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internal energy

Internal energy U is the total energy of chaotic (thermal) motion of microparticles of a system and the potential energy of their interaction. Unlike the mechanical energy of a body as a whole, internal energy does not depend on the body's speed or position in space, but is determined by its temperature, volume, and chemical composition. The first law of thermodynamics relates the change in internal energy (ΔU) to the amount of heat transferred (Q) and work done on the system (W): ΔU = Q - W.

History

The concept of internal energy was formed in the 19th century together with the science of heat — thermodynamics. Scientists like James Joule and Rudolf Clausius showed that heat is not a special substance, but a form of energy related to particle motion.

How it works

Imagine a soccer ball being inflated. By striking the ball, you compress the air inside, and the particles start moving faster — internal energy increases, the ball heats up. Heat from a campfire also makes the air molecules around it move more energetically — the air's internal energy increases, and it rises.

💡 Even ice at subzero temperature has internal energy: water molecules in the crystal lattice continue to vibrate, and only at absolute zero (−273.15 °C) does this motion theoretically cease.
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Scientists
Ludwig BoltzmannJames Clerk Maxwell
Related tags
critical pointenthalpyentropyPhase transitiontemperaturecatalysis
Laws
law of conservation of energyzeroth law of thermodynamicsthird law of thermodynamicsideal gas lawCarnot's theorem

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