CarboSchools: General CO2 chemistry (Sharing Experiments cont.)

søndag 3 mai 2009 at 23:47 | In Konferanser og kurs | 1 Comment
Tags: , , ,

Mariana Pirillo (Italy): Demonstration of different chemical reactions which produce CO2

Mariana starts by telling us that the teaching in the Italian schools are quite different from what I’m used to. All the lessons are based as lectures, with no room for the students to work with exercises, tasks, experiments, collaborative work etc in the school. This is something the students are supposed to do after school (more like our universities). This means that it can be hard to find enough time to do these hands-on experiments.

But she has found her way – and her recipe for getting the students involved is:

  1. Ask a question (or two) – “Why are we interested in CO2?”
  2. Get the students to do some background research
  3. Then get them to make a hypothesis before doing the experiment
  4. Testing of the hypothesis by hands-on experiments
  5. Communicate your results

Experiments:

Making CO2 of fizz powder.

  1. Weight of CO2 – fill two balloons, one with air (air pump) and one with CO2. Which balloon is most heavy?
  2. CO2 in water – what happens with the pH?

Sally (Germany): Demonstration of experiments on CO2 in seawater (solubility, buffering capacity, CO3)

Sally showed experiments that she has used with her 11-14 year old students, but these experiments can be used with students all the way through high school as well.

She starts up with the red cabbage experiment to get the understanding of acids and bases.

Then she addresses the main question for the students:

“Why and how can seawater be a sink of atmospheric CO2?”

Two glass jars – one with freshwater and one with seawater. Add acid (vinegar) and base (soap), and measure the change in pH for every drop that is added. Hopefully the students will see the buffer capacity of the seawater.

“Why has seawater this buffer capacity?”

Blow (CO2) in the glass jars (with/pH sensors in them, close the opening with cotton) until the pH doesn’t change anymore. “Why?”
Compare freshwater and seawater.

Crush some eggshell and put this in the freshwater that is saturated with CO2. Check the change in pH.
Do the same with the acidic seawater, and compare the results. The eggshell will not dissolve in the latter because the pH will not be low enough (it is of course a time issues though…)

Addition of carbonate will raise the pH value again.

It is possible to have an experiment with algae, and see the effect of phytoplankton on pH and CO2.

Solubility of CO2 and temperature

Sally found the idea for this experiment on the internet, but has modified it for her students. Fizz tablets in water, measure amount of gas, compare warm and cold water.

Sally uses these experiments with quite young students, but I can use these with my upper secondary students as well. Interesting.

CarboSchools: Meteorology (Sharing Experiments cont.)

søndag 3 mai 2009 at 19:28 | In Geofag, Konferanser og kurs | Leave a Comment
Tags: , , , ,

Maddalena Macario (Italy): CarboSchools.org an open source for teaching environmental education

Maddalena has focused on the Earth’s Atmosphere in her CarboSchools teaching. The context is the third year at upper secondary school (16 yrs old), after they’ve studied the gasous substances.

Duration of activity: 6 hours

Started up with lectures about the atmospheric composition and different meteorological phenomena. Weather forecasts, extreme weather, energy balance, humidity…

Maddalena has experience from different hands-on experiments, and she has found some ideas at the CS library. One experiment about humidity and saturation, and expanded with including aerosols to see how that effects the saturation values.

They also have a weather station at this school in Prato, and they have included their data at SchoolCO2web.

image

Hmmm, I’ve tried to draw the same graph as Maddalena did – with air pressure and humidity in the same graph, but the is a database connection failure. Maybe there should be a table about which dates there exists data from the different stations??

Maddalena has combined graphs with measured humidity and air pressure with the students weather forecasts, to show the commection between a higher humidity and low pressures.

The third experiment is about the greenhouse effect. It looks a bit like Rocer’s experiment.

The fourth experiment is about cloud formation due to condensation particles. This experiment is the same as I experiences at the ASE conference earlier this year, and at the Geofag teacher’s course in Oslo. (Create cloud in a bottle: Water in a bottle – smoke from a match to include smoke particles – increase pressure bu squeezing the bottle).

One of the problems she has experienced: links to websites keep changing (important to include date and time for the web pages) – databases are not stable – SchoolCO2web is not stable, makes it hard to compare your own data with data from other schools in the CarboSchools programme.

Needs: dynamic sites (blogs, fora, exchanging experiences); a database with experiments categorized by theme, key words, age of the students; news letters from CS library.

My remarks: This was very interesting – she teaches a lot of the same themes as I have in my Geoscience lectures. Nice to meet someone with this experience ;-)

Nå har jeg registrert meg på Bloggurat.

CarboSchools – Modelling (Sharing Experiments continues)

søndag 3 mai 2009 at 1:03 | In Konferanser og kurs | Leave a Comment
Tags: , , , , ,

Marc Jamous – Regional Coordinator in France – Predicting CO2 scenarios through models

image

1958 was the first year that the total amount of atmospheric CO2 was measured, which is the reason for the start year for this simplistic model. In this model you start by the total amount of atmospheric CO2, and after that you add fuel emission and land use.

imageThe first step is to add the emissions to the atmospheric amount. The second step would be to compare the measured and the calculated CO2 data. The students will then see that there in a gap between the measured and calculated values – CO2 must be absorbed somewhere else then in the atmosphere.

image

The next step is to find a suitable value for the natural absorption, as a percentage of the emissions.

This is a great introduction to climate modelling as a discussion theme with our students.

Further on it would be possible to split natural absorption in absorption by the ocean and absorption by the vegetation.

After making this model, it is now possible to include the prediction scenarios from the IPCC reports to calculate model results. It is also possible to get the students to make their own scenarios.

Camparison between the pessimistic and optimistic scenarios:

image

My concluding remarks: This was an easy but fantastic way of introducing the principles of climate modelling! I look forward to try this with my own students next year :-) I also want to thank Marc for sharing his files with us.

Blogg på WordPress.com. | Theme: Pool by Borja Fernandez.
Entries and comments feeds.