18-Env-A5 Air Quality and Pollution Control Engineering · May 2015
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
National Exams — May 2015 — 04-Env-A5 / Air Quality and Pollution Control Engineering. 3 hours duration; closed book with a candidate-prepared 8½×11 in double-sided aid sheet; Casio or Sharp approved calculator only. Any five (5) questions constitute a complete paper (the first five answers as they appear are marked); all seven are solved below for completeness. Each question is worth 20 marks with section marks shown in brackets.
Reference texts. Cooper & Alley, Air Pollution Control: A Design Approach (4th ed.); Wark, Warner & Davis, Air Pollution: Its Origin and Control (3rd ed.); Davis & Cornwell, Introduction to Environmental Engineering (6th ed.); Canadian Environmental Protection Act, 1999 (CEPA) and the Canadian Ambient Air Quality Standards (CAAQS) administered by Environment and Climate Change Canada.
Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.
A pre-combustion / combustion-modification strategy is low-NOx burner (LNB) design with staged combustion: fuel and air are introduced in stages so the primary flame zone burns fuel-rich (starving the Zeldovich reactions of O2 and lowering peak flame temperature), with the remaining air added downstream to complete burnout at lower temperature; this directly attacks both combustion parameters identified in Question 5(i) (peak temperature and local O2 availability) and typically cuts thermal NOx by 40–60% at a fraction of the capital cost of add-on control. A complementary post-combustion strategy is selective catalytic reduction (SCR): ammonia (or urea, hydrolyzed on-site to ammonia) is injected into the flue gas upstream of a catalyst bed (typically vanadium/titanium oxide) operating around 300–400 °C, where NOx is reduced to N2 and H2O via reactions such as $4\text{NO}+4\text{NH}_3+\text{O}_2\rightarrow4\text{N}_2+6\text{H}_2\text{O}$, achieving 80–90%+ NOx removal independent of what combustion modification alone can reach. The two are complementary rather than substitutes: combustion modification is cheap but plateaus well short of stringent limits, while SCR is capital-intensive but reaches deep removal on top of whatever the combustion stage already achieved.
The most common FGD process, shown above, is wet limestone scrubbing. Flue gas rises through a spray tower where it is contacted countercurrently with a recirculated slurry of finely ground limestone (CaCO3) in water. SO2 in the gas dissolves into the slurry droplets and reacts acid–base with the dissolved calcium carbonate: $$\text{SO}_2 + \text{H}_2\text{O} \rightarrow \text{H}_2\text{SO}_3, \qquad \text{CaCO}_3 + \text{H}_2\text{SO}_3 \rightarrow \text{CaSO}_3 + \text{CO}_2 + \text{H}_2\text{O}.$$ The calcium sulfite is typically further oxidized (forced-oxidation air sparged into the sump) to calcium sulfate dihydrate (gypsum, CaSO4·2H2O), a marketable byproduct used in wallboard manufacture rather than a waste requiring landfill. A mist eliminator downstream of the spray zone removes entrained slurry droplets before the scrubbed, humidified gas is reheated (in some designs) and released through the stack. Removal efficiency of 90–95%+ SO2 is routinely achieved because the process is limited by gas–liquid mass transfer and reagent stoichiometry, both of which are controlled directly by slurry recirculation rate and limestone feed rate — the design levers a plant operator adjusts to hold a permitted SO2 removal target.
Photochemical smog forms through a sunlight-driven catalytic cycle involving NOx and reactive hydrocarbons (VOCs). NO2 photolyzes under UV sunlight, $\text{NO}_2+h\nu\rightarrow\text{NO}+\text{O}$, and the resulting atomic oxygen combines with O2 to form ozone, $\text{O}+\text{O}_2\rightarrow\text{O}_3$; in a "clean" NOx-only atmosphere, O3 is then rapidly consumed by reaction with the NO produced in the first step, $\text{NO}+\text{O}_3\rightarrow\text{NO}_2+\text{O}_2$, closing a null cycle that builds no net ozone. Reactive VOCs break this null cycle: hydroxyl-radical-initiated oxidation of VOCs generates peroxy radicals (RO2•, HO2•) that oxidize NO back to NO2 without consuming ozone, so NO is regenerated as NO2 by two competing pathways (VOC-driven and O3-driven) and net ozone accumulates over the course of a sunlit day; the same VOC-oxidation chain also produces peroxyacetyl nitrate (PAN) and secondary organic aerosol, the other defining smog products. Because the cycle needs both NOx and VOCs simultaneously, and because urban smog is frequently VOC-limited (ozone production is more sensitive to VOC than to further NOx reduction in dense city cores), a targeted engineering approach is aggressive control of reactive VOC emissions — vapour recovery at fuel-dispensing and storage facilities, low-solvent/low-VOC coatings and consumer-product formulations, and evaporative-emission control on vehicles (Question 4(i)) — combined with continued NOx reduction (Question 6(i)) so that as a city's VOC-to-NOx ratio shifts over time, the smog-formation regime does not simply move from VOC-limited back to NOx-limited without a matching NOx reduction already in place.