Heat in the Earth Flashcards

1
Q

Conduction

A

transfer of heat through a material by atomic or molecular interaction within the material
- rocks are intermediate between Ionic and Covalent bonded

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2
Q

Radiation

A

direct transfer of heat as electromagnetic radiation

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3
Q

Convection

A

Transfer of heat by the movement of the molecules themselves
Advection is a special case of convection

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4
Q

Conductive heat flow

A

Heat flows from hot things to cold things

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5
Q

temperature gradient

A

proportional to the rate at which heat flows

  • larger temp gradient = high heat flow
  • small temp gradient = low heat flow
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6
Q

ionic bonding

A
electrostatic bonds 
(Na_ and Cl- in salt NaCl)
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7
Q

covalent bonding

A

sharing electrons

- diamonds, each carbon atom is surrounded by 4 other and each shares an electron)

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8
Q

Earths system

A
  • earth is an open system that exchanges energy and mass with its surroundings
  • most heat from the sun is reflected back to the atmosphere
  • heat from the sun arriving at the earth is 2x10^17 W (average over the surface this is 4x10^2 W/m2)
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9
Q

Earths Heat

A
  • earths interior is hot from volcanoes that expel hot magma and ash
  • gets hotter the deeper you go underground
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10
Q

Chile mine Heat Gradient

A

San Jose Mine, Chile 2010

  • 700m
  • 33oC
  • higher than average geothermal gradient (average 30)
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11
Q

Inner Earth system

A
  • the earths system is all part of our planet and their interactions
  • the heat from the interior is 4.7x10^13 W (8x10^-2 W/m2)
  • heat from incoming solar radiation is 17300x10^13 W
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12
Q

Heat flow mechanisms

A
  • the outer electrons of metal atoms drift and are free to move
  • when metal is heater the electrons gain kinetic energy and transfer it throughout the metal
  • plastic and wood do not move like this and do not conduct heat as well
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13
Q

Radiation as heat transfer

A
  • when a substance is hot it glows
  • heat can be transferred through radiation
  • net transfer to heat from the hotter object t the cooler object
  • works best through a transparent solid (sunshine through glass window)
  • most minerals in the earth are dark in colour and opaque and therefore radiate heat slowly
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14
Q

Convection as heat transfer

A
  • refers to heat transferred by motion of material
  • a kettle boiling, smoke rising etc. the heated fluid expands, rises (less dense) and then cools and sinks (process continues with further heating
  • a continuous cycle is called a convection cell
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15
Q

Oceanic heat flow

A
  • heat flow is higher over young oceanic crust

- ocean crust forms by intrusion of basaltic magma from below

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16
Q

Heat Transfer

A
  • therefore, convection is the most efficient method of heat energy loss from the earth interior to the surface
  • there is large scale motion beneath the earths surface
17
Q

Summary

A
  • heat can be transmitted by; conduction, convection and radiation
  • heat within the earth mostly originated from decay of radioactive elements
  • young areas of crust have much higher heat flow than older areas