Stress (): This represents the internal resistive force per unit cross-sectional area within a material. It is calculated as , where is the applied force and is the original cross-sectional area, measured in Pascals (Pa) or .
Strain (): This is a dimensionless measure of deformation representing the fractional change in length. It is defined as , where is the change in length and is the original length.
Tensile vs. Compressive: Tensile stress occurs when forces pull an object apart, leading to elongation, while compressive stress occurs when forces push inward, leading to shortening.
| Feature | Elastic Deformation | Plastic Deformation |
|---|---|---|
| Reversibility | Fully reversible upon unloading | Permanent change in shape |
| Atomic Level | Stretching of atomic bonds | Breaking and reforming of bonds |
| Energy | Stored as elastic potential energy | Dissipated as heat/internal work |
Unit Consistency: Always convert units to the SI standard (Pascals). Remember that and .
Area Calculations: Pay close attention to whether the problem provides the radius or the diameter. For a circular cross-section, or .
Graph Interpretation: The slope of the linear portion of a stress-strain graph is the Young's Modulus (). Ensure you are calculating the slope only within the proportional region.
Sanity Checks: Metals typically have Young's Moduli in the range of GPa (e.g., Steel is approx. 200 GPa). If your calculated value is in the hundreds or thousands, you likely missed a power-of-ten conversion.
Confusing Stress and Force: Students often use force directly in formulas where stress is required. Always divide the force by the cross-sectional area before applying Hooke's Law.
Strain Units: Strain is a ratio of lengths and therefore has no units. Avoid adding 'meters' or 'mm' to a strain value; it is often expressed as a decimal or a percentage.
Ductility vs. Strength: A strong material can withstand high stress, but a ductile material can undergo significant strain before breaking. They are independent properties.