John C. Kotz Paul M. Treichel John Townsend http://academic.cengage.com/kotz Chapter 11 Gases and Their Properties John C. Kotz • State University of New York, College at Oneonta Important – Read Before Using Slides in Class Instructor: This PowerPoint presentation contains photos and figures from the text, as well as selected animations and videos. For animations and videos to run properly, we recommend that you run this PowerPoint presentation from the PowerLecture disc inserted in your computer. Also, for the mathematical symbols to display properly, you must install the supplied font called “Symb_chm,” supplied as a cross-platform TrueType font in the “Font_for_Lectures” folder in the "Media" folder on this disc. If you prefer to customize the presentation or run it without the PowerLecture disc inserted, the animations and videos will only run properly if you also copy the associated animation and video files for each chapter onto your computer. Follow these steps: 1. Go to the disc drive directory containing the PowerLecture disc, and then to the “Media” folder, and then to the “PowerPoint_Lectures” folder. 2. In the “PowerPoint_Lectures” folder, copy the entire chapter folder to your computer. Chapter folders are named “chapter1”, “chapter2”, etc. Each chapter folder contains the PowerPoint Lecture file as well as the animation and video files. For assistance with installing the fonts or copying the animations and video files, please visit our Technical Support at http://academic.cengage.com/support or call (800) 423-0563. Thank you. BEHAVIOR OF GASES Chapter 11 © 2009 Brooks/Cole - Cengage 3 Importance of Gases PLAY MOVIE • Airbags fill with N2 gas in an accident. • Gas is generated by the decomposition of sodium azide, NaN3. • 2 NaN3 f 2 Na + 3 N2 © 2009 Brooks/Cole - Cengage 4 5 Hot Air Balloons — How Do They Work? PLAY MOVIE © 2009 Brooks/Cole - Cengage 6 THREE STATES OF MATTER PLAY MOVIE © 2009 Brooks/Cole - Cengage General Properties of Gases • There is a lot of “free” space in a gas. • Gases can be expanded infinitely. • Gases occupy containers uniformly and completely. • Gases diffuse and mix rapidly. © 2009 Brooks/Cole - Cengage 7 8 Properties of Gases Gas properties can be modeled using math. Model depends on— • • • • © 2009 Brooks/Cole - Cengage V = volume of the gas (L) T = temperature (K) n = amount (moles) P = pressure (atmospheres) Pressure Pressure of air is measured with a BAROMETER (developed by Torricelli in 1643) © 2009 Brooks/Cole - Cengage 9 Pressure Hg rises in tube until force of Hg (down) balances the force of atmosphere (pushing up). P of Hg pushing down related to • Hg density • column height © 2009 Brooks/Cole - Cengage 10 Pressure Column height measures P of atmosphere • 1 standard atm = 760 mm Hg = 29.9 inches Hg = about 34 feet of water SI unit is PASCAL, Pa, where 1 atm = 101.325 kPa © 2009 Brooks/Cole - Cengage 11 IDEAL GAS LAW P V = n R T Brings together gas properties. Can be derived from experiment and theory. © 2009 Brooks/Cole - Cengage 12 13 Boyle’s Law If n and T are constant, then PV = (nRT) = k This means, for example, that P goes up as V goes down. © 2009 Brooks/Cole - Cengage Robert Boyle (1627-1691). Son of Earl of Cork, Ireland. Boyle’s Law A bicycle pump is a good example of Boyle’s law. As the volume of the air trapped in the pump is reduced, its pressure goes up, and air is forced into the tire. PLAY MOVIE © 2009 Brooks/Cole - Cengage 14 15 Charles’s Law If n and P are constant, then V = (nR/P)T = kT V and T are directly related. © 2009 Brooks/Cole - Cengage Jacques Charles (17461823). Isolated boron and studied gases. Balloonist. 16 Charles’s original balloon Modern long-distance balloon © 2009 Brooks/Cole - Cengage 17 Charles’s Law Balloons immersed in liquid N2 (at -196 ˚C) will shrink as the air cools (and is liquefied). © 2009 Brooks/Cole - Cengage Charles’s Law PLAY MOVIE © 2009 Brooks/Cole - Cengage 18 Avogadro’s Hypothesis Equal volumes of gases at the same T and P have the same number of molecules. V = n (RT/P) = kn V and n are directly related. twice as many molecules © 2009 Brooks/Cole - Cengage 19 20 Avogadro’s Hypothesis f PLAY MOVIE The gases in this experiment are all measured at the same T and P. 2 H2(g) + O2(g) © 2009 Brooks/Cole - Cengage f 2 H2O(g) 21 Combining the Gas Laws • • • • • V proportional to 1/P V prop. to T V prop. to n Therefore, V prop. to nT/P V = 22.4 L for 1.00 mol when – Standard pressure and temperature (STP) – T = 273 K – P = 1.00 atm © 2009 Brooks/Cole - Cengage Using PV = nRT How much N2 is req’d to fill a small room with a volume of 960 cubic feet (27,000 L) to P = 745 mm Hg at 25 oC? R = 0.082057 L•atm/K•mol Solution 1. Get all data into proper units V = 27,000 L T = 25 oC + 273 = 298 K P = 745 mm Hg (1 atm/760 mm Hg) = 0.98 atm © 2009 Brooks/Cole - Cengage 22 Using PV = nRT How much N2 is req’d to fill a small room with a volume of 960 cubic feet (27,000 L) to P = 745 mm Hg at 25 oC? R = 0.082057 L•atm/K•mol Solution 2. Now calc. n = PV / RT (0.974 atm)(2.7 x 104 L) n= (0.0821 Lįatm/Kįmol)(298 K) n = 1.1 x 103 mol (or about 30 kg of gas) © 2009 Brooks/Cole - Cengage 23 24 Gases and Stoichiometry 2 H2O2(liq) f 2 H2O(g) + O2(g) Decompose 0.11 g of H2O2 in a flask with a volume of 2.50 L. What is the pressure of O2 at 25 oC? Of H2O? Bombardier beetle uses decomposition of hydrogen peroxide to defend itself. © 2009 Brooks/Cole - Cengage 25 Gases and Stoichiometry 2 H2O2(liq) f 2 H2O(g) + O2(g) Decompose 0.11 g of H2O2 in a flask with a volume of 2.50 L. What is the pressure of O2 at 25 oC? Of H2O? Solution Strategy: Calculate moles of H2O2 and then moles of O2 and H2O. Finally, calc. P from n, R, T, and V. © 2009 Brooks/Cole - Cengage 26 Gases and Stoichiometry 2 H2O2(liq) f 2 H2O(g) + O2(g) Decompose 0.11 g of H2O2 in a flask with a volume of 2.50 L. What is the pressure of O2 at 25 oC? Of H2O? Solution 1 mol 0.11 g H2O2 0.0032 mol 34.0 g 1 mol O 2 0.0032 mol H2O2 = 0.0016 mol O2 2 mol H2O 2 © 2009 Brooks/Cole - Cengage Gases and Stoichiometry 2 H2O2(liq) f 2 H2O(g) + O2(g) Decompose 0.11 g of H2O2 in a flask with a volume of 2.50 L. What is the pressure of O2 at 25 oC? Of H2O? Solution P of O2 = nRT/V (0.0016 mol)(0.0821 Lįatm/Kįmol)(298 K) = 2.50 L P of O2 = 0.016 atm © 2009 Brooks/Cole - Cengage 27 Gases and Stoichiometry 2 H2O2(liq) f 2 H2O(g) + O2(g) What is P of H2O? Could calculate as above. But recall Avogadro’s hypothesis. V P n at same T and P n at same T and V There are 2 times as many moles of H2O as moles of O2. P is proportional to n. Therefore, P of H2O is twice that of O2. P of H2O = 0.032 atm © 2009 Brooks/Cole - Cengage 28 29 Dalton’s Law of Partial Pressures 2 H2O2(liq) f 2 H2O(g) + O2(g) 0.032 atm 0.016 atm What is the total pressure in the flask? Ptotal in gas mixture = PA + PB + ... Therefore, Ptotal = P(H2O) + P(O2) = 0.048 atm Dalton’s Law: total P is sum of PARTIAL pressures. © 2009 Brooks/Cole - Cengage Dalton’s Law John Dalton 1766-1844 © 2009 Brooks/Cole - Cengage 30 GAS DENSITY PLAY MOVIE Higher Density air © 2009 Brooks/Cole - Cengage 31 Low density helium GAS DENSITY PV = nRT n P = V RT m P = M• V RT where M = molar mass and density (d) = m/V m PM d= = V RT © 2009 Brooks/Cole - Cengage d and M proportional 32 The Disaster of Lake Nyos • Lake Nyos in Cameroon was a volcanic lake. • CO2 built up in the lake and was released explosively on August 21, 1986. • 1700 people and hundreds of animals died. • See Chapter 14 for more information © 2009 Brooks/Cole - Cengage 33 34 USING GAS DENSITY The density of air at 15 oC and 1.00 atm is 1.23 g/L. What is the molar mass of air? 1. Calc. moles of air. V = 1.00 L P = 1.00 atm T = 288 K n = PV/RT = 0.0423 mol 2. Calc. molar mass mass/mol = 1.23 g/0.0423 mol = 29.1 g/mol © 2009 Brooks/Cole - Cengage KINETIC MOLECULAR THEORY (KMT) Theory used to explain gas laws. KMT assumptions are • Gases consist of molecules in constant, random motion. • P arises from collisions with container walls. • No attractive or repulsive forces between molecules. Collisions elastic. • Volume of molecules is negligible. © 2009 Brooks/Cole - Cengage 35 Kinetic Molecular Theory Because we assume molecules are in motion, they have a kinetic energy. KE = (1/2)(mass)(speed)2 At the same T, all gases have the same average KE. As T goes up for a gas, KE also increases — and so does speed. © 2009 Brooks/Cole - Cengage 36 Kinetic Molecular Theory At the same T, all gases have the same average KE. As T goes up, KE also increases — and so does speed. PLAY MOVIE © 2009 Brooks/Cole - Cengage 37 Kinetic Molecular Theory Maxwell’s equation 2 u = 3 RT M Root mean square speed where u is the speed and M is the molar mass. • speed INCREASES with T • speed DECREASES with M © 2009 Brooks/Cole - Cengage 38 Distribution of Gas Molecule Speeds PLAY MOVIE © 2009 Brooks/Cole - Cengage • Boltzmann plots • Named for Ludwig Boltzmann doubted the existence of atoms. • This played a role in his suicide in 1906. 39 Velocity of Gas Molecules Molecules of a given gas have a range of speeds. © 2009 Brooks/Cole - Cengage 40 Velocity of Gas Molecules Average velocity decreases with increasing mass. © 2009 Brooks/Cole - Cengage 41 42 GAS DIFFUSION AND EFFUSION DIFFUSION is the gradual mixing of molecules of different gases. © 2009 Brooks/Cole - Cengage GAS EFFUSION EFFUSION is the movement of molecules through a small hole into an empty container. See Figure 11.19 © 2009 Brooks/Cole - Cengage 43 44 GAS DIFFUSION AND EFFUSION Molecules effuse thru holes in a rubber balloon, for example, at a rate (= moles/time) that is • proportional to T • inversely proportional to M. Therefore, He effuses more rapidly than O2 at same T. © 2009 Brooks/Cole - Cengage He GAS DIFFUSION AND EFFUSION Graham’s law governs effusion and diffusion of gas molecules. Rate for A = Rate for B M of B M of A Rate of effusion is inversely proportional to its molar mass. © 2009 Brooks/Cole - Cengage Thomas Graham, 1805-1869. Professor in Glasgow and London. 45 Gas Diffusion relation of mass to rate of diffusion PLAY MOVIE See Active Figure 11.18 © 2009 Brooks/Cole - Cengage • HCl and NH3 diffuse from opposite ends of tube. • Gases meet to form NH4Cl • HCl heavier than NH3 • Therefore, NH4Cl forms closer to HCl end of tube. 46 47 Using KMT to Understand Gas Laws Recall that KMT assumptions are • Gases consist of molecules in constant, random motion. • P arises from collisions with container walls. • No attractive or repulsive forces between molecules. Collisions elastic. • Volume of molecules is negligible. © 2009 Brooks/Cole - Cengage Avogadro’s Hypothesis and Kinetic Molecular Theory PLAY MOVIE P proportional to n — when V and T are constant © 2009 Brooks/Cole - Cengage 48 49 Gas Pressure, Temperature, and Kinetic Molecular Theory PLAY MOVIE P proportional to T — when n and V are constant © 2009 Brooks/Cole - Cengage Boyle’s Law and Kinetic Molecular Theory PLAY MOVIE P proportional to 1/V — when n and T are constant © 2009 Brooks/Cole - Cengage 50 Deviations from Ideal Gas Law • Real molecules have volume. • There are intermolecular forces. – Otherwise a gas could not become a liquid. © 2009 Brooks/Cole - Cengage 51 Deviations from Ideal Gas Law Account for volume of molecules and intermolecular forces with VAN DER WAALS’s EQUATION. Measured V = V(ideal) Measured P ( P 2 n a + ----2 V ) V - nb nRT vol. correction intermol. forces © 2009 Brooks/Cole - Cengage J. van der Waals, 1837-1923, Professor of Physics, Amsterdam. Nobel Prize 1910. 52 Deviations from Ideal Gas Law Cl2 gas has a = 6.49, b = 0.0562 For 4.00 mol Cl2 in a 4.00 L tank at 100.0 oC. P (ideal) = nRT/V = 30.6 atm P (van der Waals) = 26.0 atm © 2009 Brooks/Cole - Cengage 53