Intergranular fracture

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In fracture mechanics, intergranular fracture, intergranular cracking or intergranular embrittlement occurs when a crack propagates along the grain boundaries of a material, usually when these grain boundaries are weakened. [1] The more commonly seen transgranular fracture occurs when the crack grows through the material grains. As an analogy, in a wall of bricks, intergranular fracture would correspond to a fracture that takes place in the mortar that keeps the bricks together.

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Intergranular cracking is likely to occur if there is a hostile environmental influence and is favored by larger grain sizes and higher stresses. [1] Intergranular cracking is possible over a wide range of temperatures. [2] While transgranular cracking is favored by strain localization (which in turn is encouraged by smaller grain sizes), intergranular fracture is promoted by strain homogenization resulting from coarse grains. [3]

Intergranular fracture produced by crack propagation along grain boundaries Intergranular Fracture.svg
Intergranular fracture produced by crack propagation along grain boundaries

Embrittlement, or loss of ductility, is often accompanied by a change in fracture mode from transgranular to intergranular fracture. [4] This transition is particularly significant in the mechanism of impurity-atom embrittlement. [4] Additionally, hydrogen embrittlement is a common category of embrittlement in which intergranular fracture can be observed. [5]

Intergranular fracture can occur in a wide variety of materials, including steel alloys, copper alloys, aluminum alloys, and ceramics. [6] [7] [3] In metals with multiple lattice orientations, when one lattice ends and another begins, the fracture changes direction to follow the new grain. This results in a fairly jagged looking fracture with straight edges of the grain and a shiny surface may be seen. In ceramics, intergranular fractures propagate through grain boundaries, producing smooth bumpy surfaces where grains can be easily identified.

Mechanisms of intergranular fracture

Though it is easy to identify intergranular cracking, pinpointing the cause is more complex as the mechanisms are more varied, compared to transgranular fracture. [6] There are several other processes that can lead to intergranular fracture or preferential crack propagation at the grain boundaries: [8] [6]

From an energy standpoint, the energy released by intergranular crack propagation is higher than that predicted by Griffith theory, implying that the additional energy term to propagate a crack comes from a grain-boundary mechanism. [9]

Types of intergranular fracture

Intergranular fracture can be categorized into the following: [6]

Role of solutes and impurities

At room temperature, intergranular fracture is commonly associated with altered cohesion resulting from segregation of solutes or impurities at the grain boundaries. [10] Examples of solutes known to influence intergranular fracture are sulfur, phosphorus, arsenic, and antimony specifically in steels, lead in aluminum alloys, and hydrogen in numerous structural alloys. [10] At high impurity levels, especially in the case of hydrogen embrittlement, the likelihood of intergranular fracture is greater. [6] Solutes like hydrogen are hypothesized to stabilize and increase the density of strain-induced vacancies, [11] leading to microcracks and microvoids at grain boundaries. [5]

Role of grain boundary orientation

Intergranular cracking is dependent on the relative orientation of the common boundary between two grains. The path of intergranular fracture typically occurs along the highest-angle grain boundary. [6] In a study, it was shown that cracking was never exhibited for boundaries with misorientation of up to 20 degrees, regardless of boundary type. [12] At greater angles, large areas of cracked, uncracked, and mixed behavior were seen. The results imply that the degree of grain boundary cracking, and hence intergranular fracture, is largely determined by boundary porosity, or the amount of atomic misfit. [12]

See also

Related Research Articles

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Ductility refers to the ability of a material to sustain significant plastic deformation before fracture. Plastic deformation is the permanent distortion of a material under applied stress, as opposed to elastic deformation, which is reversible upon removing the stress. Ductility is a critical mechanical performance indicator, particularly in applications that require materials to bend, stretch, or deform in other ways without breaking. The extent of ductility can be quantitatively assessed using the percent elongation at break, given by the equation:

<span class="mw-page-title-main">Fracture</span> Split of materials or structures under stress

Fracture is the appearance of a crack or complete separation of an object or material into two or more pieces under the action of stress. The fracture of a solid usually occurs due to the development of certain displacement discontinuity surfaces within the solid. If a displacement develops perpendicular to the surface, it is called a normal tensile crack or simply a crack; if a displacement develops tangentially, it is called a shear crack, slip band, or dislocation.

<span class="mw-page-title-main">Hydrogen embrittlement</span> Reduction in ductility of a metal exposed to hydrogen

Hydrogen embrittlement (HE), also known as hydrogen-assisted cracking or hydrogen-induced cracking (HIC), is a reduction in the ductility of a metal due to absorbed hydrogen. Hydrogen atoms are small and can permeate solid metals. Once absorbed, hydrogen lowers the stress required for cracks in the metal to initiate and propagate, resulting in embrittlement. Hydrogen embrittlement occurs in steels, as well as in iron, nickel, titanium, cobalt, and their alloys. Copper, aluminium, and stainless steels are less susceptible to hydrogen embrittlement.

<span class="mw-page-title-main">Tempering (metallurgy)</span> Process of heat treating used to increase the toughness of iron-based alloys

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<span class="mw-page-title-main">Transgranular fracture</span>

Transgranular fracture is a type of fracture that occurs through the crystal grains of a material. In contrast to intergranular fractures, which occur when a fracture follows the grain boundaries, this type of fracture traverses the material's microstructure directly through individual grains. This type of fracture typically results from a combination of high stresses and material defects, such as voids or inclusions, that create a path for crack propagation through the grains. A broad range of ductile or brittle materials, including metals, ceramics, and polymers, can experience transgranular fracture. When examined under scanning electron microscopy, this type of fracture reveals cleavage steps, river patterns, feather markings, dimples, and tongues. The fracture may change directions somewhat when entering a new grain in order to follow the new lattice orientation of that grain but this is a less severe direction change then would be required to follow the grain boundary. This results in a fairly smooth looking fracture with fewer sharp edges than one that follows the grain boundaries. This can be visualized as a jigsaw puzzle cut from a single sheet of wood with the wood grain showing. A transgranular fracture follows the grains in the wood, not the jigsaw edges of the puzzle pieces. This is in contrast to an intergranular fracture which, in this analogy, would follow the jigsaw edges, not the wood grain.

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<span class="mw-page-title-main">Microvoid coalescence</span>

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<span class="mw-page-title-main">Striation (fatigue)</span>

Striations are marks produced on the fracture surface that show the incremental growth of a fatigue crack. A striation marks the position of the crack tip at the time it was made. The term striation generally refers to ductile striations which are rounded bands on the fracture surface separated by depressions or fissures and can have the same appearance on both sides of the mating surfaces of the fatigue crack. Although some research has suggested that many loading cycles are required to form a single striation, it is now generally thought that each striation is the result of a single loading cycle.

<span class="mw-page-title-main">475 °C embrittlement</span> Loss of plasticity in ferritic stainless steel

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<span class="mw-page-title-main">Precipitate-free zone</span> Region around a material grain boundary free of solid impurities

In materials science, a precipitate-free zone (PFZ) refers to microscopic localized regions around grain boundaries that are free of precipitates. It is a common phenomenon that arises in polycrystalline materials where heterogeneous nucleation of precipitates is the dominant nucleation mechanism. This is because grain boundaries are high-energy surfaces that act as sinks for vacancies, causing regions adjacent to a grain boundary to be devoid of vacancies. As it is energetically favorable for heterogeneous nucleation to occur preferentially around defect-rich sites such as vacancies, nucleation of precipitates is impeded in the vacancy-free regions immediately adjacent to grain boundaries

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