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Center of Mass (COM)
A single point representing the mass-weighted average position of a system; used as the representative position for the system’s overall translational motion.
Mass-Weighted Average
An average where each position is weighted by its mass contribution; for COM: (rcm=M1∑miri).
Center of Gravity
The point where the net gravitational force effectively acts; it coincides with the center of mass only in a uniform gravitational field.
Uniform Gravitational Field
A region where (\vec g) is effectively constant in magnitude and direction, making center of gravity and center of mass coincide (common near Earth’s surface for lab-scale objects).
COM Not Necessarily Inside the Object
The center of mass can lie in empty space (e.g., a uniform ring has its COM at the center of the circle where there is no material).
System Boundary (in COM problems)
The specific set of objects included in the analysis; COM and momentum results depend on what is included (e.g., “block only” vs “block + Earth”).
Total Mass (Discrete System)
For (N) point masses, the total mass is (M=∑i=1Nmi).
Center-of-Mass Position Vector (Discrete)
Defined for point masses by (\vec r{cm}=\frac{1}{M}\sum{i=1}^N mi\vec ri).
Center-of-Mass Components
Component form: (xcm=M1∑mixi), (ycm=M1∑miyi), (zcm=M1∑mizi), using one consistent origin and axes.
Common COM Coordinate Error
Mixing coordinate systems/origins or using inconsistent sign conventions; all (xi,yi,z_i) must be measured from the same origin along the same axes.
Center-of-Mass (Continuous Distribution)
For a continuous object: (rcm=M1∫rdm), with total mass (M=∫dm).
Mass Element (dm)
An infinitesimal piece of mass used in integrals for continuous COM calculations; relates geometry to mass via density (e.g., (dm=λdx)).
Linear Mass Density (λ)
Mass per unit length for 1D objects (e.g., thin rod); commonly used with (dm=\lambda\,dx).
Surface Mass Density (\u03c3)
Mass per unit area for 2D laminae/sheets; commonly used with (dm=\sigma\,dA).
Volume Mass Density (ρ)
Mass per unit volume for 3D objects; commonly used with (dm= ho\,dV).
Uniform Density Simplification
If density is uniform, it often cancels in (\vec r_{cm}=\frac{1}{M}\int \vec r\,dm) because both numerator and denominator scale with the same constant density.
Symmetry Method for COM
Use geometric symmetry to locate COM without algebra (e.g., uniform rod midpoint, rectangle diagonal intersection, disk center).
Composite Object Method (Chunks)
Break an object into parts with known masses (mj) and known COM locations (rj), then use (rcm=M1∑jmjrj).
Convenient Origin Choice
Choosing an origin at an endpoint, corner, or symmetry point can simplify COM calculations; numerical coordinates change but the physics does not.
Center-of-Mass Velocity (Discrete)
With constant total mass: (\vec v{cm}=\frac{1}{M}\sum{i=1}^N mi\vec vi).
Center-of-Mass Acceleration (Discrete)
With constant total mass: (\vec a{cm}=\frac{1}{M}\sum{i=1}^N mi\vec ai).
Total Linear Momentum of a System
(P=∑pi=∑mivi); relates directly to COM motion for constant (M).
Momentum–COM Identity (Constant Mass)
For constant total mass: (P=Mvcm); total momentum points in the direction of COM velocity.
Center-of-Mass Form of Newton’s Second Law
Net external force controls COM acceleration: (∑Fext=Macm) (internal forces cancel in the system sum by Newton’s third law).
Key COM Consequence: Zero Net External Force
If (∑Fext=0), then (acm=0) and the COM moves with constant velocity (basis for momentum conservation in an isolated system).