Materials And States Of Matter Codexery

Stress (mechanics)

Physical quantity describing internal forces during material deformation.

Stress (mechanics)

Stress (mechanics) is a physical quantity in continuum mechanics that describes forces present during deformation of a material. It expresses the internal forces that neighboring particles of a continuous material exert on each other, with dimension of force per area and SI units of pascals (Pa). For example, a stretched elastic band experiences tensile stress and may elongate, while a crumpled sponge undergoes compressive stress and shortens. Stress increases with greater force and smaller cross-sectional area. Strain, by contrast, measures relative deformation. In solids, deformation generates an internal elastic stress that tends to restore the original shape, analogous to a spring’s reaction. In liquids and gases, only volume-changing deformations produce persistent elastic stress; gradual changes may also create viscous stress opposing the change. Significant stress can exist even without deformation, as in prestressed concrete or tempered glass. Stress may arise without external forces, from temperature changes, chemical composition shifts, or electromagnetic fields (e.g., in piezoelectric materials). The relationship between stress, strain, and strain rate can be complex, but a linear approximation often suffices for small quantities. Stress exceeding a material’s strength limits can cause permanent deformation, such as plastic flow, fracture, or cavitation. Historically, humans understood stress intuitively for millennia, enabling technologies like composite bows and Gothic cathedrals. Scientific understanding emerged in the 17th and 18th centuries with Galileo’s experimental method, Descartes’ coordinates, and Newton’s laws. Augustin-Louis Cauchy later provided the first rigorous mathematical model, defining stress as the force across an imaginary surface, linearly dependent on its normal vector and symmetric. Newton also contributed a formula for shear stress in laminar fluid flow.

field
Continuum mechanics
known_for
Describing internal forces during deformation, Cauchy stress tensor
SI_unit
Pascal (Pa) or N/m²
common_unit
Megapascal (MPa) or pounds per square inch (psi)
symbol
σ (sigma)

Quick Facts

Unit
pascal
Otherunits
psi, bar
Baseunits
Pa = kg⋅m / −1 / ⋅s / −2
Dimension
wikidata

Facts from the source article.

Lore & Background

Stress, in continuum mechanics, is a physical quantity representing the forces that arise within a material during deformation. It is defined as the force acting across a small boundary per unit area, for all possible orientations of that boundary. The dimension of stress is force per area, with SI units of newtons per square meter (N/m²), also called the pascal (Pa). Stress is typically denoted by the lowercase Greek letter sigma (σ). Greater force or a smaller cross-sectional area results in higher stress. For instance, a stretched elastic band experiences tensile stress and may elongate, while a crumpled sponge undergoes compressive stress and shortens. Stress expresses the internal forces that neighboring particles of a continuous material exert on each other; for example, particles in a vertical bar supporting an overhead weight push on those below, while particles in a pressurized liquid are pushed by surrounding particles and container walls. These macroscopic forces are the net result of numerous intermolecular forces and collisions. Strain measures the relative deformation of the material. In solids, any deformation generates an internal elastic stress that tends to restore the original shape, analogous to a spring. In liquids and gases, only volume-changing deformations produce persistent elastic stress, though gradual deformations also generate viscous stress. Significant stress can exist even without deformation, as in prestressed concrete or tempered glass, and can arise from temperature changes, chemical composition shifts, or electromagnetic fields, without net external forces. The relationship between stress, strain, and strain rate can be complex, though a linear approximation often suffices for small quantities. Stress exceeding a material’s strength limits may cause permanent deformation, fracture, or changes in crystal structure.

Reader's Guide

Augustin-Louis Cauchy gave the first rigorous and general mathematical model of a deformed elastic body by introducing the notions of stress and strain. He observed that the force across an imaginary surface was a linear function of its normal vector and must be a symmetric function. Stress is defined as the force across a small boundary per unit area for all orientations, expressed by the Cauchy traction vector. The stress state must be described by a tensor, which can be represented as a symmetric matrix of 3×3 real numbers. Stress may exist even without deformation, as in prestressed concrete and tempered glass, and can be imposed by changes in temperature, chemical composition, or electromagnetic fields. The relation between stress, strain, and strain rate can be complicated, though a linear approximation may be adequate for sufficiently small quantities. Stress exceeding certain strength limits results in permanent deformation such as plastic flow, fracture, or cavitation.

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