Traction is the force per unit area transmitted across an oriented surface. For unit normal vector n, the stress tensor gives t=σn. Its normal component is normal stress, and its tangential component is shear stress.
The hydrodynamic torque on a body about a reference point is T=∫Sr×(σ⋅n)dS, with r measured from that point and n pointing from the body into the fluid. The stress includes pressure and viscous contributions, and σ⋅n is the fluid traction on the body. Changing the reference point by d changes the torque by −d×F, where F=∫Sσ⋅ndS is the fluid force. A torque-free body has zero resultant torque, including any external torque.
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- Ambient-controlled interfacial plug current
- Anisotropic Love-wave dispersion
- Axisymmetric viscous-sheet stretching equations
- Balance of linear momentum
- Basal traction on a tectonic plate
- Betti identity for elastodynamic fields
- Buoyancy
- Cauchy solution for a steadily moving semi-infinite antiplane crack
- Cauchy's stress theorem
- Cauchy stress tensor
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