Slip
Slip is a term used in various fields to describe a range of phenomena. In the context of materials science, it refers to the deformation of a material through the movement of dislocations. In geology, it refers to the displacement of rocks along a fault. In ceramics, it is a suspension of clay, clay body or some other material in water. In engineering, it refers to the difference between the speed of a rotating magnetic field in a motor and the rotor.
Materials Science[edit | edit source]
In materials science, slip is the primary mechanism by which a material deforms plastically. It occurs when dislocations move through the crystal lattice of a material, causing the planes of atoms to shift relative to each other. This movement is facilitated by the application of a shear stress. The direction and magnitude of the slip are determined by the orientation of the dislocations and the applied stress.
Geology[edit | edit source]
In geology, slip refers to the displacement of rocks along a fault. It is measured as the relative movement of one side of the fault with respect to the other. Slip can occur in any direction along the fault plane, but is typically classified as either dip-slip (vertical movement) or strike-slip (horizontal movement).
Ceramics[edit | edit source]
In ceramics, slip is a suspension of clay, clay body or some other material in water. It is used in a variety of processes, including slip casting, decoration, and joining pieces of clay together. The properties of the slip, such as its viscosity and particle size distribution, can significantly affect the final properties of the ceramic piece.
Engineering[edit | edit source]
In engineering, slip refers to the difference between the speed of the rotating magnetic field in an induction motor and the speed of the rotor. It is usually expressed as a percentage of the synchronous speed. Slip is an important parameter in the design and operation of induction motors, as it affects the motor's efficiency and torque.
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Contributors: Prab R. Tumpati, MD
