Martensite is considered a non-equilibrium phase because it forms rapidly during the quenching process, bypassing the slow diffusion-based transformations typical of equilibrium phases. Its formation involves a shear mechanism that occurs at low temperatures, resulting in a unique crystal structure that does not correspond to the equilibrium phase diagram. This rapid transformation does not allow for the atomic rearrangements required for equilibrium, leading to its metastable nature. Consequently, martensite possesses distinct mechanical properties compared to equilibrium phases like pearlite or bainite.
Martensite transformation begins when austenite is cooled below a certain critical temperature, called the matrensite start temperature. As we go below the tmartensite start temperature, more and more martensite forms and complete transformation occurs only at a temperature called martensire finish temp. Formation of martensite require that the austenite phase must be cooled rapidly.
hardness of martensite is greater than bionite and fine pearlite.
Lath martensite and plate martensite are two morphologies of martensite formed during the rapid cooling of austenitic steel. Lath martensite appears as thin, elongated plates or laths and is typically found in low-carbon steels, resulting in a more ductile microstructure. In contrast, plate martensite consists of thicker, broader plates and is generally found in high-carbon steels, leading to higher hardness and brittleness. The differences in their formation and structure influence the mechanical properties of the steel they comprise.
It is the state at which all the three phases i.e.,solid phase,liquid phase and vapor phase are in equilibrium.
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The martenite phase does not appear on the iron-iron carbide (Fe-Fe3C) phase diagram because it is a metastable phase that forms during rapid cooling of austenite rather than being a stable equilibrium phase. The Fe-Fe3C diagram primarily represents stable phases and their transformations at equilibrium conditions, while martensite results from non-equilibrium conditions, such as quenching. Therefore, its formation and characteristics are not depicted in this equilibrium phase diagram.
Martensite transformation begins when austenite is cooled below a certain critical temperature, called the matrensite start temperature. As we go below the tmartensite start temperature, more and more martensite forms and complete transformation occurs only at a temperature called martensire finish temp. Formation of martensite require that the austenite phase must be cooled rapidly.
Because Martensite transformation is almost instantaneous, the Martensite has the identical composition of the parent phase. Formation of Martensite involves a transformation from a body-centered cubic structure to body-centered tetragonal structure. The large increase in volume that results creates a highly stressed structure.
Martensite
False. An equilibrium in which all the components are in the same phase (solid, liquid, or gas) is called a homogeneous equilibrium.
A phase diagram of the equilibrium relationship between temperature, pressure, and composition in any system.
On a phase diagram, the conditions of pressure and temperature at which two phases coexist in equilibrium are represented by a line. This line is called the phase boundary or phase equilibrium line. It separates the regions where the two phases exist in equilibrium from the region where only one phase is present.
For the condition of phase equilibrium the free energy is a minimum, the system is completely stable meaning that over time the phase characteristics are constant. For metastability, the system is not at equilibrium, and there are very slight (and often imperceptible) changes of the phase characteristics with time.
hardness of martensite is greater than bionite and fine pearlite.
A heterogeneous equilibrium refers to a chemical equilibrium in a system that contains multiple phases, such as a solid, liquid, and gas phase. In these systems, the concentrations of reactants and products in each phase are related according to the equilibrium constant.
For two reasons: 1. martensite is bct structure which prevent the movement of dislocations. 2. martensite has higher carbon concentraton.
John Ettore Ricci has written: 'The phase rule and heterogeneous equilibrium' -- subject(s): Phase rule and equilibrium