Can Visible Light Produce Heat When Absorbed?

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Discussion Overview

The discussion centers on whether visible light can produce heat when absorbed by materials, particularly focusing on the mechanisms involved in this process. Participants explore the implications of color on heat absorption and the role of visible light in heating materials, as well as the broader context of atmospheric heating.

Discussion Character

  • Exploratory
  • Debate/contested
  • Technical explanation

Main Points Raised

  • Some participants assert that dark materials absorb more thermal energy than lighter colored materials, suggesting that visible light contributes to heating.
  • Others argue that visible light photons do produce heat upon absorption, with mechanisms involving atomic and molecular motion.
  • One participant mentions exceptions, such as photovoltaic cells, where absorbed energy is used differently.
  • There is a discussion about the role of ozone in atmospheric heating, with conflicting views on whether it is primarily due to visible light absorption or heat from the ground.
  • Participants discuss the absorption of light by electrons and the subsequent conversion of energy into atomic motion, with some emphasizing the collective behavior of atoms in solids.
  • One participant challenges another's explanation of heat transfer from the ground to the atmosphere, suggesting a misunderstanding of the processes involved.
  • Mechanisms of atmospheric cooling through radiation transport in the IR and convection are also mentioned, but these discussions diverge from the original question about visible light.

Areas of Agreement / Disagreement

Participants express differing views on the role of visible light in producing heat, with some asserting it does while others question this. The discussion includes multiple competing perspectives on atmospheric heating, indicating that no consensus has been reached.

Contextual Notes

Some claims rely on specific definitions of heating and absorption, and there are unresolved questions regarding the mechanisms of energy transfer in both materials and the atmosphere.

WallyK
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"dark materials absorb more thermal energy than lighter colored materials"

Initially I thought this statement was very straight forward and obvious... then someone mentioned that visible light photons do not produce heat when absorbed and that IR was the only component that would be translated into heat. This seems to be very counter intuitive to me

Here's my question:

Say I had a flat, smooth layer of some material that happened to be colored black. Say this material is very absorptive of all visible light frequencies.

If I was able to expose this material to an energy source that only generated visible light (400-700nm) would this material rise in temperature?

If yes, what is the mechanism that converts the photons into heat?

If not, then why would color even matter since all absorption/reflection of the heat producing frequencies occur in IR (or UV)?


Thanks for any clarification you can provide
 
Last edited:
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then someone mentioned that visible light photons do not produce heat when absorbed
Usually, they do. There are some exceptions (like photovoltaic cells), where the energy is used in different ways.
If I was able to expose this material to an energy source that only generated visible light (400-700nm) would this material rise in temperature?
It would.
If yes, what is the mechanism that converts the photons into heat?
Absorption, leading to motion of atoms/molecules.
 
Whoever told you that visible light doesn't produce heat upon absorption is 100% WRONG.
 
Say I had a flat, smooth layer of some material that happened to be colored black. Say this material is very absorptive of all visible light frequencies

That's why it's black.
 
The primary mechanism for heating of the atmosphere is by ozone absorption in the visible.
 
Chestermiller said:
The primary mechanism for heating of the atmosphere is by ozone absorption in the visible.

Not true. The primary cause of atmospheric heating is due to the absorption of heat from the ground.

http://en.wikipedia.org/wiki/Troposphere#Temperature
 
mfb said:
Absorption, leading to motion of atoms/molecules.

mfb, thanks for your response. From my understanding, the visible light is absorbed by the electrons which drives them into a higher orbital state. Do you know of any references on which I can read up on how these electrons then convert their energy into atomic motion leading to heat.
 
WallyK said:
mfb, thanks for your response. From my understanding, the visible light is absorbed by the electrons which drives them into a higher orbital state. Do you know of any references on which I can read up on how these electrons then convert their energy into atomic motion leading to heat.

Actually much of the light is absorbed by the atoms/molecule as a whole and converted directly into thermal motion. Unless the light is exactly the right frequency, an electron will not absorb it and jump to a higher energy orbital.
 
Drakkith said:
Not true. The primary cause of atmospheric heating is due to the absorption of heat from the ground.

http://en.wikipedia.org/wiki/Troposphere#Temperature

Sorry. I meant to say "heating from solar radiation in the visible." Heat from the ground is absorbed by the atmosphere in the IR and re-radiated back into space so that the net heating rate of the Earth is zero (at steady state), assuming no anthropogenic perturbations.
 
  • #10
WallyK said:
mfb, thanks for your response. From my understanding, the visible light is absorbed by the electrons which drives them into a higher orbital state. Do you know of any references on which I can read up on how these electrons then convert their energy into atomic motion leading to heat.

Please note that, since we are talking about "material" (per your first post), this implies things such as solids. For the energy scale we are talking about, the property that we are dealing with are not "atomic orbitals", but rather a collective behavior of many, many atoms that have formed that solid. A isolated Cu atom has discrete energy levels, whereas the Cu wire that you are familiar with is a solid that has energy bands which are not found in individual Cu atoms.

So when you are dealing with "materials", the interaction of visible light with that material are governs by the collective behavior, not by individual atoms in that material. The light could easily be absorbed by the lattice ions, causing an increase in lattice ions vibrations.

So moral of the story here is that, if you learn that atoms in solids to not behave the same the same way as when they are individually isolated, then you have learned something.

Zz.
 
  • #11
Chestermiller said:
Sorry. I meant to say "heating from solar radiation in the visible." Heat from the ground is absorbed by the atmosphere in the IR and re-radiated back into space so that the net heating rate of the Earth is zero (at steady state), assuming no anthropogenic perturbations.

Not sure what you mean here. The ground transfers heat to the atmosphere mostly through physical contact. At the top of the atmosphere the heat can radiate away as IR, cooling the planet. Is that what you were saying?
 
  • #12
Drakkith said:
Not sure what you mean here. The ground transfers heat to the atmosphere mostly through physical contact. At the top of the atmosphere the heat can radiate away as IR, cooling the planet. Is that what you were saying?

No. The way you describe it is not how it works. See the following paper:

Owens, A. J., Hales, C. H., Filkin, D. L., Miller, C. Steed, J. M., and Jesson, J. P., A Coupled One-Dimensional Radiative-Convective, Chemistry_Transport Model of the Atmosphere, 1. Model Structure and Steady State Perturbation Calculations, Journal of Geophysical Research, Vol. 90, No. D1, Pages 2283-2311, February, 20, 1985.
 
  • #13
Chestermiller said:
Sorry. I meant to say "heating from solar radiation in the visible." Heat from the ground is absorbed by the atmosphere in the IR and re-radiated back into space so that the net heating rate of the Earth is zero (at steady state), assuming no anthropogenic perturbations.
Your posts are confusing to me, so let's just look at the numbers:

LWRadiationBudget.gif
 
  • #14
Chestermiller said:
No. The way you describe it is not how it works. See the following paper:

Owens, A. J., Hales, C. H., Filkin, D. L., Miller, C. Steed, J. M., and Jesson, J. P., A Coupled One-Dimensional Radiative-Convective, Chemistry_Transport Model of the Atmosphere, 1. Model Structure and Steady State Perturbation Calculations, Journal of Geophysical Research, Vol. 90, No. D1, Pages 2283-2311, February, 20, 1985.

Can't find a link that I can use. Mind explaining the process?
 
  • #15
Drakkith said:
Can't find a link that I can use. Mind explaining the process?
Mechanistically, cooling of the atmosphere occurs by radiation transport in the IR. Part of the IR flux from the surface is absorbed by greenhouse gases in the atmosphere, as described by Beer's law. The absorption occurs primarily in band structure of the gases. In addition, each parcel of air, based on its temperature, emits radiation to the surrounding parcels. This radiation is also absorbed by the surrounding parcels, as described by Beer's law. So there is a constant process of radiation and reabsorption. In the troposphere, thermal energy is also transferred by convection and water condensation processes. There is also radiation exchange with clouds in the troposphere. But, in the stratosphere, the primary cooling mechanism is radiation transport.
 
  • #16
We need to get back on topic. The OP's question is much simpler than this. You guys are now adding factors that just create confusion.

Zz.
 

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