25 Nov '15 08:18>1 edit
I recall an atmospheric problem example in my general chemistry textbook from about 45 years ago. The example was intended to offer a sense of the number of gas molecules in each breath of air. At first, the problem solution is compound but not difficult. The results are intended to be a little surprising.
I think that there are other derivative problems that make this a little more interesting.
Assume a standard breath of air inhaled to be about 500 cc (or ml) and at the conditions applicable for the ideal gas, e.g. sea level (1 atm etc).
Calculate the number of gas molecules in the breath of air - easy to do.
Next figure out the distribution of those gas molecules if they were equally diffused in the atmosphere.
The solution comes out to one molecule of gas for each breath inhaled over the entire planet atmosphere. Seems intuitively reasonable.
The textbook, if I recall, made the point that this meant that in the pure molecular distribution sense, with each breath of air that we all breathe in, we are statistically breathing in a molecule that was breathed in by anyone who lived on planet earth in the past, so long as time and distance allowed for full diffusion. One breath has a molecule from confucious, siddharthra, jesus, mohammed, attila the hun, julius caesar, ghengis khan, chairman mao, adolf hitler etc.
Well, it's not really true, of course. We metabolize those oxgen molecules. The nitrogen gets caught up in amino acids and nucleic acids. The molecules aren't just marbles that don't change.
But wait. What if my memory is faulty? What if the book was referring to Argon? Argon is inert and it could be true! Argon makes up about 0.934% of the earth's atmosphere. What happens if we run the numbers then?
There are corollary questions: What about water molecules? What about the atoms of our bodies?
For now, I'm just curious if anyone cares to run the calculations for argon to see if the concept holds.
Why don't I do it? Well, I'm a little troubled by the atmospheric distribution. I suppose I could readily determine the median altitude for atmospheric pressure and calculate the total volume of the atmosphere from there. That would work. But then, How does argon distribute in the altitude gradient?
I'm just curious and thought I'd toss this out there for a fun excerise in case it interests others.
I think that there are other derivative problems that make this a little more interesting.
Assume a standard breath of air inhaled to be about 500 cc (or ml) and at the conditions applicable for the ideal gas, e.g. sea level (1 atm etc).
Calculate the number of gas molecules in the breath of air - easy to do.
Next figure out the distribution of those gas molecules if they were equally diffused in the atmosphere.
The solution comes out to one molecule of gas for each breath inhaled over the entire planet atmosphere. Seems intuitively reasonable.
The textbook, if I recall, made the point that this meant that in the pure molecular distribution sense, with each breath of air that we all breathe in, we are statistically breathing in a molecule that was breathed in by anyone who lived on planet earth in the past, so long as time and distance allowed for full diffusion. One breath has a molecule from confucious, siddharthra, jesus, mohammed, attila the hun, julius caesar, ghengis khan, chairman mao, adolf hitler etc.
Well, it's not really true, of course. We metabolize those oxgen molecules. The nitrogen gets caught up in amino acids and nucleic acids. The molecules aren't just marbles that don't change.
But wait. What if my memory is faulty? What if the book was referring to Argon? Argon is inert and it could be true! Argon makes up about 0.934% of the earth's atmosphere. What happens if we run the numbers then?
There are corollary questions: What about water molecules? What about the atoms of our bodies?
For now, I'm just curious if anyone cares to run the calculations for argon to see if the concept holds.
Why don't I do it? Well, I'm a little troubled by the atmospheric distribution. I suppose I could readily determine the median altitude for atmospheric pressure and calculate the total volume of the atmosphere from there. That would work. But then, How does argon distribute in the altitude gradient?
I'm just curious and thought I'd toss this out there for a fun excerise in case it interests others.