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Explore the significance of mass flows for achieving equilibrium conditions in isolated systems. Learn about mass transport through convection and diffusion processes, with key equations and concepts explained. Gain insights into the complexities of mass balance in thermodynamics.
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MASS BALANCE: WHY MASS FLOWS? SURROUNDING Phase a Ta, Pa, mia Phase b Tb, Pb, mib NO NO ISOLATED SYSTEM WORK HEAT Ideal fixed permeable membrane ai = ith species activity Ta = TbPa= Pb mia = mia EQUILIBRIUM CONDITIONS dU=dUa+dUb = 0
MASS BALANCE: EQ.CON. ALTERATION 1 Pa increase (>Pb) [Ta = Tb; mia = mib] Phase a T, Pa, mi Phase b T, Pb, mi MASS TRASPORT (CONVECTION) permeable membrane Mass transport represents a possible way the system has to get new equilibrium conditions once the original ones have been altered.
MASS FLOW (Kg/s) =V*S*Ci V = velocity (m/s) S = cross section (m2) Ci = “i” concentration (Kg/m3) S V Ci MASS FLUX (Kg/sm2) =V*Ci V = velocity (m/s) Ci = “i” concentration (Kg/m3) S = 1 m2 V Ci
mia>mib [Ta = Tb; Pa = Pb] 2 Phase a T, P, mia Phase b T, P, mib permeable membrane MASS TRASPORT (DIFFUSION) Mass transport represents a possible way the system has to get new equilibrium conditions once the original ones have been altered.
FICK LAW DX CiX+DX S CiX MASS FLOW (Kg/s) =-S*D*DCi/DX S = cross section (m2) D = diffusion coefficient (m2/s) Ci = “i” concentration (Kg/m3) DCi/DX = gradient concentration (Kg/m2s) DCi/DX = (CiX+DX-CiX)/DX MASS FLUX (Kg/sm2) =-D*DCi/DX
MASS BALANCE Z X Y DZ DX (X+DX, Y+ DY, Z+ DZ) G (X, Y, Z) DY (X, Y+ DY, Z) (X+DX, Y+ DY, Z)
MASS BALANCE: EXPRESSION DX DZ (X, Y, Z) G DY Ci = f(X, Y, Z, t)
DX DZ (X, Y, Z) G DY DIVIDING FOR DV
FLUXES EXPRESSIONS Ideal solution Diffusion Diffusion Diffusion Convection Convection Convection Bi = mobility of the diffusing components
MASS BALANCE: CYLINDRICAL COORDINATES Jir+dr Jir+dr Jiz Jiz+dz Jir Jir Jir Jiz Jiz+dz Jir+dr r dr dz TWO DIMENSIONS r z
Ci = f(z, r, t) r dr dz Dividing by 2prdrdz