Wednesday, 25 February 2026

Ch 6: Water

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Chapter 6: Water

💧 Complete Chapter for PSTET Paper II (Social Studies)


🎯 Learning Objectives for PSTET Aspirants

After completing this chapter, you will be able to:

  • Analyze the distribution of water on Earth and understand the scarcity of usable freshwater

  • Explain the water cycle and its processes with scientific accuracy

  • Describe ocean relief features and their characteristics

  • Differentiate between waves, tides, and ocean currents with their causes and effects

  • Evaluate water as a resource for various human activities

  • Identify causes and effects of water pollution and propose conservation methods

  • Apply pedagogical strategies through models, discussions, and conservation projects


6.1 Distribution of Water on Earth: Freshwater vs. Saline Water, the Scarcity of Usable Water

🌍 The Blue Planet

Earth is often called the "Blue Planet" because water covers approximately 71% of its surface. However, this abundance is misleading when it comes to usable water .

📊 Global Water Distribution

Water TypePercentageVolume (cubic km)Location
Saline Water (Oceans)97.5%1,365,000,000Oceans and seas
Freshwater2.5%35,000,000Glaciers, ice caps, groundwater, lakes, rivers

❄️ Freshwater Breakdown

Of the 2.5% freshwater, its distribution is highly unequal:

text
                    TOTAL FRESHWATER (2.5%)
                           │
        ┌──────────────────┼──────────────────┐
        ▼                  ▼                  ▼
┌───────────────┐  ┌───────────────┐  ┌───────────────┐
│   GLACIERS    │  │  GROUNDWATER  │  │  SURFACE      │
│   & ICE CAPS  │  │               │  │  WATER        │
│     68.7%     │  │     30.1%     │  │     1.2%      │
└───────────────┘  └───────────────┘  └───────────────┘
                                              │
                              ┌───────────────┼───────────────┐
                              ▼               ▼               ▼
                       ┌───────────┐  ┌───────────┐  ┌───────────┐
                       │   LAKES   │  │  SOIL     │  │ RIVERS    │
                       │   0.26%   │  │ MOISTURE  │  │  0.006%   │
                       └───────────┘  │   0.05%   │  └───────────┘
                                      └───────────┘
Freshwater SourcePercentage of Total FreshwaterAvailability
Glaciers and Ice Caps68.7%Frozen; inaccessible
Groundwater30.1%Deep; requires pumping
Lakes0.26%Accessible but unevenly distributed
Soil Moisture0.05%For plants only
Rivers0.006%Most accessible but tiny fraction
Atmosphere0.04%Water vapor

💧 The Scarcity Reality

Usable freshwater available for human consumption is extremely limited:

FactImplication
Only 0.3% of total water is readily usableMost freshwater is locked in ice or deep underground
1.1 billion people lack access to safe drinking waterWater scarcity is a global crisis
2.4 billion lack adequate sanitationWater pollution affects health
By 2025, 1.8 billion people will live in water-scarce regionsGrowing crisis

🌊 Saline Water (Oceans and Seas)

OceanArea (million sq km)Average Depth (m)Deepest Point
Pacific Ocean165.24,280Mariana Trench (11,034 m)
Atlantic Ocean106.53,646Puerto Rico Trench (8,605 m)
Indian Ocean70.63,741Java Trench (7,725 m)
Southern Ocean20.33,270South Sandwich Trench (7,235 m)
Arctic Ocean14.11,205Eurasian Basin (5,450 m)

📝 PSTET Focus Point: The key takeaway is that although Earth has abundant water, usable freshwater is extremely scarce—only about 0.3% of total water. This understanding is fundamental for teaching water conservation.


6.2 The Water Cycle / Hydrological Cycle: Processes of Evaporation, Condensation, Precipitation, and Collection

🔄 What is the Water Cycle?

The water cycle (hydrological cycle) is the continuous movement of water on, above, and below the Earth's surface. It is a closed system—no water is lost or gained; it simply changes form and location .

text
                    ┌─────────────────────────────────────┐
                    │         CONDENSATION                │
                    │    (Water vapor → Clouds)           │
                    └───────────────┬─────────────────────┘
                                    │
                                    │
                    ┌───────────────▼─────────────────────┐
                    │                                      │
              ┌─────┴─────┐                        ┌──────┴─────┐
              │           │                        │            │
              │  PRECIPITATION                     │ EVAPORATION│
              │  (Rain, snow, hail)                │ (Water →   │
              │           │                        │  vapor)    │
              └─────┬─────┘                        └──────┬─────┘
                    │                                      │
                    │                                      │
                    └───────────────┬──────────────────────┘
                                    │
                    ┌───────────────▼─────────────────────┐
                    │              COLLECTION              │
                    │  (Oceans, lakes, rivers, groundwater)│
                    └─────────────────────────────────────┘

💨 Key Processes of the Water Cycle

1. Evaporation

AspectDescription
DefinitionProcess by which water changes from liquid to gas (water vapor)
Energy SourceSolar radiation (heat from the Sun)
Main LocationsOceans (86% of evaporation), lakes, rivers, soil
Rate FactorsTemperature, humidity, wind speed, surface area

Transpiration: Plants release water vapor through their leaves. Combined evaporation and transpiration is called evapotranspiration .

2. Condensation

AspectDescription
DefinitionProcess by which water vapor changes back to liquid water
TriggerAir cools to its dew point (saturation temperature)
RequirementsHygroscopic nuclei (dust, salt, smoke particles)
ResultsClouds, fog, dew

Cloud Formation: As warm, moist air rises, it expands and cools. When it reaches dew point, water vapor condenses around particles, forming tiny water droplets or ice crystals—clouds .

3. Precipitation

AspectDescription
DefinitionWater falling from clouds to Earth's surface
TriggerWater droplets grow too heavy to remain suspended
FormsRain, snow, sleet, hail, drizzle
Global DistributionHighest near equator, decreases toward poles

4. Collection (Runoff and Infiltration)

ProcessDescriptionDestination
RunoffWater flows over land surfaceRivers, lakes, oceans
InfiltrationWater soaks into groundGroundwater, aquifers
PercolationWater moves deeper through soil/rockDeep groundwater

📊 Water Cycle by the Numbers

ProcessVolume (cubic km/year)Percentage
Evaporation from oceans436,50086%
Evaporation from land71,00014%
Total Evaporation507,500100%
Precipitation on oceans398,00078%
Precipitation on land109,50022%
Total Precipitation507,500100%
Runoff from land to oceans38,500-

💡 Key Insight: The water cycle is balanced—total evaporation equals total precipitation. However, distribution is uneven: oceans lose more water through evaporation than they gain from precipitation, while land gains more from precipitation than it loses through evaporation. The difference is made up by runoff from land to oceans .

⏱️ Residence Time of Water

Water spends varying amounts of time in different reservoirs:

ReservoirAverage Residence Time
Glaciers20-100 years
Oceans3,000 years
Groundwater (deep)10,000+ years
Lakes50-100 years
Rivers2-6 months
Atmosphere9-10 days
Soil moisture2 weeks-1 year

6.3 Oceans and Seas

6.3.1 Ocean Relief: Features of the Ocean Floor

The ocean floor is not flat—it has varied relief features similar to continents .

text
                    ┌─────────────────────────────────────┐
                    │         CONTINENTAL SHELF           │
                    │  (Gradual slope from shore)         │
                    └───────────┬─────────────────────────┘
                                │
                    ┌───────────▼─────────────────────────┐
                    │         CONTINENTAL SLOPE           │
                    │  (Steep drop)                       │
                    └───────────┬─────────────────────────┘
                                │
                    ┌───────────▼─────────────────────────┐
                    │         CONTINENTAL RISE            │
                    │  (Gentle slope to deep ocean)       │
                    └───────────┬─────────────────────────┘
                                │
        ┌───────────────────────┼───────────────────────┐
        ▼                       ▼                       ▼
┌───────────────┐      ┌───────────────┐      ┌───────────────┐
│   ABYSSAL     │      │  MID-OCEAN    │      │   DEEP-SEA    │
│    PLAIN      │      │    RIDGE      │      │   TRENCHES    │
│  (Flat deep)  │      │ (Underwater   │      │ (Deepest      │
└───────────────┘      │  mountains)   │      │  parts)       │
                       └───────────────┘      └───────────────┘

Major Ocean Floor Features

FeatureDescriptionDepth RangeCharacteristicsExamples
Continental ShelfGently sloping submerged extension of continent0-200 mRichest fishing grounds; oil and gas deposits; sunlight reaches bottomBroad off Siberia, narrow off South America
Continental SlopeSteep slope connecting shelf to deep ocean200-3,000 mCanyons cut by turbidity currents; boundary between continental and oceanic crust-
Continental RiseGentle slope of accumulated sediments3,000-4,000 mFormed by sediment deposition from turbidity currents-
Abyssal PlainFlat, featureless deep ocean floor3,000-6,000 mCovered with fine sediments; most level places on EarthCover 40% of ocean floor
Mid-Ocean RidgeUnderwater mountain range2,000-3,000 m above floorVolcanic activity; new crust formed; longest mountain chain on EarthMid-Atlantic Ridge (16,000 km)
Deep-Sea TrenchesDeep, narrow depressions6,000-11,000 mSubduction zones; deepest parts of oceanMariana Trench (11,034 m)
SeamountsUnderwater volcanic mountainsVariesMay rise >1,000 m from ocean floor; flat-topped ones called guyotsEmperor Seamounts
Volcanic IslandsSeamounts rising above sea levelAbove sea levelFormed by volcanic activityHawaii, Andaman Islands

Important Trenches

TrenchOceanMaximum Depth (m)
Mariana TrenchPacific11,034
Tonga TrenchPacific10,882
Philippine TrenchPacific10,540
Kuril-Kamchatka TrenchPacific10,542
Puerto Rico TrenchAtlantic8,605
Java TrenchIndian7,725

Ocean Floor Sediments

TypeCompositionLocation
TerrigenousEroded from land (sand, mud)Near continents
BiogenousShells and skeletons of marine organismsDeep ocean floors
HydrogenousPrecipitated from seawater (manganese nodules)Abyssal plains
CosmogenousSpace dust and meteorite debrisRare; everywhere

6.3.2 Ocean Water Movements: Waves, Tides, and Ocean Currents

Ocean water is in constant motion, driven by various forces .

🌊 Waves

AspectDescription
DefinitionOscillatory movement of water surface
Energy SourceWind (mostly)
MotionWater particles move in circular orbits; energy moves forward, not water itself
PartsCrest (highest point), Trough (lowest point), Height (crest to trough), Length (crest to crest)
Types of Waves
TypeCauseCharacteristics
Wind WavesLocal windIrregular; short wavelength
SwellsDistant stormsRegular; long wavelength
TsunamisEarthquakes, volcanic eruptionsVery long wavelength (100-200 km); speed up to 800 km/h; destructive near shore
Tidal WavesGravitational pull of moon/sunActually tides, not true waves

Wave Behavior Near Shore:

  • Wave speed decreases in shallow water

  • Wavelength decreases

  • Wave height increases

  • Wave becomes unstable and breaks (surf)

🌕 Tides

Tides are the periodic rise and fall of sea level caused primarily by the gravitational pull of the Moon and, to a lesser extent, the Sun.

Cause of Tides
text
                    ┌─────────────────────────────────────┐
                    │         GRAVITATIONAL FORCES        │
                    └─────────────────────────────────────┘
                                    │
              ┌─────────────────────┼─────────────────────┐
              ▼                     ▼                     ▼
    ┌───────────────┐      ┌───────────────┐      ┌───────────────┐
    │   MOON'S      │      │   SUN'S       │      │  CENTRIFUGAL  │
    │  GRAVITY      │      │  GRAVITY      │      │    FORCE      │
    │ (Primary)     │      │ (Secondary)   │      │ (Opposite to  │
    └───────────────┘      └───────────────┘      │  gravity)     │
                                                   └───────────────┘

Tidal Bulges: Two bulges occur—one facing the moon (due to gravity) and one opposite the moon (due to centrifugal force). As Earth rotates, different locations pass through these bulges, experiencing two high tides and two low tides approximately every 24 hours 50 minutes .

Types of Tides
TypeFrequencyCharacteristics
Spring TidesTwice monthly (full and new moon)Sun and moon aligned; highest high tides; lowest low tides
Neap TidesTwice monthly (first and last quarter moon)Sun and moon at right angles; least tidal range
text
                    SPRING TIDES                    NEAP TIDES
              ┌─────────────────────┐         ┌─────────────────────┐
              │   Sun  Moon  Earth  │         │   Sun               │
              │      ●───●────●     │         │      ●              │
              │      │              │         │       \             │
              │      └──Gravity───► │         │        \            │
              │    (Aligned)        │         │         ● Earth     │
              │                     │         │        /            │
              │  High tides VERY    │         │       /             │
              │  HIGH; Low tides    │         │      ● Moon         │
              │  VERY LOW           │         │   (At right angles) │
              │                     │         │                     │
              │  Tidal range:       │         │  Tidal range:       │
              │  MAXIMUM            │         │  MINIMUM            │
              └─────────────────────┘         └─────────────────────┘
Importance of Tides
ImportanceDescription
NavigationHelp ships enter shallow ports during high tide
FishingFish gather during tides; traditional knowledge used
Tidal EnergyRenewable energy source (tidal power plants)
Coastal EcosystemsIntertidal zones support unique biodiversity
Waste DisposalFlush out pollutants from estuaries

🌊 Ocean Currents

Ocean currents are continuous, directed movements of ocean water flowing horizontally .

Causes of Ocean Currents
CauseTypeDescription
WindSurface currentsPlanetary winds (trade winds, westerlies) drive surface currents
Earth's RotationCoriolis effectDeflects currents to right in N. Hemisphere, left in S. Hemisphere
TemperatureThermohaline circulationCold, dense water sinks; warm water rises
SalinityThermohaline circulationHigher salinity = denser water = sinks
LandmassesObstructionContinents deflect currents
Classification of Ocean Currents

Based on Temperature:

TypeTemperatureDirectionExamples
Warm CurrentsWarmer than surrounding waterFrom equator toward polesGulf Stream, Kuroshio, Brazil Current
Cold CurrentsColder than surrounding waterFrom poles toward equatorLabrador, Canary, Benguela, Peru (Humboldt)

Based on Depth:

TypeDepthCause
Surface CurrentsTop 400 mWind-driven
Deep Water CurrentsBelow 400 mDensity differences (temperature, salinity)
Major Ocean Currents
text
                    NORTH AMERICA
                          │
        ┌─────────────────┼─────────────────┐
        │                 │                 │
        ▼                 ▼                 ▼
┌───────────────┐  ┌───────────────┐  ┌───────────────┐
│   Labrador    │  │  Gulf Stream  │  │ Canary Current│
│   Cold        │  │  Warm         │  │ Cold          │
└───────────────┘  └───────────────┘  └───────────────┘
CurrentOceanTypeDestination/Origin
Gulf StreamAtlanticWarmFrom Gulf of Mexico to NW Europe
North Atlantic DriftAtlanticWarmExtension of Gulf Stream; warms Europe
Canary CurrentAtlanticColdOff NW Africa; flows south
Benguela CurrentAtlanticColdOff SW Africa; flows north
Labrador CurrentAtlanticColdFrom Arctic to NE North America
Brazil CurrentAtlanticWarmSouth along Brazil coast
Kuroshio CurrentPacificWarmEast of Japan; "Pacific Gulf Stream"
Oyashio CurrentPacificColdFrom Arctic to NE Japan
California CurrentPacificColdWest coast of North America
Peru (Humboldt) CurrentPacificColdWest coast of South America
East Australian CurrentPacificWarmEast coast of Australia
Agulhas CurrentIndianWarmEast coast of Africa
West Australian CurrentIndianColdWest coast of Australia
Effects of Ocean Currents
EffectDescriptionExamples
Climate ModificationWarm currents raise temperatures; cold currents lower themGulf Stream warms NW Europe; Labrador Current chills NE Canada
Fog FormationCold currents cool warm, moist air → fogGrand Banks fog (Labrador Current meets Gulf Stream)
Desert FormationCold currents stabilize air, reducing rainfallAtacama Desert (Peru Current); Namib Desert (Benguela Current)
Rainfall PatternsWarm currents increase evaporation → rainfallEastern coasts of continents (warm currents)
Marine LifeCurrents distribute nutrients and larvaeUpwelling areas (cold currents) rich in fish
NavigationCurrents affect ship travel timesFollowing currents saves fuel
Thermohaline Circulation (Global Conveyor Belt)

The global conveyor belt is a deep-ocean circulation system driven by temperature and salinity differences :

text
    ┌─────────────────────────────────────────────────────────┐
    │                                                          │
    │   North Atlantic ──► Deep water forms ──► Flows south   │
    │        │                                                │
    │        ▼                                                │
    │   Southern Ocean ──► Indian Ocean ──► Pacific Ocean     │
    │        │                                                │
    │        ▼                                                │
    │   Upwelling ──► Warm surface return flow                │
    │                                                          │
    │   Complete cycle takes ~1,000 years                      │
    └─────────────────────────────────────────────────────────┘

Importance:

  • Distributes heat globally

  • Brings nutrients to surface (upwelling)

  • Regulates climate


6.4 Water as a Resource: Importance for Drinking, Irrigation, Industry, and Transportation

💧 The Many Uses of Water

Water is essential for virtually all human activities .

1. Drinking and Domestic Use

UsePercentage of Global Water UseImportance
DrinkingSmall fractionEssential for survival; humans need 2-3 liters/day
Cooking-Food preparation
Sanitation-Hygiene, disease prevention
Cleaning-Household and personal cleanliness

Global Access:

  • 71% of global population has access to safely managed drinking water

  • 2.2 billion people lack safely managed drinking water

  • 3.6 billion lack safely managed sanitation

2. Irrigation (Agriculture)

AspectDetail
Global Water Use70% of all freshwater withdrawals
In India80-90% of freshwater used for agriculture
PurposeCrop production; livestock
MethodsCanal irrigation, wells, drip irrigation, sprinklers

Water-Intensive Crops:

  • Rice: 2,500-5,000 liters per kg

  • Wheat: 1,500-2,000 liters per kg

  • Sugarcane: 1,500-2,500 liters per liter of juice

  • Cotton: 10,000-20,000 liters per kg

Punjab Context:

  • Punjab uses 85% of its water for agriculture

  • Paddy (rice) is the most water-intensive crop

  • Groundwater depletion is a serious concern—water table dropping 0.5-1.0 m per year in many areas

3. Industry

UsePercentage of Global Water UseExamples
Manufacturing19%Processing, cooling, washing
Energy Production-Thermal power plant cooling; hydropower
Mining-Mineral processing
Construction-Mixing concrete

Industrial Uses:

  • Cooling: Thermal and nuclear power plants require huge amounts

  • Processing: Food, beverage, textile, paper industries

  • Cleaning: Washing raw materials and products

  • Solvent: Chemical industries

  • Transport: Slurry pipelines

4. Transportation

ModeDescriptionImportance
Inland WaterwaysRivers, canals, lakesLow-cost transport; fuel-efficient
Ocean ShippingSeas and oceans90% of global trade by volume
Ports and HarborsCoastal infrastructureTrade hubs

India's Water Transport:

  • Inland waterways: 14,500 km navigable; National Waterways (Ganga, Brahmaputra)

  • Major ports: 12 major ports (Mumbai, Chennai, Kolkata, Kandla, etc.)

  • Minor ports: 200+ along coastline

5. Other Uses

UseDescription
RecreationSwimming, boating, fishing
HydropowerElectricity generation from flowing water
Ecosystem SupportMaintains wetlands, rivers, lakes
Cultural/ReligiousRituals, pilgrimages (Ganga, Yamuna)

6.5 Water Pollution and Conservation: Causes, Effects, and Methods

🚯 Water Pollution

Water pollution is the contamination of water bodies by harmful substances, making water unsafe for human use and damaging aquatic ecosystems .

Major Causes of Water Pollution

SourceTypesExamples
Industrial WasteChemicals, heavy metals, toxinsFactories discharge untreated effluents
Agricultural RunoffFertilizers, pesticides, animal wasteNitrogen, phosphorus cause eutrophication
Domestic SewageHuman waste, detergents, pathogensUntreated sewage into rivers
Oil SpillsCrude oil, petroleum productsTanker accidents; offshore drilling
Plastic WasteNon-biodegradable debrisMicroplastics in oceans
Thermal PollutionHeated water from power plantsReduces oxygen; harms aquatic life
Mining ActivitiesAcid mine drainage, heavy metalsContaminates groundwater and rivers

Types of Water Pollutants:

Pollutant TypeExamplesEffects
PathogensBacteria, viruses, parasitesWaterborne diseases (cholera, typhoid)
Organic MatterSewage, food wasteOxygen depletion; fish kills
NutrientsNitrogen, phosphorusEutrophication; algal blooms
ChemicalsPesticides, industrial chemicalsToxicity; bioaccumulation
Heavy MetalsLead, mercury, arsenicPoisoning; long-term health effects
SedimentsSoil erosionTurbidity; smothers aquatic life
PlasticsMicroplastics, macroplasticsIngestion by marine life; ecosystem damage

Effects of Water Pollution

EffectDescription
Human HealthWaterborne diseases (diarrhea, cholera, typhoid); 1.8 million deaths annually
Aquatic LifeFish kills; habitat destruction; biodiversity loss
EutrophicationAlgal blooms; oxygen depletion; dead zones (e.g., Gulf of Mexico)
Economic ImpactFishing industry losses; tourism decline; water treatment costs
Ecosystem DisruptionFood chain contamination; species extinction

🌱 Water Conservation

Water conservation is the practice of using water efficiently to reduce unnecessary water usage .

Why Conserve Water?

ReasonExplanation
ScarcityFreshwater is limited (only 0.3% usable)
Growing DemandPopulation growth, agriculture, industry increase demand
Groundwater DepletionOver-extraction lowers water tables
Climate ChangeAlters rainfall patterns; increases droughts
Ecosystem ProtectionMaintains rivers, lakes, wetlands

Methods of Water Conservation

1. Rainwater Harvesting

Rainwater harvesting is the collection and storage of rainwater for reuse.

text
                    ┌─────────────────────────────────────┐
                    │           RAINWATER                  │
                    │           HARVESTING                  │
                    └─────────────────────────────────────┘
                                    │
              ┌─────────────────────┼─────────────────────┐
              ▼                     ▼                     ▼
    ┌───────────────┐      ┌───────────────┐      ┌───────────────┐
    │  ROOFTOP      │      │  SURFACE      │      │  RECHARGE     │
    │  COLLECTION   │      │  RUNOFF       │      │  STRUCTURES   │
    ├───────────────┤      │  COLLECTION   │      ├───────────────┤
    │ • Gutters     │      ├───────────────┤      │ • Recharge    │
    │ • Downpipes   │      │ • Ponds       │      │   wells       │
    │ • Storage     │      │ • Tanks       │      │ • Percolation │
    │   tanks       │      │ • Check dams  │      │   pits        │
    └───────────────┘      └───────────────┘      └───────────────┘

Benefits of Rainwater Harvesting:

  • Reduces runoff and flooding

  • Recharges groundwater

  • Provides water during dry periods

  • Reduces demand on municipal supplies

  • Improves water quality (dilutes pollutants)

Traditional Methods in India:

MethodRegionDescription
KundsRajasthanCovered tanks for rainwater
JohadsRajasthanEarthen check dams
KhadinsRajasthanEmbankments to capture runoff
Ahar-PynesBiharChannels and reservoirs
Eri (Tanks)Tamil NaduVillage ponds for irrigation
KulsHimachalWater channels from streams
ZaboNagalandIntegrated systems for rainwater
2. Water-Efficient Agriculture
MethodDescriptionWater Savings
Drip IrrigationWater delivered directly to plant roots30-70% less than flood irrigation
Sprinkler IrrigationWater sprayed like rain30-50% less than flood irrigation
MulchingCover soil to reduce evaporation10-30% savings
Crop SelectionGrow less water-intensive cropsSignificant
Furrow IrrigationWater in channels between rowsMore efficient than flood
Laser Land LevelingPrecise field leveling20-30% water savings
3. Domestic Water Conservation
MethodWater Saved (per person per day)
Fix leaky taps10-50 liters
Turn off tap while brushing10-15 liters
Use bucket instead of shower50-100 liters
Dual-flush toilets20-40 liters
Water-efficient appliances30-50 liters
Reuse RO wastewater10-20 liters
4. Industrial Water Conservation
MethodDescription
RecyclingTreat and reuse water in processes
Cooling TowersRecycle cooling water
Dry CoolingAir cooling instead of water
Water AuditsIdentify and fix leaks
Efficient ProcessesModify manufacturing to use less water
5. Community and Government Initiatives
InitiativeDescription
Watershed DevelopmentIntegrated management of land and water
Check DamsSmall dams to store monsoon runoff
Pond RenovationCleaning and deepening village ponds
Groundwater RegulationControl on borewell drilling
Water PricingIncentivize conservation
Public AwarenessCampaigns, school programs

📊 Water Conservation Success Stories in India

LocationInitiativeResult
Ralegan Siddhi (Maharashtra)Watershed development, rainwater harvestingFrom drought-prone to water-sufficient
Hiware Bazar (Maharashtra)Water budgeting, contour trenchesGroundwater levels rose; prosperity increased
Arvari River (Rajasthan)Community check damsRiver revived after 60 years of drying
Sukhomajri (Haryana)Watershed managementReduced erosion; increased water availability
Tamil NaduMandatory rooftop rainwater harvestingGroundwater levels stabilized

6.6 Pedagogical Focus: Creating Models, Discussing Local Issues, and Promoting Conservation

🧒 Understanding the Learner (Classes VI-VIII)

Upper primary students:

  • Are concrete thinkers; learn through hands-on activities

  • Can understand cause-and-effect relationships

  • Develop environmental awareness and sense of responsibility

  • Can participate in community projects

🌊 Creating Models of the Water Cycle

Simple Water Cycle Model (In a Bottle)

StepInstructions
MaterialsClear plastic bottle, soil, small plant, water, cling film, elastic band, ice cubes
Step 1Cut bottle in half; keep top and bottom
Step 2Place soil and small plant in bottom; add water
Step 3Invert top portion like a funnel into bottom
Step 4Cover top with cling film; secure with band
Step 5Place ice cubes on cling film
Step 6Place in sunny spot
ObservationWater evaporates, condenses on cool film, "rains" back into soil

3D Water Cycle Model

ComponentMaterialRepresentation
SunYellow ball/paperEnergy source
OceanBlue paper/waterWater body
EvaporationArrows (blue→white)Water rising
CloudsCotton ballsCondensation
PrecipitationBlue beads/threadsRain falling
MountainsBrown paper/ clayLandforms
RiverBlue ribbonRunoff
GroundwaterBlue under brown layerInfiltration

💬 Discussing Local Water Issues

Inquiry-Based Discussion Framework

QuestionPurpose
"Where does our drinking water come from?"Identify local water sources
"Is water easily available throughout the year?"Understand seasonal variation
"Have you ever faced water shortage?"Personal connection
"What happens to dirty water from our homes?"Wastewater awareness
"Are the rivers/ponds in our area clean?"Local pollution awareness
"Why do farmers need so much water?"Agricultural water use
"How can we use less water?"Conservation thinking

Local Water Issues to Discuss

Issue TypeExamples
Groundwater DepletionFalling water table in Punjab; deep borewells
Canal Water DistributionSharing disputes; tail-end deprivation
River PollutionSutlej, Beas pollution; industrial waste
Stubble Burning and WaterLink to groundwater?
Flooding vs. DroughtSeasonal extremes
Water QualityArsenic, fluoride, salinity

🏫 Promoting Water Conservation in Schools

School-Wide Activities

ActivityDescriptionImpact
Water AuditStudents measure water usage in schoolData-driven awareness
Leak DetectionCheck all taps and pipes for leaksImmediate water savings
Rainwater Harvesting InstallationSet up system on school roofLong-term solution; learning opportunity
Poster CampaignCreate awareness postersPeer education
Water PledgeStudents commit to conservationBehavioral change
CompetitionsEssay, drawing, model-makingEngagement

Classroom Activities

Activity 1: Water Diary
DayActivityWater Used (liters)
MorningBrushing teeth (tap running)15
MorningBrushing teeth (tap off)1
Shower (10 min)100
Shower (5 min)50
Flush (old toilet)15
Flush (dual-flush, low)3

Discussion: Compare totals; identify savings

Activity 2: Water Footprint Calculation
ItemWater RequiredCalculation
1 kg rice3,000 liters3,000 × __ kg = __
1 kg wheat1,500 liters1,500 × __ kg = __
1 kg sugar1,500 liters1,500 × __ kg = __
1 cup tea30 liters30 × __ cups = __
1 kg cotton (shirt)10,000 liters10,000 × __ kg = __
Activity 3: Clean Water Experiment
StepInstructions
Materials2-liter bottle, sand, gravel, charcoal, cloth, dirty water
Step 1Cut bottle; invert top into bottom
Step 2Layer: cloth, charcoal, sand, gravel (from bottom to top)
Step 3Pour dirty water through
Step 4Observe filtered water
DiscussionHow does this relate to groundwater recharge?
Activity 4: Save Water Challenge
ChallengeDurationTracking
5-minute shower1 weekTimer; record
Turn off tap while brushing1 weekSelf-monitoring
Report leaks at home1 weekList found
Reuse RO/reverse osmosis water for plants1 weekVolume collected
Bucket instead of hose for car washing1 weekCompare usage

📝 Sample Lesson Plan: "Water Conservation in Our Community"

Lesson ComponentDescription
TopicUnderstanding and addressing local water issues
ClassVII-VIII
Duration3 class periods + fieldwork
Learning ObjectivesStudents will: (1) Identify local water sources (2) Assess water quality/availability (3) Propose conservation measures
Day 1: InvestigationDiscuss local water sources; map them; identify issues
Day 2: FieldworkVisit local water body/well; observe; interview residents
Day 3: Analysis and ActionAnalyze findings; design awareness campaign; propose solutions
AssessmentProject report; presentation; campaign materials

📝 Chapter Summary: Key Points for PSTET Revision

🔑 Water Distribution

TypePercentage
Saline water97.5%
Freshwater2.5%
Usable freshwater0.3%

🔑 Water Cycle Processes

  1. Evaporation: Liquid → gas (solar energy)

  2. Condensation: Gas → liquid (cooling)

  3. Precipitation: Water falls (rain, snow)

  4. Collection: Runoff, infiltration

🔑 Ocean Relief Features

FeatureDepthCharacteristics
Continental Shelf0-200 mFishing, oil/gas
Continental Slope200-3,000 mSteep drop
Abyssal Plain3,000-6,000 mFlat deep
Trenches6,000-11,000 mDeepest parts

🔑 Ocean Movements

MovementCauseCharacteristics
WavesWindOscillatory
TidesMoon/Sun gravityPeriodic rise/fall
CurrentsWind, temperature, salinityContinuous flow

🔑 Water Uses

  • Drinking (essential)

  • Irrigation (70% global, 80-90% India)

  • Industry (19% global)

  • Transportation (inland waterways, oceans)

🔑 Water Pollution and Conservation

Pollution SourcesConservation Methods
Industrial wasteRainwater harvesting
Agricultural runoffDrip irrigation
Domestic sewageWater-efficient practices
Oil spillsRecycling and reuse

📝 Practice Questions for PSTET Preparation

Multiple Choice Questions

  1. What percentage of Earth's water is freshwater?
    a) 97.5%
    b) 2.5%
    c) 0.3%
    d) 30.1%

  2. Which process in the water cycle involves water changing from liquid to gas?
    a) Condensation
    b) Precipitation
    c) Evaporation
    d) Infiltration

  3. The deepest part of the ocean is:
    a) Continental shelf
    b) Abyssal plain
    c) Mariana Trench
    d) Mid-ocean ridge

  4. Spring tides occur during:
    a) First quarter moon
    b) Full moon and new moon
    c) Last quarter moon
    d) All moon phases

  5. Which ocean current warms the northwest coast of Europe?
    a) Labrador Current
    b) Canary Current
    c) Gulf Stream
    d) Benguela Current

  6. What percentage of freshwater in India is used for agriculture?
    a) 50-60%
    b) 70-75%
    c) 80-90%
    d) 95-98%

  7. Which of the following is NOT a method of water conservation?
    a) Rainwater harvesting
    b) Drip irrigation
    c) Flood irrigation
    d) Mulching

  8. The Coriolis effect causes ocean currents to deflect:
    a) Right in both hemispheres
    b) Left in both hemispheres
    c) Right in Northern Hemisphere, left in Southern Hemisphere
    d) Left in Northern Hemisphere, right in Southern Hemisphere

  9. Eutrophication in water bodies is caused by excess:
    a) Oxygen
    b) Nitrogen and phosphorus
    c) Carbon dioxide
    d) Salt

  10. The standard meridian of India (82°30'E) passes through:
    a) Delhi
    b) Mumbai
    c) Mirzapur
    d) Chennai

Short Answer Questions

  1. Explain why usable freshwater is scarce despite 71% of Earth being covered with water.

  2. Describe the four main processes of the water cycle with examples.

  3. Differentiate between spring tides and neap tides.

  4. What are the causes and effects of ocean currents?

  5. List any five methods of water conservation that can be implemented at home.

Long Answer Questions

  1. Explain the distribution of water on Earth with the help of a diagram. Why is water conservation necessary?

  2. Describe the features of the ocean floor with a labeled diagram.

  3. Discuss the causes and effects of water pollution. Suggest measures to control it.

  4. As a teacher, how would you create awareness about water conservation among students? Describe any three activities.

  5. Analyze the importance of monsoon for India's water resources. How does Punjab's agriculture depend on monsoon and groundwater?


✅ Chapter Completion Checklist

Before moving to Chapter 7, ensure you can:

  • Explain global water distribution with percentages

  • Draw and explain the water cycle

  • Label ocean floor features on a diagram

  • Differentiate between waves, tides, and currents

  • Name major warm and cold currents

  • List four major uses of water with examples

  • Identify five causes of water pollution

  • Describe five water conservation methods

  • Explain rainwater harvesting

  • Plan a water cycle model activity

  • Design a local water issues discussion


🔗 Online Resources for Further Learning

ResourceDescriptionLink/How to Find
NASA Water CycleInteractive water cycle resourcesgpm.nasa.gov/education
Central Ground Water BoardGroundwater data, Indiacgwb.gov.in
National Water MissionGovernment water conservationnwm.gov.in
UN WaterGlobal water issuesunwater.org
NCERT GeographyClass VI, VII, VIII resourcesncert.nic.in
Rainwater Harvesting ManualPractical guidecseindia.org

🎓 Prepared for PSTET Aspirants

This chapter provides comprehensive coverage of "Water" as per PSTET Paper II syllabus. Water is life—understand its distribution, movements, and conservation thoroughly. For Punjab-specific context, pay special attention to groundwater depletion and agricultural water use. Use the activities to make learning engaging and impactful for your future students!