In CO2 experiment #1 I tested the hypothesis that the rate at which CO2 dissolves into water is directly related to the concentration of CO2 already dissolved in the water. The test was carried out by bubbling CO2 through the water in a 5-gallon bucket, capturing the bubbles as they reached the top, and counting how many bubbles were required to displace 5 mL — a fancy way of saying that I was measuring the volume of each bubble. Anyway, it turned out that the volume of the bubbles captured did not change significantly regardless of the concentration of CO2 already dissolved in the water. Each bubble retained a volume of between 0.0388 mL and 0.0407 mL throughout the experiment. Since the bubbles started out the same size, and were the same size when they reached the top, I had to conclude that there was no significant difference in the rate at which CO2 dissolves in water at concentrations between about 5 mg/L and 270+ mg/L.
The purpose of this experiment will be to confirm or deny the conclusion of experiment #1. I am always reluctant to rely upon one set of measurements. No matter what I am doing, if the consequences of being wrong are anything more than trivial, I prefer to double check. Independent verification is even better. That is why I want to conduct this experiment.
My current idea is to run the
experiment in a somewhat reverse fashion. Instead of capturing
gas until it displaces a certain volume, I will start with a
known volume and measure the rate at which it dissolves. My
proposal is to fill the test tube with 5 mL of CO2
and then suspend the inverted test tube in a strong water
current and measure the time required to dissolve the 5 mL of
CO2. If the results of experiment #1 are indeed
correct, the concentration of CO2 in the water
should make no significant difference in the amount of time
required to dissolve the 5 mL of CO2 from the test
tube. However, if the results of experiment #1 are not
correct, the amount of time required to dissolve the
CO2 from the test tube should increase as the
concentration of CO2 in the water is increased.