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If you load it normal to the beam axis you get bending stresses ( tension and compression) and shear stresses. If you load it along the axis you get axial stress ( tension or compression)
Stresses will be distributed equally among members if there is symmetry. It will be easier to calculate it will be easier to manufacture...
stresses applied on materials used in the industry
Whenever an elastic body subjected to loads in its 3 dimensions, the stresses will get developed along the principal axis of the body. These are the principal stresses. These stress should not exceed the yield stress of the material. Von Mises (1913) postulated that, even though none of the principal stresses exceeds the yield stress of the material, it is possible for yielding of the same from the combination of stresses. The Von Mises criterion is a formula (refer any textbook which content failure theories for Ductile Materials) for combining these 3 stresses into an equivalent stress, which is then compared to the yield stress of the material.
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The three stresses are compression, tension, and shearing.
Bending, Shearing, Torsion, Shearing, and Compression.
The three main types of stress in a rock are shearing, tension, and compression.
Shearing stress is one of three kinds of stresses. Compressional and tensional are the others. Shearing stress is associated with transform. The other two kinds of plate boundaries are convergent and divergent.
Tangential loads are forces applied perpendicular to a surface or structure. They can cause twisting or shearing stresses in an object rather than direct compression or tension. These loads are important to consider in engineering and design to ensure the structural integrity of the system.
Compression, tension, and shearing are all types of mechanical stresses that occur in materials. Compression involves forces that act to compress or shorten the material, while tension involves forces that act to stretch or elongate the material. Shearing involves forces that act parallel to a surface, causing sliding or distortion of material layers. All three types of stress can cause deformation or failure in materials if they exceed the material's strength.
Strike slip faults are formed as a result of shear stresses. However strictly speaking all faults are in a shear stress state as there is usually movement in differing directions along both sides of the fault however in the other cases, compressive or tensile stresses are the cause of the initial fault formation.
Normal faults are the result of tensile stresses.
The energy possessed by a body by virtue of its position relative to others, stresses within itself, electric charge, and other factors. This stored energy of position is referred to as potential energy.
Its called potential energy. Which is the energy possessed by a body by virtue of its position relative to others, stresses within itself, electric charge, and other factors. Since I gave you this answer you now have to look up this band called Falling in Reverse. My favorite band
The three types of stress in plates are tensile stress (stretching), compressive stress (compressing), and shear stress (sliding or tearing). These stresses can cause deformation or failure in the material if they exceed its strength.
Normal faulting results from expansive stresses, where the hanging wall moves down relative to the footwall due to tensional forces pulling the plates apart. This type of faulting is common at divergent plate boundaries where new crust is being formed.