
The Orowan mechanism is a dislocation behavior in materials science in which dislocations bypass obstacles they cannot cut through—namely, hard or non-shearable second-phase particles—by looping around them and continuing their path. This mechanism is named after Hungarian metallurgist Egon Orowan, who in the 1930s published seminal work explaining the presence of dislocations in crystals and their role in strengthening. The Orowan mechanism is one of the fundamental strengthening mechanisms tha
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CeCeramics are materials that are inorganic and typically have a crystalline structure, processed at high temperatures, and are hard, brittle, and heat-resistant. They are generally electrically insulating. They are one of the four main material groups in materials science. Ceramics stand out due to their structural strength, thermal and wear resistance, and chemical stability. They are used in both high-temperature applications and traditional applications. In materials engineering, the mechanica
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Emircan Şahin

Martensite is a very hard microstructural component formed in iron-carbon alloys (particularly steels) through a diffusionless phase transformation.Formation MechanismThe martensitic phase forms when steel is cooled extremely rapidly—for example, by quenching in water. Under normal slow cooling conditions, carbon atoms in the austenite structure diffuse out and form iron carbide (Fe₃C, or cementite). However, when cooling is too rapid, the carbon atoms cannot move and become “trapped” in place.
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The Hall–Petch relationship is a fundamental principle in materials science and metallurgy that describes an inverse correlation between grain size and mechanical strength. This relationship states that as the average crystal grain size of a material decreases, its yield strength (or hardness) increases. This phenomenon was independently discovered in the early 1950s by E. O. Hall and N. J. Petch through separate investigations and is named after these two scientists. Hall (1951) established the
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