- #1
fireflies
- 210
- 12
I am stuck with this question: why can't we use the equation
c(rms)=√(3RT/M) for problems when no of moles is not 1?
Because I think the mole will be deduced as
c(rms)=√(3nRT/nM) =√(3RT/M)
For instance I found this problem, given atmospheric pressure is 10^5 Pa, molecular mass of
Nitrogen is 28, and at STP the density is 1.25 kg/m^3. What is the c(rms) at 100°C?
If the problem is solved with c(rms)=√(3P/rho) the answer is 576.35 which is the actual answer, and when taken the above equation the answer is 18.22
Then what's wrong with my concept?
c(rms)=√(3RT/M) for problems when no of moles is not 1?
Because I think the mole will be deduced as
c(rms)=√(3nRT/nM) =√(3RT/M)
For instance I found this problem, given atmospheric pressure is 10^5 Pa, molecular mass of
Nitrogen is 28, and at STP the density is 1.25 kg/m^3. What is the c(rms) at 100°C?
If the problem is solved with c(rms)=√(3P/rho) the answer is 576.35 which is the actual answer, and when taken the above equation the answer is 18.22
Then what's wrong with my concept?