Figure 1: In a naive analogy, energy in a physical system may be compared to water in lakes, rivers and the sea. Only the water that is above the sea level can be used to do work (e.g. propagate a turbine). Entropy represents the water contained in the sea. * In classical physics, the entropy of a physical system is proportional to the quantity of energy no longer available to do physical work. Entropy is central to the second law of thermodynamics, which states that in an isolated system any activity increases the entropy. * In quantum mechanics, von Neumann entropy extends the notion of entropy to quantum systems by means of the density matrix. * In probability theory, the entropy of a random variable measures the uncertainty about the value that might be assumed by the variable. * In information theory, the compression entropy of a message (e.g. a computer file) quantifies the information content carried by the message in terms of the best lossless compression rate. * In the theory of dynamical systems, entropy quantifies the exponential complexity of a dynamical system or the average flow of information per unit of time. * In sociology, entropy is the natural decay of structure (such as law, organization, and convention) in a social system. * In the common sense, entropy means disorder or chaos. ## Contents * 1 History * 2 Entropy in physics * 2.1 Thermodynamical entropy - macroscopic approach * 2.2 Boltzmann entropy and Gibbs entropy - microscopic approach * 2.3 Entropy in quantum mechanics * 2.4 Black hole entropy * 3 Entropy in mathematics * 3.1 Shannon entropy * 3.2 Interpretation of Shannon entropy * 3.3 Properties of the information function and of the Shannon entropy * 3.4 Conditional entropy * 3.5 Properties of the conditional entropy * 3.6 Kolmogorov-Sinai entropy * 3.7 Interpretation of the Kolmogorov-Sinai entropy of a process * 3.8 The main entropy theorems in ergodic theory * 3.9 Topological entropy * 4 Compression entropy * 5 Entropy as disorder * 6 Connections between different meanings of entropy * 7 References * 8 Subpages * 9 External links * 10 See also ## [edit] History The term entropy was coined in 1865 [Cl] by the German physicist Rudolf Clausius from Greek en- = in + trope = a turning (point). The word reveals an analogy to energy and etymologists believe that it was designed to denote the form of energy that any energy eventually and inevitably turns into \-- a useless heat. The idea was inspired by an earlier formulation by Sadi Carnot [Ca] of what is now known as the second law of thermodynamics. The Austrian physicist Ludwig Boltzmann [B] and the American scientist Willard Gibbs [G] put entropy into the probabilistic setup of statistical mechanics (around 1875). This idea was later developed by Max Planck. Entropy was generalized to quantum mechanics in 1932 by John von Neumann [N]. Later this led to the invention of entropy as a term in probability theory by Claude Shannon [Sh] (1948), popularized in a joint book [SW] with Warren Weaver, that provided foundations for information theory. The concept of entropy in dynamical systems was introduced by Andrei Kolmogorov [K] and made precise by Yakov Sinai [Si] in what is now known as the Kolmogorov-Sinai entropy. The formulation of Maxwell's paradox by James C. Maxwell (around 1871) triggered a search for the physical meaning of information, which resulted in the finding by Rolf Landauer [L] (1961) of the heat equivalent of the erasure of one bit of information, which brought the notions of entropy in thermodynamics and information theory together. The term entropy is now used in many other sciences (such as sociology), sometimes distant from physics or mathematics, where it no longer maintains its rigorous quantitative character. Usually, it roughly means disorder, chaos, decay of diversity or tendency toward uniform distribution of kinds. ## [edit] Entropy in physics ### [edit] Thermodynamical entropy - macroscopic approach In thermodynamics, a physical system is a collection of objects (bodies) whose state is parametrized by several characteristics such as the distribution of density, pressure, temperature, velocity, chemical potential, etc. The change of entropy of a physical system when it passes from one state to another equals \\[ \Delta S = \int \frac {dQ}T, \\] where \\(dQ\\) denotes an element of heat being absorbed (or emitted; then it has negative sign) by a body, \\(T\\) is the absolute temperature of that body at that moment, and the integration is over all elements of heat active in the passage. The above formula allows one to compare the entropies of different states of a system, or to compute the entropy of each state up to a constant (which is satisfactory in most cases). The absolute value of entropy is established by the third law of thermodynamics. Notice that when an element \\(dQ\\) of heat is transmitted from a warmer body at temperature \\(T_1\\) to a cooler one at temperature \\(T_2\ ,\\) then the entropy of the first body changes by \\(-\frac {dQ}{T_1}\ ,\\) while that of the other rises by \\(\frac {dQ}{T_2}\ .\\) Since \\(T_2