William
Kovarik |
Fuels and Society C: How Lead was Finally Removed from Gasoline 1. Nitrogen and Oxygen - The NOx and Tropospheric Ozone (O3) Problem |
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Back to: Start Chemical Principles
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Nitrogen and Oxygen
Consider the chemical reactions: N2 + O2 --> 2NO 3/2O2 ----> O3 Macroscopic Observations of the Air Around Us:
What is your intuitive answer? What is the evidence that it does not? Is it important, for example that the earth's atmosphere consists of 79% nitrogen and 20% oxygen and virtually no ozone and the two substances appear to coexist without undergoing any spontaneous chemical reaction?
Microscopic Evaluation: The sequence is this: Nitric oxide molecules form a colorless gas but the substance is highly reactive in the presence of oxygen. In the atmosphere, NO molecules react with oxygen rapidly to form NO2. NO2 production starts a cascade of chemical reactions that produces the oxygen allotrope, ozone (O3). Ozone is harmful in the lower atmosphere. More complex reactions of ozone cause photochemical smog. Look at this sequence of chemical reactions: NO + 1/2O2 --> 1/2NO2(brown gas) sunlight O + O2 -----> O3 The brown gas, nitrogen dioxide is split back to NO and an oxygen atom and the oxygen atom reacts with an oxygen molecule to form ozone. Take a moment to sum the chemical reactions just as you would partial algebraic equations: 3/2O2 ----> O3 Note that:
Thermodynamics and the Production of NO: As in the cracking of hexane to propane and propene that we discussed earlier, thermodynamic principle explain to us the production of NO.
N2 + O2 --> 2NO And for the reaction at room temperature - 298 degrees Celsius: delta G = delta H - T delta S at standard temperature: delta G0 = 44kcal - (298K)(5cal/K) = +42kcal The process is not spontaneous. Even if we look at a temperature of 2400 degrees Celsius, delta G0 is = 32kcal so the process is not spontaneous. So how does NO occur? Let us look at the equation relating G,H and S. It derives the properties at standard state, that is, for gases, a pressure of 1 atmosphere for each component and a temperature of 298 degrees Celsius. But we are far from standard state. How can the equation be modified to reflect deviations from standard, the real condition of generation of small concentrations of products in a process that is non spontaneous at standard conditions? At equilibrium, that is at the point where forward and reverse reactions are taking place at the same rate: delta G = delta G0 + RT ln (Q) in which T =
temperature Celsius In this expression, if the system is at equilibrium, delta G = 0 and the ratio Q = Keq the equilibrium constant. This equation implies that in ANY chemical process that is at equilibrium, SOME of all species will be present. But in the case of the production of NO, the equilibrium constant determined by the ratios at equilibrium is 10-15 at 298 degrees Celsius. This implies a tiny concentration of NO, but remember,each process must be activated to the transition state to proceed to products. And at the low temperature, the reaction rate to give NO is negligible because of high activation energy required. At 2400 degrees Celsius, however, the Keq = 0.05 and coupled with the ease of reaching the transition state, NO is formed. The gas mixture quickly cools and the composition is frozen and an engine exhausts as much as 4g/mile of NO to the atmosphere. Chemical Kinetics, Catalysis and the Production of Ozone: If we look at the sequence of ozone production again: NO + 1/2O2 --> 1/2NO2(brown gas) sunlight O + O2 -----> O3 we see a chain reaction in which the presence of three components are necessary to convert oxygen to ozone. Both NO and NO2 are formed and destroyed in the process. Their concentration does not change at equilibrium yet they are essential to the process. They are each catalysts - substances that effectively reduce the transition state requirements for a process to go forward. Sunlight is a catalyst also - and a catalyst without which the process does not go forward. The decomposition of NO2 to NO and O requires sunlight and indeed the smog forming processes abate at night as determined by measurements of the airborne pollutants. There was a chemical solution to the nitrogen oxide problem. A catalytic converter could be introduced to convert the nitrogen oxides in the exhaust back to the elements. 1. You will recognize that ozone in the upper atmosphere is necessary. The destruction of the ozone layer by refrigerant gases has been slowed by development of new refrigerants stemming from application of chemical concepts. |
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