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![]() I was thinking about the greenhouse effect, and this question occured to me: in the space around me, what's more common, atoms or photons? -- Sleepalot aa #1385 |
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In message , Sleepalot
writes I was thinking about the greenhouse effect, and this question occured to me: in the space around me, what's more common, atoms or photons? In the universe as a whole the photon to baryon ratio is 10^9. So the question that now needs to be answered is by how much is the baryon density (and photon density) enhanced in the space around you, and what is the average number of baryons per atom in that region. The answer to this depends on how big a space you're thinking of. -- Stewart Robert Hinsley |
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Stewart Robert Hinsley wrote:
In message , Sleepalot writes I was thinking about the greenhouse effect, and this question occured to me: in the space around me, what's more common, atoms or photons? In the universe as a whole the photon to baryon ratio is 10^9. Lol. Ok, I've looked up "baryon" - it's neutrons and protons, but not electrons, yes? Is the universe still amost entirely hydrogen? So the question that now needs to be answered is by how much is the baryon density (and photon density) enhanced in the space around you, and what is the average number of baryons per atom in that region. The answer to this depends on how big a space you're thinking of. I did have a further think, bearing in mind this is a near-the-Earth-surface situation. So, around here 1 litre of air contains about 1 Avogadro number of atoms. For photons, I'm working from my understanding of cathode ray tubes: an electron hits an atom of phosphor, causing the emmision of a photon. So an amp of cathode current (way too high) would be a coulomb of electons per second giving an equal number of photons. So (say) 10mA would be 10^16 photons per second in 10^23 atoms .....no that's wrong because those photons wouldn't hang around that long. Does this make sense? Am I on the right track? -- Sleepalot aa #1385 |
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In message , Sleepalot
writes Stewart Robert Hinsley wrote: In message , Sleepalot writes I was thinking about the greenhouse effect, and this question occured to me: in the space around me, what's more common, atoms or photons? In the universe as a whole the photon to baryon ratio is 10^9. Lol. Ok, I've looked up "baryon" - it's neutrons and protons, but not electrons, yes? Is the universe still amost entirely hydrogen? Wikipedia says 75%. (I wouldn't be surprised if it gives other numbers elsewhere.) So the question that now needs to be answered is by how much is the baryon density (and photon density) enhanced in the space around you, and what is the average number of baryons per atom in that region. The answer to this depends on how big a space you're thinking of. I did have a further think, bearing in mind this is a near-the-Earth-surface situation. So, around here 1 litre of air contains about 1 Avogadro number of atoms. Fide Wikipedia density at sea level is 1.2g/L. A mole of atmosphere has a mass of 28.97g. Hence a litre contains roughly 1/24th of a mole of molecules, or 1/12th of a mole of atoms. For photons, I'm working from my understanding of cathode ray tubes: an electron hits an atom of phosphor, causing the emmision of a photon. So an amp of cathode current (way too high) would be a coulomb of electons per second giving an equal number of photons. You'd want to take the efficiency of the CRT into account. I don't know how efficient they are, but LCD displays require considerably less power, so I infer that CRTs are not particularly efficient. It might be more convenient to work from the energy of the photons (E=hv) and the luminosity of the display. So (say) 10mA would be 10^16 photons per second in 10^23 atoms .....no that's wrong because those photons wouldn't hang around that long. There's all sorts of other photons zipping around - the cosmic microwave background, radio waves from all sorts of artificial sources and heat from all surfaces, as well as visible light. I would think that you can neglect X-ray and gamma photons, but I'm not sure that you can neglect the longer wavelength parts of the spectra. You're right that if you're talking about the cubic meter in front of a CRT you have to divide by 3x10^8 (plus some geometrical correction factor). Does this make sense? Am I on the right track? You could start from the solar constant. From this you can get an estimate of the downward flux of photons from the sun. Let a be the albedo of the Earth's surface. Let N be the downward flux. The downward and upward energy fluxes must balance. Ignoring the greenhouse effect, and the internal heat generation of the earth, the total flux of photons is [(1+a) + x(1-a)]N, where x is the ratio of the energy of incoming light and outgoing heat photons (finger in the air, x is about 10, giving [1+a+x-ax]N = [1+x-a(x-1)]N. That comes out at about 8N. A mobile phone generates less that 1/1000th of the solar constant. But the energy of a photon is about 1/500000th of that of a visible light photon. So when your mobile phone is switched the photon density in your vicinity due to the mobile phone far exceeds that due to visible light. To get an accurate value for the photon density you have to integrate across the spectrum, for all sources. AM radio photons are another 1000 times less energetic that mobile phone photons, so it requires very little power density from this for the photon density to be significant. -- Stewart Robert Hinsley |
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Stewart Robert Hinsley wrote:
[snip] Thanks for the reply. It's going to take me a while to process all that. -- Sleepalot aa #1385 |
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On Thu, 17 Jul 2008 13:17:42 +0100, Sleepalot wrote:
I was thinking about the greenhouse effect, and this question occured to me: in the space around me, what's more common, atoms or photons? Answer: atoms. All we need here are rough numbers - an order of magnitude or two is close enough. The space around you is a box roughly 2m x 1m x1, =2m3. As has been stated 1 mole (6e23) of air weighs about 30g, and we know that 1m3 of air weighs about 1000g, so the space around you contains ~ 60 moles of air, or 6e23 * 60 approx 4e25 molecules. My astro camera (to keep it on topic) has a sensitive area of about 6mm x 6mm or 4e-6 m2. It has a well-depth of about 40,000 photons and a QE of about 0.5 and contains 1million pixels, so each pixel has an area of 4e-6 / 1e6 ~ 4e-12m2. During daytime, I'd guess the sensor gets saturated in about 1mSec So the photon flux is 4e4 photons per pixel in 1e-3 sec, or 4e7 photons per second, but double this for the 50% quantum efficiency gives us 8e7 (call it 1e8 photons per pixel per second.) Now multiply this by the number of pixels per square metre (1/4e-12) gives us a flux of 2.5e19 photons per sq. metre per second. Assume all the photons come from above (it keeps the maths simple, but the direction doesn't matter), then the number of photons in your 2m high box is the flux multiplied by the time they take to travel 2metres - which is 2 / 3e8 = 7e-9 seconds. Multiply this by the flux gives a result of 7e-9 * 2.5e19 is roughly 2e11 photons in your "box" at any one time. Let's double that to allow for all the non-visible photons and double it again for the hell of it. The number of photons is still a long way short of the number of molecules. At night it's even less. -- .. Pete Lynch I have learned from my mistakes and .. Marlow ... I am sure I can repeat them exactly .. www.pete-lynch.com --- Peter Cooke. |
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Peter Lynch wrote:
On Thu, 17 Jul 2008 13:17:42 +0100, Sleepalot wrote: I was thinking about the greenhouse effect, and this question occured to me: in the space around me, what's more common, atoms or photons? Answer: atoms. All we need here are rough numbers - an order of magnitude or two is close enough. The space around you is a box roughly 2m x 1m x1, =2m3. As has been stated 1 mole (6e23) of air weighs about 30g, and we know that 1m3 of air weighs about 1000g, so the space around you contains ~ 60 moles of air, or 6e23 * 60 approx 4e25 molecules. My astro camera (to keep it on topic) has a sensitive area of about 6mm x 6mm or 4e-6 m2. It has a well-depth of about 40,000 photons and a QE of about 0.5 and contains 1million pixels, so each pixel has an area of 4e-6 / 1e6 ~ 4e-12m2. During daytime, I'd guess the sensor gets saturated in about 1mSec So the photon flux is 4e4 photons per pixel in 1e-3 sec, or 4e7 photons per second, but double this for the 50% quantum efficiency gives us 8e7 (call it 1e8 photons per pixel per second.) Now multiply this by the number of pixels per square metre (1/4e-12) gives us a flux of 2.5e19 photons per sq. metre per second. Assume all the photons come from above (it keeps the maths simple, but the direction doesn't matter), then the number of photons in your 2m high box is the flux multiplied by the time they take to travel 2metres - which is 2 / 3e8 = 7e-9 seconds. Multiply this by the flux gives a result of 7e-9 * 2.5e19 is roughly 2e11 photons in your "box" at any one time. Let's double that to allow for all the non-visible photons and double it again for the hell of it. The number of photons is still a long way short of the number of molecules. At night it's even less. Hello Peter, thanks for the reply - which I'm pleased to say I got the jist of. I liked your method - using your camera as a photon counter. So, we've got e11 photons in e25 molecules, and that's 1 photon in e14 molecules - it's amazingly low, but there'll be another one along in an instant. Right, so if I head off towards the Sun for about 100 miles I'm going to run out of molecules in my 2m3 while retaining a broadly comparable photon density, yes? -- Sleepalot aa #1385 |
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Stewart Robert Hinsley wrote:
You could start from the solar constant. From this you can get an estimate of the downward flux of photons from the sun. Let a be the albedo of the Earth's surface. Let N be the downward flux. The downward and upward energy fluxes must balance. Ignoring the greenhouse effect, and the internal heat generation of the earth, the total flux of photons is [(1+a) + x(1-a)]N, where x is the ratio of the energy of incoming light and outgoing heat photons (finger in the air, x is about 10, giving [1+a+x-ax]N = [1+x-a(x-1)]N. That comes out at about 8N. Sorry Stewart, I'm out of my depth here. You seem to be saying that there are (perhaps) 8 times as many photons going out (with lower energies) as coming in. Have I got that right? -- Sleepalot aa #1385 |
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In message , Sleepalot
writes Stewart Robert Hinsley wrote: You could start from the solar constant. From this you can get an estimate of the downward flux of photons from the sun. Let a be the albedo of the Earth's surface. Let N be the downward flux. The downward and upward energy fluxes must balance. Ignoring the greenhouse effect, and the internal heat generation of the earth, the total flux of photons is [(1+a) + x(1-a)]N, where x is the ratio of the energy of incoming light and outgoing heat photons (finger in the air, x is about 10, giving [1+a+x-ax]N = [1+x-a(x-1)]N. That comes out at about 8N. Sorry Stewart, I'm out of my depth here. You seem to be saying that there are (perhaps) 8 times as many photons going out (with lower energies) as coming in. Have I got that right? Yes, with caveats. The energy reaching the surface of the Earth from the Sun is dominated by visible and near infrared wavelengths, because 1) that's where the peak of the solar energy production is 2) radiation at many other wavelengths is absorbed by the atmosphere. The same amount of energy, plus a small contribution from the internal heat production of the Earth, must leave the surface of the Earth. Some is just reflected. Some heats the surface. Some of this heat is carried away by convection (and subsequently radiated by the atmosphere), and some is radiated, at considerably longer wavelengths and lower energies, with a consequent increase in the number of photons. Because of absorption of infra-red radiation by the atmosphere there's also an incoming flux of infra-red photons reradiated by the atmosphere. This why I specified ignoring the greenhouse effect. The other caveat is while the solar energy flux is dominated by visible and near-infrared wavelengths this doesn't mean that the solar photon flux is. AM radio wavelengths are a trillion times longer than visible light wavelengths, so the solar energy flux has to be very small for the photon flux at those wavelengths to be negligible. A bit of googling suggests that it is indeed negligible. -- Stewart Robert Hinsley |
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