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For a simple case, the effect can be modeled by an uniaxial energy distribution.
The uniaxial anisotropy is mainly determined by the first two terms.
For , where is the yield stress in uniaxial tension.
It was a uniaxial test in which the bearing was also under a full structure load.
For all other directions in uniaxial and biaxial crystals the speeds are different.
A magnetic particle with uniaxial anisotropy has one easy axis.
The strength of a joint is defined as the force required to break the strap in uniaxial tension.
Yield occurs when the pressure is greater than the uniaxial yield stress.
In uniaxial tension, true stress is then greater than nominal stress.
By its basic definition the uniaxial stress is given by:
Fluoborite is uniaxial, just like all other hexagonal minerals.
Stress versus strain data should be obtained in both uniaxial and biaxial forms.
The accompanying diagram shows a uniaxial crystal being tested between crossed polars.
In the uniaxial manner of tension, tensile stress is induced by pulling forces.
The equations for equibiaxial tension are equivalent to those governing uniaxial compression.
They are said to be uniaxial.
For uniaxial extension in the -direction, the principal stretches are .
In an optical spectrum changbaiite is uniaxial positive and it can be biaxial.
A crystal with only one optic axis is called a uniaxial crystal.
In the widely used Stoner-Wohlfarth model, the anisotropy is uniaxial.
In the simplest form, uniaxial birefringence, there is only one special direction in the material.
Many models of magnetization represent the anisotropy as uniaxial and ignore higher order terms.
Its density is 4.03 g/cm and it is uniaxial.
Consider a composite material under uniaxial tension .
Crystals are classified according to the number of optic axes (uniaxial, biaxial) they have.