Springs provide conservative forces, useful in conservation of energy equations.
Introduction to forces that vary over time.
Kinetic Energy & Gravitational Potential Energy: Previous topics learned.
Elastic Potential Energy: Work done on a spring stores energy.
Ideal Spring: No weight, behaves perfectly under force.
Stretching a Spring:
Force applied causes spring to stretch.
Stretch denoted as (x), representing change in length (delta (l)).
Linear Relationship: More force results in more stretch.
Doubling the force doubles the stretch length.
Can represent as:
(F = kx) (where (F) is the force, (k) is spring constant, (x) is displacement from equilibrium).
Definition: Spring force (F_s = -kx)
Negative sign indicates a restoring force (forces are in opposite directions).
Examples:
Pull down on the spring, it pulls up.
Measures stiffness of a spring.
Calculated as (k = \frac{F}{x}) = force per unit stretch.
Higher (k) = stiffer spring.
Units: Newtons per meter (N/m).
Measure force and displacement to determine spring constant:
Graphical method: Slope of the force versus displacement graph yields (k).
Single data point method: Use mass hanging to find stretching distance for (k).
Ideal springs obey Hooke's Law until limits are reached (non-linear behavior occurs when overstretched).
Real-world springs may not behave perfectly and have limits to elasticity.
A 50-kg person stretches a 50 cm long spring to a new length—it can be analyzed using Hooke's Law.