Heat in the Earth Flashcards
Conduction
transfer of heat through a material by atomic or molecular interaction within the material
- rocks are intermediate between Ionic and Covalent bonded
Radiation
direct transfer of heat as electromagnetic radiation
Convection
Transfer of heat by the movement of the molecules themselves
Advection is a special case of convection
Conductive heat flow
Heat flows from hot things to cold things
temperature gradient
proportional to the rate at which heat flows
- larger temp gradient = high heat flow
- small temp gradient = low heat flow
ionic bonding
electrostatic bonds (Na_ and Cl- in salt NaCl)
covalent bonding
sharing electrons
- diamonds, each carbon atom is surrounded by 4 other and each shares an electron)
Earths system
- 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)
Earths Heat
- earths interior is hot from volcanoes that expel hot magma and ash
- gets hotter the deeper you go underground
Chile mine Heat Gradient
San Jose Mine, Chile 2010
- 700m
- 33oC
- higher than average geothermal gradient (average 30)
Inner Earth system
- 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
Heat flow mechanisms
- 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
Radiation as heat transfer
- 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
Convection as heat transfer
- 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
Oceanic heat flow
- heat flow is higher over young oceanic crust
- ocean crust forms by intrusion of basaltic magma from below