Carbon Dioxide: Experiment #5: Ocean Acidity. |
|
The bad news, good news and more bad news about elevated
CO2 levels in the atmosphere. |
|
In experiment #2, we showed that
CO2 comes from car exhaust as the engine burns gasoline making CO2 and water. When CO2 dissolves in water, we showed that it becomes carbonic acid. |
|
If this water is the ocean, this
carbonic acid threatens the marine animals that use calcium carbonate to
create their exoskeletons and shells. |
|
There are many ways humans have damaged marine life; for example, pollution, over fishing, dredging, and blasting are the obvious ways. Adding carbon dioxide to the atmosphere is a more hidden way of harming marine life; a way that slowly dissolves their bodies. |
|
Many sea creatures build its shell or exoskeleton with calcium carbonate; unfortunately, that can be dissolved with acid formed by carbon dioxide dissolving into the ocean. Let's see how that happens... | |
First carbon dioxide in the atmosphere combines with ocean
water to make an acid called carbonic acid (note: some CO2 dissolves in water without combining with water). Like most acids, carbonic acid releases a hydrogen ion
(H+). Its called an ion because it has a charge. Here it's a plus
one charge. The hydrogen ion (H+) is the
active ingredient of acids. H+
is a proton, so it's small and powerful. |
|
Water not strong enough: Water (H2O) has one end that is partially positive and the other end is partially negative. The positive end is attracted to the negative carbonate (CO32-). The negative end of water is attracted to the positive calcium ion (Ca2+). Water is trying to pull the calcium carbonate apart but the attraction of calcium ion to the carbonate ion is too strong, so the shell stays intact. | |
H+
ions (protons) are strong enough: (1) H+ ions (protons) released by carbonic acid hitch a ride on water molecules and then get attracted to the negative charges on the carbonate (CO32-). (2) the protons break away from the water and slide into the calcium carbonate getting in between the positive calcium and negative oxygen atoms. (3) The calcium ion (Ca2+) get replaced by the protons (H+ ions). (4) The displaced calcium ion gets surrounded by water. (5) The small protons continue to slip in and displace the calcium ions. (6) The carbonate with a proton attached (together they are called bicarbonate) is also surrounded by water. The outcome is calcium carbonate dissolves, and the marine animal looses its shell or exoskeleton and dies. CaCO3(s) + H+(aq) --> Ca2+(aq) + HCO3-(aq) |
|
To demonstrate that CO2 makes water acidic, we will bubble CO2 through water. Instead of the source of CO2 being your automobile, it will be yourself. Yes, you contribute to global warming and to the oceans acidity, too (but to a much lesser amount than your automobile). |
|
We will detect the CO2 in two ways. Both ways show that the acidity of water increases when CO2 is added. One way of showing it is by directly measuring pH. The other way is the same as we did in the car exhaust lab, but this time, you will provide the CO2. |
|
Air Stone: |
|
Attach Air Stone to Tubing: (There's also blue tubing on the portable air pump, but you should use the loose segment of tubing.)
|
|
Gases Dissolve better in Cold Water: |
|
Place Ice and Water in Beaker: So to get more of the carbon dioxide from our breath to
dissolve in the water, we are going to blow into a beaker of ice water
using some tubing attached to an air stone. The concentration of CO2
in air from our lungs is about 4% (4 CO2 molecules with the
remaining 96 being oxygen, water, and nitrogen). With car exhaust, CO2
concentration is about 12%. |
|
Place Air Stone with Tubing into Beaker: Place the air stone into the water and it should be submerged in the water. |
|
Blow into tubing: Blow into the tubing to get bubbles coming out of the air stone. It does take a bit of force to keep the air flowing. If you are asthmatic or have some lung problems, you might get someone else to do that for you. Continue blowing for about 3 minutes. It's OK to take some short breaks during that time. |
|
Use pH test strip: You can use either pH test strip to see if the water has become acidic. The 0-14 pH range paper covers the whole range and the pH 4.0-7.0 test papers work because that's the range that a weak acid like carbonic acid could fall within.
|
|
Dip pH test strip into the Water: |
|
Check pH paper with Color Chart: Here I found out the water had a pH between 5 and 6.
That means there's about 10 (pH6) to 100 (pH5) times more H+ ions (acid) in the water
after I blew carbon dioxide into it than when it started as neutral tap
water (which would have been pH 7). |
|
Indirect detection of acid: |
|
Lime Water: Just like we did in the Car Exhaust experiment, we will use some lime water (saturated calcium hydroxide) as our alkaline solution. The reaction shows that the acid from the carbonic acid will combine with the hydroxide ions (OH-) to form water. |
|
Measure 3mL of water: Use your Purified Water bottle and the small graduated cylinder to measure out 3 milliliters of water. This is the same thing you did with car exhaust lab. |
|
Add 1 mL of lime water: Use a clean plastic pipette to transfer about 1 milliliter of lime water (calcium hydroxide solution) to the graduated cylinder bringing the level up to the 4mL mark. |
|
Pour diluted lime water into beaker: Pour the four milliliters of the diluted lime water into the small 50 mL beaker. |
|
Add Phenolphthalein: Add about 2 to 4 drops of your phenolphthalein solution (made in Exp 2) to the diluted lime water. The solution should turn a dark pink. If it doesn't then the lime water may have gotten neutralized by CO2 in the air. If the cap to the test tube with the lime water isn't air tight, air can get in. The CO2 in the air will neutralize the lime water's OH- ions. In that case, find the test tube with sodium bicarbonate, and add a few grains of the powder to this solution. Stir it and see if it turns pink. If not, add a few more grains of sodium bicarbonate. Sodium bicarbonate produces some OH- ions in the water. Phenolphthalein is pronounced feenol-thay-leen. |
|
The phenolphthalein we added will have two structures.
When clear it is the left structure. It becomes the right structure as
it turns pink in the lime water (Ca2+ and OH-).
What happens is these negative hydroxide (OH-)
ions pull off the hydrogen atoms to form water (H2O) See red
arrows. When the hydrogen atoms are pulled off, they leave their electrons
behind becoming H+ ions. The extra electrons cause a shifting
of electrons that generates the right-side structure. One outcome is the
central carbon (blue arrow) gets connected
to the upper left ring by sharing two electrons (called a double bond
and indicated with a double line). In the right structure notice the double
bonds (double lines) alternate with single bonds (single lines). This
allows electrons to jump around the whole structure. This free movement
of electrons allows them to absorb various frequencies of light. The solution
is pink because it is absorbing most colors but lets pink color pass through. |
|
Blow into Beaker: |
|
Here are
the steps. 2) The acid neutralizes the OH- from the lime water. 3) The carbonate and calcium combine to make chalk 4) Additional H+ created attaches to the phenolphthalein returning it to its clear form (5). |
|
The changing of dark pink to clear is an indicator that
carbon dioxide from your breath entered the water, turned to acid, neutralized
the alkaline solution, and returned the phenolphthalein to its clear form.
|
|
If you can see this effect with your own breath, imagine the effect that millions of cars and thousands of fossil fuel power plants have on the ocean. The below picture shows the lights from space but that indicates the regions where cars and power plants are located. That also means where the most carbon dioxide is being produced and released. The bright eastern United States and Europe show dense areas of population. | |
Instead of just imagining the effects of the extra carbon dioxide. Ships have been sent crisscrossing the ocean taking readings of the carbon dioxide levels. The below map shows the concentration of anthropogenic (man-made) carbon dioxide at the surface of the ocean. We shouldn't be surprised that the highest levels (red) sit between the areas of high population density as the Earth lights picture above showed. | |
The concentration of "mmol kg-1" stands for millimoles of carbon dioxide per kilogram of sea water. A "mole" is a quantity measurement in chemistry that is equal to 6 x 1023 atoms or molecules. Since "milli" means one thousandth, a millimole would be 6 x 1020 atoms or molecules. So the red along the eastern coast of United States is 0.06 millimoles of carbon dioxide, which means 0.06 x 6x1020= 3.6 x 1021 molecules of carbon dioxide for each kilogram (about a liter) of ocean water. This doesn't count the carbon dioxide molecules that reacted with water to form carbonic acid. This is just the dissolved carbon dioxide gas. | |
High levels of acid dissolve calcium carbonate shells and exoskeletons. Even slightly elevated levels of acid will slow the making of the shells and exoskeleton (calcification). Since pre-industrial times, the pH of the ocean has gone from about 8.18 to about 8.08. That 0.1 difference equates to about a 25% increase in H+ ion concentration. By the end of the century, the increase is expected to be about 225%. That's what has got many oceanographers worried because some corals are dying now from current elevated H+ levels. They worry what will happen if that jumps nine fold (25% to 225%). | |
Congratulations on finishing the lab. Send the photos and the pH data (from the first part) to costello107@chemistryland.com |