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CSIR-UGC NET Environmental Chemistry: practice questions

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 papers
9worked here, free
18written to this exam in this subject
5syllabus units

What this subject covers

The 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)

What CSIR-UGC NET asks from it

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.

Where the 18 questions fall

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 acidification5
Chemical equilibrium, thermodynamics and reaction kinetics4
Stratospheric ozone chemistry and ozone-depleting substances4
Composition and structure of the atmosphere3
Redox reactions, pe-pH diagrams and redox zonation2

9 practice questions, worked

Choose an answer, then open the working. Each explanation says why the right answer is right and why the others are not.

1 · Chemical equilibrium, thermodynamics and reaction kinetics · medium

According to Le Chatelier's principle, raising the temperature of an exothermic equilibrium will

  1. shift it towards the reactants
  2. have no effect on the equilibrium position
  3. shift it towards the products
  4. double the equilibrium constant
Answer and working

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

2 · Chemical equilibrium, thermodynamics and reaction kinetics · medium

If the reaction quotient Q is smaller than the equilibrium constant K, the reaction will

  1. proceed in the reverse direction
  2. stop permanently
  3. proceed in the forward direction
  4. already be at equilibrium
Answer and working

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

3 · The carbonate system and ocean acidification · medium

Which carbonate species dominates dissolved inorganic carbon at pH 8.3 in fresh water at 25 °C (pKa1 6.35, pKa2 10.33)?

  1. Bicarbonate, about 98 per cent
  2. Dissolved CO2, about 98 per cent
  3. Carbonate, about 98 per cent
  4. Equal amounts of all three species
Answer and working

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

4 · Redox reactions, pe-pH diagrams and redox zonation · medium

A redox potential of +0.40 V is measured at 25 °C. What is the corresponding pe (pe = E/0.0592)?

  1. -6.8
  2. 0.024
  3. 6.8
  4. 0.40
Answer and working

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

5 · Redox reactions, pe-pH diagrams and redox zonation · hard

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?

  1. E is unchanged
  2. E decreases by 0.592 V
  3. E decreases by 0.0592 V
  4. E increases by 0.0592 V
Answer and working

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

6 · Composition and structure of the atmosphere · medium

Which radical is called the 'detergent of the atmosphere' because it initiates oxidation of most trace gases?

  1. The hydroxyl radical (OH)
  2. The nitrate radical (NO3)
  3. The superoxide ion (O2⁻)
  4. The chlorine atom (Cl)
Answer and working

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

7 · Composition and structure of the atmosphere · hard

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?

  1. 0.1 year
  2. 5500 years
  3. 2500 years
  4. 10 years
Answer and working

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

8 · Stratospheric ozone chemistry and ozone-depleting substances · medium

In a catalytic ozone-destruction cycle, Cl + O3 → ClO + O2 is followed by ClO + O → Cl + O2. What is the net reaction?

  1. 2O3 → 3O2 + Cl
  2. Cl + O3 → ClO + O2
  3. O2 → 2O
  4. O + O3 → 2O2
Answer and working

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

9 · Stratospheric ozone chemistry and ozone-depleting substances · medium

Why does the Antarctic ozone hole form mainly in spring?

  1. Ozone is produced only in autumn over Antarctica
  2. Spring winds blow ozone towards the equator
  3. Volcanic eruptions occur mostly in spring
  4. Spring sun frees cloud-activated chlorine
Answer and working

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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Read the subject

Environmental ChemistryThe full study manual, free CSIR-UGC NETFormat, sections and how it has changed

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