GROUP EXERCISE NUMBER TWO CHM 1045 -- Dr. Light The Mole Only students working together in a group may submit solutions to the group exercises. Each group should get together, discuss, and agree on how the solution to the exercise should be done. A group solution is then written out and submitted, with all members of the group who participated signing the front cover page. The solution should be worked out neatly (preferably printed or typewritten--at least make it legible), should contain a cover page with the group name and signatures, and all pages should be stapled together. The solution is due at the end of class on Wednesday, February 21. MOLES FOR NOLES or How big is a mole, anyway? or In touch with your ancestors. Argon is a stable element that is gaseous and makes up 0.94% of the atmosphere. All the atoms in the atmosphere today have been there since the early development of the atmosphere. What is the likelihood that you will breathe one or more atoms that passed through the lungs of Julius Caesar, Alexander the Great, or some other historic notable? To approach such a question, we sometimes carry out what are referred to as "back of the envelope" calculations--i.e. we are not looking for precise answers as much as estimates, and often assumptions have to be built into the process, with us later deciding how the answer would change if the assumptions changed. Have a go at this one. There is not really a "right" answer. What is important is your thinking and approach in how you go about combining assumptions with known quantities. A suggested way of addressing the question is as follows. If someone takes one breath of air, and sufficient time elapses for all the molecules in that breath to disperse uniformly throughout the earth`s atmosphere, then how many breaths would a second person have to take in order to inhale at least one atom of Ar? Following are some needed data and some hints: Assume the height of the atmosphere is 20 km (its higher, but contains very little gas above that height). You can calculate the volume as the volume of a shell obtained by subtracting the volume of the sphere representing the earth from the volume of the sphere representing the earth plus its atmosphere. You can also estimate the volume by multiplying the surface area of the earth by the height of the atmosphere. (What are the problems associated with each way of estimating the volume?) (Later on when we study gases in Chapter 10, we can explain another way to calculate the quantity of gas in the atmosphere). The radius of the earth is 6.37 x 10^3 km. The volume of a sphere is 4/3ăr^3, and the surface area of a sphere is 4ăr^2. At the surface of the earth there are about 0.044 moles of a gas in a volume of one liter. Assume one breath is a volume of about 0.5 liters. In considering the distribution of atoms and molecules throughout the atmosphere, assume the average molecular density of the atmosphere to be one-half that value or about 0.022 moles of gas in a volume of one liter.