HEAT CAPACITY RATIO for GASES (G)
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Entropy: Ideal Gas Processes
Chapter 19: The Kinec Theory of Gases Thermodynamics = macroscopic picture Gases micro -> macro picture One mole is the number of atoms in 12 g sample Avogadro’s Number of carbon-12 23 -1 C(12)—6 protrons, 6 neutrons and 6 electrons NA=6.02 x 10 mol 12 atomic units of mass assuming mP=mn Another way to do this is to know the mass of one molecule: then So the number of moles n is given by M n=N/N sample A N = N A mmole−mass € Ideal Gas Law Ideal Gases, Ideal Gas Law It was found experimentally that if 1 mole of any gas is placed in containers that have the same volume V and are kept at the same temperature T, approximately all have the same pressure p. The small differences in pressure disappear if lower gas densities are used. Further experiments showed that all low-density gases obey the equation pV = nRT. Here R = 8.31 K/mol ⋅ K and is known as the "gas constant." The equation itself is known as the "ideal gas law." The constant R can be expressed -23 as R = kNA . Here k is called the Boltzmann constant and is equal to 1.38 × 10 J/K. N If we substitute R as well as n = in the ideal gas law we get the equivalent form: NA pV = NkT. Here N is the number of molecules in the gas. The behavior of all real gases approaches that of an ideal gas at low enough densities. Low densitiens m= enumberans tha oft t hemoles gas molecul es are fa Nr e=nough number apa ofr tparticles that the y do not interact with one another, but only with the walls of the gas container. -
On the Equation of State of an Ideal Monatomic Gas According to the Quantum-Theory, In: KNAW, Proceedings, 16 I, 1913, Amsterdam, 1913, Pp
Huygens Institute - Royal Netherlands Academy of Arts and Sciences (KNAW) Citation: W.H. Keesom, On the equation of state of an ideal monatomic gas according to the quantum-theory, in: KNAW, Proceedings, 16 I, 1913, Amsterdam, 1913, pp. 227-236 This PDF was made on 24 September 2010, from the 'Digital Library' of the Dutch History of Science Web Center (www.dwc.knaw.nl) > 'Digital Library > Proceedings of the Royal Netherlands Academy of Arts and Sciences (KNAW), http://www.digitallibrary.nl' - 1 - 227 high. We are uncertain as to the cause of this differencc: most probably it is due to an nncertainty in the temperature with the absolute manometer. It is of special interest to compare these observations with NERNST'S formula. Tbe fourth column of Table II contains the pressUl'es aceord ing to this formula, calc111ated witb the eonstants whieb FALCK 1) ha~ determined with the data at bis disposal. FALOK found the following expression 6000 1 0,009983 log P • - --. - + 1. 7 5 log T - T + 3,1700 4,571 T . 4,571 where p is the pressure in atmospheres. The correspondence will be se en to be satisfactory considering the degree of accuracy of the observations. 1t does riot look as if the constants could be materially improved. Physics. - "On the equation of state oj an ideal monatomic gflS accoJ'ding to tlw quantum-the01'Y." By Dr. W. H. KEEsmr. Supple ment N°. 30a to the Oommunications ft'om the PhysicaL Labora tory at Leiden. Oommunicated by Prof. H. KAl\IERLINGH ONNES. (Communicated in the meeting of May' 31, 1913). -
Ideal Gasses Is Known As the Ideal Gas Law
ESCI 341 – Atmospheric Thermodynamics Lesson 4 –Ideal Gases References: An Introduction to Atmospheric Thermodynamics, Tsonis Introduction to Theoretical Meteorology, Hess Physical Chemistry (4th edition), Levine Thermodynamics and an Introduction to Thermostatistics, Callen IDEAL GASES An ideal gas is a gas with the following properties: There are no intermolecular forces, except during collisions. All collisions are elastic. The individual gas molecules have no volume (they behave like point masses). The equation of state for ideal gasses is known as the ideal gas law. The ideal gas law was discovered empirically, but can also be derived theoretically. The form we are most familiar with, pV nRT . Ideal Gas Law (1) R has a value of 8.3145 J-mol1-K1, and n is the number of moles (not molecules). A true ideal gas would be monatomic, meaning each molecule is comprised of a single atom. Real gasses in the atmosphere, such as O2 and N2, are diatomic, and some gasses such as CO2 and O3 are triatomic. Real atmospheric gasses have rotational and vibrational kinetic energy, in addition to translational kinetic energy. Even though the gasses that make up the atmosphere aren’t monatomic, they still closely obey the ideal gas law at the pressures and temperatures encountered in the atmosphere, so we can still use the ideal gas law. FORM OF IDEAL GAS LAW MOST USED BY METEOROLOGISTS In meteorology we use a modified form of the ideal gas law. We first divide (1) by volume to get n p RT . V we then multiply the RHS top and bottom by the molecular weight of the gas, M, to get Mn R p T . -
Thermodynamics Molecular Model of a Gas Molar Heat Capacities
Thermodynamics Molecular Model of a Gas Molar Heat Capacities Lana Sheridan De Anza College May 7, 2020 Last time • heat capacities for monatomic ideal gases Overview • heat capacities for diatomic ideal gases • adiabatic processes Quick Recap For all ideal gases: 3 3 K = NK¯ = Nk T = nRT tot,trans trans 2 B 2 and ∆Eint = nCV ∆T For monatomic gases: 3 E = K = nRT int tot,trans 2 and so, 3 C = R V 2 and 5 C = R P 2 Reminder: Kinetic Energy and Internal Energy In a monatomic gas the three translational motions are the only degrees of freedom. We can choose 3 3 E = K = N k T = nRT int tot,trans 2 B 2 (This is the thermal energy, so the bond energy is zero { if we liquify the gas the bond energy becomes negative.) Equipartition Consequences in Diatomic Gases Reminder: Equipartition of energy theorem Each degree of freedom for each molecule contributes an and 1 additional 2 kB T of energy to the system. A monatomic gas has 3 degrees of freedom: it can have translational KE due to motion in 3 independent directions. A diatomic gas has more ways to move and store energy. It can: • translate • rotate • vibrate 21.3 The Equipartition of Energy 635 Equipartition21.3 The Equipartition Consequences of Energy in Diatomic Gases Predictions based on our model for molar specific heat agree quite well with the Contribution to internal energy: Translational motion of behavior of monatomic gases, but not with the behavior of complex gases (see Table the center of mass 21.2). -
Atkins' Physical Chemistry
Statistical thermodynamics 2: 17 applications In this chapter we apply the concepts of statistical thermodynamics to the calculation of Fundamental relations chemically significant quantities. First, we establish the relations between thermodynamic 17.1 functions and partition functions. Next, we show that the molecular partition function can be The thermodynamic functions factorized into contributions from each mode of motion and establish the formulas for the 17.2 The molecular partition partition functions for translational, rotational, and vibrational modes of motion and the con- function tribution of electronic excitation. These contributions can be calculated from spectroscopic data. Finally, we turn to specific applications, which include the mean energies of modes of Using statistical motion, the heat capacities of substances, and residual entropies. In the final section, we thermodynamics see how to calculate the equilibrium constant of a reaction and through that calculation 17.3 Mean energies understand some of the molecular features that determine the magnitudes of equilibrium constants and their variation with temperature. 17.4 Heat capacities 17.5 Equations of state 17.6 Molecular interactions in A partition function is the bridge between thermodynamics, spectroscopy, and liquids quantum mechanics. Once it is known, a partition function can be used to calculate thermodynamic functions, heat capacities, entropies, and equilibrium constants. It 17.7 Residual entropies also sheds light on the significance of these properties. 17.8 Equilibrium constants Checklist of key ideas Fundamental relations Further reading Discussion questions In this section we see how to obtain any thermodynamic function once we know the Exercises partition function. Then we see how to calculate the molecular partition function, and Problems through that the thermodynamic functions, from spectroscopic data. -
REFPROP Documentation Release 10.0
REFPROP Documentation Release 10.0 EWL, IHB, MH, MML May 21, 2018 CONTENTS 1 REFPROP Graphical User Interface3 1.1 General Information...........................................3 1.2 Menu Commands.............................................6 1.3 DLLs................................................... 26 2 REFPROP DLL documentation 27 2.1 High-Level API............................................. 27 2.2 Legacy API................................................ 55 i ii REFPROP Documentation, Release 10.0 REFPROP is an acronym for REFerence fluid PROPerties. This program, developed by the National Institute of Standards and Technology (NIST), calculates the thermodynamic and transport properties of industrially important fluids and their mixtures. These properties can be displayed in Tables and Plots through the graphical user interface; they are also accessible through spreadsheets or user-written applications accessing the REFPROP dll. REFPROP is based on the most accurate pure fluid and mixture models currently available. It implements three models for the thermodynamic properties of pure fluids: equations of state explicit in Helmholtz energy, the modified Benedict-Webb-Rubin equation of state, and an extended corresponding states (ECS) model. Mixture calculations employ a model that applies mixing rules to the Helmholtz energy of the mixture components; it uses a departure function to account for the departure from ideal mixing. Viscosity and thermal conductivity are modeled with either fluid-specific correlations, an ECS method, or in some cases the friction theory method. CONTENTS 1 REFPROP Documentation, Release 10.0 2 CONTENTS CHAPTER ONE REFPROP GRAPHICAL USER INTERFACE 1.1 General Information 1.1.1 About REFPROP REFPROP is an acronym for REFerence fluid PROPerties. This program, developed by the National Institute of Standards and Technology (NIST), calculates the thermodynamic and transport properties of industrially important fluids and their mixtures. -
Physical Chemistry Laboratory, I CHEM 445 Experiment 5 Heat Capacity Ratio for Gases (Revised, 1/10/03)
1 Physical Chemistry Laboratory, I CHEM 445 Experiment 5 Heat Capacity Ratio for Gases (Revised, 1/10/03) The heat capacity for a substance is the amount of heat needed to raise the temperature of the substance by 1 oC or 1 K. The heat capacities depend on the chemical nature of the substance, on the physical state of the substance, on the temperature, and on whether P or V is held constant during the process: CP or CV. For liquids and solids, CV ≈ CP and the two terms are often used interchangeably. However, for ideal gases, it is well known (Tinoco, Jr., Sauer, and Wang or Noggle) that − − CP = CV + R (1) − In this equation, C = molar heat capacity of the gas, either at constant pressure or at constant volume. The bar over a symbol refers to that quantity per mol of substance. The molar heat capacities are defined by the equations, − − − ∂ E − ∂ H CV = and CP = (2) ∂T ∂T V P For a monatomic gas, there is no rotational or vibrational energy and if the temperature is relatively low, only the ground electronic state of the species is populated to any extent. Consequently, only translational energy is involved; and from kinetic theory, − 3R − 5R CV = and CP = (3) 2 2 For polyatomic gases, there are additional forms of energy that contribute to the heat capacity. − − − − E = E(trans) + E(rot) + E(vib) (4) For many simple diatomic molecules, however, the vibrational contribution to the heat 5R capacity is small, and in the neighborhood of room temperature,C = . However, the V 2 heat capacities of diatomic molecules increase with increasing temperature as the vibrational modes become active. -
A Reference Equation of State for the Thermodynamic Properties of Nitrogen for Temperatures from 63.151 to 1000 K and Pressures to 2200 Mpa Roland Span, Eric W
A Reference Equation of State for the Thermodynamic Properties of Nitrogen for Temperatures from 63.151 to 1000 K and Pressures to 2200 MPa Roland Span, Eric W. Lemmon, Richard T Jacobsen, Wolfgang Wagner, and Akimichi Yokozeki Citation: Journal of Physical and Chemical Reference Data 29, 1361 (2000); doi: 10.1063/1.1349047 View online: http://dx.doi.org/10.1063/1.1349047 View Table of Contents: http://scitation.aip.org/content/aip/journal/jpcrd/29/6?ver=pdfcov Published by the AIP Publishing Articles you may be interested in A Reference Equation of State for the Thermodynamic Properties of Ethane for Temperatures from the Melting Line to 675 K and Pressures up to 900 MPa J. Phys. Chem. Ref. Data 35, 205 (2006); 10.1063/1.1859286 A New Functional Form and New Fitting Techniques for Equations of State with Application to Pentafluoroethane (HFC-125) J. Phys. Chem. Ref. Data 34, 69 (2005); 10.1063/1.1797813 The IAPWS Formulation 1995 for the Thermodynamic Properties of Ordinary Water Substance for General and Scientific Use J. Phys. Chem. Ref. Data 31, 387 (2002); 10.1063/1.1461829 New Equation of State for Ethylene Covering the Fluid Region for Temperatures From the Melting Line to 450 K at Pressures up to 300 MPa J. Phys. Chem. Ref. Data 29, 1053 (2000); 10.1063/1.1329318 Thermodynamic Properties of Air and Mixtures of Nitrogen, Argon, and Oxygen From 60 to 2000 K at Pressures to 2000 MPa J. Phys. Chem. Ref. Data 29, 331 (2000); 10.1063/1.1285884 This article is copyrighted as indicated in the article. -
Physical Chemistry I
Physical Chemistry I Andrew Rosen August 19, 2013 Contents 1 Thermodynamics 5 1.1 Thermodynamic Systems and Properties . .5 1.1.1 Systems vs. Surroundings . .5 1.1.2 Types of Walls . .5 1.1.3 Equilibrium . .5 1.1.4 Thermodynamic Properties . .5 1.2 Temperature . .6 1.3 The Mole . .6 1.4 Ideal Gases . .6 1.4.1 Boyle’s and Charles’ Laws . .6 1.4.2 Ideal Gas Equation . .7 1.5 Equations of State . .7 2 The First Law of Thermodynamics 7 2.1 Classical Mechanics . .7 2.2 P-V Work . .8 2.3 Heat and The First Law of Thermodynamics . .8 2.4 Enthalpy and Heat Capacity . .9 2.5 The Joule and Joule-Thomson Experiments . .9 2.6 The Perfect Gas . 10 2.7 How to Find Pressure-Volume Work . 10 2.7.1 Non-Ideal Gas (Van der Waals Gas) . 10 2.7.2 Ideal Gas . 10 2.7.3 Reversible Adiabatic Process in a Perfect Gas . 11 2.8 Summary of Calculating First Law Quantities . 11 2.8.1 Constant Pressure (Isobaric) Heating . 11 2.8.2 Constant Volume (Isochoric) Heating . 11 2.8.3 Reversible Isothermal Process in a Perfect Gas . 12 2.8.4 Reversible Adiabatic Process in a Perfect Gas . 12 2.8.5 Adiabatic Expansion of a Perfect Gas into a Vacuum . 12 2.8.6 Reversible Phase Change at Constant T and P ...................... 12 2.9 Molecular Modes of Energy Storage . 12 2.9.1 Degrees of Freedom . 12 1 2.9.2 Classical Mechanics . -
CHEM 477 Physical Chemistry Laboratory - 2
Colorado State University CHEM 477 Physical Chemistry Laboratory - 2 Notes for Heat-Capacity Ratio of Gases The following is a set of short notes to outline the experiment in question and to provide helpful guidance to those executing the experiment. A. The thermodynamic property of a gas consisting of the ratio of its heat capacity at constant pressure to its heat capacity at constant volume can be readily and accurately measured by the speed of acoustic waves, that is, sound in that gas. This measurement will be performed on several different gases. B. For an ideal gas the heat capacity ratio is understood by thermodynamic analysis of the configuration, that is, the number of motional degrees of freedom, of the gas. C. This is a straight-forward measurement but requires control over a number of experimental variables and a good understanding of related thermodynamics. D. Spend sufficient time learning how to use the apparatus in order to make high- quality measurements of the speed of sound using AIR only. E. Demonstrate to the teaching staff the quality of your measurements BEFORE attempting to use any other gas. F. Determine the relevance of the temperature and the pressure of the gas to the speed of sound within it. There is ample literature available to answer these two separate questions definitively, not trivially. G. Do not confuse heat capacity with heat capacity ratio. These are separate yet related. Your focus ought to be primarily and deeply on the heat capacity ratio. H. Review the reference by Garland et. al. and follow its Results and Discussion topics in your written laboratory report. -
Chapter 10 100 Years of Progress in Gas-Phase Atmospheric Chemistry Research
CHAPTER 10 WALLINGTON ET AL. 10.1 Chapter 10 100 Years of Progress in Gas-Phase Atmospheric Chemistry Research T. J. WALLINGTON Research and Advanced Engineering, Ford Motor Company, Dearborn, Michigan J. H. SEINFELD California Institute of Technology, Pasadena, California J. R. BARKER Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, Michigan ABSTRACT Remarkable progress has occurred over the last 100 years in our understanding of atmospheric chemical composition, stratospheric and tropospheric chemistry, urban air pollution, acid rain, and the formation of airborne particles from gas-phase chemistry. Much of this progress was associated with the developing un- derstanding of the formation and role of ozone and of the oxides of nitrogen, NO and NO2, in the stratosphere and troposphere. The chemistry of the stratosphere, emerging from the pioneering work of Chapman in 1931, was followed by the discovery of catalytic ozone cycles, ozone destruction by chlorofluorocarbons, and the polar ozone holes, work honored by the 1995 Nobel Prize in Chemistry awarded to Crutzen, Rowland, and Molina. Foundations for the modern understanding of tropospheric chemistry were laid in the 1950s and 1960s, stimulated by the eye-stinging smog in Los Angeles. The importance of the hydroxyl (OH) radical and its relationship to the oxides of nitrogen (NO and NO2) emerged. The chemical processes leading to acid rain were elucidated. The atmosphere contains an immense number of gas-phase organic compounds, a result of emissions from plants and animals, natural and anthropogenic combustion processes, emissions from oceans, and from the atmospheric oxidation of organics emitted into the atmosphere. -
Physics 1401 - Final Exam Chapter 13 Review
Physics 1401 - Final Exam Chapter 13 Review 11. The coefficient of linear expansion of steel is 12 ⋅ 10 –6/C°. A railroad track is made of individual rails of steel 1.0 km in length. By what length would these rails change between a cold day when the temperature is –10 °C and a hot day at 30 °C? (a) 0.62 cm (c) 48 cm (e) 620 cm (b) 24 cm (d) 480 cm 12. The coefficient of linear expansion of aluminum is 23 ⋅ 10 –6/C°. A circular hole in an aluminum plate is 2.725 cm in diameter at 0 °C. What is the diameter of the hole if the temperature of the plate is raised to 100 C? (a) 0.0063 cm (c) 2.731 cm (e) 2.788 cm (b) 2.728 cm (d) 2.757 cm 14 . A copper plate has a length of 0.12 m and a width of 0.10 m at 25 °C. The plate is uniformly heated to 175 °C. If the linear expansion coefficient for copper is 1.7 ⋅ 10 –5/C°, what is the change in the area of the plate as a result of the increase in temperature? (a) 2.6 ⋅ 10 –5 m2 (c) 3.2 ⋅ 10 –6 m2 (e) 7.8 ⋅ 10 –7 m2 (b) 6.1 ⋅ 10 –5 m2 (d) 4.9 ⋅ 10 –7 m2 Review Final Exam-New .doc - 1 - 17 . A steel string guitar is strung so that there is negligible tension in the strings at a temperature of 24.9 °C.