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18-Env-A5 Air Quality and Pollution Control Engineering · December 2014

Question 1 of 7: Sources and Classification of Atmospheric Pollutants

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

National Exams — December 2014 — 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 1: Sources and Classification of Atmospheric Pollutants (20 marks)

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.

(i) SO2 Concentration in Flue Gas and Secondary Pollutant Formation

Given. A fuel is burnt with the stoichiometric amount of oxygen (supplied as air):

Given data
QuantitySymbolValue
Fuel quantity$n_{fuel}$100 mol, formula C8H17 (as printed)
Sulphur content of fuel—3% by mass
Oxidant—Stoichiometric O2, supplied as air (21% O2, 79% N2 by volume)

Find. The SO2 concentration in the flue gas (ppmv and % by volume).

Check: the source prints the fuel formula as C8H17 — the printed formula is unambiguous, but an odd hydrogen count is not a stable saturated hydrocarbon (the alkane series is CnH2n+2, e.g. octane C8H18). The boxed answer below uses C8H17 exactly as printed; the C8H18 (octane) reading is computed alongside for comparison and changes the answer by only about 1.4% (1656 vs. 1679 ppm), so the conclusion is insensitive to which formula is intended.

Approach. Find the moles of sulphur from the 3%-by-mass fuel composition, balance the stoichiometric combustion equation for the hydrocarbon, add the O2 consumed oxidizing S to SO2, bring in N2 from the air, then divide moles SO2 by total moles of flue gas.

  1. Molar mass and sulphur content of the fuel. $M_{fuel} = 8(12.011)+17(1.008) = 113.22\ \text{g/mol}$. For 100 mol: $m_{fuel} = 11{,}322\ \text{g}$, so $m_S = 0.03(11{,}322) = 339.7\ \text{g}$, i.e. $$n_S = \frac{339.7}{32.07} = \boxed{10.59\ \text{mol S}}.$$
  2. Balance the hydrocarbon combustion. $\text{C}_8\text{H}_{17} + 12.25\,\text{O}_2 \rightarrow 8\,\text{CO}_2 + 8.5\,\text{H}_2\text{O}$ (from $x+y/4 = 8+17/4=12.25$). For 100 mol fuel: $\text{O}_{2,fuel} = 1225\ \text{mol}$, $\text{CO}_2 = 800\ \text{mol}$, $\text{H}_2\text{O}=850\ \text{mol}$.
  3. Add sulphur oxidation and bring in nitrogen. $\text{S}+\text{O}_2\rightarrow\text{SO}_2$ needs $10.59$ mol O2, so $\text{O}_{2,total} = 1225+10.59 = 1235.6\ \text{mol}$. At stoichiometric air (21% O2/79% N2), $$N_2 = 1235.6\times\frac{79}{21} = 4648\ \text{mol}.$$
  4. Total flue gas and SO2 fraction. $n_{flue} = \text{CO}_2+\text{H}_2\text{O}+\text{SO}_2+N_2 = 800+850+10.59+4648 = 6309\ \text{mol}$, so $$y_{SO_2} = \frac{10.59}{6309} = \boxed{1679\ \text{ppmv}\ (0.168\%\ \text{v/v})}.$$
QuantityValue
Moles of sulphur, $n_S$10.59 mol
Total O2 required (stoichiometric)1236 mol
Total flue gas produced6309 mol
SO2 concentration≈ 1679 ppmv (0.168% v/v)

Secondary air pollutants are not emitted directly from the stack; they form in the atmosphere when primary combustion products react further, usually driven by sunlight. SO2 oxidizes slowly to SO3 and, with atmospheric moisture, to sulfate aerosol (H2SO4 mist) — a major contributor to acid deposition and fine-particle haze. NOx and volatile organic compounds released alongside SO2 undergo photochemical reactions catalyzed by sunlight and hydroxyl radicals to form ground-level ozone (O3) and peroxyacetyl nitrate (PAN), the defining pollutants of photochemical smog. Because secondary pollutant formation depends on residence time, sunlight intensity and the presence of co-pollutants, its severity is often worse tens to hundreds of kilometres downwind of the source rather than at the stack itself.

(ii) Indoor Air Pollutants

Radon (222Rn) is a naturally occurring radioactive noble gas that seeps from soil and rock (particularly uranium-bearing bedrock, common across parts of Canada) through foundation cracks and sumps. Its short-lived decay progeny attach to airborne dust and, once inhaled, irradiate lung tissue; long-term exposure is the second leading cause of lung cancer after smoking. Formaldehyde and other VOCs off-gas continuously from pressed-wood products, adhesives, paints and new furnishings; they cause eye/respiratory irritation, headaches, and some (formaldehyde itself) are classified as human carcinogens at elevated chronic exposure.

Two engineering controls: (1) mechanical ventilation with heat recovery (HRV/ERV) continuously dilutes indoor air with outdoor air while recovering the energy penalty, directly lowering both radon and VOC concentrations; for radon specifically, sub-slab depressurization (a fan-driven vent pipe drawing soil gas from beneath the foundation before it enters the building) is the standard mitigation. (2) Source control — specifying low-VOC/no-added-urea-formaldehyde materials and allowing off-gassing (bake-out) before occupancy — reduces the emission rate itself rather than diluting after the fact.

(iii) Outdoor VOC Release — Formaldehyde

Selecting formaldehyde released from an industrial operation (e.g., a resin or wood-products plant): Health impacts — (1) it is a potent respiratory and eye irritant even at low ppm concentrations, aggravating asthma and causing upper-airway inflammation in nearby residents; (2) IARC classifies formaldehyde as a human carcinogen (nasopharyngeal cancer) under chronic exposure. Ecological impacts — (1) as a highly reactive VOC it is an efficient ozone precursor, contributing disproportionately to downwind photochemical smog formation relative to its emission mass; (2) it is phytotoxic at elevated concentrations, damaging leaf tissue and reducing photosynthetic productivity in vegetation near the release point.

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