How much salt is there in sea water? What concentration do you need before crystals start forming? What will those crystals look like? I am sure those are the kind of questions that keep you awake at night!
Of course this can easily assessed experimentally. On a visit to the University of Bergen’s Centre for Science Education just now, I was shown the result of such an experiment: A litre of water was mixed with 35 grams of salt to simulate sea water with its typical salinity. Below, you see what the beaker looked like after sitting out for three months.
You can see that salt crystals are forming at the walls of the beaker, but that their structure depends on depth below the initial water level (see the 1000 ml mark on the beaker).
When there is still a lot of water in the beaker, crystals look like ornate flowers. Then, the less water is left in the beaker, the more square the crystals become. And at the bottom of the beaker, you see the typical salt crystals you would expect.
Actually, even though they look like the kind of salt crystals I would expect, apparently someone who knows about crystallography commented that there must be other stuff in there than just cooking salt since the crystals don’t look the way they should. I need to read up on this! :-)
Anyway, this is an experiment that I want to do myself, so maybe in three months time there will be more pictures of this!
Thanks for a very nice lunch, Olaug, Frede, Andreas, Morven and Elin! Looking forward to working with you a lot more in the future! :-)
P.S.: with this blog post I am testing to blog pretty much “real time” from my mobile phone, so if you notice anything odd, please let me know!
Yes! You should add marshmallows to prevent heat transfer both by evaporation and conduction.
Actually, no matter what temperature you like your chocolate best at – you should always add marshmallows! :-)
For those of you who want to read more about marshmallows and ocean mixing, check out a very nice post here. For those others getting worried that I’ll only talk about tea until the end of time – nope! Tea week is now officially over and we’ll be back with “real oceanography content” pretty soon!
After the frustrations of taking pictures of steam in my last post, I decided that I could use the very same cute mug to show other stuff, too. I know it has been done over and over again, but we have new students every year, don’t we, so someone has to keep telling the old stories, right?
So. When should you pour the milk into your tea? Right away or a little later?
The answer, as you know, is “it depends”.
Do you want your tea as hot as possible? Then put the milk in right away and it won’t cool the tea down as much. Want the milk to cool down the tea as much as possible? Then wait for as long as you can before pouring it in.
The explanation behind this is of course that the cooling due to evaporation is happening faster the larger the temperature difference between the tea and the surrounding air. If you let it sit without milk, due to the larger temperature difference it cools down faster than if you poured in the cold milk, thus cooling it closer to room temperature, and then waited.
And there are even occasions when you would you put milk into the cup before adding the tea: If you have delicate china and don’t want to risk ruining it by pouring in almost boiling tea. Plus allegedly that way the milk doesn’t scald and form those weird flakes?
Why would it be interesting to talk about this in a science class?
As a kid I used to wonder why blowing on a hot soup or beverage should be a good idea. Wouldn’t my breath be warmer than room temperature, and hence shouldn’t the soup get warmer instead of colder?
Then I didn’t think about this question for 25 or so years (scary, I know), and then today, when I was blowing on my tea, I realized that by now I knew why I was doing it, even though I had never related my science knowledge to the everyday act of blowing on hot tea.
So why do we blow on hot tea?
The main reason is that at the tea’s surface, evaporation takes place. We can oftentimes see the steam coming off. The molecules that left the cup condense in a fog over the cup. If they stay in place, evaporation will slow. If we blow them away, the air is replaced with colder surrounding air, and evaporation continues.
Another reason is that as we blow on the surface, we create ripples. Hence the surface area is larger than before and more exchange can happen over a larger area. But I would guess that that effect is much smaller than the first one.
The main reason I wanted to write this blog post was because I could see the picture I wanted to show before my eyes: This sweet cup with the rabbit on the handle and the steam rising from it. Turns out it is really difficult to take pictures of that! At least with my camera and my lack of patience. And believe me – I tried for a full 15 minutes with different light sources at different angles and everything! So for now all you get to see is the video below where it is slightly better visible than in a still picture – and please try to imagine the steam! And I will be back once I’ve figured out how to document it properly!