Brittleness - Definition of Brittleness

In materials science, brittleness is understood as the lack of ductility. Understanding the difference between brittle and ductile material is highly important for engineers. Some fractures (e.g., brittle fractures) occur under specific conditions without warning and can cause major damage to materials. The brittle fracture occurs suddenly and catastrophically without any warning, resulting in spontaneous and rapid crack propagation. Studying fracture mechanics may assist in understanding how fracture occurs in materials.

In the tensile test, the fracture point is the point of strain where the material physically separates. At this point, the strain reaches its maximum value, and the material fractures, even though the corresponding stress may be less than the ultimate strength at this point. Ductile materials have a fracture strength lower than the ultimate tensile strength (UTS), whereas, in brittle materials, the fracture strength is equivalent to the UTS. If a ductile material reaches its ultimate tensile strength in a load-controlled situation, it will continue to deform, with no additional load application, until it ruptures. However, if the loading is displacement-controlled, the deformation of the material may relieve the load, preventing rupture. It is possible to distinguish some common characteristics among the stress-strain curves of various groups of materials.

Fracture of Material

$fracture$ A fracture is the separation of an object or material into two or more pieces under the action of stress. Engineers need to understand fracture mechanisms. Some fractures (e.g., brittle fractures) occur under specific conditions without warning and can cause major damage to materials. The brittle fracture occurs suddenly and catastrophically without any warning, resulting in spontaneous and rapid crack propagation. However, for ductile fracture, the presence of plastic deformation warns that failure is imminent, allowing preventive measures to be taken. Studying fracture mechanics may assist in understanding how fracture occurs in materials.

In the tensile test, the fracture point is the point of strain where the material physically separates. At this point, the strain reaches its maximum value, and the material fractures, even though the corresponding stress may be less than the ultimate strength at this point. Ductile materials have a fracture strength lower than the ultimate tensile strength (UTS), whereas, in brittle materials, the fracture strength is equivalent to the UTS. If a ductile material reaches its ultimate tensile strength in a load-controlled situation, it will continue to deform, with no additional load application, until it ruptures. However, if the loading is displacement-controlled, the deformation of the material may relieve the load, preventing rupture. It is possible to distinguish some common characteristics among the stress-strain curves of various groups of materials. On this basis, it is possible to divide materials into two broad categories; namely:

Ductile Materials. Ductility is the ability of a material to be elongated in tension. Ductile material will deform (elongate) more than brittle material. Ductile materials show large deformation before fracture. In ductile fracture, extensive plastic deformation (necking) takes place before fracture. Ductile fracture (shear fracture) is better than brittle fracture because there is slow propagation and an absorption of a large amount of energy before fracture. Any fracture process involves two steps, crack formation and propagation, in response to an imposed stress. The mode of fracture is highly dependent on the mechanism of crack propagation. Cracks in ductile materials are said to be stable (i.e., resist extension without an increase in applied stress). For brittle materials, cracks are unstable. That means crack propagation, once started, continues spontaneously without an increase in stress level. Ductility is desirable in the high temperature and high-pressure applications in reactor plants because of the added stresses on the metals. High ductility in these applications helps prevent brittle fracture.
$brittle fracture$ Brittle Materials. When subjected to stress, brittle materials break with little elastic deformation and without significant plastic deformation. Brittle materials absorb relatively little energy before fracture, even high-strength materials. In brittle fracture (transgranular cleavage), no apparent plastic deformation takes place before fracture. In crystallography, cleavage is the tendency of crystalline materials to split along definite crystallographic structural planes. Any fracture process involves two steps, crack formation and propagation, in response to an imposed stress. The mode of fracture is highly dependent on the mechanism of crack propagation. For brittle materials, cracks are unstable. That means crack propagation, once started, continues spontaneously without an increase in stress level. Cracks propagate rapidly (speed of sound) and occur at high speeds – up to 2133.6 m/s in steel. It should be noted that smaller grain sizes, higher temperatures, and lower stress tend to mitigate crack initiation. Larger grain sizes, lower temperatures, and higher stress favor crack propagation. A stress level below which a crack will not propagate at any temperature. This is called the lower fracture propagation stress. For brittle fracture, the fracture surface is relatively flat and perpendicular to the direction of the applied tensile load. In general, a brittle fracture requires three conditions:
- Flaw such as a crack
- Stress is sufficient to develop a small deformation at the crack tip
- The temperature at or below DBTT

Ductile–brittle Transition Temperature

Liberty Ship - Hull Failure — Brittle fracture of the U.S. Liberty Ship Esso Manhattan

As was written, the distinction between brittleness and ductility isn’t readily apparent, especially because both ductility and brittle behavior are dependent not only on the material in question but also on the temperature (ductile-brittle transition) of the material. The effect of temperature on the nature of the fracture is of considerable importance, and many steels exhibit ductile fracture at elevated temperatures and brittle fracture at low temperatures. The temperature above which material is ductile and below which it is brittle is known as the ductile-brittle transition temperature (DBTT), nil ductility temperature (NDT), or nil ductility transition temperature. This temperature is not precise but varies according to prior mechanical and heat treatment and the nature and amounts of impurity elements. It can be determined by some drop-weight tests (for example, the Charpy or Izod tests).

The ductile-brittle transition temperature (DBTT) is the temperature at which the fracture energy passes below a predetermined value (e.g., 40 J for a standard Charpy impact test). Ductility is an essential requirement for steels used in constructing reactor components, such as the reactor vessel. Therefore, the DBTT is of significance in the operation of these vessels. In this case, the grain’s size determines the metal’s properties. For example, smaller grain size increases tensile strength, tends to increase ductility, and decreases DBTT. Grain size is controlled by heat treatment in the specifications and manufacturing of reactor vessels. The DBTT can also be lowered by small additions of selected alloying elements such as nickel and manganese to low-carbon steels.

Typically, the low alloy reactor pressure vessel steels are ferritic steels that exhibit the classic ductile-to-brittle transition behavior with decreasing temperature. This transitional temperature is of the highest importance during plant heat-up.

Failure modes:

Low toughness region: Main failure mode is the brittle fracture (transgranular cleavage). In brittle fracture, no apparent plastic deformation takes place before fracture. Cracks propagate rapidly.
High toughness region: Main failure mode is the ductile fracture (shear fracture). In ductile fracture, extensive plastic deformation (necking) takes place before fracture. Ductile fracture is better than brittle fracture because there is slow propagation and an absorption of a large amount of energy before fracture.

In some materials, the transition is sharper and typically requires a temperature-sensitive deformation mechanism. For example, in materials with a body-centered cubic (bcc) lattice, the DBTT is readily apparent, as the motion of screw dislocations is very temperature sensitive because the rearrangement of the dislocation core before slip requires thermal activation. This can be problematic for steels with a high ferrite content. This famously resulted in serious hull cracking in Liberty ships in colder waters during World War II, causing many sinkings. The vessels were constructed of a steel alloy with adequate toughness according to room-temperature tensile tests. The brittle fractures occurred at relatively low ambient temperatures, at about 4°C (40°F), in the vicinity of the transition temperature of the alloy. It must be noted that low-strength FCC metals (e.g., copper alloys) and most HCP metals do not experience a ductile-to-brittle transition and retain tough also for lower temperatures. On the other hand, many high-strength metals (e.g., very high-strength steels) also do not experience a ductile-to-brittle transition, but, in this case, they remain very brittle.

DBTT can also be influenced by external factors such as neutron radiation, which leads to an increase in internal lattice defects, a corresponding decrease in ductility, and an increase in DBTT.

Irradiation Embrittlement

During the operation of a nuclear power plant, the material of the reactor pressure vessel and the material of other reactor internals are exposed to neutron radiation (especially to fast neutrons >0.5MeV), which results in localized embrittlement of the steel and welds in the area of the reactor core. This phenomenon, known as irradiation embrittlement, results in a steady increase in DBTT. It is not likely that the DBTT will approach the normal operating temperature of the steel. However, there is a possibility that when the reactor is being shut down or during an abnormal cooldown, the temperature may fall below the DBTT value. At the same time, the internal pressure is still high. Therefore nuclear regulators require that a reactor vessel material surveillance program be conducted in water-cooled power reactors.

Stress Corrosion Cracking

One of the most serious metallurgical problems and one that is a major concern in the nuclear industry is stress-corrosion cracking (SCC). Stress-corrosion cracking results from applied tensile stress and a corrosive environment combined. Both influences are necessary. SCC is a type of intergranular attack corrosion that occurs at the grain boundaries under tensile stress. It tends to propagate as stress opens cracks subject to corrosion, which are then corroded further, weakening the metal by further cracking. The cracks can follow intergranular or transgranular paths, and there is often a tendency for crack branching. Failure behavior is characteristic of a brittle material, even though the metal alloy is intrinsically ductile. SCC can lead to unexpected sudden failure of normally ductile metal alloys subjected to tensile stress, especially at elevated temperatures. SCC is highly chemically specific in that certain alloys are likely to undergo SCC only when exposed to a small number of chemical environments.

The most effective means of preventing SCC in reactor systems are:

designing properly
reducing stress
removing critical environmental species such as hydroxides, chlorides, and oxygen
avoiding stagnant areas and crevices in heat exchangers where chloride and hydroxide might become concentrated.

Stress-corrosion cracking may cause, for example, a failure of nuclear fuel rods after inappropriate power changes, rod movement, and plant startup. Certain austenitic stainless steels and aluminium alloys crack in the presence of chlorides, and mild steel cracks in the presence of alkali (boiler cracking). Low alloy steels are less susceptible than high alloy steels but are subject to SCC in water containing chloride ions. Nickel-based alloys, however, are not affected by chloride or hydroxide ions. An example of a nickel-based alloy resistant to stress-corrosion cracking is Inconel.

Special Reference: U.S. Department of Energy, Material Science. DOE Fundamentals Handbook, Volume 1 and 2. January 1993.

Stress-corrosion Cracking as Fuel Failure Mechanism

Cladding prevents radioactive fission products from escaping the fuel matrix into the reactor coolant and contaminating it. Various fuel failure root causes have been identified in the past. IThesecauses were predominantly fabrication defects or fretting in the early days of PWR and BWR operations. One possible cause is the pellet-cladding interaction (PCI), which may be caused by stress-corrosion cracking. Stress-corrosion cracking may cause, for example, a failure of nuclear fuel rods after inappropriate power changes, rod movement, and plant startup.

In nominal operating conditions, pellet temperature stands at about 1,000° C at the center and 400–500° C at the periphery. If there is a major increase in power, the temperature at the pellet center rises steeply (> 1,500° C, or even > 2,000° C). In this case, a difference in thermal expansions between fuel cladding and fuel pellets causes an increase in stress in the fuel cladding. PCI fuel failure is caused by stress-corrosion cracking on the inside surface of the cladding, which results from the combined effects of fuel pellet expansion (especially at pellet radial cracks and the presence of an aggressive fission product environment (especially gaseous iodine). Such a failure occurs experimentally after a few minutes of holding time at sustained high power levels.

Special Reference: CEA, Nuclear Energy Division. Nuclear Fuels, ISBN 978-2-281-11345-7

Hydrogen Embrittlement

Hydrogen embrittlement is one of many forms of stress-corrosion cracking. Hydrogen embrittlement results from the combined action of applied tensile stress and a corrosive hydrogen environment. Both influences are necessary. In this case, the corrosive agent is hydrogen in its atomic form (H as opposed to the molecular form, H₂), which diffuses interstitially through the crystal lattice, and concentrations as low as several parts per million can lead to cracking. Although embrittlement of materials takes many forms, hydrogen embrittlement in high-strength steels has the most devastating effect because of the catastrophic nature of the fractures when they occur. Hydrogen embrittlement is the process by which steel loses its ductility and strength due to tiny cracks that result from the internal pressure of hydrogen (H₂), which forms at the grain boundaries. In the case of steel, hydrogen diffuses along the grain boundaries and combines with the carbon to form methane gas. The methane gas collects in small voids along the grain boundaries, where it builds up enormous pressures that initiate cracks and decrease the ductility of the steel. A brittle fracture can occur if the metal is under high tensile stress.

It is a complex process that is not completely understood because of the variety and complexity of mechanisms that can lead to embrittlement. Many mechanisms have been proposed to explain hydrogen embrittlement. Mechanisms proposed to explain embrittlement include the formation of brittle hydrides and creating voids that can lead to bubbles and pressure build-up within a material. Hydrogen is introduced to the surface of a metal, and individual hydrogen atoms diffuse through the metal structure. Because the solubility of hydrogen increases at higher temperatures, raising the temperature can increase the diffusion of hydrogen.

For hydrogen embrittlement to occur, a combination of three conditions is required:

the presence and diffusion of hydrogen
a susceptible material
stress

In zirconium alloys, hydrogen embrittlement is caused by zirconium hydriding. At nuclear reactor facilities, the term “hydrogen embrittlement” generally refers to the embrittlement of zirconium alloys caused by zirconium hydriding.

Special Reference: U.S. Department of Energy, Material Science. DOE Fundamentals Handbook, Volume 1 and 2. January 1993.

Hydrogen Embrittlement of Zirconium Alloys

Internal Hydriding. Inadvertent inclusion of hydrogen-containing materials inside a fuel rod can result in hydriding and thus embrittlement fuel cladding. Hydrogen sources were mainly residual moisture or organic contamination in fuel pellets/rods. This cause of failure has been practically eliminated through improved manufacturing.
Delayed hydride cracking (DHC). Delayed hydride cracking is time-dependent crack initiation and propagation through fracture of hydrides that can form ahead of the crack tip. This type of failure can be initiated by long cracks at the outer surface of the cladding, which can propagate in an axial/radial direction. This failure mechanism may potentially limit high burnup operation.

The aggressive agent in this respect is primary circuit water, at a temperature of some 300° C. This oxidizes zirconium according to the reaction:

Zr + 2H₂O→ZrO₂ + 2H₂

resulting in the formation of solid oxide on the metal’s surface.

Part of the hydrogen produced by the corrosion of zirconium in water combines with the zirconium to form a separate phase of zirconium hydride (ZrH1.5) platelets. Hydrogen migrates under the effect of the thermal gradient to accumulate in the less hot regions, forming hydrides that are liable to cause brittleness in the cladding as the fuel cools down. The metal then becomes embrittled (ductility decreases) and fractures easily. Cracks begin to form in the zirconium hydride platelets and are propagated through the metal.

Hydrogen embrittlement is also very important for high-temperature steam oxidation of zirconium alloys.

References:

Materials Science:

U.S. Department of Energy, Material Science. DOE Fundamentals Handbook, Volume 1 and 2. January 1993.
U.S. Department of Energy, Material Science. DOE Fundamentals Handbook, Volume 2 and 2. January 1993.
William D. Callister, David G. Rethwisch. Materials Science and Engineering: An Introduction 9th Edition, Wiley; 9 edition (December 4, 2013), ISBN-13: 978-1118324578.
Eberhart, Mark (2003). Why Things Break: Understanding the World by the Way It Comes Apart. Harmony. ISBN 978-1-4000-4760-4.
Gaskell, David R. (1995). Introduction to the Thermodynamics of Materials (4th ed.). Taylor and Francis Publishing. ISBN 978-1-56032-992-3.
González-Viñas, W. & Mancini, H.L. (2004). An Introduction to Materials Science. Princeton University Press. ISBN 978-0-691-07097-1.
Ashby, Michael; Hugh Shercliff; David Cebon (2007). Materials: engineering, science, processing, and design (1st ed.). Butterworth-Heinemann. ISBN 978-0-7506-8391-3.
J. R. Lamarsh, A. J. Baratta, Introduction to Nuclear Engineering, 3d ed., Prentice-Hall, 2001, ISBN: 0-201-82498-1.

See above:

Material Properties