SUMMARY
The magnitude of the velocity vector in polar coordinates is calculated using the expression ##\vec{v} = 4 \hat{r} + 6 \hat{\theta}##, resulting in a magnitude of ##\sqrt{52}## or approximately 7.21 m/s. The acceleration can be derived using two methods: the centripetal acceleration formula ##a = \frac{v^2}{r}## yields 17.33 m/s², while the derived acceleration vector ##\vec{a} = -12 \hat{r} + 16 \hat{\theta}## gives a magnitude of 20 m/s². The discrepancy arises because the motion is not uniform circular motion, necessitating consideration of the time rate of change of the basis vectors in polar coordinates.
PREREQUISITES
- Understanding of polar coordinates and their basis vectors, ##\hat{r}## and ##\hat{\theta}##.
- Knowledge of vector calculus, particularly in deriving velocity and acceleration vectors.
- Familiarity with the Pythagorean theorem as applied to vector magnitudes.
- Concept of centripetal acceleration and its application in non-uniform motion.
NEXT STEPS
- Study the derivation of velocity and acceleration in polar coordinates using the formulas provided.
- Learn about the time derivatives of basis vectors in polar coordinates.
- Explore examples of non-uniform circular motion and its implications on acceleration calculations.
- Investigate the relationship between Cartesian and polar coordinate systems in vector analysis.
USEFUL FOR
Students and professionals in physics, particularly those studying mechanics and dynamics, as well as engineers working with polar coordinate systems in their analyses.