General equations for modeling geochemical transport in open systems
نویسنده
چکیده
This set of notes will try to set down in one coherent place, a general set of equations for calculating changes of major element, reactive trace element and U-series nuclides in an open system. Given the continuous form of the equations we will also deal with scaling and discrete forms using Semi-Lagrangian advection schemes. The key to these derivations will be using general conservation of mass for a melt phase and a solid phase
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