Motion in a Plane - Comprehensive Study Guide
Introduction to Motion in Two and Three Dimensions
1D vs. Multi-dimensional Kinematics:
In one-dimensional motion (along a straight line), directional aspects are fully specified using positive ( ) and negative ( ) signs because only two directions are possible.
In two-dimensional motion (in a plane) or three-dimensional motion (in space), specifying direction requires vectors.
Scope of Two-Dimensional Kinematics:
Vector algebra provides the foundation for defining velocity and acceleration in two dimensions.
Two-dimensional motion with constant acceleration includes important applications such as projectile motion and uniform circular motion.
Kinematic equations developed for two-dimensional motion can be directly extended to three-dimensional motion.
Scalars and Vectors
Scalars:
Defined as physical quantities that possess magnitude only and are specified completely by a single real number along with a proper unit.
Scalar quantities follow the ordinary rules of algebra (addition, subtraction, multiplication, and division).
Addition and subtraction of scalar quantities are meaningful only if the quantities have identical units; multiplication and division can be performed on scalars with different units.
Examples of Scalars:
Distance between two points.
Mass of an object.
Temperature of a body (e.g., maximum temperature of and minimum temperature of yield a scalar difference of ).
Time at which an event occurs.
Perimeter of a rectangle (e.g., sides of and yield a scalar perimeter ).
Volume and density (e.g., a uniform aluminum cube of side has volume and mass , yielding a scalar density of ).
Vectors:
Defined as physical quantities that possess both a magnitude and a direction, and satisfy the triangle law of addition or equivalently the parallelogram law of addition.
Examples of Vectors: Displacement, velocity, acceleration, and force.
Vector Notation:
Printed in boldface type (e.g., , , ).
Handwritten with an arrow placed above the letter (e.g., , ).
Magnitude (absolute value) is denoted by lightface type or vertical bars: or .
Position and Displacement Vectors:
Position Vector: Drawn from a chosen origin to the particle's position at time , denoted as . The length of the line segment represents magnitude, and the arrow specifies direction.
Displacement Vector: When a particle moves from position (at time ) to position (at time ), the displacement vector (or ) is the straight line drawn from initial position (tail) to final position (tip).
Displacement is independent of the actual path taken ( , , or ); it depends solely on the initial and final position coordinates.
The magnitude of displacement is always less than or equal to the actual path length traversed by the object.

Equality of Vectors:
Two vectors and are defined as equal ( ) if and only if they have both equal magnitude and identical direction.
Free Vectors: Vectors that can be translated parallel to themselves without changing their physical meaning.
Localised Vectors: Vectors whose line of application or point of application is fixed in a physical context.

Multiplication of Vectors by Real Numbers
Multiplication by a Positive Real Number:
Multiplying a vector by a positive scalar results in a vector whose direction is identical to and whose magnitude is .
Example: Multiplying by yields with double the magnitude in the same direction.
Multiplication by a Negative Real Number:
Multiplying a vector by a negative scalar ( ) produces a vector directed opposite to with a magnitude of .
Example: Multiplying by produces a vector of equal magnitude pointing in the opposite direction ( ); multiplying by produces with times the magnitude in the opposite direction.
Dimensional Changes:
If is a scalar physical quantity possessing its own dimensions, the dimension of is the product of the dimensions of and .
Example: Multiplying a velocity vector by a time duration scalar yields a displacement vector.
Addition and Subtraction of Vectors — Graphical Method
Triangle Method (Head-to-Tail Method):
To add vector to vector , place the tail of at the head of .
The resultant vector is drawn from the tail of to the head of , forming the third side of a triangle.
Properties of Vector Addition:
Commutative Law:
Associative Law:
Null Vector (Zero Vector):
Adding two equal and opposite vectors yields a null vector: .
Magnitude: .
Direction: Indeterminate / non-specifiable.
Algebraic Properties:
Physical Meaning: Represents zero change, such as the net displacement of an object moving along a closed loop back to its starting point.
Vector Subtraction:
Subtraction of vector from is defined as the addition of and -$ \mathbf{B} :
Parallelogram Method:
Bring the tails of vectors and to a common origin .
Complete a parallelogram using lines parallel to and passing through their respective heads.
The resultant vector is represented by the diagonal passing through the common origin .

Resolution of Vectors and Unit Vectors
General Vector Resolution:
Any vector lying in a plane can be uniquely resolved into two component vectors along non-zero, non-collinear vectors and in the same plane:
where and are real numbers.
Unit Vectors:
Defined as a dimensionless, unitless vector of magnitude pointing in a specified direction.
Used strictly to specify direction.
Standard Cartesian unit vectors along , , and axes are written as , , and respectively:
Expressing a general vector using its unit direction vector :
Rectangular Components in Two Dimensions:
A vector in the plane resolved along orthogonal unit vectors and :
Component magnitudes in terms of magnitude and inclination angle relative to the -axis:
Reconstructing magnitude and direction from components and :

Rectangular Components in Three Dimensions:
Direction cosines relative to spatial angles (with -axis), (with -axis), and (with -axis):
Vector representation in 3D:
Magnitude in 3D:
Position vector in 3D:
Vector Addition — Analytical Method
Addition via Components (2D):
For vectors and :
Addition via Components (3D):
For and :
Linear Combinations:
For :
Law of Cosines and Law of Sines:
For two vectors and with an enclosed angle :
Law of Cosines (Magnitude of Resultant ):
Law of Sines:
where is the angle made by with vector , and is the angle made by with vector . - Direction angle :

Motion in a Plane: Position, Displacement, Velocity, and Acceleration
Position Vector and Displacement:
Position vector at coordinates :
Displacement between at time and at time :
Average and Instantaneous Velocity:
Average Velocity:
The direction of is identical to the direction of .
Instantaneous Velocity:
The instantaneous velocity vector at any point along a path is always directed tangentially to the path at that point in the direction of motion.
Magnitude of Instantaneous Velocity (Speed):
Direction angle relative to -axis:
Average and Instantaneous Acceleration:
Average Acceleration:
Instantaneous Acceleration:
where:
In two or three dimensions, velocity and acceleration vectors do not need to be collinear; they can form any angle between and .

Motion in a Plane with Constant Acceleration
Kinematic Equations for Constant Acceleration:
Velocity as a function of time:
In component form:
Position vector as a function of time:
In component form:
Independence of Perpendicular Motions:
Motion in two dimensions under constant acceleration is mathematically equivalent to two independent, simultaneous one-dimensional motions occurring along mutually perpendicular axes.
Projectile Motion
Definition and Principles:
A projectile is any object launched into space that continues in motion under the influence of gravity alone (neglecting air resistance).
Historical Principle (Galileo, 1632): Projectile motion consists of two independent components:
A horizontal component with constant velocity ( ).
A vertical component with constant downward acceleration due to gravity ( ).
Initial Conditions:
Initial launch speed at elevation angle relative to horizontal:
Initial coordinates at origin: , .
Kinematic Equations at Time :
Horizontal position:
Vertical position:
Horizontal velocity component: (constant throughout flight).
Vertical velocity component: .
Equation of Trajectory (Path Shape):
Substituting into the vertical position equation yields:
This equation is of the form (where and are constants), demonstrating that the trajectory of a projectile is a parabola.

Key Projectile Formulas:
Time to Maximum Height (): At peak height, :
Total Time of Flight (): Setting at impact:
Maximum Height Reached (): Substituting into :
Horizontal Range (): Total horizontal distance covered during total time of flight :
Maximum Horizontal Range (): For a given launch speed , is maximized when :
Symmetry of Ranges: Complementary elevation angles and yield identical horizontal ranges because .
Uniform Circular Motion
Definition:
Motion of an object traversing a circular path of radius at a constant speed .
Although speed is constant, velocity continuously changes direction (tangential to the circular arc at every point), causing acceleration.
Centripetal Acceleration ():
Direction: Always points along the radius inward toward the center of the circle ("center-seeking").
Magnitude:
Published by Christiaan Huygens in 1673.
Note: Centripetal acceleration vector is not constant because its direction continuously changes as the particle moves, even though its magnitude is constant.
Angular Speed ():
Rate of change of angular displacement :
Relation to linear speed (with arc length ):
Centripetal acceleration in terms of angular speed:
Period () and Frequency ():
Period ( ): Time required to complete one full revolution.
Frequency ( ): Number of revolutions per unit time.
Linear speed in terms of period and frequency:
Angular speed in terms of frequency:
Centripetal acceleration in terms of frequency:

Summary and Key Formulae
Scalar vs Vector:
Scalars: Magnitude only, combined by standard arithmetic.
Vectors: Magnitude and direction, combined by vector algebra.
Vector Addition & Resolution:
Commutative:
Associative:
2D Resolution: with , , , .
Resultant Magnitude (Law of Cosines):
Law of Sines:
2D Kinematics:
Position:
Instantaneous Velocity:
Instantaneous Acceleration:
Constant Acceleration Equations:
Projectile Motion Equations:
Horizontal Position:
Vertical Position:
Trajectory Equation:
Time of Peak Height:
Time of Flight:
Peak Height:
Horizontal Range:
Uniform Circular Motion Equations:
Centripetal Acceleration:
Speed & Angular Speed Relation:
Points to Ponder
Path length traversed between two points is generally greater than or equal to the magnitude of displacement. They are equal if and only if the path is a straight line without direction reversal.
Average speed is greater than or equal to the magnitude of average velocity over a given time interval.
Kinematic equations for constant acceleration do not apply to uniform circular motion because the direction of acceleration changes continuously.
Resultant velocity of an object subject to two velocities and is . Relative velocity of object 1 with respect to object 2 is .
The net acceleration in circular motion is directed strictly toward the center only if the speed is constant (uniform circular motion).
Trajectory shape is determined by both acceleration and initial conditions (initial position and initial velocity).
Solved Examples
Example 3.1:
Problem: Rain is falling vertically at . Wind starts blowing east to west at . Determine the direction an umbrella should be held.
Solution:
Rain velocity (downward), wind velocity (westward).
Resultant speed:
Angle made by resultant with vertical:
Umbrella should be held in the vertical plane at an angle of about with the vertical toward the east.
Example 3.2:
Problem: Find magnitude and direction of resultant of two vectors and at angle .
Solution:
Magnitude: (Law of Cosines).
Direction angle relative to :
Example 3.3:
Problem: Motorboat racing north at , water current at in direction east of south. Find resultant velocity.
Solution:
Angle between boat velocity (north) and current velocity ( east of south): .
Resultant magnitude using Law of Cosines:
Angle relative to north using Law of Sines: east of north.
Example 3.4:
Problem: Position .
(a) Find and .
(b) Find magnitude and direction of at .
Solution:
(a) . .
(b) At : . Magnitude: . Direction: with -axis.
Example 3.5:
Problem: Particle starts at origin at with and constant acceleration .
(a) Find -coordinate when .
(b) Find speed at this time.
Solution:
(a) Position . . Solving quadratic: . At : .
(b) Velocity at :
At : . Speed .
Example 3.6:
Problem: Prove Galileo's statement that ranges are equal for elevation angles exceeding or falling short of by equal amounts .
Solution:
Launch angles: and .
Double angles : and .
Since and , the ranges are equal.
Example 3.7:
Problem: Stone thrown horizontally at from cliff height . Find time to hit ground and impact speed ( ).
Solution:
Vertical motion: .
Velocity components at impact:
- Impact speed: .
Example 3.8:
Problem: Ball thrown at at above horizontal. Calculate maximum height, time of flight, and horizontal range.
Solution:
(a) Maximum height: .
(b) Time of flight: .
(c) Horizontal range: .
Example 3.9:
Problem: Insect in circular groove of radius completes 7 revolutions in . Find angular speed, linear speed, and acceleration.
Solution:
(a) Angular speed: . Linear speed: .
(b) Acceleration vector is not constant because its direction changes continuously (inward toward center). Magnitude of centripetal acceleration: .
Conceptual Questions and Exercises
Classification of Quantities (Scalar vs Vector):
Scalars: Volume, mass, speed, density, number of moles, angular frequency, work, current, temperature, pressure, time, power, total path length, energy, gravitational potential, coefficient of friction, charge.
Vectors: Acceleration, velocity, displacement, angular velocity, force, angular momentum, linear momentum, electric field, magnetic moment, relative velocity, impulse.
Vector Inequalities:
(Equality holds when and act along the same direction).
(Equality holds when and act along opposite directions).
(Equality holds when and act along opposite directions).
(Equality holds when and act along the same direction).