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Termodinâmica e calorimetria · GCSE Physics Topic 3 (Thermal Properties)

Simulador de calor específico e calorimetria

Simulador de capacidade térmica específica e calorimetria: Q = c·m·Δt e brisa marítima

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  • Dedução ao vivo
  • Modo projetor
  • Folha de exercícios A4
Cálculo local · Privado
Laboratório interativo de ciências Cálculos matemáticos e físicos puramente locais no navegador sem coleta de dados pessoais.
Janela de simulação 3D● 60 FPS
Predefinições e armadilhas comuns:

Variáveis de controle do experimento

J
kg

Deduções e métricas em tempo real

Aumento de temperatura de A
--
Aumento de temperatura de B
--
Razão dos aumentos de temperatura
--
Sentido da brisa
--
Dedução de fórmulas em tempo real
Fórmula fundamental: --
Substituição de valores: --
Estado físico: --

Exemplos clássicos e armadilhas de exame

Worked Problem

Problema: 2kg of water heats from 20°C to 70°C. Find absorbed heat. If 2kg of unknown liquid absorbs same heat rising 100°C, find its specific heat.
Derivação passo a passo:
  1. Q = 4200 * 2 * 50 = 420 kJ. For liquid: c = Q / (m*Δt) = 420,000 / (2*100) = 2100 J/(kg°C) (kerosene).

Worked Problem

Problema: In comparing specific heat capacities, why must identical heaters be used?
Derivação passo a passo:
  1. Conversion method! Identical heaters output heat at an equal rate, so heating time directly gauges absorbed heat energy.

Folha de investigação em aula e exercícios

Q1. Variant 1: Why do residential heating radiators and car cooling systems universally choose water as the medium?
Q2. Variant 2: In comparing water vs cooking oil, a student heated "equal volumes". Is this valid?
Q3. Variant 3: An 800°C iron block drops into cold water. Does heat gained strictly equal heat lost?

Perguntas frequentes e erros comuns

What physics explains the extreme desert diurnal temperature swing in Xinjiang?
Sand has very low heat capacity (~1/5 of water). Intense daytime sun shoots temperatures up; rapid nocturnal radiation drops temperature toward freezing.
Why do farmers flood rice paddy seedlings before cold nights and drain them in the morning?
Water's high heat capacity buffers night frost: slow cooling keeps soil warm at night. Draining water in daytime lets thin soil heat fast.
Does absorbing heat always raise temperature? Does losing heat always lower it?
Not during phase changes! Melting ice and boiling water absorb heat at constant temperature (latent heat); freezing releases heat at constant temperature.
How to avoid confusing heat, temperature, and internal energy in physics exams?
Heat is a transfer process (absorbed/released, never "contained"). Temperature is a state. Internal energy is microscopic energy possessed by all matter.