
A physical system that exchanges energy or matter with its environment.An open system in physics is any system that exchanges energy, matter, or information with its surroundings. This is the opposite of an isolated system, which is completely self-contained. Most real-world systems are open: a living cell, a planet, a cup of coffee cooling on a table. The concept is fundamental because it determines how we apply the laws of thermodynamics and quantum mechanics. In an open system, entropy can decrease locally at the expense of increasing entropy elsewhere, which is how life and complex structures emerge.
The concept of open systems was formalized in the mid-20th century, particularly through the work of Ilya Prigogine, who studied dissipative structures in chemical systems and won the Nobel Prize in Chemistry in 1977 for his contributions to non-equilibrium thermodynamics.
In an open system, the exchange with the environment introduces new variables that must be accounted for. In thermodynamics, this means the system's internal energy can change due to heat flow, work done, or matter transfer. In quantum mechanics, an open system becomes entangled with its environment, leading to decoherence — the loss of quantum superposition. The mathematical framework for open quantum systems uses master equations or Lindblad operators to describe how the system's state evolves under the influence of its surroundings.
Open system models are essential in engineering (heat exchangers, engines), climate science (Earth's energy balance), and quantum technology (correcting for decoherence in quantum computers).
The Earth is an open system that receives energy from the Sun but exchanges almost no matter with space — which is why the planet can maintain a low-entropy biosphere despite the second law of thermodynamics.


