Reflection and refraction: the same thing at the atomic level?

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Discussion Overview

The discussion revolves around the concepts of reflection and refraction at the atomic level, particularly in relation to the atmosphere and how light interacts with it. Participants explore the nature of color perception, scattering, and the differences between solid objects and gases in terms of light interaction.

Discussion Character

  • Debate/contested
  • Conceptual clarification
  • Exploratory

Main Points Raised

  • Some participants propose that the atmosphere is colorless, with blue light being scattered more due to its shorter wavelength, while others argue that this does not mean the atmosphere reflects light.
  • There is a contention regarding whether the atmosphere reflects light at all, with some asserting that it does not reflect light like solids do, while others suggest that atomic interactions can be seen as a form of reflection.
  • One participant mentions that Rayleigh scattering is a form of reflection between atoms, questioning the nature of light absorption and re-emission in this context.
  • Another participant points out that the speed of light between atoms is not well-defined for spacings smaller than the wavelength of light, complicating the discussion of light's behavior in the atmosphere.
  • There is a discussion about how objects like cups reflect light and how their perceived color changes with different light sources, paralleling the discussion about the atmosphere.
  • Some participants clarify that the atmosphere reflects about 30% of incoming light, referencing the concept of albedo, while others emphasize that this reflection is not like that of a mirror.
  • Reflection is noted to not be limited to specular reflection, with some participants agreeing that the term may not apply to atomic interactions in the same way it does for larger objects.

Areas of Agreement / Disagreement

Participants express multiple competing views regarding the nature of reflection and refraction at the atomic level, particularly in the context of the atmosphere. The discussion remains unresolved, with no consensus reached on the definitions and implications of these concepts.

Contextual Notes

Limitations include the dependence on definitions of reflection and refraction, as well as the complexity of light interactions at the atomic level, which are not fully resolved in the discussion.

AcesHigh
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I got cornered in a discussion on the internet... I am not sure if I am right or not (I thought I was when I started). If you guys here tell me I am wrong, I have no problem admitting if I am indeed wrong

person1 said:
The atmosphere is colourless, you are seeing blue because the length of the waves which is percepted as blue are scattered the most in the atmosphere, because blue has the shortest waves (easy to scatter)

It's all about perception, but the atmosphere is still colourless no matter in what way the light scatters.
It's like saying a glass pyramid is coloured blue just because you are standing in the blue light spectrum looking at the pyramid.
AcesHigh said:
But Person 1... there is no such thing as objects having color. Everything in the world is colorless and what you see is refracted light. Everything is atoms (which are mostly empty) with light waves reflecting at electrons. Depending on the distribution of the atoms, light will get scattered and reflected in different ways and wavelenghts, and what you see are those different wavelenghts of light. Same as with the atmosphere.

Person 2 said:
Refraction =/= reflection. The atmosphere is colorless because it does not reflect any light, regardless of refraction.

The point being, observational evidence falls below experimental in the hierarchy of evidence, and many times contradicts the latter. If I find a burnt matchstick on the ground next to a mound of ash, it does not mean the matchstick was used to light a fire there.

AcesHigh said:
at the atomic level, it´s the same thing.

Whenever light interacts with a medium, (reflection or refraction) the interaction is an electron from the medium absorbing the photon and re-emitting it. There's a very good book on this by Richard Feynman called QED: The Strange Theory of Light and Matter

Person 2 said:
And how does light absorption with no re-emission fit into your explanation? This will surely stimulate your nugget.
Regardless of the atomic interactions, what you stated is a totally moot point in this discussion that addresses nothing. All gases are colorless at STP and even under these alternate environments. Blue sky appears due to Rayleigh scattering while at the same instance a non-blue sky is visible under Mie scattering. That should be indicative of the fact that the atmosphere is colorless. Can't say the same about a solid object such as wood or cement that reflects a constant color of light no matter what angle it is observed from.
This is why observational evidence alone is not considered solid evidence in modern day scientific literature.
first... person 2 said "Refraction =/= reflection. The atmosphere is colorless because it does not reflect any light, regardless of refraction.".

Does atmosphere really does not reflect any light? It seems to me that at atomic level, Rayleigh Scattering is reflection of light between atoms. Due to different medium, the APPARENT velocity of light is different, but between the atoms, it´s still the same old constant C. What changes is the length of the path light travels to get across the medium.

Isn´t it?
 
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AcesHigh said:
Does atmosphere really does not reflect any light?
Not in the way solids can do that as coherent effect of the whole surface.
AcesHigh said:
Due to different medium, the APPARENT velocity of light is different, but between the atoms, it´s still the same old constant C.
"Speed of light in between atoms" is not well-defined for atom spacings smaller than the wavelength of light.

The atmosphere scatters blue light more than red light. If you look close to the sun at sunset or sunrise, you'll see red. Does that make the atmosphere red?
 
mfb said:
Not in the way solids can do that as coherent effect of the whole surface.

yes, I understand that... but that is when we think "as a whole". When we think about the atmosphere as atoms, aren´t the atoms in the atmosphere reflecting the light?
The atmosphere scatters blue light more than red light. If you look close to the sun at sunset or sunrise, you'll see red. Does that make the atmosphere red?

no. But does seeing a red cup makes that cup red? As far as I understand, that cup is not red, it´s just reflecting more red light. From some angles and IF there is red light component falling unto it. If you shine a blue light unto it, it´won´t be red anymore. Also near the borders of the cup, it will reflect light differently, in a more cohesive way, so that you see highlights or reflections in other colors (like blue or white)
 
The atmosphere as a whole reflects about 30% of the incoming light (from the sun).
See "albedo".
 
AcesHigh said:
yes, I understand that... but that is when we think "as a whole". When we think about the atmosphere as atoms, aren´t the atoms in the atmosphere reflecting the light?
Solids are more than a collection of individual atoms. You cannot explain properties of solids by looking at isolated atoms.
For the atmosphere, that works, sure.
nasu said:
The atmosphere as a whole reflects about 30% of the incoming light (from the sun).
See "albedo".
Well, "reflection" - it's not like a mirror. It scatters light, some of it leaves Earth without reaching the ground.
 
Reflection is not limited to specular reflection. A piece of paper reflects light but is not a mirror.

But I agree that reflection does not properly apply to atoms.
 

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