CSIR-UGC NET — Earth, Atmospheric, Ocean and Planetary Sciences · India · National Testing Agency for CSIR
Original practice questions written to the published syllabus · not past papersThe chemistry of water, soil and air that pollution, treatment and climate subjects assume: equilibria, the carbonate system, redox, gas solubility, ozone and smog chemistry. GATE ES Section 2 in full.
In the exams: GATE ES Section 2; UGC NET Environmental Sciences Unit 2; ICAR AIEEA-PG Physical Science Unit II (chemistry)
CUET-PG Environmental Sciences and CSIR-UGC NET (Earth, Atmospheric, Ocean and Planetary Sciences)
Carbonate chemistry and ocean acidification, atmospheric composition and ozone chemistry, and basic equilibrium and redox principles.
How our questions for CSIR-UGC NET spread across the units of Environmental Chemistry. Difficulty: 0 easy, 10 medium, 8 hard.
| The carbonate system and ocean acidification | 5 | |
| Chemical equilibrium, thermodynamics and reaction kinetics | 4 | |
| Stratospheric ozone chemistry and ozone-depleting substances | 4 | |
| Composition and structure of the atmosphere | 3 | |
| Redox reactions, pe-pH diagrams and redox zonation | 2 |
Choose an answer, then open the working. Each explanation says why the right answer is right and why the others are not.
According to Le Chatelier's principle, raising the temperature of an exothermic equilibrium will
A. shift it towards the reactants
Adding heat favours the endothermic direction, which for an exothermic forward reaction is the reverse; K decreases.
Further reading: See the manual sources: Sawyer, McCarty & Parkin; Manahan; Stumm & Morgan; Seinfeld & Pandis; IS 10500; WMO/UNEP ozone assessment
If the reaction quotient Q is smaller than the equilibrium constant K, the reaction will
C. proceed in the forward direction
Q < K means too few products; ΔG = RT ln(Q/K) is negative, so the forward reaction proceeds.
Further reading: See the manual sources: Sawyer, McCarty & Parkin; Manahan; Stumm & Morgan; Seinfeld & Pandis; IS 10500; WMO/UNEP ozone assessment
Which carbonate species dominates dissolved inorganic carbon at pH 8.3 in fresh water at 25 °C (pKa1 6.35, pKa2 10.33)?
A. Bicarbonate, about 98 per cent
Between pKa1 and pKa2 bicarbonate dominates; at pH 8.3, near the midpoint, about 98% is HCO3⁻.
Further reading: See the manual sources: Sawyer, McCarty & Parkin; Manahan; Stumm & Morgan; Seinfeld & Pandis; IS 10500; WMO/UNEP ozone assessment
A redox potential of +0.40 V is measured at 25 °C. What is the corresponding pe (pe = E/0.0592)?
C. 6.8
pe = 0.40/0.0592 = 6.8. Multiplying gives 0.024; the sign is positive for an oxidising potential; 0.40 is E itself.
Further reading: See the manual sources: Sawyer, McCarty & Parkin; Manahan; Stumm & Morgan; Seinfeld & Pandis; IS 10500; WMO/UNEP ozone assessment
Using the Nernst equation E = E° − (0.0592/n) log Q at 25 °C, what happens to E for a one-electron reduction when Q increases tenfold?
C. E decreases by 0.0592 V
Δ(log Q) = 1 with n = 1 lowers E by 0.0592 V.
Further reading: See the manual sources: Sawyer, McCarty & Parkin; Manahan; Stumm & Morgan; Seinfeld & Pandis; IS 10500; WMO/UNEP ozone assessment
Which radical is called the 'detergent of the atmosphere' because it initiates oxidation of most trace gases?
A. The hydroxyl radical (OH)
OH, formed from ozone photolysis and water vapour, oxidises methane, CO, VOCs, SO2 and NO2.
Further reading: See the manual sources: Sawyer, McCarty & Parkin; Manahan; Stumm & Morgan; Seinfeld & Pandis; IS 10500; WMO/UNEP ozone assessment
A gas has an atmospheric burden of 5000 Tg and is removed at 500 Tg per year. Assuming steady state, what is its atmospheric lifetime?
D. 10 years
Lifetime = burden ÷ removal rate = 5000/500 = 10 years.
Further reading: See the manual sources: Sawyer, McCarty & Parkin; Manahan; Stumm & Morgan; Seinfeld & Pandis; IS 10500; WMO/UNEP ozone assessment
In a catalytic ozone-destruction cycle, Cl + O3 → ClO + O2 is followed by ClO + O → Cl + O2. What is the net reaction?
D. O + O3 → 2O2
Adding the steps cancels Cl and ClO, giving O + O3 → 2O2; chlorine is regenerated.
Further reading: See the manual sources: Sawyer, McCarty & Parkin; Manahan; Stumm & Morgan; Seinfeld & Pandis; IS 10500; WMO/UNEP ozone assessment
Why does the Antarctic ozone hole form mainly in spring?
D. Spring sun frees cloud-activated chlorine
Winter PSCs convert reservoirs to Cl2 and HOCl; spring sunlight releases Cl atoms that destroy ozone rapidly.
Further reading: See the manual sources: Sawyer, McCarty & Parkin; Manahan; Stumm & Morgan; Seinfeld & Pandis; IS 10500; WMO/UNEP ozone assessment
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