The Maxwell-Boltzmann Distribution



Similar documents
1. The Kinetic Theory of Matter states that all matter is composed of atoms and molecules that are in a constant state of constant random motion

KINETIC MOLECULAR THEORY OF MATTER

Study the following diagrams of the States of Matter. Label the names of the Changes of State between the different states.

Kinetic Theory of Gases

Kinetic Theory: Atomic and Molecular Explanation of Pressure and Temperature

Chemistry 13: States of Matter

13.1 The Nature of Gases. What is Kinetic Theory? Kinetic Theory and a Model for Gases. Chapter 13: States of Matter. Principles of Kinetic Theory

A. Kinetic Molecular Theory (KMT) = the idea that particles of matter are always in motion and that this motion has consequences.

Name Date Class STATES OF MATTER. SECTION 13.1 THE NATURE OF GASES (pages )

Chapter 1 Student Reading

Chapter 5 Student Reading

10.7 Kinetic Molecular Theory Kinetic Molecular Theory. Kinetic Molecular Theory. Kinetic Molecular Theory. Kinetic Molecular Theory

Gas Laws. Heat and Temperature

THE KINETIC THEORY OF GASES

HEAT UNIT 1.1 KINETIC THEORY OF GASES Introduction Postulates of Kinetic Theory of Gases

Surface Tension. the surface tension of a liquid is the energy required to increase the surface area a given amount

Chapter Test A. States of Matter MULTIPLE CHOICE. a fixed amount of STAs2 a. a solid. b. a liquid. c. a gas. d. any type of matter.

SAM Teachers Guide Heat and Temperature

There is no such thing as heat energy

Unit 3: States of Matter Practice Exam

VAPORIZATION IN MORE DETAIL. Energy needed to escape into gas phase GAS LIQUID. Kinetic energy. Average kinetic energy

THE IDEAL GAS LAW AND KINETIC THEORY

Multiple Choice For questions 1-10, circle only one answer.

CLASSICAL CONCEPT REVIEW 8

States of Matter CHAPTER 10 REVIEW SECTION 1. Name Date Class. Answer the following questions in the space provided.

7. Gases, Liquids, and Solids 7.1 Kinetic Molecular Theory of Matter

Name Class Date. In the space provided, write the letter of the term or phrase that best completes each statement or best answers each question.

Online Changing States of Matter Lab Solids What is a Solid? 1. How are solids different then a gas or a liquid?

Kinetic Molecular Theory and Gas Laws

Humidity, Condensation, Clouds, and Fog. Water in the Atmosphere

CHAPTER 12. Gases and the Kinetic-Molecular Theory

Convection, Conduction & Radiation

Lesson 6: Earth and the Moon

(1) The size of a gas particle is negligible as compared to the volume of the container in which the gas is placed.

TEACHER BACKGROUND INFORMATION THERMAL ENERGY

Chapter 12 - Liquids and Solids

States of Matter and the Kinetic Molecular Theory - Gr10 [CAPS]

Preview of Period 5: Thermal Energy, the Microscopic Picture

Chapter 18 Temperature, Heat, and the First Law of Thermodynamics. Problems: 8, 11, 13, 17, 21, 27, 29, 37, 39, 41, 47, 51, 57

CHEMISTRY 113 EXAM 4(A)

Chapter 2, Lesson 5: Changing State Melting

Vacuum Evaporation Recap

Solids, Liquids, and Gases

THE HUMIDITY/MOISTURE HANDBOOK

CHEM 120 Online Chapter 7

Modern Construction Materials Prof. Ravindra Gettu Department of Civil Engineering Indian Institute of Technology, Madras

Kinetic Theory of Gases. Chapter 33. Kinetic Theory of Gases

Work and Energy. Work = Force Distance. Work increases the energy of an object. Energy can be converted back to work.

KINDERGARTEN WATER 1 WEEK LESSON PLANS AND ACTIVITIES

SECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES

The Ideal Gas Law. Gas Constant. Applications of the Gas law. P = ρ R T. Lecture 2: Atmospheric Thermodynamics

Temperature Measure of KE At the same temperature, heavier molecules have less speed Absolute Zero -273 o C 0 K

Phys222 W11 Quiz 1: Chapters Keys. Name:

PHYS-2010: General Physics I Course Lecture Notes Section XIII

Thermochemistry. r2 d:\files\courses\ \99heat&thermorans.doc. Ron Robertson

Thermodynamics. Thermodynamics 1

Lecture Notes: Gas Laws and Kinetic Molecular Theory (KMT).

Characteristics of the. thermosphere

Thermodynamics AP Physics B. Multiple Choice Questions

Kinetic Theory & Ideal Gas

EXPERIMENT 15: Ideal Gas Law: Molecular Weight of a Vapor

Practice Test. 4) The planet Earth loses heat mainly by A) conduction. B) convection. C) radiation. D) all of these Answer: C

First Grade Unit A: PHYSICAL SCIENCE Chapter 1: Observing Solids, Liquids and Gases Lessons 1 to 5

1 Introduction. Taking the logarithm of both sides of Equation 1.1:

KINETIC THEORY OF MATTER - molecules in matter are always in motion - speed of molecules is proportional to the temperature

Gas Laws. The kinetic theory of matter states that particles which make up all types of matter are in constant motion.

Calorimetry: Heat of Vaporization

Chapter 2: Forms of Energy

Topic 3b: Kinetic Theory

Chem 112 Intermolecular Forces Chang From the book (10, 12, 14, 16, 18, 20,84,92,94,102,104, 108, 112, 114, 118 and 134)

Phase diagram of water. Note: for H 2 O melting point decreases with increasing pressure, for CO 2 melting point increases with increasing pressure.

Properties and Classifications of Matter

Test 5 Review questions. 1. As ice cools from 273 K to 263 K, the average kinetic energy of its molecules will

Statistical Mechanics, Kinetic Theory Ideal Gas. 8.01t Nov 22, 2004

Melting Range 1 Experiment 2

Preview of Period 2: Forms of Energy

The Gas Laws. Our Atmosphere. Pressure = Units of Pressure. Barometer. Chapter 10

Kinetic Molecular Theory of Matter

atm = 760 torr = 760 mm Hg = kpa = psi. = atm. = atm. = 107 kpa 760 torr 1 atm 760 mm Hg = 790.

Mixtures. reflect. How is seawater different from pure water? How is it different from rocky soil?

Define the notations you are using properly. Present your arguments in details. Good luck!

Chapter 10. Can You draw the Lewis structure for a given covalently bonded molecule?

Chapter 13 - LIQUIDS AND SOLIDS

Why? Intermolecular Forces. Intermolecular Forces. Chapter 12 IM Forces and Liquids. Covalent Bonding Forces for Comparison of Magnitude

Temperature. PJ Brucat

Exam 4 Practice Problems false false

Chapter 17: Change of Phase

Temperature. Number of moles. Constant Terms. Pressure. Answers Additional Questions 12.1

2. Room temperature: C. Kelvin. 2. Room temperature:

Every mathematician knows it is impossible to understand an elementary course in thermodynamics. ~V.I. Arnold

What Is Energy? Energy and Work: Working Together. 124 Chapter 5 Energy and Energy Resources

ES 106 Laboratory # 2 HEAT AND TEMPERATURE

What is Energy? What is the relationship between energy and work?

CHEMISTRY STANDARDS BASED RUBRIC ATOMIC STRUCTURE AND BONDING

The Structure of Water Introductory Lesson

Chapter 4 Practice Quiz

(Walter Glogowski, Chaz Shapiro & Reid Sherman) INTRODUCTION

Chapter 3 Student Reading

CHAPTER 2 Energy and Earth

Review 1. Multiple Choice Identify the choice that best completes the statement or answers the question.

Transcription:

The Maxwell-Boltzmann Distribution Gases are composed of atoms or molecules. These atoms or molecules do not really interact with each other except through collisions. In many cases, we may think of a gas as a collection of tiny billiard balls flying through space, hitting one another again and again. Even if we were to think that all atoms or molecules had the same speed to begin with (although we do not), the constant collisions would result in a spread of many speeds. Some atoms could have very high speeds, others low ones. In real gases at equilibrium there is a distribution of speeds (Fig. E07.4.1). This distribution is called the Maxwell-Boltzmann distribution, and it depends on temperature, as shown. The high temperature curve has proportionally many more fast molecules or atoms than the low temperature curves. As the temperature rises, the highest point on the curve is pushed out to higher v, and the maximum is pushed down toward the axis. All curves shown in Fig. E07.4.1 have a similarity in their shape. Fig. E07.4.1 The number of particles at speed v varies with the absolute temperature, as the shape of the curve changes. However, the distribution really has the same profile; the distribution is pushed to the left and upward as temperature decreases, and is pushed to the right and down as the temperature increases.

Energy, Ch. 7, extension 4 The Maxwell-Boltzmann Distribution 2 It is also possible to show that the average kinetic energy of an atom or molecule, < 1 2 mv2 >, is directly proportional to the absolute temperature T. For example, for a gas of individual atoms such as neon, < 1 2 mv2 > = 3 2 kt, where m is the atomic mass and k is a constant known as Boltzmann s constant. The average of the square of the speed increases with temperature, just as is seen in the curves. We can actually experience the effects of the Maxwell-Boltzmann distribution by performing a few evaporation experiments. What is evaporation, and why does it require energy? Recall that the atoms or molecules of all materials are in constant motion. Materials of course differ. We are generally familiar with three states, or phases, of material: solid, liquid, and gas. To understand evaporation, we must look at the differences among the three phases. In solids, the molecules are cemented into their relative positions despite their incessant motion. There is a structure that is maintained. We are familiar with many solids that have crystalline structure. The symmetry of the crystal reflects the symmetry of the bonds between the atoms or molecules composing the crystal. Most solids do not exhibit such a clearly ordered structure, but they are structured nevertheless. In liquids, the interatomic or intermolecular forces attracting the atoms or molecules to each other are weaker than those in solids. This allows the atoms or molecules to move somewhat in relation to one another, while still keeping the liquid together. This weakened interatomic force is the reason that liquids can take on the shapes of their containers. The attractive force between liquid molecules is evidenced by the phenomenon of surface tension. The beading of water, for example, is due to surface tension. Inside a

Energy, Ch. 7, extension 4 The Maxwell-Boltzmann Distribution 3 liquid, and away from the boundary, molecules are surrounded by other molecules of the same type and are thus attracted in all directions equally. This is another way of saying that there is no net force at all on molecules inside the liquid; those molecules are in equilibrium. For the molecules on or very near the liquid surface, however, attractive forces come only from inside the liquid to act on them. Thus, they are attracted back to the liquid surface should they try to depart. In gases, such as water vapor, the molecules are essentially free to move wherever they are going. That is, the attractive forces are essentially negligible. There is no surface tension. In all these phases, molecules are dancing about in some way. In the solid, the molecules vibrate in various ways about their fixed positions in the solid lattice. In liquids, this dance of the molecules also occurs. Even in transparent liquids, we are not able to see the motion of the liquid molecules. In some liquids that contain very large molecules, the large molecules can be kicked about randomly under the impact of the smaller, invisible liquid molecules. If the molecules are large enough to be seen, we can then see the effect of the random motion on the larger molecules. This visible motion is termed Brownian motion. The properties of materials at temperatures above absolute zero that is, those materials exhibiting the molecular motion are described by distributions giving the relative numbers of molecules at the different speeds of motion possible for the material. The Maxwell-Boltzmann distribution of Fig. E07.1 a illustrates the properties of the distribution of speeds in typical gases or liquids: there is a range of speeds of molecules, and there is a most probable speed at a given temperature. Thus, in any gas or liquid, there are many molecules going fast and many going slow. In fact, the distribution shows

Energy, Ch. 7, extension 4 The Maxwell-Boltzmann Distribution 4 that we can measure the temperature by determining the average molecular speed (see Fig. E07.1 b). Molecules approaching the boundary of a liquid generally are trapped back into the liquid by the surface tension. The very fast molecules may be able to penetrate the surface barrier and escape the liquid altogether. The more surface available, of course, the faster the rate of escape. The rate also increases as the temperature increases because of the boosting of molecules to higher speeds. Fig. E07.4.2 This illustrates what happens to a distribution when almost all the faster particles are suddenly removed. The effect is a cooling, since temperature is a measure of average thermal energy. We may distinguish two sorts of evaporation. In liquids with a relatively small surface area, the liquid absorbs heat from the surroundings to keep the temperature of the liquid fixed as the faster molecules escape. The absorbed heat speeds up some molecules, restoring the original Maxwell-Boltzmann distribution. The total number of molecules in the liquid decreases, but the distribution which depends only on temperature remains the same. In the second sort of evaporation, the surface area is relatively large. Thus, the faster molecules leave the surface rapidly enough that the liquid cannot absorb enough heat to restore the original distribution. In this case of non-equilibrium evaporation, the distribution quickly becomes truncated. (It looks as shown in Fig. E07.4.2). Since the absolute temperature measures the average kinetic energy of a gas, a departure of high-

Energy, Ch. 7, extension 4 The Maxwell-Boltzmann Distribution 5 kinetic-energy molecules, shown in Fig. E07.4.2, will cause a thermometer to record a lower temperature. This effect is enhanced when the material in question has a smaller surface tension. For example, the effect is much greater for alcohol than for water. Conversely, the temperature drop is much smaller for a liquid with a large surface tension. Lubricating oil exhibits a tiny temperature drop compared to water. Gasoline spilled on our hands makes the skin feel cool because the gasoline molecules evaporate rapidly. This effect can easily be seen with tap water, a paper towel, and a thermometer able to register temperatures around 10 C to 20 C. Wet the towel and wrap it around the bulb of the thermometer. You should be able to observe a decrease in temperature of a few degrees. The Maxwell-Boltzmann distribution can also be used to explain how the hydrogen and helium originally in Earth s atmosphere disappeared, while the nitrogen and oxygen show little sign of imminent departure. Recall that for a gas of individual atoms < 1 2 mv2 > = 3 2 kt. For a gas of molecules such as oxygen and nitrogen, which have two atoms in a molecule, a similar relation, < 1 2 mv2 > = 5 2 kt, holds. The atmosphere s temperature changes little on average from year to year; for a fixed T, the smaller m is, the larger < v 2 > will be. The square root of < v 2 >, called the root-mean-square speed (v rms ) is a measure of how fast the atoms or molecules are whizzing around. The root-mean-square speed for hydrogen is 14 times as great as that for nitrogen because the mass of the nitrogen molecule is fourteen times that of hydrogen. Similarly, the root-mean-square speed of helium is 7 times as great as that for nitrogen because the mass of a nitrogen molecule is seven times that of a helium atom. In fact, the

Energy, Ch. 7, extension 4 The Maxwell-Boltzmann Distribution 6 root-mean-square speeds in Earth s atmosphere of hydrogen, helium, nitrogen, and oxygen are, respectively, 1.93 km/s, 1.37 km/s, 0.52 km/s, and 0.48 km/s. Escape speed is the speed an object has to go to escape Earth s gravity. Escape speed for Earth is only 11.2 km/s. A rocket ship to Mars must go at a speed greater than 11.2 km/s to escape from Earth. If a gas molecule has a speed in excess of 11.2 km/s, it will escape totally from Earth. Hydrogen and helium have a mean speed that is a significant fraction of the escape speed. For this reason, there is almost no hydrogen or helium in Earth s present atmosphere. Because of the rapid (exponential) decrease in number of particles with increasing speed, the distribution tells us that there are proportionally about a million times more hydrogen molecules with speeds exceeding 11.2 km/s than nitrogen molecules. Because of the large volume of the atmosphere, the loss of hydrogen molecules proceeds in a quasi-equilibrium fashion, with slower molecules gaining energy and the distribution preserving its shape. After a geologically short time, almost all hydrogen will have escaped, while practically no nitrogen will have been lost.