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Termodinámica y energía · GCSE Physics Topic 3 (Thermal Properties)

Simulador de calor específico y calorimetría

Simulador de capacidad calorífica específica y brisa marina: Q = c·m·Δt e inercia térmica

  • Cálculo en cliente
  • Sin registro
  • Derivación en vivo
  • Modo proyector
  • Hoja de trabajo A4
Cálculo local · Privado
Laboratorio interactivo de ciencias Cálculo matemático y físico puramente en el cliente. Los datos se procesan localmente sin almacenar información personal.
Ventana de simulación 3D● 60 FPS
Preajustes y errores frecuentes:

Variables de control del experimento

J
kg

Derivaciones y métricas en tiempo real

Aumento de temperatura de A
--
Aumento de temperatura de B
--
Razón de aumentos de temperatura
--
Sentido de la brisa
--
Derivación de fórmulas en tiempo real
Fórmula básica: --
Sustitución de valores: --
Estado físico: --

Ejemplos clásicos y análisis de errores en exámenes

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.
Derivación paso a paso:
  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?
Derivación paso a paso:
  1. Conversion method! Identical heaters output heat at an equal rate, so heating time directly gauges absorbed heat energy.

Hoja de indagación en clase y tareas

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?

Preguntas frecuentes y errores conceptuales

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.