Linked from

The 23 pages that link to Shear stress, each with the reason it gives.

• Sediment transportRelated: Boundary shear stress is a key measure of a flow’s ability to move grains.

• ViscosityRelated: Shear stress is the applied force that viscosity relates to deformation rate.

• Stress (mechanics)Broader topic: It describes the sliding action that accompanies many loaded materials.

• DislocationRelated: Resolved shear stress drives dislocation motion along favorable slip systems.

• Aeolian processesNarrower topic: Wind exerts shear stress on the ground to mobilize grains.

• Fault (geology)Related: Shear stress drives relative motion across many fault surfaces.

• Newtonian fluidRelated: It is the stress component that scales with shear rate in the defining law.

• Non-Newtonian fluidRelated: It is the applied mechanical quantity related to deformation rate in fluid flow.

• Shear strengthNarrower topic: Shear strength is the limiting value of this stress before failure.

• Blunt traumaRelated: Blunt forces can shear tissue layers and blood vessels as the body deforms.

• Shear modulusRelated: It is the load in the numerator of the shear-modulus definition.

• Food rheologyRelated: Rheological tests use it to describe the loading that drives food flow.

• Strength of materialsRelated: It governs resistance to sliding failure and torsional loading.

• Stress concentrationRelated: Notches and holes can amplify shear stress as well as normal stress.

• FasciaRelated: Sliding between fascial layers involves shear forces at their interfaces.

• Mohr–Coulomb theoryRelated: Failure is predicted when this component reaches the strength specified by the criterion.

• MyloniteRelated: Shear stress drives the deformation concentrated in mylonite-forming zones.

• FastenerRelated: Fasteners often carry loads that try to slide joined parts past one another.

• Avulsion injuryRelated: Tangential forces can separate skin and underlying tissue in degloving avulsions.

• Cross-flow filtrationRelated: Tangential flow creates surface shear that can limit accumulation of retained material.

• Sediment gravity flowRelated: Gravity generates downslope stress that must overcome resistance within the sediment.

• Byerlee's lawRelated: Sliding begins when applied shear stress overcomes frictional strength.

• Power-law fluidRelated: The model predicts shear stress from the imposed shear rate.