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Matter in Our Surroundings - States of Matter

Grade 9CBSE

Review the key concepts, formulae, and examples before starting your quiz.

🔑Concepts

Matter is made up of tiny particles which have spaces between them, are continuously moving, and attract each other. The kinetic energy of particles increases with a rise in temperature (TT).

Solid State: Characterized by definite shape, distinct boundaries, and fixed volumes. Particles have minimum space and maximum force of attraction. Solids are generally incompressible.

Liquid State: Particles have no fixed shape but a fixed volume. They take the shape of the container. The rate of diffusion of liquids is higher than solids because particles move freely.

Gaseous State: Particles have no fixed shape or volume. They have maximum kinetic energy and move randomly at high speeds. Gases are highly compressible, as seen in LPGLPG (Liquefied Petroleum Gas) and CNGCNG (Compressed Natural Gas).

Change of State: Temperature and pressure determine the state of a substance. Increasing temperature provides energy to overcome intermolecular forces (e.g., SolidFusionLiquidVaporisationGasSolid \xrightarrow{Fusion} Liquid \xrightarrow{Vaporisation} Gas).

Latent Heat of Fusion: The amount of heat energy required to change 1 kg1\text{ kg} of a solid into liquid at atmospheric pressure at its melting point. For ice, this is approximately 3.34×105 J/kg3.34 \times 10^5\text{ J/kg}.

Latent Heat of Vaporization: The heat energy required to change 1 kg1\text{ kg} of a liquid to gas at atmospheric pressure at its boiling point. Steam at 373 K373\text{ K} has more energy than water at the same temperature due to this latent heat.

Sublimation and Deposition: Sublimation is the direct change from solid to gas without becoming liquid (e.g., Ammonium Chloride NH4ClNH_4Cl, Solid CO2CO_2). Deposition is the direct change from gas to solid.

Evaporation: A surface phenomenon where particles from the surface of a liquid gain enough energy to overcome forces of attraction and change into vapor. Factors affecting it include surface area, temperature, humidity, and wind speed.

📐Formulae

T(K)=T(C)+273.15T(K) = T(^{\circ}C) + 273.15

Density(ρ)=Mass(m)Volume(V)Density (\rho) = \frac{Mass (m)}{Volume (V)}

Q=mLQ = m \cdot L

Rate of EvaporationSurface Area×Temperature×Wind SpeedHumidityRate\ of\ Evaporation \propto \frac{Surface\ Area \times Temperature \times Wind\ Speed}{Humidity}

💡Examples

Problem 1:

Convert the temperature of 25C25^{\circ}C to the Kelvin scale.

Solution:

Using the formula T(K)=T(C)+273.15T(K) = T(^{\circ}C) + 273.15, we get T(K)=25+273.15=298.15 KT(K) = 25 + 273.15 = 298.15\text{ K}.

Explanation:

To convert Celsius to Kelvin, we add the constant 273.15273.15 to the Celsius value because the Kelvin scale starts at absolute zero.

Problem 2:

Why does a desert cooler cool better on a hot dry day?

Solution:

On a hot dry day, the temperature is high and humidity is low. This increases the rate of evaporation of H2OH_2O.

Explanation:

Evaporation is an endothermic process that causes cooling. Higher temperatures and lower humidity significantly increase the evaporation rate from the pads of the cooler, leading to a greater cooling effect.

Problem 3:

Identify the state of Dry Ice and what happens when pressure is decreased to 11 atmosphere.

Solution:

Dry ice is solid carbon dioxide (CO2CO_2). When pressure is decreased to 1 atm1\text{ atm}, it transforms directly into the gaseous state.

Explanation:

Solid CO2CO_2 is stored under high pressure. This process of changing directly from solid to gas is called sublimation.