Engineering Physics of High-Temperature Materials. Nirmal K. Sinha. Читать онлайн. Newlib. NEWLIB.NET

Автор: Nirmal K. Sinha
Издательство: John Wiley & Sons Limited
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Жанр произведения: Техническая литература
Год издания: 0
isbn: 9781119420460
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      Dislocations generally require proper lattice ordering to move through a material at low energy. Barriers to the motion of dislocations can be created by the presence of other defects in the crystal, such as point defects, grain boundaries, other dislocations, and the precipitation of a secondary phase. In particular, precipitates can act as locations through which the dislocation might become pinned or must bend in order to continue moving. Bending around precipitates can often lead to the formation of dislocation loops formed around precipitates.

      2.3.3.3 Planar Defects

      There are a variety of planar defects that can occur within crystals. Many of these are due to dislocation and the slip of atomic planes. A common imperfection is a result of stacking faults – a deviation of the stacking sequence of layers in a crystal, often due to a missing or added layer. Stacking faults occur in a number of crystal structures, but the common example is that in close‐packed structures. For example, the ABCABCABC sequence of an FCC crystal could be disrupted by a missing C‐layer giving an ABCABABCABC structure.

      Another type of planar defect is the twin boundary. This defect introduces a plane of mirror symmetry. For example, in the FCC structure, stacking sequence of a twin boundary would be ABCAB‐C‐BACBA.

      A third type of planar defect is called the antiphase boundary. This defect occurs in ordered alloys where the crystallographic direction remains the same, but each side of the boundary has an opposite phase. For example, for the HCP crystal ABABABAB, an antiphase boundary takes the form of ABABBABA.

      2.3.3.4 Intragranular Precipitates

      Precipitates in a material are generally impurity phases that segregate during the solidification process. Precipitation can produce many different sizes of particles and can have vastly different impacts on material properties. Intergranular precipitates segregate into grain boundaries and take up volume between grains whereas intragranular precipitates are contained within grains and disrupt the crystal structure.

      Trinity of Precipitate Classification

      GEOMETRICALLY CLOSE‐PACKED

      TOPOLOGICALLY CLOSE‐PACKED

      CARBIDE

      The process of precipitation hardening relies on changes in a material's solid solubility with temperature to produce fine particles of an impurity phase within grain interiors, which impede the movement of dislocations. During precipitation hardening, alloys must be kept at elevated temperature for a significant amount of time, called aging, for precipitation to take place. However, not all precipitates are created equal, and engineers must be careful to design the system and processes to produce the desired precipitates. There are three general classifications for precipitates: (i) Geometrically close‐packed (GCP) precipitates are phases that are close‐packed in all directions and generally provide positive influences on mechanical properties. (ii) Topologically close‐packed (TCP) precipitates are not close‐packed throughout the whole structure. They often have close‐packed layers separated by relatively large interatomic distances due to sandwiching larger atoms (Bowman 2000). With fewer available slip planes, these precipitates tend to have brittle behavior. Moreover, nonideal TCP phases can grow at the expense of desired GCP phases and result in a depletion zone of the desired participate phase (Belan 2016). (iii) Carbide precipitates can have quite different phase structures than their surroundings and can have extremely important impacts – both desired and undesired – on properties.

      2.3.3.5 Boundary Defects

      Solid materials are rarely made of pure single crystals. Different grains in polycrystalline material can be recognized by a mismatch in atomic alignment between regions in the solid. The grain boundaries are, in themselves, a source of great imperfection within a solid.

      Small mismatches (less than 10–15° depending on the material) are called low‐angle grain boundaries or more commonly “subgrain boundaries.” Subgrain boundaries include “tilt” and “twist” boundaries and contain dislocations of various types. The energy of subgrain boundaries depends upon the degree of misorientation and types of dislocations.

      High‐angle grain boundaries – or simply grain boundaries – separate regions with high mismatch in lattice arrangement. Grain boundaries are disordered regions associated with high energy. The disorder of grain boundaries is a result of not only lattice mismatch of adjacent grains, but also the segregation of various impurities and voids into the edge of the grains. Grain boundaries tend to have lower density and higher reactivity than the grains themselves. They can also act as conduits or pathways for various processes, such as corrosion, into the bulk.

      Grain boundaries are an extremely important influence in a variety of material properties and processes, including yield and tensile strength, elongation, and formability. Often, GB effects are expressed as a variation of the property with grain size. In fact, the impact of grain size (and thus GB area), grain boundary chemistry, and grain boundary morphology are all important parameters. Many of these effects will be discussed throughout the text.

      2.3.3.6 Bulk or Volume Defects

      Bulk defects are larger‐scale defects in the solid and can often be viewed even with the naked eye. Bulk defects include (i) inclusions – generally unwanted second‐phase particles; (ii) cracks and microcracks – regions where the material has discontinuities or fractures; and (iii) pores – voids present in the material often as a result of volume change resulting from phase changes. As might be expected, bulk defects can have a significant impact on optical, thermal, and mechanical properties of a material.

      Naturally occurring flint is a form of silica or silicon dioxide (SiO2), like sand or quartz. Arrowheads were often made during the Stone Age by fracturing flint stones. Chemically, flint is related to common soda‐lime window glasses composed of more than 70% silica. Thus, glass is one of the oldest man‐made materials that found widespread use since the Stone Age. Today, the skyline of big cities around the world is highlighted with towering glass‐clad skyscrapers.

      Freshly drawn glass fibers are stronger