Curvilinear Motion: Polar Coordinates - Statics and Dynamics
- Which of the following correctly describes the acceleration vector of the particle at this instant? Answer: m/s², where m/s² and m/s²; both and the Coriolis term vanish explicitly because implies When a particle moves in polar coordinates, its acceleration has two components derived by differentiating the position vector twice: and . The key insight for circular motion problems is that a constant radius means and , which simplifies these formulas — but you must still write them out completely and justify each simplification explicitly. Answer D does exactly this. Since m = const, and . Substituting: m/s² and m/s², giving m/s². Every term is accounted for and every zero is justified — that's rigorous physics. Answer A arrives at the same numerical result but drops and without explanation. On an exam, silently omitting terms suggests you don't know why they vanish — D is preferred precisely because it demonstrates full understanding. Answer B corrupts the formula by adding a spurious term, as if an extra velocity-dependent contribution exists in the transverse direction. No such term appears in the correct derivation. Answer C incorrectly flips the sign of the centripetal term, treating as positive. The centripetal acceleration always points inward (toward the center), meaning must be negative. Study tip: Always write both full polar acceleration formulas first, then substitute and with an explicit reason. Showing your zeros is what separates a complete solution from a lucky answer.
- What is the radial component of acceleration at this instant? Answer: m/s², found by correctly computing and using at the given instant When analyzing motion in polar coordinates, your go-to formulas for acceleration components are and . The key challenge is correctly computing by differentiating the path equation, then carefully substituting the actual values at the given instant. Since , differentiating once gives , and differentiating again gives . At : m, m/s². Plugging into the radial acceleration formula: m/s². That's exactly what B computes — it correctly evaluates at the given instant rather than leaving it as a generic expression. A is tempting because is correct, but it substitutes symbolically and treats as a number (likely ) without properly evaluating , yielding the wrong numerical result of m/s². C uses the wrong sign in the formula — adding instead of subtracting it. The centripetal term always subtracts in ; mixing up this sign is one of the most common errors in polar kinematics. D correctly finds , but then substitutes instead of , confusing two entirely different terms from the acceleration formula. Your study tip: always write the polar acceleration formulas from scratch before substituting — it forces you to catch sign errors and prevents mixing up , , and .
- What is the angle that the net force vector makes with the radial direction (measured from toward )? Answer: , using m/s² and m/s² When working with polar coordinate dynamics, your first job is always to write down the correct acceleration formulas before plugging in any numbers. The two components are: With , m, , rad/s, and rad/s², these give: The negative means the radial force points inward (). The angle measured from toward is therefore , confirming C. Choice A corrupts the radial formula by subtracting a spurious term, leaving instead of 16 — the radial acceleration has no dependence whatsoever. Choice B gets both acceleration magnitudes right but flips the arctangent ratio, effectively measuring the angle from rather than from , which swaps numerator and denominator. Choice D correctly finds m/s² but inflates the transverse acceleration to 12 m/s² by tacking on an extra term that has no place in the formula. Study tip: Memorize both polar acceleration formulas as a matched pair and check each term's origin — every symbol has a physical meaning, so phantom terms (like in or in ) should raise an immediate red flag.
- What is at this instant? Answer: m/s, using the correct decomposition with m/s When a particle moves in polar coordinates, its velocity has two orthogonal components: a radial component (along the direction) and a transverse component (along the direction). Because these components are perpendicular, speed is found using the Pythagorean theorem: . This is the foundational formula to recall whenever you're given polar-coordinate kinematics. Applying it here, the transverse speed is m/s. Solving for : m/s. That's answer A, the correct choice. B is wrong because it subtracts the components algebraically — m/s — as if velocity were a scalar sum. Orthogonal vectors don't add or subtract that way; you must use the Pythagorean relationship. C makes the mistake of dropping the radius , plugging in rad/s directly instead of the transverse speed m/s. Remember: has units of rad/s, not m/s — multiplying by converts it to a speed. D adds instead of subtracting it, which would make larger than — physically impossible, since is just one component of the total velocity. Study tip: Always write first, then identify which quantity is unknown. Never forget the in — it's one of the most common errors on polar-coordinate problems.
- At s, what is the magnitude of the net force acting on the particle? Answer: N, found using m/s² and m/s² When a particle moves in polar coordinates, you need two acceleration components — radial and transverse — even when no external transverse force is applied. The key formulas are and . These components arise purely from the geometry of curvilinear motion, not just from applied forces. For this problem, derive the kinematics from and : you get , , , and . At s: m/s² and m/s². Since these are orthogonal components, the net acceleration magnitude is , giving N. This confirms B is correct. A makes a conceptually seductive mistake: because no transverse force is externally applied, it assumes . But is a kinematic quantity — it equals zero only if the motion itself demands it, not simply because you didn't push sideways. Here, the Coriolis term is nonzero, so m/s² and a transverse force must exist. C correctly identifies both components but drops the factor of 2 from the Coriolis term, halving to 6 m/s² — a purely algebraic error. D adds and as scalars rather than combining them as perpendicular vectors using the Pythagorean theorem. Remember: in polar coordinates, "no applied transverse force" is a physics claim you must verify kinematically — never assume it.
- What is at this instant? Answer: m/s², found by differentiating the constraint twice to obtain , then solving for with m and m/s When a particle's path is given as a constraint relating and , your job is to extract velocity and acceleration information by differentiating that constraint with respect to time — not by guessing at kinematic formulas. Start with . Differentiating once: . At rad, m. Substituting gives m/s. Differentiating the first derivative again using the product rule on : . Solving for : m/s². That's answer A, and it's correct. Answer B introduces a spurious term, as if appeared inside the differentiation of — it doesn't. The constraint only involves , not in a way that generates that extra term. Answer C drops the factor of 2 in front of when rearranging, a careless algebra error that changes the result entirely. Answer D sets up the correct formula but substitutes instead of — a classic numerical slip where the student forgets to square the velocity value. Study tip: Always compute intermediate quantities — especially , — explicitly before substituting into the second-derivative equation. Writing each step prevents the kind of substitution error that traps answer D.
- A student claims: 'Since the rod is straight and frictionless, the transverse acceleration of the bead must be zero.' Which of the following best evaluates this claim? Answer: The claim is incorrect. m/s² . The rod exerts a normal (transverse) force on the bead to produce this acceleration; calling the rod 'frictionless' only means no force acts along the rod, not that the transverse force is zero. When analyzing bead-on-rotating-rod problems, you need to carefully distinguish between two different things the word "frictionless" tells you — and one thing it absolutely does not tell you. The transverse acceleration in polar coordinates is . Plugging in the given values: . This is real, nonzero acceleration — meaning a real, nonzero transverse force must exist. That force is the normal force the rod walls exert on the bead as it slides outward. D is correct because it recognizes this: "frictionless" only eliminates force along the rod (tangential contact), not perpendicular to the rod (normal contact). The rod must push the bead sideways to keep it on the rotating path. A is wrong on two counts: it incorrectly concludes , and then doubles down by claiming and cannot coexist — they clearly can, and the Coriolis term captures exactly this situation. B is wrong because averaging over a full revolution doesn't make zero at any given instant. The problem asks about conditions at a specific moment, not a time-averaged result. C contains a subtle but serious error: it calls "fictitious" because polar coordinates are supposedly non-inertial. Polar coordinates are a coordinate system used within an inertial frame — they are not a rotating reference frame. The acceleration and the force are both completely real. Study tip: On rotating-constraint problems, always ask yourself: "What does 'frictionless' actually eliminate?" It kills forces along the constraint surface, never the normal force perpendicular to it.
- At this instant, which statement correctly describes the relationship between the radial and transverse velocity components? Answer: m/s and m/s; the radial component is half the transverse component because while m/s, so m/s When analyzing particle motion in polar coordinates, your first move should always be to identify the velocity components using the standard formulas: and . The key is correctly applying the chain rule to find . Since , differentiating with respect to time gives . At , we get m, so m/s. The transverse component is simply m/s. This makes C correct — the radial component is exactly half the transverse component, a direct consequence of the 0.5 coefficient in the exponent. Choice A reaches the right value for but incorrectly claims m/s as well. The transverse velocity is m/s, not 2. The 45° angle conclusion falls apart because the components are not equal. Choice B reverses the logic entirely — claiming as if the chain-rule coefficient multiplies alone rather than the full product , yielding inflated and dimensionally inconsistent numbers. Choice D invents a fictional "curvature correction" to . No such correction exists — is exact in polar coordinates regardless of how depends on . Your study tip: when you see , always compute via the chain rule as , then plug into the standard polar velocity formulas without modification.