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Entropy01:18

Entropy

The first law of thermodynamics is quantitatively formulated via an equation relating the internal energy of a system, the heat exchanged by it, and the work done on it. A quantitative formulation of the second law of thermodynamics leads to defining a state function, the entropy.
When an ideal gas expands isothermally, the disorder in the gas increases. From the molecular perspective, the gas molecules have more volume to move around in.
Consider an infinitesimal step in the expansion, which...
Entropy02:39

Entropy

Salt particles that have dissolved in water never spontaneously come back together in solution to reform solid particles. Moreover, a gas that has expanded in a vacuum remains dispersed and never spontaneously reassembles. The unidirectional nature of these phenomena is the result of a thermodynamic state function called entropy (S). Entropy is the measure of the extent to which the energy is dispersed throughout a system, or in other words, it is proportional to the degree of disorder of a...
Entropy and the Second Law of Thermodynamics01:20

Entropy and the Second Law of Thermodynamics

The second law of thermodynamics can be stated quantitatively using the concept of entropy. Entropy is the measure of disorder of the system.
The relation  between entropy and disorder can be illustrated with the example of the phase change of ice to water. In ice, the molecules are located at specific sites giving a solid state, whereas, in a liquid form, these molecules are much freer to move. The molecular arrangement has therefore become more randomized. Although the change in average...
Entropy and the Second Law of Thermodynamics01:26

Entropy and the Second Law of Thermodynamics

Consider an isolated system in which a hot object is placed in contact with a cold one. This is an irreversible process that eventually leads both objects to reach the same equilibrium temperature. It is crucial to note that the constituents of any substance exhibit increased disorder at higher temperatures. As a cold substance absorbs heat, its constituents become more disordered. The energy transfer from a hotter object to a cooler one increases the system's disorder or randomness. This...
The Second Law of Thermodynamics01:14

The Second Law of Thermodynamics

In the quest to identify a property that may reliably predict the spontaneity of a process, a promising candidate has been identified: entropy. Scientists refer to the measure of randomness or disorder within a system as entropy. High entropy means high disorder and low energy. To better understand entropy, think of a student’s bedroom. If no energy or work were put into it, the room would quickly become messy. It would exist in a very disordered state, one of high entropy. Energy must be put...
Entropy Change in Reversible Processes01:10

Entropy Change in Reversible Processes

In the Carnot engine, which achieves the maximum efficiency between two reservoirs of fixed temperatures, the total change in entropy is zero. The observation can be generalized by considering any reversible cyclic process consisting of many Carnot cycles. Thus, it can be stated that the total entropy change of any ideal reversible cycle is zero.
The statement can be further generalized to prove that entropy is a state function. Take a cyclic process between any two points on a p-V diagram.

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Related Experiment Video

Updated: Jun 18, 2026

Unraveling Entropic Rate Acceleration Induced by Solvent Dynamics in Membrane Enzymes
09:42

Unraveling Entropic Rate Acceleration Induced by Solvent Dynamics in Membrane Enzymes

Published on: January 16, 2016

Time-dependent, irreversible entropy production and geodynamics.

Klaus Regenauer-Lieb1, Ali Karrech, Hui Tong Chua

  • 1Western Australian Geothermal Centre of Excellence, University of Western Australia, Western Australia 6009, Australia. klaus.regenauer-lieb@csiro.au

Philosophical Transactions. Series A, Mathematical, Physical, and Engineering Sciences
|December 2, 2009
PubMed
Summary

Entropy production offers a new method to model complex geodynamic processes. This approach provides bounds for planetary heat transfer without needing detailed material data, advancing thermodynamic principles in geosciences.

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Last Updated: Jun 18, 2026

Unraveling Entropic Rate Acceleration Induced by Solvent Dynamics in Membrane Enzymes
09:42

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Published on: January 16, 2016

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Published on: December 4, 2017

Area of Science:

  • Geophysics and Thermodynamics
  • Continuum Mechanics
  • Planetary Science

Background:

  • Geodynamic theories often rely on the principle of maximum entropy production, a restriction of the second law of thermodynamics.
  • Classical limit analysis in continuum mechanics is limited to stress and strain rates, excluding thermal effects.

Purpose of the Study:

  • To introduce entropy production as an abstraction tool for complex geodynamic processes.
  • To extend limit analysis to include temperature-dependent problems and thermal feedbacks.
  • To derive bounds for geodynamic solutions using an entropy balance equation.

Main Methods:

  • Derivation of an entropy balance equation in integral form from the equation of motion and the first law of thermodynamics.
  • Decomposition of entropy into reversible and irreversible terms.
  • Application of the extrema of the entropy balance equation to constrain geodynamic solutions.

Main Results:

  • The proposed method provides upper and lower bounds for geodynamic solutions, extending classical limit analysis.
  • The approach successfully constrains heat transfer processes in a simplified planetary system without detailed material parameters.
  • Thermal feedbacks are shown to play a significant role in temperature-dependent geodynamic problems.

Conclusions:

  • Entropy production serves as a powerful abstraction tool for complex geodynamics, particularly for thermal processes.
  • The method offers a way to derive bounds for self-driven heat transfer in planetary systems.
  • Further refinement is possible by incorporating specific dissipation processes like plasticity and viscous creep.