| MadSci Network: Earth Sciences |
Hello, Kurtz, and thanks for your question. To answer it, I’m just going to say a little about visible light for openers. Visible light is a small range of wavelengths in the electromagnetic spectrum – which goes from gamma rays and x-rays at the short wavelength end to radio and radar at the long end. Our eyes see only a tiny fraction, from about 400 nanometres (a nanometre is one billionth of a metre) to about 700nm, and humans have three separate types of receptors for colour vision called cones. The signals from these are processed in our brains to give us our perceptions of colour. We see red at the longer wavelength end – near 700nm and we see blue at the short end near 400nm. So, we are seeing long wavelengths in sunsets and sunrises, and short wavelengths when we look up at the blue sky. The reason for this is that the white light from the sun has to travel through the Earth’s atmosphere to reach our eyes. At noon, with the sun at its highest, the path through the atmosphere is shortest. At sunset, though, we are looking at the sun through a much longer path of atmosphere. The atmosphere is full of particles – water droplets, dust etc. These scatter light – but small particles scatter short wavelengths much more than they do long. This means that as the sun sinks in the sky, and the path containing these particles gets longer and longer, less blue light gets through as it is scattered more. This leaves the normally white light filtered to a red or orangey colour. Meanwhile, further west, where the sun is still high in the sky, people who look skywards see all this blue light which is being scattered by the atmosphere. Hence blue sky and red sunsets are due to the same effect – differential scattering of light of different wavelengths. To demonstrate this with household materials, here are a couple of suggestions: Milk is a suspension of fat particles in water, and appears bluey-white when diluted for the same light scattering reasons. If you can find a nice rectangular glass tank (fish tank) – and the longer the better, fill it with water and add a couple of teaspoons of milk. Not too much – just enough to make it go a little bit cloudy. If you have a good torch – a Maglite is good for this, shine it through the tank from one end to the other. You shoud be able to observe the light emerging at the far end being much redder after adding the milk than before, and equally the light scattered out of the sides of tank will be blueish. Another trick to show the effect with a Maglight is with “clear” gluesticks. They are not completely clear, and contain small opaque particles which scatter light. If you have several glue sticks try shining the light lengthways through one, two, three and so on by taping them end to end. You should see the end where the light emerges get redder and redder as you add more sticks. In the chemlab., you can make colloidal suspensions to show the effect even better. Your teacher can do this with sodium thiosulphate and sulphuric acid. Adding the acid to a solution of thiosulphate causes precipitation of very fine colloidal particles of sulphur which makes for very good light scattering. Have fun experimenting, and thanks for your question.
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