Our planet Earth, precisely speaking its surface shell, might be considered as a huge multiphase batch biochemical reactor heated by the Sun, whose energy is a unique resource. The Sun ensures our earthly life unconditionally; moreover, it compensates the heat losses of land, water, and ice by radiation emitted from the Earth surface to its surrounding space at night. It is evident that in this macroreactor the complex transport phenomena occur in many phases, involving mass, heat, and momentum. Obviously, such a responsive batch system is strongly limited by raw resources of all elements including carbon materials necessary for a good living standard and utilized both in the energy production and for the main industrial chemical processes.