A steady well-mixed hot salty reservoir receives volumeflux Q and loses the same flux over aweir. Heat and salt balances are Q(Ti−T)=AFT and Q(Si−S)=AFS. If βFS/(αFT)=RF and αFT=b(αΔT)4/3/Rρ2, define R0=β(Si−S∞)/[α(Ti−T∞)]. Then ηs=(RF/R0)θs and C=Ab[α(Ti−T∞)]1/3/(QR02). For R0>1 and 0≤RF<1 the interface is statically stable while preferential heat transfer can drive double-diffusive convection.