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| You will need these materials. |
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| Fill one lid with water and put a few drops of food colouring in the centre. |
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| Fill the second the lid with water and place a Smartie in the centre. What happens this time? |
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Try this: Sweet solution
You will need
- Jar lids
- Food colouring
- Smarties
- Water
What to do
- Fill a jar lid with water.
- Wait until the surface is perfectly flat, without any waves or ripples.
- Place a few drops of food colouring in the centre of the lid. Observe for a few minutes. What do you predict will happen?
- Fill another jar lid with water and allow it to settle.
- Place a Smartie in the middle of the lid. Observe for a few minutes. What do you predict will happen?
What’s happening?
When you drop the food colouring into the water, it spreads out a little but stays as one blob of colour in the middle of the dish.
When you drop the Smartie into the water, something different happens. At first the water around the Smartie becomes coloured. Over time, the coloured water spreads out to the edges of the lid, creating a ring of colour, while the water around the Smartie is colourless.
Smarties have a sugar coating, and the top layer of this sugar coating is coloured. When the Smartie is placed in the water the sugar slowly dissolves, creating a layer of sugar solution around the Smartie.
Solutions are denser than pure water, so the water around the Smartie is now denser than the rest of the water in the lid. When there is a difference in densities of fluids, the denser fluid flows towards the less dense fluid. The coloured water around the Smartie flows away from it.
When all the colour has dissolved off the Smartie, the uncoloured sugar around the Smartie begins to dissolve. This creates a clear sugar solution around the Smartie which keeps pushing the coloured solution further away from the Smartie, creating the ring that we observe.
Applications
An example of this phenomenon is in the oceans. In the polar regions, surface water freezes, which creates a layer of water under the ice that is saltier and thus denser than normal sea water.
The denser, saltier water sinks to the bottom and more surface water flows in to fill the gap under the ice. Some of this water freezes, again creating denser, saltier water which sinks.
This process creates a huge volume of descending water. As it sinks to the bottom of the ocean, it pushes the water already there out, eventually pushing it towards the equator. When it gets closer to the equator it warms up and rises and begins flowing back towards the poles.
This current is known as the thermohaline circulation and is involved in a number of the Earth’s ocean and climate processes.
By Patrick Mahony
More information
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