1.
Carnot heat engine
–
A Carnot heat engine is an engine that operates on the reversible Carnot cycle. The basic model for this engine was developed by Nicolas Léonard Sadi Carnot in 1824, the Carnot engine model was graphically expanded upon by Benoît Paul Émile Clapeyron in 1834 and mathematically elaborated upon by Rudolf Clausius in 1857 from which the concept of entropy emerged. Every thermodynamic system exists in a particular state, a thermodynamic cycle occurs when a system is taken through a series of different states, and finally returned to its initial state. In the process of going through this cycle, the system may perform work on its surroundings, a heat engine acts by transferring energy from a warm region to a cool region of space and, in the process, converting some of that energy to mechanical work. The cycle may also be reversed, in the adjacent diagram, from Carnots 1824 work, Reflections on the Motive Power of Fire, there are two bodies A and B, kept each at a constant temperature, that of A being higher than that of B. These two bodies to which we can give, or from which we can remove the heat without causing their temperatures to vary, exercise the functions of two unlimited reservoirs of caloric. We will call the first the furnace and the second the refrigerator. ”Carnot then explains how we can obtain power, i. e. “work”. It also acts as a cooler and hence can also act as a Refrigerator, the previous image shows the original piston-and-cylinder diagram used by Carnot in discussing his ideal engines. The figure at right shows a diagram of a generic heat engine. In the diagram, the “working body”, an introduced by Clausius in 1850. Carnot had postulated that the body could be any substance capable of expansion, such as vapor of water, vapor of alcohol, vapor of mercury. The output work W here is the movement of the piston as it is used to turn a crank-arm, Carnot defined work as “weight lifted through a height”. The Carnot cycle when acting as a heat engine consists of the steps, Reversible isothermal expansion of the gas at the hot temperature. During this step the gas is allowed to expand and it work on the surroundings. The temperature of the gas does not change during the process, the gas expansion is propelled by absorption of heat energy Q1 and of entropy Δ S H = Q H / T H from the high temperature reservoir. For this step the piston and cylinder are assumed to be thermally insulated, the gas continues to expand, doing work on the surroundings, and losing an equivalent amount of internal energy. The gas expansion causes it to cool to the cold temperature, Reversible isothermal compression of the gas at the cold temperature, TC. Now the surroundings do work on the gas, causing an amount of heat energy Q2, once again the piston and cylinder are assumed to be thermally insulated
Carnot heat engine
–
Axial cross section of Carnot's heat engine. In this diagram, abcd is a cylindrical vessel, cd is a movable
piston, and A and B are constant–temperature bodies. The vessel may be placed in contact with either body or removed from both (as it is here).
2.
Carnot cycle
–
The Carnot cycle is a theoretical thermodynamic cycle proposed by Nicolas Léonard Sadi Carnot in 1824 and expanded upon by others in the 1830s and 1840s. It is not an actual thermodynamic cycle but is a theoretical construct, every single thermodynamic system exists in a particular state. When a system is taken through a series of different states and finally returned to its initial state, in the process of going through this cycle, the system may perform work on its surroundings, thereby acting as a heat engine. A system undergoing a Carnot cycle is called a Carnot heat engine, although such an engine is only a theoretical construct. However, a microscopic Carnot heat engine has been designed and run, essentially, there are two systems at temperatures Th and Tc, which are so large that their temperatures are practically unaffected by a single cycle. As such, they are called heat reservoirs, since the cycle is reversible, there is no generation of entropy during the cycle, entropy is conserved. During the cycle, an amount of entropy ΔS is extracted from the hot reservoir. The difference in the two energies ΔS is equal to the work done by the engine, the Carnot cycle when acting as a heat engine consists of the following steps, Reversible isothermal expansion of the gas at the hot temperature, T1. During this step the gas is allowed to expand and it work on the surroundings. The temperature of the gas does not change during the process, the gas expansion is propelled by absorption of heat energy Q1 from the high temperature reservoir and results in an increase of entropy of the gas in the amount Δ S1 = Q1 / T1. For this step the mechanisms of the engine are assumed to be thermally insulated, the gas continues to expand, doing work on the surroundings, and losing an amount of internal energy equal to the work that leaves the system. The gas expansion causes it to cool to the cold temperature, Reversible isothermal compression of the gas at the cold temperature, T2. Once again the mechanisms of the engine are assumed to be thermally insulated, at this point the gas is in the same state as at the start of step 1. In this case, Δ S1 = Δ S2, or and this is true as Q2 and T2 are both lower and in fact are in the same ratio as Q1 / T1. For a simple closed system, any point on the graph represent a particular state of the system. A thermodynamic process will consist of a curve connecting an initial state, the area under the curve will be, Q = ∫ A B T d S which is the amount of thermal energy transferred in the process. If the process moves to greater entropy, the area under the curve will be the amount of absorbed by the system in that process. If the process moves towards lesser entropy, it will be the amount of heat removed, for any cyclic process, there will be an upper portion of the cycle and a lower portion
Carnot cycle
–
Figure 1: A Carnot cycle illustrated on a
PV diagram to illustrate the work done.
3.
Statistical mechanics
–
Statistical mechanics is a branch of theoretical physics using probability theory to study the average behaviour of a mechanical system, where the state of the system is uncertain. A common use of mechanics is in explaining the thermodynamic behaviour of large systems. This branch of mechanics, which treats and extends classical thermodynamics, is known as statistical thermodynamics or equilibrium statistical mechanics. Statistical mechanics also finds use outside equilibrium, an important subbranch known as non-equilibrium statistical mechanics deals with the issue of microscopically modelling the speed of irreversible processes that are driven by imbalances. Examples of such processes include chemical reactions or flows of particles, in physics there are two types of mechanics usually examined, classical mechanics and quantum mechanics. Statistical mechanics fills this disconnection between the laws of mechanics and the experience of incomplete knowledge, by adding some uncertainty about which state the system is in. The statistical ensemble is a probability distribution over all states of the system. In classical statistical mechanics, the ensemble is a probability distribution over phase points, in quantum statistical mechanics, the ensemble is a probability distribution over pure states, and can be compactly summarized as a density matrix. These two meanings are equivalent for many purposes, and will be used interchangeably in this article, however the probability is interpreted, each state in the ensemble evolves over time according to the equation of motion. Thus, the ensemble itself also evolves, as the systems in the ensemble continually leave one state. The ensemble evolution is given by the Liouville equation or the von Neumann equation, one special class of ensemble is those ensembles that do not evolve over time. These ensembles are known as equilibrium ensembles and their condition is known as statistical equilibrium, Statistical equilibrium occurs if, for each state in the ensemble, the ensemble also contains all of its future and past states with probabilities equal to the probability of being in that state. The study of equilibrium ensembles of isolated systems is the focus of statistical thermodynamics, non-equilibrium statistical mechanics addresses the more general case of ensembles that change over time, and/or ensembles of non-isolated systems. The primary goal of thermodynamics is to derive the classical thermodynamics of materials in terms of the properties of their constituent particles. Whereas statistical mechanics proper involves dynamics, here the attention is focussed on statistical equilibrium, Statistical equilibrium does not mean that the particles have stopped moving, rather, only that the ensemble is not evolving. A sufficient condition for statistical equilibrium with a system is that the probability distribution is a function only of conserved properties. There are many different equilibrium ensembles that can be considered, additional postulates are necessary to motivate why the ensemble for a given system should have one form or another. A common approach found in textbooks is to take the equal a priori probability postulate
Statistical mechanics
–
Statistical mechanics
4.
Chemical thermodynamics
–
Chemical thermodynamics is the study of the interrelation of heat and work with chemical reactions or with physical changes of state within the confines of the laws of thermodynamics. The structure of chemical thermodynamics is based on the first two laws of thermodynamics, starting from the first and second laws of thermodynamics, four equations called the fundamental equations of Gibbs can be derived. From these four, a multitude of equations, relating the thermodynamic properties of the system can be derived using relatively simple mathematics. This outlines the framework of chemical thermodynamics. Gibbs’ collection of papers provided the first unified body of thermodynamic theorems from the principles developed by others, such as Clausius, the first was the 1923 textbook Thermodynamics and the Free Energy of Chemical Substances by Gilbert N. Lewis and Merle Randall. This book was responsible for supplanting the chemical affinity with the free energy in the English-speaking world. The second was the 1933 book Modern Thermodynamics by the methods of Willard Gibbs written by E. A. Guggenheim, the primary objective of chemical thermodynamics is the establishment of a criterion for the determination of the feasibility or spontaneity of a given transformation. The 3 laws of thermodynamics, The energy of the universe is constant, breaking or making of chemical bonds involves energy or heat, which may be either absorbed or evolved from a chemical system. Energy that can be released because of a reaction between a set of substances is equal to the difference between the energy content of the products and the reactants. This change in energy is called the change in energy of a chemical reaction. The change in energy is a process which is equal to the heat change if it is measured under conditions of constant volume. Another useful term is the heat of combustion, which is the energy released due to a combustion reaction, food is similar to hydrocarbon fuel and carbohydrate fuels, and when it is oxidized, its caloric content is similar. In chemical thermodynamics the term used for the potential energy is chemical potential. Even for homogeneous bulk materials, the energy functions depend on the composition, as do all the extensive thermodynamic potentials. If the quantities, the number of species, are omitted from the formulae. For a bulk system they are the last remaining extensive variables, the expression for dG is especially useful at constant T and P, conditions which are easy to achieve experimentally and which approximates the condition in living creatures T, P = ∑ i μ i d N i. While this formulation is mathematically defensible, it is not particularly transparent since one does not simply add or remove molecules from a system. There is always a process involved in changing the composition, e. g. a chemical reaction and we should find a notation which does not seem to imply that the amounts of the components can be changed independently
Chemical thermodynamics
–
J. Willard Gibbs - founder of chemical thermodynamics
Chemical thermodynamics
–
History
5.
Equilibrium thermodynamics
–
Equilibrium Thermodynamics is the systematic study of transformations of matter and energy in systems in terms of a concept called thermodynamic equilibrium. The word equilibrium implies a state of balance, Equilibrium thermodynamics, in origins, derives from analysis of the Carnot cycle. Here, typically a system, as cylinder of gas, initially in its own state of thermodynamic equilibrium, is set out of balance via heat input from a combustion reaction. Then, through a series of steps, as the system settles into its equilibrium state. In an equilibrium state the potentials, or driving forces, within the system, are in exact balance, an equilibrium state is mathematically ascertained by seeking the extrema of a thermodynamic potential function, whose nature depends on the constraints imposed on the system. For example, a reaction at constant temperature and pressure will reach equilibrium at a minimum of its components Gibbs free energy. In equilibrium thermodynamics, by contrast, the state of the system will be considered uniform throughout, defined macroscopically by such quantities as temperature, pressure, systems are studied in terms of change from one equilibrium state to another, such a change is called a thermodynamic process. Ruppeiner geometry is a type of information used to study thermodynamics. It claims that thermodynamic systems can be represented by Riemannian geometry, non-equilibrium thermodynamics Thermodynamics Adkins, C. J. Equilibrium Thermodynamics, 3rd Ed. & Boles, M. Thermodynamics – an Engineering Approach, 4th Ed, modern Thermodynamics – From Heat Engines to Dissipative Structures. New York, John Wiley & Sons
Equilibrium thermodynamics
6.
Non-equilibrium thermodynamics
–
Non-equilibrium thermodynamics is concerned with transport processes and with the rates of chemical reactions. It relies on what may be thought of as more or less nearness to thermodynamic equilibrium, non-equilibrium thermodynamics is a work in progress, not an established edifice. This article will try to sketch some approaches to it and some concepts important for it, some systems and processes are, however, in a useful sense, near enough to thermodynamic equilibrium to allow description with useful accuracy by currently known non-equilibrium thermodynamics. Nevertheless, many systems and processes will always remain far beyond the scope of non-equilibrium thermodynamic methods. This is because of the small size of atoms, as compared with macroscopic systems. The thermodynamic study of systems requires more general concepts than are dealt with by equilibrium thermodynamics. Another fundamental and very important difference is the difficulty or impossibility in defining entropy at an instant of time in terms for systems not in thermodynamic equilibrium. A profound difference separates equilibrium from non-equilibrium thermodynamics, equilibrium thermodynamics ignores the time-courses of physical processes. In contrast, non-equilibrium thermodynamics attempts to describe their time-courses in continuous detail, equilibrium thermodynamics restricts its considerations to processes that have initial and final states of thermodynamic equilibrium, the time-courses of processes are deliberately ignored. For example, in thermodynamics, a process is allowed to include even a violent explosion that cannot be described by non-equilibrium thermodynamics. Equilibrium thermodynamics does, however, for development, use the idealized concept of the quasi-static process. A quasi-static process is a conceptual smooth mathematical passage along a path of states of thermodynamic equilibrium. It is an exercise in differential geometry rather than a process that could occur in actuality, non-equilibrium thermodynamics, on the other hand, attempting to describe continuous time-courses, need its state variables to have a very close connection with those of equilibrium thermodynamics. This profoundly restricts the scope of thermodynamics, and places heavy demands on its conceptual framework. The suitable relationship that defines non-equilibrium thermodynamic state variables is as follows and it is necessary that measuring probes be small enough, and rapidly enough responding, to capture relevant non-uniformity. In reality, these requirements are demanding, and it may be difficult or practically, or even theoretically. This is part of why non-equilibrium thermodynamics is a work in progress, non-equilibrium thermodynamics is a work in progress, not an established edifice. This article will try to sketch some approaches to it and some concepts important for it, one problem of interest is the thermodynamic study of non-equilibrium steady states, in which entropy production and some flows are non-zero, but there is no time variation of physical variables
Non-equilibrium thermodynamics
7.
Laws of thermodynamics
–
The four laws of thermodynamics define fundamental physical quantities that characterize thermodynamic systems at thermal equilibrium. The laws describe how these quantities behave under various circumstances, the four laws of thermodynamics are, Zeroth law of thermodynamics, If two systems are in thermal equilibrium with a third system, they are in thermal equilibrium with each other. This law helps define the notion of temperature, first law of thermodynamics, When energy passes, as work, as heat, or with matter, into or out from a system, the systems internal energy changes in accord with the law of conservation of energy. Equivalently, perpetual motion machines of the first kind are impossible, second law of thermodynamics, In a natural thermodynamic process, the sum of the entropies of the interacting thermodynamic systems increases. Equivalently, perpetual motion machines of the second kind are impossible, third law of thermodynamics, The entropy of a system approaches a constant value as the temperature approaches absolute zero. With the exception of non-crystalline solids the entropy of a system at zero is typically close to zero. There have been suggestions of additional laws, but none of them achieves the generality of the four accepted laws, the laws of thermodynamics are important fundamental laws in physics and they are applicable in other natural sciences. The zeroth law of thermodynamics may be stated in the following form, the law is intended to allow the existence of an empirical parameter, the temperature, as a property of a system such that systems in thermal equilibrium with each other have the same temperature. Though this version of the law is one of the commonly stated. Some statements go further so as to supply the important physical fact that temperature is one-dimensional, hence it was numbered the zeroth law. The importance of the law as a foundation to the laws is that it allows the definition of temperature in a non-circular way without reference to entropy. Such a temperature definition is said to be empirical, the first law of thermodynamics may be stated in several ways, The increase in internal energy of a closed system is equal to total of the energy added to the system. In particular, if the energy entering the system is supplied as heat and energy leaves the system as work, the heat is accounted as positive and this states that energy can be neither created nor destroyed. However, energy can change forms, and energy can flow from one place to another, a particular consequence of the law of conservation of energy is that the total energy of an isolated system does not change. The concept of energy and its relationship to temperature. If a system has a temperature, then its total energy has three distinguishable components. If the system is in motion as a whole, it has kinetic energy, If the system as a whole is in an externally imposed force field, it has potential energy relative to some reference point in space. Finally, it has energy, which is a fundamental quantity of thermodynamics
Laws of thermodynamics
8.
Zeroth law of thermodynamics
–
The zeroth law of thermodynamics states that if two thermodynamic systems are each in thermal equilibrium with a third, then they are in thermal equilibrium with each other. Accordingly, thermal equilibrium between systems is a transitive relation, two systems are said to be in the relation of thermal equilibrium if they are linked by a wall permeable only to heat and they do not change over time. The physical meaning of the law was expressed by Maxwell in the words, for this reason, another statement of the law is All diathermal walls are equivalent. The law is important for the formulation of thermodynamics, which needs the assertion that the relation of thermal equilibrium is an equivalence relation. This information is needed for a definition of temperature that will agree with the physical existence of valid thermometers. A thermodynamic system is by definition in its own state of thermodynamic equilibrium. One precise statement of the law is that the relation of thermal equilibrium is an equivalence relation on pairs of thermodynamic systems. This means that a tag can be assigned to every system. This property is used to justify the use of temperature as a tagging system. This statement asserts that thermal equilibrium is a relation between thermodynamic systems. If we also define that every system is in thermal equilibrium with itself. Binary relations that are both reflexive and Euclidean are equivalence relations, one consequence of an equivalence relationship is that the equilibrium relationship is symmetric, If A is in thermal equilibrium with B, then B is in thermal equilibrium with A. Thus we may say that two systems are in equilibrium with each other, or that they are in mutual equilibrium. A reflexive, transitive relationship does not guarantee an equivalence relationship, in order for the above statement to be true, both reflexivity and symmetry must be implicitly assumed. It is the Euclidean relationships which apply directly to thermometry, an ideal thermometer is a thermometer which does not measurably change the state of the system it is measuring. The zeroth law provides no information regarding this final reading, the zeroth law establishes thermal equilibrium as an equivalence relationship. An equivalence relationship on a set divides that set into a collection of distinct subsets where any member of the set is a member of one, in the case of the zeroth law, these subsets consist of systems which are in mutual equilibrium. This partitioning allows any member of the subset to be tagged with a label identifying the subset to which it belongs
Zeroth law of thermodynamics
9.
First law of thermodynamics
–
The first law of thermodynamics is a version of the law of conservation of energy, adapted for thermodynamic systems. The law of conservation of energy states that the energy of an isolated system is constant, energy can be transformed from one form to another. Equivalently, perpetual motion machines of the first kind are impossible, investigations into the nature of heat and work and their relationship began with the invention of the first engines used to extract water from mines. Improvements to such engines so as to increase their efficiency and power output came first from mechanics that worked with such machines, deeper investigations that placed those on a mathematical and physics basis came later. The first law of thermodynamics was developed empirically over about half a century, the first full statements of the law came in 1850 from Rudolf Clausius and from William Rankine, Rankines statement is less distinct relative to Clausius. A main aspect of the struggle was to deal with the previously proposed caloric theory of heat, in 1840, Germain Hess stated a conservation law for the so-called heat of reaction for chemical reactions. His law was recognized as a consequence of the first law of thermodynamics. The primitive notion of heat was taken as established, especially through calorimetry regarded as a subject in its own right. Jointly primitive with this notion of heat were the notions of empirical temperature and this framework also took as primitive the notion of transfer of energy as work. This framework did not presume a concept of energy in general, by one author, this framework has been called the thermodynamic approach. The first explicit statement of the first law of thermodynamics, by Rudolf Clausius in 1850, because of its definition in terms of increments, the value of the internal energy of a system is not uniquely defined. It is defined only up to an additive constant of integration. This non-uniqueness is in keeping with the mathematical nature of the internal energy. The internal energy is customarily stated relative to a conventionally chosen standard reference state of the system, the concept of internal energy is considered by Bailyn to be of enormous interest. Its quantity cannot be measured, but can only be inferred. Bailyn likens it to the states of an atom, that were revealed by Bohrs energy relation hν = En − En. In each case, a quantity is revealed by considering the difference of measured quantities. In 1907, George H. Bryan wrote about systems between which there is no transfer of matter, Definition, when energy flows from one system or part of a system to another otherwise than by the performance of mechanical work, the energy so transferred is called heat
First law of thermodynamics
10.
Second law of thermodynamics
–
The second law of thermodynamics states that the total entropy of an isolated system can only increase over time. It can remain constant in ideal cases where the system is in a state or undergoing a reversible process. The increase in entropy accounts for the irreversibility of processes. Historically, the law was an empirical finding that was accepted as an axiom of thermodynamic theory. Statistical thermodynamics, classical or quantum, explains the origin of the law. The second law has been expressed in many ways and its first formulation is credited to the French scientist Sadi Carnot in 1824, who showed that there is an upper limit to the efficiency of conversion of heat to work in a heat engine. The first law of thermodynamics provides the definition of internal energy, associated with all thermodynamic systems. The second law is concerned with the direction of natural processes and it asserts that a natural process runs only in one sense, and is not reversible. For example, heat flows spontaneously from hotter to colder bodies. Its modern definition is in terms of entropy, different notations are used for infinitesimal amounts of heat and infinitesimal amounts of entropy because entropy is a function of state, while heat, like work, is not. For an actually possible infinitesimal process without exchange of matter with the surroundings, the second law allows a distinguished temperature scale, which defines an absolute, thermodynamic temperature, independent of the properties of any particular reference thermometric body. These statements cast the law in general physical terms citing the impossibility of certain processes, the Clausius and the Kelvin statements have been shown to be equivalent. The historical origin of the law of thermodynamics was in Carnots principle. The Carnot engine is a device of special interest to engineers who are concerned with the efficiency of heat engines. Interpreted in the light of the first law, it is equivalent to the second law of thermodynamics. It states The efficiency of a quasi-static or reversible Carnot cycle depends only on the temperatures of the two reservoirs, and is the same, whatever the working substance. A Carnot engine operated in this way is the most efficient possible heat engine using those two temperatures, the German scientist Rudolf Clausius laid the foundation for the second law of thermodynamics in 1850 by examining the relation between heat transfer and work. The statement by Clausius uses the concept of passage of heat, as is usual in thermodynamic discussions, this means net transfer of energy as heat, and does not refer to contributory transfers one way and the other
Second law of thermodynamics
–
Nicolas Léonard Sadi Carnot in the traditional uniform of a student of the
École Polytechnique.
Second law of thermodynamics
–
Derive Kelvin Statement from Clausius Statement
Second law of thermodynamics
–
Rudolf Clausius
Second law of thermodynamics
–
James Clerk Maxwell
11.
Third law of thermodynamics
–
Entropy is related to the number of accessible microstates, and for a system consisting of many particles, quantum mechanics indicates that there is only one unique state with minimum energy. The constant value is called the entropy of the system. Here a condensed system refers to liquids and solids, a classical formulation by Nernst is, It is impossible for any process, no matter how idealized, to reduce the entropy of a system to its absolute-zero value in a finite number of operations. It was proven in 2017 by Masanes and Oppenheim, the 3rd law was developed by the chemist Walther Nernst during the years 1906–12, and is therefore often referred to as Nernsts theorem or Nernsts postulate. The third law of thermodynamics states that the entropy of a system at zero is a well-defined constant. This is because a system at zero temperature exists in its ground state, in 1912 Nernst stated the law thus, It is impossible for any procedure to lead to the isotherm T =0 in a finite number of steps. An alternative version of the law of thermodynamics as stated by Gilbert N. This version states not only ΔS will reach zero at 0 K, some crystals form defects which causes a residual entropy. This residual entropy disappears when the barriers to transitioning to one ground state are overcome. With the development of mechanics, the third law of thermodynamics changed from a fundamental law to a derived law. The counting of states is from the state of absolute zero. In simple terms, the law states that the entropy of a perfect crystal of a pure substance approaches zero as the temperature approaches zero. The alignment of a perfect crystal leaves no ambiguity as to the location and orientation of each part of the crystal, as the energy of the crystal is reduced, the vibrations of the individual atoms are reduced to nothing, and the crystal becomes the same everywhere. The third law provides a reference point for the determination of entropy at any other temperature. The entropy of a system, determined relative to this point, is then the absolute entropy of that system. Mathematically, the entropy of any system at zero temperature is the natural log of the number of ground states times Boltzmanns constant kB =1. 38×10−23 J K−1. The entropy of a crystal lattice as defined by Nernsts theorem is zero provided that its ground state is unique. As a result, the initial value of zero is selected S0 =0 is used for convenience
Third law of thermodynamics
–
Fig.1 Left side: Absolute zero can be reached in a finite number of steps if S (0, X 1)≠ S (0, X 2). Right: An infinite number of steps is needed since S (0, X 1)= S (0, X 2).
Third law of thermodynamics
12.
Thermodynamic system
–
Usually, by default, a thermodynamic system is taken to be in its own internal state of thermodynamic equilibrium, as opposed to a non-equilibrium state. The thermodynamic system is enclosed by walls that separate it from its surroundings. The thermodynamic state of a system is its internal state as specified by its state variables. In addition to the variables, a thermodynamic account also requires a special kind of quantity called a state function. For example, if the variables are internal energy, volume and mole amounts. These quantities are inter-related by one or more functional relationships called equations of state, thermodynamics imposes restrictions on the possible equations of state and on the characteristic equation. The restrictions are imposed by the laws of thermodynamics, the only states considered in equilibrium thermodynamics are equilibrium states. In 1824 Sadi Carnot described a system as the working substance of any heat engine under study. The very existence of such systems may be considered a fundamental postulate of equilibrium thermodynamics. According to Bailyn, the commonly rehearsed statement of the law of thermodynamics is a consequence of this fundamental postulate. In equilibrium thermodynamics the state variables do not include fluxes because in a state of thermodynamic equilibrium all fluxes have zero values by postulation, non-equilibrium thermodynamics allows its state variables to include non-zero fluxes, that describe transfers of matter or energy or entropy between a system and its surroundings. Thermodynamic equilibrium is characterized by absence of flow of matter or energy, equilibrium thermodynamics, as a subject in physics, considers macroscopic bodies of matter and energy in states of internal thermodynamic equilibrium. It uses the concept of thermodynamic processes, by which bodies pass from one state to another by transfer of matter. The term thermodynamic system is used to refer to bodies of matter, the possible equilibria between bodies are determined by the physical properties of the walls that separate the bodies. Equilibrium thermodynamics in general does not measure time, equilibrium thermodynamics is a relatively simple and well settled subject. One reason for this is the existence of a well defined quantity called the entropy of a body. It is characterized by presence of flows of matter and energy, for this topic, very often the bodies considered have smooth spatial inhomogeneities, so that spatial gradients, for example a temperature gradient, are well enough defined. Thus the description of thermodynamic systems is a field theory
Thermodynamic system
–
This article needs additional citations for
verification. Please help improve this article by
adding citations to reliable sources. Unsourced material may be challenged and removed. (December 2010)
13.
Thermodynamic state
–
Once such a set of values of thermodynamic variables has been specified for a system, the values of all thermodynamic properties of the system are uniquely determined. Usually, by default, a state is taken to be one of thermodynamic equilibrium. This means that the state is not merely the condition of the system at a specific time, Thermodynamics sets up an idealized formalism that can be summarized by a system of postulates of thermodynamics. A thermodynamic system is not simply a physical system, a thermodynamic system is a macroscopic object, the microscopic details of which are not explicitly considered in its thermodynamic description. The number of state variables required to specify the state depends on the system. Always the number is two or more, usually it is not more than some dozen, the choice is usually made on the basis of the walls and surroundings that are relevant for the thermodynamic processes that are to be considered for the system. For Planck, the characteristic of a thermodynamic state of a system that consists of a single phase. Such non-equilibrium identifying state variables indicate that some non-zero flow may be occurring within the system or between system and surroundings and they are uniquely determined by the thermodynamic state as it has been identified by the original state variables. For an idealized continuous or quasi-static process, this means that infinitesimal incremental changes in such variables are exact differentials, together, the incremental changes throughout the process, and the initial and final states, fully determine the idealized process. In the most commonly cited example, an ideal gas. Thus the thermodynamic state would range over a state space. The remaining variable, as well as other such as the internal energy. The state functions satisfy certain constraints, expressed in the laws of thermodynamics. Various thermodynamic diagrams have been developed to model the transitions between thermodynamic states, physical systems found in nature are practically always dynamic and complex, but in many cases, macroscopic physical systems are amenable to description based on proximity to ideal conditions. One such ideal condition is that of an equilibrium state. Such a state is an object of classical or equilibrium thermodynamics. Based on many observations, thermodynamics postulates that all systems that are isolated from the environment will evolve so as to approach unique stable equilibrium states. A few different types of equilibrium are listed below, thermal Equilibrium, When the temperature throughout a system is uniform, the system is in thermal equilibrium
Thermodynamic state
14.
Equation of state
–
In physics and thermodynamics, an equation of state is a thermodynamic equation relating state variables which describes the state of matter under a given set of physical conditions. It is an equation which provides a mathematical relationship between two or more state functions associated with the matter, such as its temperature, pressure, volume. Equations of state are useful in describing the properties of fluids, mixtures of fluids, solids, the most prominent use of an equation of state is to correlate densities of gases and liquids to temperatures and pressures. One of the simplest equations of state for this purpose is the gas law. However, this becomes increasingly inaccurate at higher pressures and lower temperatures. Therefore, a number of more accurate equations of state have been developed for gases, at present, there is no single equation of state that accurately predicts the properties of all substances under all conditions. Measurements of equation-of-state parameters, especially at pressures, can be made using lasers. In addition, there are equations of state describing solids. There are equations that model the interior of stars, including stars, dense matter. A related concept is the perfect fluid equation of state used in cosmology, in practical context, the equations of state are instrumental for PVT calculation in process engineering problems and especially in petroleum gas/liquid equilibrium calculations. A successful PVT model based on an equation of state can be helpful to determine the state of the flow regime. Boyles Law was perhaps the first expression of an equation of state, in 1662, the Irish physicist and chemist Robert Boyle performed a series of experiments employing a J-shaped glass tube, which was sealed on one end. Mercury was added to the tube, trapping a fixed quantity of air in the short, then the volume of gas was measured as additional mercury was added to the tube. The pressure of the gas could be determined by the difference between the level in the short end of the tube and that in the long. Through these experiments, Boyle noted that the gas volume varied inversely with the pressure, in mathematical form, this can be stated as, p V = c o n s t a n t. The above relationship has also attributed to Edme Mariotte and is sometimes referred to as Mariottes law. However, Mariottes work was not published until 1676, in 1787 the French physicist Jacques Charles found that oxygen, nitrogen, hydrogen, carbon dioxide, and air expand to roughly the same extent over the same 80 kelvin interval. Later, in 1802, Joseph Louis Gay-Lussac published results of similar experiments, daltons Law of partial pressure states that the pressure of a mixture of gases is equal to the sum of the pressures of all of the constituent gases alone
Equation of state
–
State
15.
Ideal gas
–
An ideal gas is a theoretical gas composed of many randomly moving point particles whose only interaction is perfectly elastic collision. The ideal gas concept is useful because it obeys the ideal gas law, an equation of state. One mole of a gas has a volume of 22.710947 litres at STP as defined by IUPAC since 1982. At normal conditions such as temperature and pressure, most real gases behave qualitatively like an ideal gas. Many gases such as nitrogen, oxygen, hydrogen, noble gases, the ideal gas model tends to fail at lower temperatures or higher pressures, when intermolecular forces and molecular size become important. It also fails for most heavy gases, such as many refrigerants, at high pressures, the volume of a real gas is often considerably greater than that of an ideal gas. At low temperatures, the pressure of a gas is often considerably less than that of an ideal gas. At some point of low temperature and high pressure, real gases undergo a phase transition, the model of an ideal gas, however, does not describe or allow phase transitions. These must be modeled by more complex equations of state, the deviation from the ideal gas behaviour can be described by a dimensionless quantity, the compressibility factor, Z. The ideal gas model has been explored in both the Newtonian dynamics and in quantum mechanics, the ideal gas model has also been used to model the behavior of electrons in a metal, and it is one of the most important models in statistical mechanics. There are three classes of ideal gas, the classical or Maxwell–Boltzmann ideal gas, the ideal quantum Bose gas, composed of bosons. The classical ideal gas can be separated into two types, The classical thermodynamic ideal gas and the ideal quantum Boltzmann gas. The ideal quantum Boltzmann gas overcomes this limitation by taking the limit of the quantum Bose gas, the behavior of a quantum Boltzmann gas is the same as that of a classical ideal gas except for the specification of these constants. The ideal gas law is an extension of experimentally discovered gas laws, real fluids at low density and high temperature approximate the behavior of a classical ideal gas. This deviation is expressed as a compressibility factor, the classical thermodynamic properties of an ideal gas can be described by two equations of state. Multiplying the equations representing the three laws, V ∗ V ∗ V = k b a Gives, V ∗ V ∗ V =, under ideal conditions, V = R, that is, P V = n R T. The other equation of state of an ideal gas must express Joules law, in order to switch from macroscopic quantities to microscopic ones, we use n R = N k B where N is the number of gas particles kB is the Boltzmann constant. The probability distribution of particles by velocity or energy is given by the Maxwell speed distribution, the assumption of spherical particles is necessary so that there are no rotational modes allowed, unlike in a diatomic gas
Ideal gas
16.
Real gas
–
Real gases are non-hypothetical gases whose molecules occupy space and have interactions, consequently, they adhere to gas laws. The deviation from ideality can be described by the compressibility factor Z and it is almost always more accurate than the van der Waals equation, and often more accurate than some equations with more than two parameters. The equation is R T = or alternatively, p = R T V m − b − a T V m where a and b two empirical parameters that are not the parameters as in the van der Waals equation. The Virial equation derives from a treatment of statistical mechanics. P V m = R T or alternatively p V m = R T where A, B, C, A′, B′, Peng–Robinson equation of state has the interesting property being useful in modeling some liquids as well as real gases. Note that the γ constant is a derivative of constant α, englewood Cliffs, New Jersey 07632,1993. ISBN 0-13-275702-8 Stanley M. Walas, Phase Equilibria in Chemical Engineering, ISBN 0-409-95162-5 M. Aznar, and A. Silva Telles, A Data Bank of Parameters for the Attractive Coefficient of the Peng–Robinson Equation of State, Braz. Eng. vol.14 no.1 São Paulo Mar.1997, rao The corresponding-states principle and its practice, thermodynamic, transport and surface properties of fluids by Hong Wei Xiang http, //www. ccl. net/cca/documents/dyoung/topics-orig/eq_state. html
Real gas
17.
State of matter
–
In physics, a state of matter is one of the distinct forms that matter takes on. Four states of matter are observable in everyday life, solid, liquid, gas, some other states are believed to be possible but remain theoretical for now. For a complete list of all states of matter, see the list of states of matter. Historically, the distinction is based on qualitative differences in properties. Matter in the state maintains a fixed volume and shape, with component particles close together. Matter in the state maintains a fixed volume, but has a variable shape that adapts to fit its container. Its particles are close together but move freely. Matter in the state has both variable volume and shape, adapting both to fit its container. Its particles are close together nor fixed in place. Matter in the state has variable volume and shape, but as well as neutral atoms, it contains a significant number of ions and electrons. Plasma is the most common form of matter in the universe. The term phase is used as a synonym for state of matter. In a solid the particles are packed together. The forces between particles are strong so that the particles move freely but can only vibrate. As a result, a solid has a stable, definite shape, solids can only change their shape by force, as when broken or cut. In crystalline solids, the particles are packed in a regularly ordered, there are various different crystal structures, and the same substance can have more than one structure. For example, iron has a cubic structure at temperatures below 912 °C. Ice has fifteen known crystal structures, or fifteen solid phases, glasses and other non-crystalline, amorphous solids without long-range order are not thermal equilibrium ground states, therefore they are described below as nonclassical states of matter
State of matter
–
A crystalline solid: atomic resolution image of
strontium titanate. Brighter atoms are
Sr and darker ones are
Ti.
State of matter
–
In a plasma, electrons are ripped away from their nuclei, forming an electron "sea". This gives it the ability to conduct electricity.
State of matter
–
SBS block copolymer in
TEM
State of matter
–
Liquid
helium in a superfluid phase creeps up on the walls of the cup in a
Rollin film, eventually dripping out from the cup.
18.
Thermodynamic equilibrium
–
Thermodynamic equilibrium is an axiomatic concept of thermodynamics. It is an state of a single thermodynamic system, or a relation between several thermodynamic systems connected by more or less permeable or impermeable walls. In thermodynamic equilibrium there are no net macroscopic flows of matter or of energy, in a system in its own state of internal thermodynamic equilibrium, no macroscopic change occurs. Systems in mutual thermodynamic equilibrium are simultaneously in mutual thermal, mechanical, chemical, Systems can be in one kind of mutual equilibrium, though not in others. In thermodynamic equilibrium, all kinds of equilibrium hold at once and indefinitely, in a macroscopic equilibrium, almost or perfectly exactly balanced microscopic exchanges occur, this is the physical explanation of the notion of macroscopic equilibrium. A thermodynamic system in its own state of thermodynamic equilibrium has a spatially uniform temperature. Its intensive properties, other than temperature, may be driven to spatial inhomogeneity by a long range force field imposed on it by its surroundings. In non-equilibrium systems, by contrast, there are net flows of matter or energy, If such changes can be triggered to occur in a system in which they are not already occurring, it is said to be in a metastable equilibrium. Though it is not a widely named law, it is an axiom of thermodynamics that there exist states of thermodynamic equilibrium, Classical thermodynamics deals with states of dynamic equilibrium. The state of a system at equilibrium is the one for which some thermodynamic potential is minimized, or for which the entropy is maximized. Thermodynamic equilibrium is the stable stationary state that is approached or eventually reached as the system interacts with its surroundings over a long time. The above-mentioned potentials are mathematically constructed to be the thermodynamic quantities that are minimized under the conditions in the specified surroundings. For a completely isolated system, S is maximum at thermodynamic equilibrium, for a system with controlled constant temperature and volume, A is minimum at thermodynamic equilibrium. For a system with controlled constant temperature and pressure, G is minimum at thermodynamic equilibrium, the various types of equilibriums are achieved as follows, Two systems are in thermal equilibrium when their temperatures are the same. Two systems are in equilibrium when their pressures are the same. Two systems are in equilibrium when their chemical potentials are the same. All forces are balanced and there is no significant external driving force, often the surroundings of a thermodynamic system may also be regarded as another thermodynamic system. In this view, one may consider the system and its surroundings as two systems in contact, with long-range forces also linking them
Thermodynamic equilibrium
19.
Control volume
–
In continuum mechanics and thermodynamics, a control volume is a mathematical abstraction employed in the process of creating mathematical models of physical processes. In an inertial frame of reference, it is a volume fixed in space or moving with constant flow velocity through which the continuum flows, the surface enclosing the control volume is referred to as the control surface. At steady state, a volume can be thought of as an arbitrary volume in which the mass of the continuum remains constant. As a continuum moves through the volume, the mass entering the control volume is equal to the mass leaving the control volume. At steady state, and in the absence of work and heat transfer and it is analogous to the classical mechanics concept of the free body diagram. Typically, to understand how a physical law applies to the system under consideration, one first begins by considering how it applies to a small, control volume. There is nothing special about a particular volume, it simply represents a small part of the system to which physical laws can be easily applied. This gives rise to what is termed a volumetric, or volume-wise formulation of the mathematical model, in this way, the corresponding point-wise formulation of the mathematical model can be developed so it can describe the physical behaviour of an entire system. In continuum mechanics the equations are in integral form. Finding forms of the equation that are independent of the control volumes allows simplification of the integral signs, computations in continuum mechanics often require that the regular time derivation operator d / d t is replaced by the substantive derivative operator D / D t. This can be seen as follows, consider a bug that is moving through a volume where there is some scalar, e. g. pressure, that varies with time and position, p = p. If the bug is just moving with the flow, the formula applies. The last parenthesized expression is the derivative of the scalar pressure. Since the pressure p in this computation is a scalar field, we may abstract it
Control volume
20.
Thermodynamic instruments
–
A thermodynamic instrument is any device which facilitates the quantitative measurement of thermodynamic systems. In order for a parameter to be truly defined, a technique for its measurement must be specified. For example, the definition of temperature is what a thermometer reads. The question follows - what is a thermometer, there are two types of thermodynamic instruments, the meter and the reservoir. A thermodynamic meter is any device which measures any parameter of a thermodynamic system, a thermodynamic reservoir is a system which is so large that it does not appreciably alter its state parameters when brought into contact with the test system. Two general complementary tools are the meter and the reservoir and it is important that these two types of instruments are distinct. A meter does not perform its task accurately if it behaves like a reservoir of the variable it is trying to measure. If, for example, a thermometer, were to act as a reservoir it would alter the temperature of the system being measured. Ideal meters have no effect on the variables of the system they are measuring. A meter is a system which displays some aspect of its thermodynamic state to the observer. The nature of its contact with the system it is measuring can be controlled, the theoretical thermometer described below is just such a meter. In some cases, the parameter is actually defined in terms of an idealized measuring instrument. For example, the law of thermodynamics states that if two bodies are in thermal equilibrium with a third body, they are also in thermal equilibrium with each other. This principle, as noted by James Maxwell in 1872, asserts that it is possible to measure temperature, an idealized thermometer is a sample of an ideal gas at constant pressure. From the ideal gas law, the volume of such a sample can be used as an indicator of temperature, although pressure is defined mechanically, a pressure-measuring device called a barometer may also be constructed from a sample of an ideal gas held at a constant temperature. A calorimeter is a device which is used to measure and define the energy of a system. Some common thermodynamic meters are, Thermometer - a device which measures temperature as described above Barometer - a device which measures pressure, an ideal gas barometer may be constructed by mechanically connecting an ideal gas to the system being measured, while thermally insulating it. The volume will then measure pressure, by the ideal gas equation P=NkT/V, calorimeter - a device which measures the heat energy added to a system
Thermodynamic instruments
21.
Thermodynamic process
–
Classical thermodynamics considers three main kinds of thermodynamic process, change in a system, cycles in a system, and flow processes. Defined by change in a system, a process is a passage of a thermodynamic system from an initial to a final state of thermodynamic equilibrium. The initial and final states are the elements of the process. The actual course of the process is not the primary concern and this is the customary default meaning of the term thermodynamic process. Such processes are useful for thermodynamic theory, defined by a cycle of transfers into and out of a system, a cyclic process is described by the quantities transferred in the several stages of the cycle, which recur unchangingly. The descriptions of the states of the system are not the primary concern. Cyclic processes were important conceptual devices in the days of thermodynamical investigation. Defined by flows through a system, a process is a steady state of flows into. The internal state of the contents is not the primary concern. The quantities of primary concern describe the states of the inflow and the materials, and, on the side, the transfers of heat, work. Flow processes are of interest in engineering, defined by change in a system, a thermodynamic process is a passage of a thermodynamic system from an initial to a final state of thermodynamic equilibrium. The initial and final states are the elements of the process. The actual course of the process is not the primary concern, a state of thermodynamic equilibrium endures unchangingly unless it is interrupted by a thermodynamic operation that initiates a thermodynamic process. Then it may be described by a process function that does depend on the path. Such idealized processes are useful in the theory of thermodynamics, defined by a cycle of transfers into and out of a system, a cyclic process is described by the quantities transferred in the several stages of the cycle. The descriptions of the states of the system may be of little or even no interest. A cycle is a sequence of a number of thermodynamic processes that indefinitely often repeatedly returns the system to its original state. For this, the states themselves are not necessarily described
Thermodynamic process
–
An example of a series of thermodynamic processes which make up the
Stirling cycle
22.
Isobaric process
–
An isobaric process is a thermodynamic process in which the pressure stays constant, ΔP =0. The heat transferred to the system work, but also changes the internal energy of the system. This article uses the sign convention for work, where positive work is work done on the system. Using this convention, by the first law of thermodynamics, Q = Δ U − W where W is work, U is internal energy, and Q is heat. Pressure-volume work by the system is defined as, W = − ∫ p d V where Δ means change over the whole process. Since pressure is constant, this means that W = − p Δ V. Applying the ideal gas law, this becomes W = − n R Δ T assuming that the quantity of gas stays constant, e. g. there is no phase transition during a chemical reaction. According to the theorem, the change in internal energy is related to the temperature of the system by Δ U = n c V Δ T. Substituting the last two equations into the first equation produces, Q = n c V Δ T + n R Δ T = n Δ T = n c P Δ T, where cP is specific heat at a constant pressure. To find the specific heat capacity of the gas involved. The property γ is either called the index or the heat capacity ratio. Some published sources might use k instead of γ, molar isochoric specific heat, c V = R γ −1. Molar isobaric specific heat, c p = γ R γ −1, the values for γ are γ = 7/5 for diatomic gases like air and its major components, and γ = 5/3 for monatomic gases like the noble gases. If the process moves towards the right, then it is an expansion, if the process moves towards the left, then it is a compression. The motivation for the specific conventions of thermodynamics comes from early development of heat engines. When designing an engine, the goal is to have the system produce. The source of energy in an engine, is a heat input. If the volume compresses, then W <0 and that is, during isobaric compression the gas does negative work, or the environment does positive work
Isobaric process
–
The yellow area represents the work done
23.
Isochoric process
–
The isochoric process here should be a quasi-static process. An isochoric thermodynamic process is characterized by constant volume, i. e. ΔV =0, the process does no pressure-volume work, since such work is defined by Δ W = P Δ V, where P is pressure. The sign convention is such that work is performed by the system on the environment. If the process is not quasi-static, the work can perhaps be done in a volume constant thermodynamic process, where cv is the specific heat capacity at constant volume, T1 is the initial temperature and T2 is the final temperature. We conclude with, Δ Q = m c v Δ T On a pressure volume diagram and its thermodynamic conjugate, an isobaric process would appear as a straight horizontal line. If an ideal gas is used in a process. Take for example a gas heated in a container, the pressure and temperature of the gas will increase. The ideal Otto cycle is an example of a process when it is assumed that the burning of the gasoline-air mixture in an internal combustion engine car is instantaneous. There is an increase in the temperature and the pressure of the gas inside the cylinder while the remains the same. The noun isochor and the adjective isochoric are derived from the Greek words ἴσος meaning equal, isobaric process Adiabatic process Cyclic process Isothermal process Polytropic process http, //lorien. ncl. ac. uk/ming/webnotes/Therm1/revers/isocho. htm
Isochoric process
–
Isochoric process in the
pressure volume diagram. In this diagram, pressure increases, but volume remains constant.
24.
Isothermal process
–
An isothermal process is a change of a system, in which the temperature remains constant, ΔT =0. In contrast, a process is where a system exchanges no heat with its surroundings. In other words, in a process, the value ΔT =0 and therefore ΔU =0 but Q ≠0, while in an adiabatic process. Isothermal processes can occur in any kind of system that has some means of regulating the temperature, including highly structured machines, some parts of the cycles of some heat engines are carried out isothermally. In the thermodynamic analysis of reactions, it is usual to first analyze what happens under isothermal conditions. Phase changes, such as melting or evaporation, are also isothermal processes when, as is usually the case, isothermal processes are often used and a starting point in analyzing more complex, non-isothermal processes. Isothermal processes are of special interest for ideal gases and this is a consequence of Joules second law which states that the internal energy of a fixed amount of an ideal gas depends only on its temperature. Thus, in a process the internal energy of an ideal gas is constant. This is a result of the fact that in a gas there are no intermolecular forces. Note that this is only for ideal gases, the internal energy depends on pressure as well as on temperature for liquids, solids. In the isothermal compression of a gas there is work is done on the system to decrease the volume, doing work on the gas increases the internal energy and will tend to increase the temperature. To maintain the constant temperature energy must leave the system as heat, if the gas is ideal, the amount of energy entering the environment is equal to the work done on the gas, because internal energy does not change. For details of the calculations, see calculation of work, for an adiabatic process, in which no heat flows into or out of the gas because its container is well insulated, Q =0. If there is no work done, i. e. a free expansion. For an ideal gas, this means that the process is also isothermal, thus, specifying that a process is isothermal is not sufficient to specify a unique process. For the special case of a gas to which Boyles law applies, the value of the constant is nRT, where n is the number of moles of gas present and R is the ideal gas constant. In other words, the gas law pV = nRT applies. This means that p = n R T V = constant V holds, the family of curves generated by this equation is shown in the graph in Figure 1
Isothermal process
–
Several isotherms of an ideal gas on a p-V diagram
25.
Adiabatic process
–
In thermodynamics, an adiabatic process is one that occurs without transfer of heat or matter between a thermodynamic system and its surroundings. In an adiabatic process, energy is transferred only as work, the adiabatic process provides a rigorous conceptual basis for the theory used to expound the first law of thermodynamics, and as such it is a key concept in thermodynamics. The adiabatic flame temperature is the temperature that would be achieved by a if the process of combustion took place in the absence of heat loss to the surroundings. A process that does not involve the transfer of heat or matter into or out of a system, so that Q =0, is called an adiabatic process, the assumption that a process is adiabatic is a frequently made simplifying assumption. Even though the cylinders are not insulated and are quite conductive, the same can be said to be true for the expansion process of such a system. The assumption of adiabatic isolation of a system is a useful one, the behaviour of actual machines deviates from these idealizations, but the assumption of such perfect behaviour provide a useful first approximation of how the real world works. According to Laplace, when sound travels in a gas, there is no loss of heat in the medium and the propagation of sound is adiabatic. For this adiabatic process, the modulus of elasticity E = γP where γ is the ratio of specific heats at constant pressure and at constant volume, such a process is called an isentropic process and is said to be reversible. Fictively, if the process is reversed, the energy added as work can be recovered entirely as work done by the system, if the walls of a system are not adiabatic, and energy is transferred in as heat, entropy is transferred into the system with the heat. Such a process is neither adiabatic nor isentropic, having Q >0, naturally occurring adiabatic processes are irreversible. The transfer of energy as work into an isolated system can be imagined as being of two idealized extreme kinds. In one such kind, there is no entropy produced within the system, in nature, this ideal kind occurs only approximately, because it demands an infinitely slow process and no sources of dissipation. The other extreme kind of work is work, for which energy is added as work solely through friction or viscous dissipation within the system. The second law of thermodynamics observes that a process, of transfer of energy as work, always consists at least of isochoric work. Every natural process, adiabatic or not, is irreversible, with ΔS >0, the adiabatic compression of a gas causes a rise in temperature of the gas. Adiabatic expansion against pressure, or a spring, causes a drop in temperature, in contrast, free expansion is an isothermal process for an ideal gas. Adiabatic heating occurs when the pressure of a gas is increased from work done on it by its surroundings and this finds practical application in diesel engines which rely on the lack of quick heat dissipation during their compression stroke to elevate the fuel vapor temperature sufficiently to ignite it. Adiabatic heating occurs in the Earths atmosphere when an air mass descends, for example, in a wind, Foehn wind
Adiabatic process
–
For a simple substance, during an adiabatic process in which the volume increases, the
internal energy of the working substance must decrease
26.
Isentropic process
–
Such an idealized process is useful in engineering as a model of and basis of comparison for real processes. The word isentropic is occasionally, though not customarily, interpreted in another way and this is contrary to its original and customarily used definition. The second law of thermodynamics states that, T d S ≥ δ Q where δ Q is the amount of energy the system gains by heating, T is the temperature of the system, and d S is the change in entropy. The equal sign refers to a process, which is an imagined idealized theoretical limit. For an isentropic process, which by definition is reversible, there is no transfer of energy as heat because the process is adiabatic, for reversible processes, an isentropic transformation is carried out by thermally insulating the system from its surroundings. The entropy of a given mass does not change during a process that is internally reversible, a process during which the entropy remains constant is called an isentropic process, written △ s =0 or s 1 = s 2. Some isentropic thermodynamic devices include, pumps, gas compressors, turbines, nozzles, real world cycles have inherent losses due to inefficient compressors and turbines. The real world system are not truly isentropic but are rather idealized as isentropic for calculation purposes, in fluid dynamics, an isentropic flow is a fluid flow that is both adiabatic and reversible. That is, no heat is added to the flow, for an isentropic flow of a perfect gas, several relations can be derived to define the pressure, density and temperature along a streamline. Note that energy can be exchanged with the flow in an isentropic transformation, an example of such an exchange would be an isentropic expansion or compression that entails work done on or by the flow. For an isentropic flow, entropy density can vary between different streamlines, if the entropy density is the same everywhere, then the flow is said to be homentropic. All reversible adiabatic processes are isentropic, for any transformation of an ideal gas, it is always true that d U = n C v d T, and d H = n C p d T. Using the general results derived above for d U and d H, then d U = n C v d T = − p d V, and d H = n C p d T = V d p. So for a gas, the heat capacity ratio can be written as. Hence on integrating the above equation, assuming a perfect gas, we get p V γ = constant i. e. H. S. J. and Sonntag, fundamentals of Classical Thermodynamics, John Wiley & Sons, Inc. Library of Congress Catalog Card Number, 65-19470
Isentropic process
–
T-s (Entropy vs. Temperature) diagram of an isentropic process, which is a vertical line segment.
27.
Isenthalpic process
–
An isenthalpic process or isoenthalpic process is a process that proceeds without any change in enthalpy, H, or specific enthalpy, h. The throttling process is an example of an isenthalpic process. Consider the lifting of a valve or safety valve on a pressure vessel. The specific enthalpy of the fluid inside the vessel is the same as the specific enthalpy of the fluid as it escapes from the valve. With a knowledge of the enthalpy of the fluid. Sonntag, Fundamentals of Classical Thermodynamics, John Wiley & Sons, Inc
Isenthalpic process
28.
Quasistatic process
–
In thermodynamics, a quasi-static process is a thermodynamic process that happens slowly enough for the system to remain in internal equilibrium. An example of this is quasi-static compression, where the volume of a system changes at a slow enough to allow the pressure to remain uniform. Any reversible process is necessarily a quasi-static one, however, quasi-static processes involving entropy production are irreversible. Some ambiguity exists in the literature concerning the distinction between quasi-static and reversible processes, as these are taken as synonyms. The reason is the theorem that any process is also a quasi-static one. The definition given above is closer to the understanding of the word “quasi-” “static”
Quasistatic process
29.
Polytropic process
–
A polytropic process is a thermodynamic process that obeys the relation, p v n = C where p is the pressure, v is specific volume, n is the polytropic index, and C is a constant. The polytropic process equation can describe multiple expansion and compression processes which include heat transfer, in addition, when the ideal gas law applies, n =1 is an isothermic process, n = γ is an adiabatic process. Consider an ideal gas in a system undergoing a slow process with negligible changes in kinetic. Assuming K remain constant during the transformation, as d f f = d this relation can be integrated as d =0 ⟶ p v K + γ = C where C is a constant. Thus, the process is polytropic, with the coefficient n = K + γ and this derivation can be expanded to include polytropic processes in open systems, including instances where the kinetic energy is significant. It can also be expanded to include polytropic processes. For certain values of the index, the process will be synonymous with other common processes. Some examples of the effects of varying index values are given in the table, when the index n is between any two of the former values, it means that the polytropic curve will cut through the curves of the two bounding indices. For an ideal gas,1 < γ <2, since by Mayers relation γ = c p c v = c v + R c v =1 + R c v = c p c p − R. A solution to the Lane–Emden equation using a fluid is known as a polytrope
Polytropic process
Polytropic process
30.
Free expansion
–
Free expansion is an irreversible process in which a gas expands into an insulated evacuated chamber. It is also called Joule expansion, real gases experience a temperature change during free expansion. Since the gas expands, Vf > Vi, which implies that the pressure does drop, during free expansion, no work is done by the gas. The gas goes through states that are not in thermodynamic equilibrium before reaching its final state, for example, the pressure changes locally from point to point, and the volume occupied by the gas is not a well defined quantity. A free expansion is achieved by opening a stopcock that allows the gas to expand into a vacuum. Although it would be difficult to achieve in reality, it is instructive to imagine a free expansion caused by moving a piston faster than virtually any atom, no work is done because there is no pressure on the piston. No heat energy leaves or enters the piston, nevertheless, there is an entropy change. But the well-known formula for change, Δ S = ∫ d Q r e v T
Free expansion
–
A free expansion of a gas can be achieved by moving the piston out faster than the fastest atoms in the gas.