Free convection heat transfer with internal sources of heat in a liquid core of the Earth by the account of magnetic forces is considered. The core of the Earth is considered as a spherical layer. For temperature the ...Free convection heat transfer with internal sources of heat in a liquid core of the Earth by the account of magnetic forces is considered. The core of the Earth is considered as a spherical layer. For temperature the boundary conditions Ⅰ, Ⅱ, Ⅲ sorts were considered. As a result of the numerical decision of a task the fields of temperature, stream function, local and average of Nusselt number are obtained.展开更多
文摘Free convection heat transfer with internal sources of heat in a liquid core of the Earth by the account of magnetic forces is considered. The core of the Earth is considered as a spherical layer. For temperature the boundary conditions Ⅰ, Ⅱ, Ⅲ sorts were considered. As a result of the numerical decision of a task the fields of temperature, stream function, local and average of Nusselt number are obtained.
