Infinite element method 1970-01-01
The Infinite Element Method (IEM) is a numerical analysis technique used to solve problems involving unbounded domains, particularly in engineering and physics. It extends the finite element method (FEM) by allowing for an effective treatment of problems where fields (such as electromagnetic, acoustic, or structural fields) can extend infinitely far from the region of interest. This approach is particularly useful for problems with infinite or semi-infinite domains, such as wave propagation, soil formation, and fluid dynamics.
Kirchhoff–Love plate theory 1970-01-01
Kirchhoff–Love plate theory is a mathematical framework used to analyze the behavior of thin, flat plates under various loading conditions. It is an extension of classical plate theory, developed by researchers such as Gustav Kirchhoff and Augustin-Louis Cauchy, among others. This theory is especially relevant in civil and mechanical engineering, as it provides insights into the deflections, stresses, and overall behavior of plate structures, which are common in beams, floors, roofs, and other structural elements.
Limit load (physics) 1970-01-01
In the context of physics and engineering, particularly in structural mechanics, **limit load** refers to the maximum load that a structure or component can carry without experiencing failure. This load is associated with the onset of plastic deformation, where the material will no longer return to its original shape upon unloading. The limit load is an important concept in the design and analysis of structures, as it helps engineers determine the safety and reliability of various materials and configurations under expected loads.
Mie–Grüneisen equation of state 1970-01-01
The Mie–Grüneisen equation of state is a thermodynamic relation used primarily to describe the behavior of materials under high pressure and high temperature conditions, especially in the context of shock physics and materials science. It combines elements of both the Mie equation of state, which describes the pressure-volume relationship in a material, and the Grüneisen parameter, which accounts for the effect of temperature on the material's response to pressure.
Mooney–Rivlin solid 1970-01-01
The Mooney–Rivlin solid is a mathematical model used to describe the mechanical behavior of hyperelastic materials, which are materials that can undergo large elastic deformations. Named after the contributions of Melvin Mooney and Ronald Rivlin, this model is particularly useful in the field of rubber-like materials and soft biological tissues, which can experience significant stretching and compressibility.
Murnaghan equation of state 1970-01-01
The Murnaghan equation of state is an equation that describes the relationship between pressure, volume, and temperature in materials, particularly in solid-state physics and materials science. It is particularly useful for modeling the behavior of solids under pressure, capturing how their volume changes with varying pressure conditions.
Objective stress rate 1970-01-01
The term "objective stress rate" can refer to different concepts depending on the context in which it is used, such as in psychology, economics, engineering, or other fields. Here are a couple of potential interpretations: 1. **Psychological Context**: In psychology, the objective stress rate could refer to quantifiable measures of stress experienced by individuals, which could be assessed through physiological indicators like heart rate, cortisol levels, or other measurable factors.
Ogden hyperelastic model 1970-01-01
The Ogden hyperelastic model is a mathematical framework used in the field of solid mechanics to describe the nonlinear elastic behavior of rubber-like materials and biological tissues. It is particularly useful for modeling materials that exhibit large deformations, which is often the case for elastomers and certain biological materials.
Orthotropic material 1970-01-01
Orthotropic materials are a specific type of anisotropic material that has unique mechanical properties in three mutually perpendicular directions. This means that their material properties (such as elasticity, strength, and thermal expansion) vary based on the direction in which they are measured. The term "orthotropic" typically applies to materials that exhibit different behaviors in three orthogonal principal material directions, which are usually referred to as the x, y, and z axes.
Plate theory 1970-01-01
Plate theory, often referred to as plate tectonics, is a scientific theory that explains the structure and movement of the Earth's lithosphere, which is the rigid outer layer of the Earth. This theory describes how the lithosphere is divided into several large and small plates that float on the semi-fluid asthenosphere beneath them. These tectonic plates are constantly moving, and their interactions at plate boundaries can lead to various geological phenomena, including earthquakes, volcanic activity, and the formation of mountain ranges.
Polynomial hyperelastic model 1970-01-01
The polynomial hyperelastic model is a type of constitutive model used in material science and solid mechanics to describe the mechanical behavior of hyperelastic materials. Hyperelastic materials are those that can undergo large elastic deformations, such as rubber and biological tissues, and they can return to their original shape after the removal of applied loads.
Proper orthogonal decomposition 1970-01-01
Proper Orthogonal Decomposition (POD) is a mathematical technique primarily used in the field of applied mathematics, engineering, and data analysis for reducing the dimensionality of a dataset. It is often employed in fluid dynamics, control theory, and more generally in problems involving complex systems where simplification is beneficial for analysis and computation.
Representative elementary volume 1970-01-01
The Representative Elementary Volume (REV) is a concept used primarily in the fields of materials science, geophysics, and hydrology. It refers to the smallest volume over which measurements can be taken so that the average properties of the material or medium are representative of the whole sample. The concept is crucial for understanding the macroscopic behavior of heterogeneous materials, such as soils, rocks, and composite materials.
Reversibly assembled cellular composite materials 1970-01-01
Reversibly assembled cellular composite materials refer to a class of materials that can be assembled and disassembled through reversible processes, often leveraging non-covalent interactions or physical forces rather than enduring chemical bonds. These materials combine the structural features of cellular architectures, which can provide enhanced mechanical properties, lightweight characteristics, and other desirable attributes, with the ability to be reconfigured or recycled without loss of functionality.
Rheometry 1970-01-01
Rheometry is the study of the flow and deformation of materials, primarily focusing on their rheological properties. It involves the measurement of how substances respond to applied stress or strain, which helps in understanding their viscous (flow) and elastic (deformation) behavior. Rheometry is crucial in various fields such as material science, pharmaceuticals, food science, and polymer science, where the flow properties of materials can significantly impact processing and product performance.
Shakedown (continuum mechanics) 1970-01-01
In continuum mechanics, the term "shakedown" refers to a phenomenon where a structure subjected to repeated or cyclic loading stabilizes after a certain number of load cycles. Initially, when a structure is subjected to cyclic loading which exceeds its elastic limits, it may experience plastic deformations. However, after some cycles, the material may reach a state where it can endure the imposed loads without further plastic deformation.
Shear rate 1970-01-01
Shear rate is a measure of the rate at which one layer of a fluid moves in relation to another layer. It is a critical concept in fluid dynamics and rheology, particularly for non-Newtonian fluids, where the viscosity (resistance to flow) can vary with shear rate. Mathematically, shear rate (\( \dot{\gamma} \)) is defined as the change in velocity (speed) of a fluid layer divided by the distance between the layers.
Shear stress 1970-01-01
Shearing (physics) 1970-01-01
Shearing, in physics, refers to a type of deformation that occurs when a force is applied parallel to a surface or plane within a material. This results in the material layers sliding past one another, which alters their shape without necessarily changing their volume. Shearing is a crucial concept in mechanics and materials science, as it helps to explain how materials deform under different types of load.
Simple shear 1970-01-01
Simple shear is a type of deformation that occurs in materials when they are subjected to shear stress. In this mode of deformation, layers of material slide past each other while the overall volume remains constant. It is characterized by the parallel displacement of adjacent layers, which results in an angular distortion of the material. In a simple shear scenario, one side of an object is moved in one direction while the opposite side is held in place or moved in the opposite direction, creating a shear strain.