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CBSE · Class 7 · 🔬 Science · Chapter 7

Heat Transfer in Nature

ConductionConvectionRadiationGood and Poor Conductors of HeatSea and Land BreezeWater Cycle

Chapter 7, 'Heat Transfer in Nature', introduces students to the fundamental ways heat moves from one place to another: conduction, convection, and radiation. It explains why some materials are good conductors while others are insulators, and how these principles apply to everyday phenomena like cooking and coastal breezes. The chapter also delves into the water cycle, infiltration, and the formation of groundwater and aquifers, highlighting the continuous movement and storage of water on Earth. Understanding these concepts is crucial for comprehending natural processes and their impact on our environment.

Conduction of Heat

Heat conduction in a metal strip
Heat conduction in a metal strip

Heat transfer ka ek mode jisme heat energy particles ke direct contact se transfer hoti hai, without actual movement of particles. Ye mainly solids mein hota hai.

  • Mechanism:
  • Hotter end ke particles vibrate karte hain aur apni energy adjacent cooler particles ko transfer karte hain.
  • Ye process tab tak chalta rehta hai jab tak poore object mein thermal equilibrium achieve na ho jaye.
  • Particles apni mean position se move nahi karte, sirf vibrate karte hain.
  • Conductors:
  • Materials jo heat ko easily pass hone dete hain. Example: metals (iron, copper, aluminium).
  • Cooking utensils metals ke bane hote hain kyunki wo heat ke good conductors hote hain, jisse food quickly cook hota hai.
  • Insulators (Poor Conductors):
  • Materials jo heat ko easily pass nahi hone dete. Example: wood, plastic, glass, air, clay, porcelain.
  • Insulators ka use heat loss ko prevent karne ke liye kiya jata hai (jaise hot drinks ke cups, house walls).

Conduction ka Daily Life mein Application:

  • Cooking Utensils: Metal ke hote hain taaki heat food tak efficiently pahunche.
  • Handles of Utensils: Plastic ya wood ke hote hain taaki haath na jale, kyunki ye insulators hain.
  • Winter Clothes: Woolen clothes air ko trap karte hain, aur trapped air ek insulator ki tarah act karti hai, jo body heat ko bahar jane se rokti hai.
  • Houses: Double-glazed windows mein air ki layer hoti hai, jo heat transfer ko reduce karti hai.

[IMAGE: heat_conduction_in_a_metal_strip_fig71] mein dekho kaise heat metal strip mein travel karti hai aur wax pins ko melt karti hai.

📖Definition

Conduction: Heat transfer ka process jisme heat hotter part se colder part mein direct contact ke through transfer hoti hai, without actual movement of particles.

Important

Solids mein heat transfer ka primary mode conduction hai.

Convection in Liquids and Gases

Convection in water
Convection in water
Hot air rising up
Hot air rising up

Convection heat transfer ka wo mode hai jisme heat actual particle movement ke through transfer hoti hai. Ye mainly liquids aur gases mein hota hai.

  • Mechanism:
  • Jab liquid ya gas ko heat kiya jata hai, toh heated particles less dense ho jaate hain aur upar uthte hain.
  • Cooler, denser particles unki jagah lene ke liye neeche aate hain.
  • Ye continuous movement ek convection current banata hai, jo heat ko distribute karta hai.
  • Examples:
  • Boiling Water: Jab pani garam hota hai, toh bottom ka pani garam hokar upar uthta hai aur thanda pani neeche aata hai. [IMAGE: convection_in_water_fig75b]
  • Room Heater: Room heater room ke bottom mein rakha jata hai. Garam hawa upar uthti hai aur thandi hawa neeche aati hai, jisse poora room garam hota hai.
  • Air Conditioner: AC room ke upper part mein lagaya jata hai. Thandi hawa dense hoti hai, neeche aati hai aur garam hawa upar uthti hai, jisse room cool hota hai.
  • Wind Formation: Land aur Sea Breeze convection ke hi examples hain (next topic mein detail mein padhenge).

Convection Current Formation:

  1. Heating: Fluid (liquid or gas) ka bottom layer heat absorb karta hai.
  2. Expansion & Density Change: Heat hone par fluid expand karta hai aur uski density kam ho jaati hai.
  3. Rising: Less dense, warmer fluid upar uthta hai.
  4. Cooling & Sinking: Upar pahunch kar fluid cool hota hai, contract karta hai aur denser ho jaata hai.
  5. Descending: Denser, cooler fluid neeche aata hai, jahan wo phir se heat hota hai.
  6. Cycle: Ye cycle repeat hota rehta hai, jisse heat transfer hoti hai.

[IMAGE: convection_hot_air_rises_fig73b] mein dekho kaise candle flame se garam hawa upar uthti hai aur paper cup ko move karti hai.

📖Definition

Convection: Heat transfer ka process jisme heat actual movement of particles (liquids aur gases mein) ke through transfer hoti hai.

Remember

Convection currents fluids (liquids aur gases) mein hi form hote hain kyunki unke particles freely move kar sakte hain.

Land Breeze and Sea Breeze

Sea breeze during the day
Sea breeze during the day
Land breeze at night
Land breeze at night
Temperature measurement of soil and water
Temperature measurement of soil and water

Land aur Sea Breeze convection currents ke natural examples hain jo coastal areas mein observe kiye jaate hain. Ye land aur water ki different heating aur cooling rates ke karan hote hain.

Sea Breeze (Din ke Samay):

  • Din mein: Land water se zyada jaldi garam hota hai.
  • Land ke upar ki air garam hokar less dense ho jaati hai aur upar uthti hai.
  • Isse land par low-pressure area create hota hai.
  • Sea ka pani land se slow garam hota hai, isliye sea ke upar ki air cooler aur denser hoti hai.
  • Ye cooler air sea se land ki taraf move karti hai low-pressure area ko fill karne ke liye. Is movement ko Sea Breeze kehte hain.
  • [IMAGE: sea_breeze_during_the_day_fig77a] mein dekho.

Land Breeze (Raat ke Samay):

  • Raat mein: Land water se zyada jaldi thanda hota hai.
  • Land ke upar ki air cooler aur denser ho jaati hai.
  • Sea ka pani land se slow thanda hota hai, isliye sea ke upar ki air warmer aur less dense hoti hai aur upar uthti hai.
  • Isse sea par low-pressure area create hota hai.
  • Cooler air land se sea ki taraf move karti hai low-pressure area ko fill karne ke liye. Is movement ko Land Breeze kehte hain.
  • [IMAGE: land_breeze_fig77b] mein dekho.

Importance:

  • Coastal areas mein temperature ko moderate rakhte hain.
  • Din mein sea breeze coastal areas ko cool rakhti hai.
  • Raat mein land breeze coastal areas se heat ko sea ki taraf le jaati hai.

Activity 7.4 (Temperature Measurement of Soil and Water): Ye activity demonstrate karti hai ki soil (land) water se zyada jaldi garam aur thanda hota hai. Isliye land aur sea breeze form hote hain.

📖Definition

Sea Breeze: Din ke samay cooler air ka sea se land ki taraf movement.

📖Definition

Land Breeze: Raat ke samay cooler air ka land se sea ki taraf movement.

💡Tip

Land aur water ki specific heat capacities mein difference ke karan ye phenomena hote hain. Land ki specific heat capacity kam hoti hai, isliye wo jaldi garam aur thanda hota hai.

Radiation as a Mode of Heat Transfer

Modes of Heat Transfer
Modes of Heat Transfer

Radiation heat transfer ka wo mode hai jisme heat energy electromagnetic waves ke form mein transfer hoti hai. Is process ko koi medium nahi chahiye.

  • Mechanism:
  • Har garam object heat radiate karta hai.
  • Ye heat waves vacuum (jaise space) se bhi travel kar sakti hain.
  • Jab ye waves kisi object par padti hain, toh object unhe absorb karta hai aur garam ho jata hai.
  • Key Characteristics:
  • No Medium Required: Conduction aur convection ke opposite, radiation ko heat transfer ke liye kisi solid, liquid ya gas ki zaroorat nahi hoti.
  • Speed of Light: Radiant heat light ki speed se travel karti hai.
  • All Objects Radiate: Har object, chahe wo kitna bhi thanda ho, heat radiate karta hai. Bas hotter objects zyada radiate karte hain.
  • Examples:
  • Sunlight: Sun se Earth tak heat radiation ke through pahunchti hai. Space mein koi medium nahi hai, phir bhi heat pahunchti hai.
  • Bonfire/Heater: Jab hum bonfire ya room heater ke paas khade hote hain, toh humein heat radiation ke through feel hoti hai.
  • Hot Utensil: Ek garam utensil se nikalne wali heat ko hum bina touch kiye bhi feel kar sakte hain, ye radiation hai.

Good and Bad Absorbers/Emitters of Radiation:

  • Dark, dull surfaces heat radiation ke good absorbers aur good emitters hote hain.
  • Light, shiny surfaces heat radiation ke poor absorbers aur poor emitters (good reflectors) hote hain.

Daily Life Applications:

  • Winter Clothes: Dark-coloured clothes winter mein prefer kiye jaate hain kyunki wo sunlight ko zyada absorb karte hain aur humein garam rakhte hain.
  • Summer Clothes: Light-coloured clothes summer mein prefer kiye jaate hain kyunki wo sunlight ko reflect karte hain aur humein cool rakhte hain.
  • Cooking Utensils ka Bottom: Cooking utensils ka bottom black kiya jata hai taaki wo flame se zyada heat absorb kar sakein.
  • Thermos Flask: Shiny inner surface radiation se heat loss ko minimize karta hai.

[IMAGE: modes_of_heat_transfer_fig78] mein teeno modes of heat transfer ek saath dikhaye gaye hain.

📖Definition

Radiation: Heat transfer ka process jisme heat electromagnetic waves ke form mein transfer hoti hai, without requiring any medium.

Important

Sun se Earth tak heat sirf radiation ke through pahunchti hai.

The Water Cycle and its Processes

Water cycle
Water cycle

Water Cycle (ya Hydrologic Cycle) Earth par water ka continuous movement hai. Ye Sun ki heat energy se driven hota hai aur isme kai processes involve hote hain.

  • Key Processes:
  1. Evaporation:
  • Sun ki heat energy ke karan water bodies (oceans, rivers, lakes) se water liquid state se gaseous state (water vapour) mein convert hota hai.
  • Plants se bhi water vapour air mein release hota hai, jise Transpiration kehte hain.
  • Ye process water vapour ko atmosphere mein le jaata hai.
  1. Condensation:
  • Atmosphere mein upar uthne par water vapour thanda hota hai.
  • Cooling ke karan water vapour liquid water droplets ya ice crystals mein convert ho jaata hai.
  • Ye tiny droplets clouds form karte hain.
  1. Precipitation:
  • Jab clouds mein water droplets ya ice crystals bade aur heavy ho jaate hain, toh wo gravity ke karan Earth ki surface par girte hain.
  • Precipitation ke forms hain: rain, snow, hail, sleet.
  1. Collection:
  • Precipitation ka kuch part oceans, rivers, lakes mein collect ho jaata hai.
  • Kuch part soil mein seep ho jaata hai (infiltration) aur groundwater banata hai.
  • Kuch part surface runoff ke through rivers aur streams mein flow karta hai.

Water Cycle ka Significance:

  • Water Distribution: Earth par water ko redistribute karta hai.
  • Water Purification: Natural process se water ko purify karta hai.
  • Climate Regulation: Heat energy ko absorb aur release karke climate ko regulate karta hai.
  • Life Support: Plants aur animals ke liye fresh water provide karta hai.

[IMAGE: water_cycle_fig79] mein water cycle ke different stages ko dekho.

📖Definition

Water Cycle: Earth par water ka continuous movement, jisme evaporation, condensation aur precipitation jaise processes involve hote hain.

Remember

Water cycle Sun ki heat energy se driven hota hai.

Infiltration and Groundwater Storage

Water flow through different soils
Water flow through different soils
Aquifer and seepage of water
Aquifer and seepage of water

Precipitation ke baad, water ka ek significant portion Earth ki surface ke neeche chala jaata hai. Ye process aur iske storage ko samajhna important hai.

  • Infiltration:
  • Ye wo process hai jisme surface water soil aur rocks ke through seep karta hai aur neeche ki taraf move karta hai.
  • Infiltration rate soil type, vegetation cover, aur land slope par depend karta hai.
  • Soil Types aur Infiltration:
  • Gravely soil mein bade pores hote hain, isliye water fast seep karta hai.
  • Sandy soil mein moderate pores hote hain, isliye water moderately seep karta hai.
  • Clayey soil mein bahut fine pores hote hain, isliye water very slow seep karta hai ya surface par hi ruk jaata hai.
  • [IMAGE: water_flow_through_different_soils_fig710] mein different soil types mein water flow dekho.
  • Groundwater:
  • Infiltration ke through jo water surface ke neeche jaata hai, wo soil particles ke beech ke pore spaces aur rocks ki openings mein store ho jaata hai. Is stored water ko groundwater kehte hain.
  • Groundwater fresh water ka ek important source hai.
  • Aquifers:
  • Underground layers of sediments (jaise sand, gravel) aur rocks jo water ko store aur transmit kar sakte hain, unhe aquifers kehte hain.
  • Aquifers water ko store karne ke liye porous aur permeable hone chahiye.
  • Wells aur borewells aquifers se groundwater nikalne ke liye use kiye jaate hain.
  • Water table groundwater ki upper surface hoti hai.
  • [IMAGE: aquifer_and_seepage_of_water_fig712] mein aquifer aur water table ko dekho.

Importance of Groundwater:

  • Drinking Water: Kai areas mein drinking water ka primary source.
  • Agriculture: Irrigation ke liye use hota hai.
  • Ecosystem Support: Rivers, lakes aur wetlands ko sustain karta hai.

Groundwater Depletion:

  • Over-pumping for irrigation, industrial use, aur domestic supply ke karan groundwater levels kam ho rahe hain.
  • Isse water scarcity aur land subsidence jaise problems ho sakte hain.
  • Rainwater harvesting aur sustainable water management practices groundwater ko recharge karne ke liye essential hain.
📖Definition

Infiltration: Surface water ka soil aur rocks ke through seep hokar neeche jaana.

📖Definition

Groundwater: Water jo infiltration ke baad soil aur rocks ke pore spaces mein store hota hai.

📖Definition

Aquifers: Underground layers of permeable sediments aur rocks jo groundwater store aur transmit karte hain.

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