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CBSE Class 11 Chemistry Chapter 14 Notes: Environmental Chemistry

Detailed CBSE Class 11 Chemistry notes on Environmental Chemistry: atmospheric pollution, greenhouse effect, acid rain, ozone depletion, water pollution (BOD, COD), soil pollution, and the 12 principles of green chemistry.

Updated 11 June 202616 min read

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Chapter Introduction

Environmental Chemistry studies the chemical processes occurring in the environment and the impact of human activities on them. This chapter connects chemistry to real-world issues — air pollution, water contamination, soil degradation, ozone depletion, global warming, and acid rain. It also introduces green chemistry as a sustainable approach. This chapter is important for CBSE exams and often appears as short-answer and case-study questions. Understanding the chemical reactions behind environmental phenomena is essential for scoring well.


Key Definitions

TermDefinition
Environmental pollutionUndesirable changes in the physical, chemical, or biological characteristics of air, water, or land that harmfully affect human life, other organisms, or the environment
PollutantA substance present in the environment in greater than natural abundance that causes adverse effects
ContaminantA substance that does not occur in nature but is introduced by human activity
SourceThe place or process from which a pollutant originates
SinkThe medium that removes or stores a pollutant from the environment
ReceptorThe organism or system affected by the pollutant
BODBiochemical Oxygen Demand — the amount of dissolved oxygen required by aerobic microorganisms to decompose organic matter in water at 20°C over 5 days
CODChemical Oxygen Demand — the total oxygen required to oxidise all organic matter chemically (biodegradable + non-biodegradable)
EutrophicationNutrient enrichment of water bodies (especially N and P) leading to excessive algal growth and oxygen depletion
Greenhouse effectWarming of Earth's surface due to atmospheric gases that trap infrared radiation
Acid rainRain with pH below 5.0, caused by SO₂ and NOₓ reacting with atmospheric water
Green chemistryDesign of chemical processes that minimise or eliminate the use and generation of hazardous substances
Atom economyMeasure of how efficiently reactants are incorporated into the final product; % atom economy = (MW of desired product / MW of all products) × 100

Atmospheric Pollution

Tropospheric Pollution

The troposphere (0–11 km) contains most of the air mass. Tropospheric pollutants include:

Gaseous Pollutants

PollutantMajor SourcesEffects
COIncomplete combustion of fossil fuels, automobile exhaustBinds with haemoglobin (carboxyhaemoglobin), reducing O₂ transport; fatal at high concentrations
SO₂Fossil fuel combustion (coal), smelting, volcanic eruptionsRespiratory irritant; causes bronchitis, asthma; precursor to acid rain
NOₓ (NO, NO₂)Automobile exhaust, power plants, lightningRespiratory irritant; precursor to acid rain and photochemical smog; forms HNO₃
HydrocarbonsIncomplete combustion, petroleum refining, vehicle exhaustSome are carcinogenic; precursors to photochemical smog
O₃ (tropospheric)Formed from NOₓ + VOCs + sunlightRespiratory irritant; damages crops and vegetation

Particulate Matter

TypeSizeExamplesSources
Smoke0.5–5 μmCarbon particlesCombustion of coal, wood
Dust1–100 μmMineral particlesConstruction, mining, wind erosion
Fumes0.1–1 μmMetallic oxide particlesMetallurgical processes
Mist0.1–10 μmLiquid dropletsSpray, condensation
Smog—Mixture of smoke + fogVehicular and industrial emissions

Types of smog:

TypeCompositionConditionsLocation
Classical (reducing) smogSmoke + SO₂ + fogCool, humid climateLondon-type
Photochemical (oxidising) smogNOₓ + VOCs + O₃ + PAN + sunlightWarm, sunny climateLos Angeles-type

Photochemical smog formation: 1. NO₂ + hv (λ < 400 nm) → NO + O• 2. O• + O₂ → O₃ 3. O₃ + hydrocarbons → PAN (peroxyacyl nitrates), aldehydes 4. PAN is a powerful lachrymator (tear-inducing) and damages vegetation

Global Warming and Greenhouse Effect

The greenhouse effect is essential for life on Earth (without it, average temperature would be −18°C instead of +15°C). Enhanced greenhouse effect from excess gases is causing global warming.

Greenhouse Gases

GasSourcesGlobal Warming Potential (GWP)Atmospheric Lifetime
CO₂Fossil fuel combustion, deforestation1 (reference)50–200 years
CH₄Rice paddies, cattle, landfills, natural gas leaks2812 years
N₂OFertilisers, industrial processes265114 years
CFCsRefrigerants, aerosols, foam blowing agents4,750–14,00045–100 years

Key greenhouse effect reactions:

  • CO₂ + H₂O (photosynthesis) ← balanced naturally, but excess CO₂ overwhelms the sink
  • CH₄ is 28 times more potent than CO₂ per molecule but exists in lower concentrations
  • CFCs are the most potent greenhouse gases per molecule but exist in very small concentrations

Consequences of global warming: 1. Rise in sea level (thermal expansion + melting ice caps) 2. Changes in rainfall patterns (droughts and floods) 3. Loss of biodiversity and habitat 4. Increased frequency of extreme weather events 5. Spread of tropical diseases to temperate regions 6. Impact on agriculture and food security

Acid Rain

Acid rain is rain with pH below 5.0 (normal rain pH ≈ 5.6 due to dissolved CO₂).

Formation reactions:

From sulphur dioxide:

  • 2SO₂(g) + O₂(g) → 2SO₃(g)
  • SO₃(g) + H₂O(l) → H₂SO₄(aq)

From nitrogen oxides:

  • 2NO₂(g) + H₂O(l) → HNO₃(aq) + HNO₂(aq)
  • 4NO₂(g) + O₂(g) + 2H₂O(l) → 4HNO₃(aq)

Effects of acid rain:

Area AffectedEffect
Buildings and monumentsCorrosion of marble: CaCO₃ + H₂SO₄ → CaSO₄ + CO₂ + H₂O
Aquatic lifeLowers pH of lakes/rivers; fish eggs fail to hatch; aluminium leaching toxic to fish
SoilLeaches essential nutrients (Ca²⁺, Mg²⁺, K⁺); mobilises heavy metals
PlantsDamages leaves (chlorosis, necrosis); reduces photosynthesis
Human healthRespiratory problems; skin irritation

Control measures:

  • Use low-sulphur coal or natural gas
  • Install scrubbers in power plants (limestone slurry absorbs SO₂)
  • Catalytic converters in vehicles (reduce NOₓ emissions)
  • Liming of acidified lakes (CaCO₃ neutralises acid)

Stratospheric Pollution: Ozone Depletion

The ozone layer (stratosphere, 15–35 km) shields Earth from harmful UV radiation (200–315 nm).

Formation of ozone:

  • O₂ + hv (λ < 240 nm) → 2O• (photodissociation)
  • O• + O₂ → O₃ (ozone formation)

Natural destruction:

  • O₃ + hv → O₂ + O•
  • O₃ + O• → 2O₂

CFC-mediated destruction (catalytic cycle):

Step 1: CFCl₃ + hv → CFCl₂ + Cl• (UV breaks C—Cl bond in stratosphere)

Step 2: Cl• + O₃ → ClO• + O₂ (chlorine destroys ozone)

Step 3: ClO• + O• → Cl• + O₂ (chlorine regenerated)

Net reaction: O₃ + O• → 2O₂ (single Cl atom destroys ~100,000 O₃ molecules)

Ozone hole: Observed over Antarctica, especially during spring (September–October). Extreme cold (−85°C) leads to formation of polar stratospheric clouds (PSCs), which provide surfaces for heterogeneous reactions that convert inactive chlorine reservoirs (HCl, ClONO₂) into active Cl₂.

Montreal Protocol (1987): International agreement to phase out CFC production. Replaced by HCFCs (less ozone-depleting) and HFCs (no ozone-depleting potential, but some are greenhouse gases).


Water Pollution

Sources and Types

Pollutant TypeExamplesSources
PathogensBacteria, viruses, parasitesDomestic sewage, animal waste
Organic wastesSewage, food processing wasteDomestic and industrial discharge
Chemical pollutantsHeavy metals (Pb, Hg, Cd), pesticidesIndustrial effluents, agricultural runoff
NutrientsNitrates, phosphatesFertiliser runoff, detergents
Thermal pollutantsHeated waterPower plant cooling systems
Radioactive wastesUranium, caesiumNuclear power plants, medical waste

Eutrophication

Eutrophication is the excessive enrichment of water bodies with nutrients (especially N and P), leading to:

1. Excessive growth of algae and aquatic plants (algal bloom) 2. Depletion of dissolved oxygen as algae die and decompose 3. Death of fish and other aquatic organisms 4. Discolouration and foul smell of water 5. Loss of biodiversity

Water Quality Parameters

ParameterDefinitionClean Water ValuePolluted Water Value
BODOxygen required by microorganisms to decompose organic matter in 5 days at 20°C< 5 ppm> 5 ppm (severely polluted: > 20 ppm)
CODTotal oxygen required to oxidise all organic matter chemically (KMnO₄ or K₂Cr₂O₇)< 10 ppm> 10 ppm
DODissolved oxygen concentration6–8 ppm< 4 ppm (stressful for fish)
pHAcidity/alkalinity6.5–8.5Outside 6.5–8.5

BOD vs COD:

FeatureBODCOD
MeasuresBiodegradable organic matter onlyBiodegradable + non-biodegradable organic matter
MethodBiological (microorganisms)Chemical (strong oxidising agent)
Time5 days2–3 hours
ValueAlways ≤ CODAlways ≥ BOD
UseMunicipal wastewaterIndustrial wastewater (often toxic to microorganisms)

Soil Pollution

Sources

SourcePollutantEffect
PesticidesDDT, BHC, malathion, aldrinBioaccumulation in food chains; toxicity to non-target organisms
FertilisersNitrates, phosphatesSoil acidification; eutrophication of nearby water
Industrial wasteHeavy metals (Pb, Hg, Cd, As)Toxic to soil organisms and plants; enter food chain
Biomedical wastePathogens, pharmaceuticalsDisease transmission; antibiotic resistance
PlasticsPolythene, PVCNon-biodegradable; persist for hundreds of years
Electronic wasteLead, mercury, cadmiumLeach into groundwater

Bioaccumulation and biomagnification:

  • Bioaccumulation: Increase in concentration of a substance within a single organism over time
  • Biomagnification: Increase in concentration of a substance at each trophic level in a food chain

Example: DDT concentration increases from water (0.003 ppb) → phytoplankton → zooplankton → small fish → large fish → fish-eating birds (25 ppm) — a magnification of about 10 million times.


Green Chemistry

Green chemistry is the design of chemical products and processes that reduce or eliminate the use and generation of hazardous substances. It is not about cleaning up pollution after it occurs, but about preventing it at the source.

The 12 Principles of Green Chemistry

No.PrincipleExplanationExample
1PreventionPrevent waste rather than treat or clean it upDesign synthesis to minimise by-products
2Atom economyMaximise incorporation of all reactant atoms into the final productAddition reactions have higher atom economy than substitution
3Less hazardous synthesesUse methods that generate less toxic substancesUse H₂O₂ instead of Cl₂ for bleaching
4Designing safer chemicalsDesign chemicals that are effective but have reduced toxicityDesign pesticides that target specific pests
5Safer solvents and auxiliariesAvoid toxic solvents; use water, supercritical CO₂, or solvent-free methodsUse water-based paints instead of organic solvents
6Design for energy efficiencyMinimise energy requirements; run reactions at ambient T and PUse catalysts to lower activation energy
7Use renewable feedstocksUse raw materials that are renewable rather than depletableUse biomass instead of petroleum
8Reduce derivativesAvoid unnecessary protecting groups and functional group interconversionsDirect synthesis rather than multi-step protection/deprotection
9CatalysisUse catalytic rather than stoichiometric reagentsUse enzymes or metal catalysts
10Design for degradationDesign chemicals that break down into harmless productsBiodegradable plastics
11Real-time analysisMonitor and control processes in real time to prevent pollutionIn-line sensors for process control
12Inherently safer chemistryChoose substances that minimise risk of accidentsUse less volatile, less flammable solvents

Atom Economy

Formula% Atom Economy = (Molecular weight of desired product / Sum of molecular weights of all products) × 100
Reaction TypeAtom EconomyReason
Addition reaction100%All atoms of reactants appear in the product
Rearrangement100%Atoms are reorganised, none lost
Substitution< 100%A leaving group is expelled
Elimination< 100%A small molecule is lost

Example: Synthesis of ibuprofen

  • Old process: 6 steps, 40% atom economy, large waste
  • Green process: 3 steps, 77% atom economy (BHC Company process), much less waste

Greener Alternatives in Practice

Conventional MethodGreener AlternativeAdvantage
Dry cleaning with perchloroethylene (C₂Cl₄)Supercritical CO₂ cleaningNon-toxic, no ozone depletion
Bleaching paper with Cl₂Bleaching with H₂O₂No chlorinated dioxins formed
Petrol-powered vehiclesCNG (compressed natural gas) or electricLower SO₂, NOₓ, and particulate emissions
Lead-based paintsWater-based paintsEliminates lead exposure
Stoichiometric oxidising agentsCatalytic oxidation with H₂O₂Less waste, milder conditions
Organic solvents in synthesisSolvent-free or aqueous synthesisNo VOC emissions

Strategies for Pollution Control

Air Pollution Control

StrategyHow It WorksTarget Pollutant
Catalytic convertersPt/Pd/Rh catalysts convert CO → CO₂, NOₓ → N₂, unburnt HC → CO₂ + H₂OCO, NOₓ, hydrocarbons
ScrubbersLimestone (CaCO₃) slurry absorbs SO₂ in exhaust gasSO₂
Electrostatic precipitatorsElectrically charged plates remove particulate matterFly ash, dust
Unleaded petrolEliminates Pb emissionsLead
CNG/LPGCleaner combustion than petrol/dieselCO, NOₓ, particulates

Water Pollution Control

StrategyDescription
Primary treatmentPhysical screening and sedimentation to remove suspended solids
Secondary treatmentBiological oxidation using aerobic bacteria to reduce BOD
Tertiary treatmentChemical treatment (coagulation, filtration, disinfection) to remove dissolved pollutants
Effluent treatment plants (ETP)Treat industrial wastewater before discharge
Sewage treatment plants (STP)Treat domestic wastewater
Rainwater harvestingRecharge groundwater; reduce urban runoff

Soil Pollution Control

StrategyDescription
BioremediationUse microorganisms to degrade organic pollutants in soil
PhytoremediationUse plants to absorb, accumulate, or degrade contaminants
CompostingConvert organic waste into nutrient-rich soil amendment
Reducing pesticide useIntegrated pest management (IPM); organic farming
Proper waste disposalSegregation at source; recycling; safe landfill design

Common Mistakes to Avoid

1. Confusing BOD and COD: BOD measures only biodegradable organic matter (biological process, 5 days). COD measures total organic matter including non-biodegradable (chemical process, hours). COD ≥ BOD always. 2. Attributing ozone depletion to CO₂: CO₂ does NOT deplete ozone. CFCs and halons are the ozone-depleting substances. CO₂ causes global warming, not ozone depletion. 3. Normal rain pH: Normal rain is slightly acidic (pH ≈ 5.6) due to dissolved CO₂ forming carbonic acid. Acid rain is defined as pH < 5.0, not pH < 7. 4. CFC mechanism: Remember the catalytic cycle — one Cl atom destroys ~100,000 O₃ molecules. Write the full cycle: Cl• + O₃ → ClO• + O₂; ClO• + O• → Cl• + O₂. 5. Green chemistry is NOT environmental chemistry: Green chemistry is about designing processes to prevent pollution at the source. Environmental chemistry studies pollution that has already occurred. 6. Photochemical smog vs classical smog: Classical smog (London-type) = smoke + SO₂ + fog (reducing). Photochemical smog (LA-type) = NOₓ + VOCs + sunlight (oxidising, contains O₃ and PAN). 7. Atom economy calculation: Use the sum of molecular weights of ALL products in the denominator, not just reactants. For addition reactions, atom economy = 100%.


Exam Tips

  • Most-asked questions: Acid rain formation (2–3 marks), ozone depletion mechanism (3 marks), greenhouse gases and GWP (2 marks), BOD vs COD (2 marks), green chemistry principles (3 marks), eutrophication (2 marks)
  • Acid rain equations: Practise writing the SO₂ → H₂SO₄ and NOₓ → HNO₃ reaction sequences
  • Ozone depletion cycle: Write the catalytic cycle with Cl• as the catalyst. Net: O₃ + O → 2O₂
  • BOD and COD: Know the definitions, differences, and typical values. Clean water: BOD < 5 ppm; polluted water: BOD > 5 ppm
  • Green chemistry: At least 4–5 of the 12 principles should be memorised with examples. Atom economy formula is frequently asked.
  • Montreal Protocol: Know the year (1987) and that it phased out CFCs
  • Biomagnification: Explain with the DDT example — concentration increases at each trophic level

Quick Revision Notes

Atmospheric Pollution

  • Tropospheric: CO, SO₂, NOₓ, hydrocarbons, particulates, smog
  • Classical smog: reducing, smoke + SO₂ + fog (London-type)
  • Photochemical smog: oxidising, NOₓ + VOCs + sunlight + O₃ + PAN (LA-type)

Global Warming

  • Greenhouse gases: CO₂ (GWP = 1), CH₄ (GWP = 28), N₂O (GWP = 265), CFCs (GWP = 4750–14000)
  • Greenhouse effect: gases absorb and re-emit infrared radiation from Earth
  • Consequences: sea level rise, climate change, biodiversity loss

Acid Rain

  • Caused by SO₂ → H₂SO₄ and NOₓ → HNO₃
  • Normal rain pH ≈ 5.6; acid rain pH < 5.0
  • Effects: marble corrosion, lake acidification, soil leaching, plant damage
  • Control: scrubbers, catalytic converters, low-sulphur fuels

Ozone Depletion

  • Ozone layer: 15–35 km altitude, absorbs UV-B (200–315 nm)
  • CFCs release Cl• which catalytically destroys O₃
  • One Cl atom destroys ~100,000 O₃ molecules
  • Montreal Protocol (1987): phased out CFCs
  • Ozone hole: observed over Antarctica during spring

Water Pollution

  • BOD: biological, 5 days, biodegradable organics only (< 5 ppm = clean)
  • COD: chemical, hours, all organics (≥ BOD always)
  • Eutrophication: nutrient enrichment → algal bloom → O₂ depletion → fish kill
  • Biomagnification: pollutant concentration increases at each trophic level

Soil Pollution

  • Sources: pesticides, heavy metals, biomedical waste, plastics
  • DDT biomagnification: concentration increases up the food chain

Green Chemistry

  • 12 principles: prevention, atom economy, safer synthesis, safer chemicals, safer solvents, energy efficiency, renewable feedstocks, reduce derivatives, catalysis, design for degradation, real-time analysis, safer chemistry
  • Atom economy = (MW desired product / MW all products) × 100
  • Addition reactions = 100% atom economy

Frequently Asked Questions

The greenhouse effect is the warming of Earth's surface and lower atmosphere caused by certain gases in the atmosphere that absorb and re-emit infrared radiation emitted by Earth. The major greenhouse gases are: CO₂ (from fossil fuel combustion, deforestation), CH₄ (from rice paddies, cattle, landfills), N₂O (from fertilisers, industrial processes), and CFCs (from refrigerants, aerosols). These gases are transparent to incoming short-wavelength solar radiation but absorb the long-wavelength infrared radiation emitted by Earth, trapping heat. Without the natural greenhouse effect, Earth's average temperature would be about −18°C instead of +15°C.