M=∫∫∫ρdV Z =∫∫∫(f+φ)ρdV while ρ(x,y,z) is density,M is mass,T is temperature f(1/ρ,T) is helmholtz free energy per unit mass φ(x,y,z) is potential energy per unit mass it's said that when Δz=0 the system is in equilibrium mass doesn't change ΔM=0 then how to solve these two equations so as to make the statement that f+φ+ρ(∂f/∂ρ)=constant , independent of x,y,z ?
How far are you able to get on your own? It looks like we need to use the chain rule in differentiating f with respect to ρ.
Maybe we can also use integration by parts and split Z into two integrals to get it to look like M? Some interesting things to play around with.
Δ∫∫∫(f+φ)ρdV =∫∫∫[Δ(f+φ)ρ+(f+φ)Δρ]dV =∫∫∫[ρΔf+ρΔφ+(f+φ)Δρ]dV =∫∫∫{ρ[(∂f/∂ρ)Δρ+(∂f/∂T)ΔT]+ρΔφ+(f+φ)Δρ}dV =∫∫∫{[f+φ+ρ(∂f/∂ρ)]Δρ+ρΔφ+ρ(∂f/∂T)ΔT}dV then i don't know how to get any further
Where, \(\Delta=\nabla^2\)?
Never mind, that just looks awkward, what do you mean, then, by \(\Delta M=0\)?
it's calculus of variation.To my knowledge,i think it's about time. the mass doesn't change from time to time i think
That's what I thought, if you want to make it so, make sure to not use capital delta \(\delta M\) is more appropriate. I'll be right back, see what I can do.
I must say, I'm currently stumped. It seems like a continuity equation, but I'm not sure what to do with the variations, since it's not a functional we're referring to.
I mean, we could simply go with the assumption that the system is in equilibrium when, given some small \(|\delta \rho|>0\) we have that \(\delta z=0\). Then it's quite simple.
well after reading books i find every similar problem it goes that way [f+φ+ρ(∂f/∂ρ)]Δρ then f+φ+ρ(∂f/∂ρ) is constant [g+φ]Δρ then g+φ is constant what i can't figure out is that when it's with Δρ then it's ''coefficient'' must be constant
does it get something to do with ΔM=∫∫∫ ΔρdV=0 ?
That's what I'm thinking. Perhaps integration by parts on the first integral; but that gives an odd result.
What book is this, anyways? It'd be nice to know a bit more about the context.
well that book is in chinese and it's a bit old
@dan815
Again, if we do go by the first definition (which I what I think it means) that for some variation \(\delta \rho \ne 0\), we have that \(\delta z=0\), then the statement is fairly clear. I mean, this is the only thing that makes sense, because any other variation yields unwanted terms, so we'd need stricter conditions to clean them up.
but what about other terms like ρΔφ+ρ(∂f/∂T)ΔT ?
All are zero because each is independent of \(\rho\).
why Δφ is zero? i'm wondering if Δ means the variation from time to time
In this case, it just means a given variation. \(\delta \phi\) is zero since it is completely independent of density (only dependent on position), and \(\delta T\) is the same.
Join our real-time social learning platform and learn together with your friends!