P1

Page 1

  • OCR (A) Physics GCSE

  • Topic P1: Matter Summary Notes


Page 2: The Particle Model

How & Why the Atomic Model Has Changed Over Time

  • 1800: Dalton proposed that everything is made of indivisible tiny spheres called atoms.

  • 1897: JJ Thomson discovered the electron, leading to the Plum Pudding Model.

  • 1911: Rutherford revealed that most of the atom is empty space through the Gold Foil Experiment.

  • 1913: Rutherford's Model was developed further.


Page 3: Structure & Size of the Atom

  • Atom Structure:

    • Positively charged nucleus (protons + neutrons)

    • Negatively charged electrons orbiting the nucleus

  • Subatomic Particle Details:

    • Proton: Mass = 1, Charge = +1

    • Neutron: Mass = 1, Charge = 0

    • Electron: Mass ≈ 0 (0.0005), Charge = -1

  • Size: Atom = 10^(-10) meters; nucleus is 10,000 times smaller.

  • Density Formula:

    • Density (ρ) = Mass (kg) / Volume (m³)

  • Density Differences:

    • Solids & liquids have higher densities compared to gases due to closer particle spacing.

    • Ice is less dense than water.


Page 4: Changes of State

Conservation of Mass

  • Mass remains constant during changes of state (e.g., 20g liquid = 20g gas).

  • Changes are physical and reversible.

Heating a System

  • Heat vs Temperature:

    • Temperature measures average kinetic energy.

    • Heat is energy measured on an absolute scale.

  • Heat absorption outcomes:

    • Increases temperature at the same state.

    • Changes state at constant temperature.

Specific Heat Capacity & Latent Heat

  • Specific Heat Capacity (c):

    • Energy to raise 1kg by 1ºC.

    • Formula: E = mc∆T (J/kg°C).

  • Specific Latent Heat (l):

    • Energy to change 1kg without temperature change.

    • Formula: E = ml (J/kg).


Page 5: Pressure (Physics Only)

Molecule Motion

  • Particles in fluids move randomly.

  • Pressure formula: Pressure (p) = Force/Area.

  • Pressure increases with more frequent and forceful particle collisions.

Temperature & Pressure

  • At constant volume: Pressure ∝ Temperature (p ∝ T).

  • Increasing temperature increases pressure due to particle speed.

Volume & Pressure

  • At constant temperature: Pressure ∝ 1/Volume (p ∝ 1/V).

Temperature, Volume & Work

  • At constant pressure: Volume ∝ Temperature (V ∝ T).

  • Work done on fluids increases temperature.


Page 6: Increasing Pressure & Temperature

  • Adding gas = more particle collisions = higher pressure.

  • Reducing volume = more frequent collisions = higher pressure.

  • Earth's Atmosphere:

    • Isothermal and uniform density.

  • Atmospheric Pressure decreases with altitude due to fewer air molecules.

Floating & Sinking

  • Objects float if weight < displaced fluid weight.

  • Buoyancy counteracts weight of floating objects.


Page 7: Pressure & Buoyancy

Pressure & Depth

  • Water depth increases weight of the water column = higher pressure.

  • Pressure due to liquid column = Height × Density × g (10).

  • Example: A ping pong ball floats due to having less density than water.

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