Polythene is a type of plastic that is generally considered to be ductile. This means it can deform without breaking when subjected to stress or strain, making it suitable for a variety of applications where flexibility is required.
Silver is malleable, ductile, and sectile.
This depends on the confining pressure, the temperature and the strain rate applied to the mineral. In general for minerals (and other materials), the lower the rate of strain, the more likely ductile or plastic creep deformation will occur. The higher the strain rate, the more likely brittle deformation is to occur. As the confining pressure increases, an objects shear strength will increase (this usually coincides with a greater depth of burial) and due to the earth's thermal gradient an increase in temperature. As the shear strength increases, brittle failure is less likely and the higher temperature means that plastic deformations or creep are more likely to occur.
In a stress-strain curve, the part that represents ductile deformation is typically found in the region after the elastic limit and before the ultimate tensile strength. This section shows a significant amount of plastic deformation, where the material can undergo permanent shape changes without breaking. The slope in this region is less steep than in the elastic region, indicating that the material can absorb more energy and deform gradually under stress.
Isotropic materials have the same mechanical properties in all directions. This means they exhibit identical responses to stress or strain, regardless of the direction in which they are applied. Isotropic materials are characterized by having uniformity and symmetry in their properties.
The strain liquid is a type of liquid that has unique characteristics and properties. It is known for its viscosity, which is the thickness or resistance to flow. Strain liquids can also exhibit elasticity, meaning they can return to their original shape after being deformed. Additionally, strain liquids can display non-Newtonian behavior, where their viscosity changes depending on the applied stress or shear rate.
Polythene is a type of plastic that is generally considered to be ductile. This means it can deform without breaking when subjected to stress or strain, making it suitable for a variety of applications where flexibility is required.
The relationship between viscosity and strain in materials under deformation is that viscosity is a measure of a material's resistance to flow, while strain is the amount of deformation a material undergoes when subjected to stress. In general, materials with higher viscosity tend to exhibit less strain under deformation, as they are more resistant to flow and deformation. Conversely, materials with lower viscosity are more likely to experience higher levels of strain when deformed, as they flow more easily.
The factors that determine whether a rock behaves as a brittle or ductile material include temperature, confining pressure, strain rate, mineral composition, and presence of pre-existing fractures. Higher temperatures and lower confining pressures tend to promote ductile behavior, while lower temperatures and higher confining pressures favor brittle behavior. The strain rate, mineral composition, and presence of pre-existing fractures can also influence whether a rock will exhibit brittle or ductile behavior.
A strain gage is used to measure the strain, or local deformation, of an object. As the object deforms to stress, the gage also is deformed and its electrical resistance is changed. This change is then measured.
initially there is the linear elastic region which obeys the hooks law :stress is directly proportional to the strain. at the end of the linear elastic region the ductile material reaches the yield point beyond which any change in dimensions become permanent. the material goes through a yield plateau in which stress is constant and the strain changes. after crossing the yield plateau the ductile material goes through the strain hardening region in which the deformation is permanent but as the region goes on the stress increases with the strain. here the strength of the ductile material increases as it is strain hardened. at a point it reaches the ultimate load point. This is the maximum load taken by the material. after which further deformation causes decrease in strength or the stress goes on decreasing finally breaking at the breaking load point. this region is called the post-ultimate region.
When plastic deformation occurs in a material, it causes permanent changes in its shape or structure due to the movement of dislocations within the material. This results in the material being able to retain its deformed shape even after the applied stress is removed. The material typically experiences strain hardening, where it becomes stronger and less ductile as deformation continues.
Yes, it is - it has a yield point and can strain quite a bit 20% or so before failure
The type of strain that results when rock responds to stress by permanently deforming without breaking is known as ductile strain. This occurs when rocks are subjected to high temperatures and pressures, allowing them to bend or flow rather than fracture. Ductile deformation is typically observed in deeper crustal levels where conditions promote such behavior. This contrasts with brittle strain, where rocks break or fracture under stress.
Volumetric strain of a deformed body is defined as the ratio of the change in volume of the body to the deformation to its original volume. If V is the original volum and dV the change in volume occurred due to the deformation, the volumetric strain ev induced is given by ev =dV/V Consider a uniform rectangular bar of length l, breadth b and depth d as shown in figure. Its volume V is given by, This means that volumetric strain of a deformed body is the sum of the linear strains in three mutually perpendicular directions.
Deformation of rocks refers to the physical changes in shape, volume, and structure that occur in response to stress and strain. This process can result in features like folds, faults, and joints in rocks. Deformation can be brittle, where rocks break and form faults, or ductile, where rocks change shape without fracturing.
If you stretch a rubber band then release it, it will return to its original shape. That is by definition elastic strain. Anything that returns to its original shape after being affected by force underwent elastic strain. If it is permanently deformed (ie you bent a paperclip out of place and it wont return to its original shape) then it passes the elastic strain region and suffered plastic strain.