dislocation tangles — the hardening rate rises sharply to ~G/300. In Stage III (dynamic recovery), cross-slip becomes significant, enabling dislocation annihilation and a decreasing hardening rate. The onset temperature of Stage III is lower for high-SFE metals (Al begins Stage III at room temperature) and higher for low-SFE metals (Cu shows pronounced Stage II hardening). This progression is the single-crystal mechanistic basis for the polycrystalline stress-strain curve observed in engineering testing.
6. Von Mises Criterion: Five Independent Systems for Polycrystalline Ductility
In a polycrystal, each grain is surrounded by neighbours with different orientations. Plastic deformation of one grain imposes a strain state on its neighbours. For the polycrystal to deform without internal cracking, each grain must be capable of accommodating an arbitrary imposed strain. An arbitrary homogeneous strain tensor has 5 independent components (the sixth is fixed by volume conservation). Therefore, a minimum of 5 independent slip systems must be available in each grain.
Independence is assessed by matrix rank: the 12 FCC slip systems, when expressed as strain tensors, have a maximum rank of 5 — the exact Von Mises minimum. BCC satisfies the criterion through the combination of {110}, {112}, and {123} systems. Pure HCP basal slip has a rank of only 2 — it cannot accommodate c-axis strains. Prismatic slip brings the rank to 4. Only pyramidal ⟨c+a⟩ slip provides the fifth independent component and brings rank to 5. The practical consequence is observed directly: wrought Ti-6Al-4V achieves elongations of 10–15% because pyramidal ⟨c+a⟩ slip operates; wrought pure magnesium at room temperature achieves only 5–8% because pyramidal CRSS is very high at room temperature, limiting effective independent systems to 4.
6.1 Taylor Factor and Polycrystal Yield Stress
The Taylor model extends Schmid’s Law to polycrystals. For a random crystallographic texture, the Taylor factor M relates the macroscopic yield stress to the single-crystal CRSS:
σ_y = M × τ_CRSS
where:
M = Taylor factor = 1 / ⟨m⟩_average (effective, accounting for constraints)
M ≈ 3.06 for random FCC polycrystal (Von Mises isotropic average)
M ≈ 2.75 for random BCC polycrystal
M ≈ 4.5–6.5 for random HCP polycrystal (when non-basal CRSS is high)
Texture shifts M significantly:
{111}⟨110⟩ gamma-fibre (deep-draw BCC steel) : M decreases in-plane
{001}⟨100⟩ cube texture (FCC Al sheet) : M ≈ 2.45 (strong anisotropy)
Basal fibre (Mg sheet, c∥ normal direction) : M increases for ND compression
Controlling texture through thermomechanical processing — recrystallisation annealing temperatures, rolling reductions, and cooling rates — is how manufacturers tailor the directionality of yield strength, r-value (plastic strain ratio), and formability limit in automotive sheet, beverage can stock (Al-Mg alloys), and electrical transformer silicon steel. The annealing and normalising article covers the recovery and recrystallisation mechanisms that determine final texture in processed sheet.
7. Engineering Implications: Slip Systems and Material Selection
7.1 Formability and Deep Drawing
The limiting draw ratio (LDR) in deep drawing — the maximum cup height achievable before tearing — scales directly with the number and symmetry of available slip systems. FCC metals with 12 equally accessible slip systems have LDR values of 2.1–2.8 (dependent on texture). BCC ferritic steels with the gamma-fibre texture achieve LDR up to 2.8–3.0 because the {111} planes (favoured by this texture) carry the least thickness strain in the drawing direction, maximising the r-value (r > 2). HCP metals are more restrictive — commercially pure titanium sheet can be deep-drawn but requires elevated temperature (150–200°C) to activate non-basal systems and prevent cracking at grain boundaries. Pure magnesium sheet must be rolled and deep-drawn above ~200°C for the same reason.
7.2 Cryogenic Service and DBTT
Selecting materials for cryogenic service (LNG at −162°C, liquid nitrogen at −196°C, liquid helium at −269°C) requires specifying FCC alloys with no DBTT. The standard material pairs are: FCC austenitic stainless steels (304L, 316L, 347) for pressure vessels and piping; FCC aluminium alloys (5083, 6061-T6) for cryogenic storage tanks; and FCC nickel-based alloys (Inconel 625, Invar) for extreme service. BCC ferritic steels are inadmissible below −40°C without Charpy qualification, per ASME Section VIII and EN 13445. For welded BCC structures, see the HAZ microstructure article — the coarse-grained HAZ of a BCC weld has the highest DBTT of any region in the weldment.
7.3 Work Hardening and Forming Limit
The work-hardening exponent n (from σ = Kεn) determines the necking resistance and forming limit of sheet metal. Low-SFE FCC metals (copper, austenitic stainless steel) with restricted cross-slip achieve n = 0.4–0.6 — dislocation accumulation in planar tangles produces sustained work hardening that delays localised necking. High-SFE FCC metals (aluminium) achieve n = 0.15–0.25 — cross-slip enables recovery, limiting hardening. BCC steels achieve n = 0.2–0.35, with grain boundary-locking from carbon/nitrogen interstitials producing Lüders band instability at yield (upper/lower yield point) that must be suppressed by temper rolling for automotive press applications. Understanding slip system character is therefore directly actionable in sheet metal process design.
For further context on how microstructure and composition interact with slip system activation, the articles on martensite formation, bainite microstructure, pearlite colony growth, and quenching and tempering of steel provide the transformation metallurgy context in which engineered slip-system behaviour is exploited.
Frequently Asked Questions
What determines which slip system activates first in a crystal?
Why does stacking fault energy affect work hardening rate?
How does texture affect yield strength in polycrystalline metals?
What is the Von Mises criterion and why does it matter for polycrystal ductility?
Why do BCC metals have a ductile-to-brittle transition temperature but FCC metals do not?
What slip systems operate in HCP titanium and why are they important?
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How does twinning supplement slip in HCP metals?
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