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CVEN 5424 Environmental Organic Chemistry Lecture 8 – Henry’s Law Constant and Air-Water Exchange Kinetics
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Announcements Reading Chapter 6, Air-Water Partition Chapters 18, 19, and 20 (for next lecture) Problem sets PS 3 due today PS 4 out today; due next Tuesday Office hours – semester Wednesday 9-10 am Thursday 4-5:30 pm Monday 9-10:30 am Exam 1 Tues Feb 16, noon, to Thurs Feb 18, 10 am
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Air-Water Exchange Equilibrium
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Air-Water Exchange Phase transfers pure liquid or solid to gas pure liquid vapor p*
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Air-Water Exchange Phase transfers pure liquid or solid to gas pure liquid, solid, or gas to water pure liquid vapor pure liquid aqueous solution p*C w sat
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Air-Water Exchange Another phase exchange air-water exchange = pure liquid aqueous solution vapor aqueous solution vapor
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Air-Water Exchange Phase exchange A water A air Henry’s Law constants (bar L mol -1 ) dimensionless (mol L a -1 mol -1 L w )
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Air-Water Exchange compound Henry’s Law constant K aw (dimensionless) benzene10 -0.65 phenol10 -4.59 trichloroethene10 -0.31 phenanthrene10 -2.85 2,2’,5,5’-tetrachlorobiphenyl10 -1.70
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Air-Water Exchange Estimates by vapor pressure / solubility
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Air-Water Exchange Estimates by vapor pressure / solubility
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Air-Water Exchange Example: chloroethene (a gas) estimated K aw = 10 -0.04 experimental K aw = 10 -0.05
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Air-Water Exchange Example: chlorobenzene (a liquid) estimated K aw = 10 -0.80 experimental K aw = 10 -0.82
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Air-Water Exchange Example: pyrene (a solid) estimated K aw = 10 -3.32 experimental K aw = 10 -3.36
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Air-Water Exchange
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Temperature dependence enthalpy of liquid-air phase change, al H Two components of al H: vap H - w H E enthalpy to vaporize vap H, related to p L * (excess) enthalpy to solubilize w H E, related to C w sat for solids and gases, melting and condensation enthalpies cancel out
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Air-Water Exchange Liquid: (getting to gas phase) (getting out of water phase)
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Air-Water Exchange Liquid: Solid: (getting to gas phase) (getting out of water phase)
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Air-Water Exchange Liquid: Solid: Gas: gas already in gas phase (getting to gas phase) (getting out of water phase)
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Air-Water Exchange dichlorodifluoromethane (gas) toluene (liquid) naphthalene (solid) pyrene (solid)
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Air-Water Exchange Temperature dependence liquids (e.g., benzene, tetrachloroethylene) ln p* 1/T ln C w sat 1/T ln K H 1/T =+
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Air-Water Exchange Temperature dependence solids (e.g., naphthalene, 1,4-dichlorobenzene) ln p* 1/T ln C w sat 1/T ln K H 1/T =+
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Air-Water Exchange Temperature dependence gases (e.g., vinyl chloride, chloromethane) ln p* 1/T ln C w sat 1/T ln K H 1/T =+
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Air-Water Exchange Effect of salt Salting out decreases solubility; increases K aw
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Air-Water Exchange Effect of salt Salting out decreases solubility; increases K aw
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Air-Water Exchange Effect of salt pyrene, K aw = 10 -3.32 seawater [salt] tot = 0.5 M K S = 0.30
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Air-Water Exchange Effect of co-solvents Co-solvents increase solubility; decrease K H
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Air-Water Exchange Effect of co-solvents Co-solvents increase solubility; decrease K H
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Air-Water Exchange Effect of co-solvents naphthalene, K aw = 10 -1.74 20% acetone solution f v = 0.2 c = 6.5
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Air-Water Exchange Partition between air and water importance of keeping bubbles out of water samples for VOCs 40 mL vial 39 mL water, 1 mL bubble VOC is chloromethane K aw = 10 0.16 what fraction of the chloromethane is in the bubble?
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Air-Water Exchange Partition between air and water
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Air-Water Exchange Partition between air and water
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Air-Water Exchange Partition between air and water
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Air-Water Exchange Kinetics Chapter 18 Transport by Random Motion read Sections 1, 3 Example 18.3 errata Answer a, b, and c are actually b, c, and d Answer d is actually a skim Sections 2, 4 Chapter 19 Transport Through Boundaries read Sections 1, 2 (skip advanced topics) skim Sections 3, 4 skip Section 5
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Air-Water Exchange Kinetics Equilibrium versus kinetics water air
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Air-Water Exchange Kinetics A barge carrying chloroform down the Mississippi River runs aground and ruptures. The spill contaminates a large volume of water at C w sat of CHCl 3. The wind speed at 2 m height is 3 m s -1. The mean depth of the river is 10 m. The water and air temperature are 20 C. What is the initial flux of chloroform from the river? What is the half-life of chloroform volatilization?
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Air-Water Exchange Kinetics Equilibrium versus kinetics water air
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Quiz Which compound will volatilize faster? compound K H (bar L mol -1 ) M w (Da) carbon tetrachloride21153.8 vinyl chloride2262.5
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Quiz Which compound will volatilize faster? diffusion coefficient inversely proportional to molecular weight compound K H (bar L mol -1 ) M w (Da) carbon tetrachloride21153.8 vinyl chloride2262.5
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Air-Water Exchange Kinetics Fick’s Laws – molecular diffusion F flux (mass per area per time; e.g., mol m -2 s -1 ) D diffusion (area per time; m 2 s -1 ) C concentration (mass per volume; mol L -1 ) x spatial coordinate (length; m)
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Air-Water Exchange Kinetics Diffusion coefficient
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Air-Water Exchange Kinetics Diffusion coefficient Einstein, A. (1905) Ann. d. Physik 17, 549. Stokes, G. G. (1851) Cambridge Philos. Trans. 9, 8-106.
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Air-Water Exchange Kinetics Diffusion in air inversely proportional to molar volume compound mw (g mol -1 ) V (cm 3 mol -1 ) D a (cm 2 s -1 ) H2OH2O18 0.26 methane16250.28 benzene78890.12 tetrachloroethene1661110.086 2,2’,4,4’,5,5’- hexachlorobiphenyl 3613230.059
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Air-Water Exchange Kinetics Molar volume element contribution (cm 3 mol -1 ) C16.5 H2.0 O5.5 N5.7 S17.0 Cl19.5 rings-20.2 Fuller et al. (1966)
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Air-Water Exchange Kinetics Molar volume element contribution (cm 3 mol -1 ) C16.5 H2.0 O5.5 N5.7 S17.0 Cl19.5 rings-20.2 Fuller et al. (1966)
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Air-Water Exchange Kinetics Molar volume element contribution (cm 3 mol -1 ) C16.5 H2.0 O5.5 N5.7 S17.0 Cl19.5 rings-20.2 Fuller et al. (1966)
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Air-Water Exchange Kinetics Estimating D a (Fuller et al., 1966) T absolute temperature (K) mw air average molecular mass of air (28.97 g mol -1 ) mw c molecular mass of compound (g mol -1 ) P air total pressure of the air (atm) V air average molar volume of air (20.1 cm 3 mol -1 ) V c molar volume of compound (cm 3 mol -1 )
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Air-Water Exchange Kinetics Estimating D a relative to known compound water, benzene, etc.
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Air-Water Exchange Kinetics Diffusion of tetrachloroethene in air at 25 C
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Air-Water Exchange Kinetics Diffusion of tetrachloroethene in air at 25 C
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Air-Water Exchange Kinetics Diffusion in water inversely proportional to molar volume compound mw (g mol -1 ) V (cm 3 mol -1 ) D w (cm 2 s -1 ) O2O2 3218 2.1 10 -5 methane1625 3.0 10 -5 benzene7889 1.3 10 -5 tetrachloroethene166111 0.92 10 -5 2,2’,4,4’,5,5’- hexachlorobiphenyl 361323 0.63 10 -5
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Air-Water Exchange Kinetics Estimating D w viscosity of the water (cp, 10 -2 g cm -1 s -1 ) V molar volume of the compound
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Air-Water Exchange Kinetics Estimating D w diffusion volume molecular weight
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Air-Water Exchange Kinetics Diffusion of PCE in water at 25 C
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Air-Water Exchange Kinetics Diffusion of PCE in water at 25 C
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Air-Water Exchange Kinetics Diffusion of PCE in water at 25 C
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Air-Water Exchange Kinetics Flux of molecules across air-water interface driven by concentration gradient controlled by molecular diffusion Water across air-water interface evaporation Gases across air-water interface oxygen carbon dioxide
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Air-Water Exchange Kinetics
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Evaporation, that random breach of surface tension by molecules "which happen to acquire exceptionally high velocities.“ Brave "happening"! – they fly the minute distance across and join another state of matter, sacrificing, as they depart, heat to the attraction of the molecules still water, like a wedlocked beauty leaving behind her filmy nightgowns as she flees to a better lover. John Updike, Ode to Evaporation
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Air-Water Exchange Kinetics Three models: stagnant film surface renewal boundary layer
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Air-Water Exchange Kinetics Stagnant film model stagnant air layer below well-mixed air stagnant water layer above well- mixed water equilibrium applies only in boundary layers most applicable to ocean, lakes, slow rivers well-mixed water well-mixed air C zwzw zaza 0 CwCw C a/w C w/a CaCa stagnant water ~0.01 cm stagnant air ~0.1 cm
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Air-Water Exchange Kinetics Surface renewal model parcels of air spend some time at interface parcels of water spend some time at interface equilibrium between parcels at interface most applicable to smaller, faster-flowing streams in which stagnant films unlikely water air C 0 CwCw C a/w C w/a CaCa
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Air-Water Exchange Kinetics Boundary layer model similar to stagnant film model continuous, not step-like, drop in diffusivity accounts for turbulence most versatile, recommended by SGI
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Air-Water Exchange Kinetics A barge carrying chloroform down the Mississippi River runs aground and ruptures. The spill contaminates a large volume of water at C w sat of CHCl 3. The wind speed at 2 m height is 3 m s -1. The mean depth of the river is 10 m. The water and air temperature are 20 C. What is the initial flux of chloroform from the river? What is the half-life of chloroform volatilization?
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Air-Water Exchange Kinetics Spills in the Mississippi River oil (crude, diesel) at least 44 major spills post-Katrina 27,000,000 L xylene tanker collided with barge 160,000 L “pyrolysis gasoline” tanker collided with barge product of ethylene manufacture; benzene 17,000 L cumene barge accident at lock 31,000 L
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Air-Water Exchange Kinetics Spills in the Mississippi River ethylene glycol leaking railroad tank car 77,000 L pentachlorophenol ship accident; required dredging 16 tons fluorosilicic acid (H 2 SiF 6 ) highly corrosive acid; used for fluoridation leaking tank; causing damage to other tanks at chemical transfer facility; pumped into river 1,700,000 L chloroform barge sank near Baton Rouge 500,000 L
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“ I entered upon the small enterprise of ‘learning’ twelve or thirteen hundred miles of the great Mississippi with the easy confidence of my time of life. If I had really known what I was about to require of my faculties, I should not have had the courage to begin. I supposed that all a pilot had to do was to keep his boat in the river, and I did not consider that that could be much of a trick, since it was so wide.” - Mark Twain, Life on the Mississippi
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Air-Water Exchange Kinetics Stagnant film model (Whitman, 1923) flux v w water piston velocity resistance of the water side CO 2 moving through water v a air piston velocity resistance of the air side H 2 O moving through air piston velocity (cm s -1 ) “resistance” conc. gradient (mol cm -3 ) “driving force” flux (mol cm -2 s -1 )
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Air-Water Exchange Kinetics C w chloroform solubility, C w sat C w = 10 -1.19 M = 10 -4.19 mol cm -3 this is the initial concentration, so the flux is only initial C a wind continuously brings air free of chloroform C a 0 K aw chloroform K H = 10 0.60 bar L mol -1 (at 25 C) K aw = 0.16
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Air-Water Exchange Kinetics Piston velocity of chloroform through water v w estimate for CO 2, relate to CHCl 3 depends solely on wind speed (Eqn. 20-17) u 10 wind speed at 10 m height (m s -1 )
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Air-Water Exchange Kinetics Piston velocity of chloroform through water v w correct wind speed for height (Eqn. 20-14) u z wind speed at height z (m s -1 ) z height of wind measurement (m) 3 m s -1 at 2 m height
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Air-Water Exchange Kinetics Piston velocity of chloroform through water v w relating CHCl 3 to CO 2 (Eqn 20-25)
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Air-Water Exchange Kinetics Temperature correction for v w two “corrections” at the same time D w (T 2 ) for unknown compound for temperatures other than 20 C
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Air-Water Exchange Kinetics Piston velocity of chloroform through water v w
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Air-Water Exchange Kinetics Piston velocity of chloroform through air v a estimate for H 2 O, relate to CHCl 3 depends solely on wind speed (Eqn. 20-15)
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Air-Water Exchange Kinetics Piston velocity of chloroform through air v a relating CHCl 3 to H 2 O (Eqn. 20-27)
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Air-Water Exchange Kinetics Temperature correction for v a two “corrections” at the same time D a (T 2 ) for unknown compound for temperatures other than 20 C
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Air-Water Exchange Kinetics Piston velocity of chloroform through air v a
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Air-Water Exchange Kinetics Flux of chloroform through air-water interface “water-side controlled” or “water-side limited”
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Air-Water Exchange Kinetics Half-life of chloroform volatilization rate expression simplification of flux (mol cm -2 s -1 ) (mol cm -3 s -1 ) (cm s -1 mol cm -3 )
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Air-Water Exchange Kinetics Half-life of chloroform volatilization total mass volatilized per time (mol s -1 )
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Air-Water Exchange Kinetics Half-life of chloroform volatilization total mass volatilized per time
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Air-Water Exchange Kinetics Half-life of chloroform volatilization volatilization rate coefficient (s -1 ) (cm s -1 ) (cm)
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Air-Water Exchange Kinetics Half-life of chloroform volatilization change in C w with time:
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Air-Water Exchange Kinetics Half-life of chloroform volatilization
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Next Lecture Air-water exchange kinetics using the boundary layer model
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