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Because no reaction relation was found, we considered CaO to be a mobile component (i.e., a component that was not preserved before and after the reaction) and omitted it from the system.
Following [ 40], a CRN is defined above as a finite set of species S ⊆ S and a reaction relation R ⊆ ℛ S = ℕ S × ℕ S × ℙ over complexes ℕ S. In the CRNT approach [ 1], a CRN is instead defined as finite set of complexes C ⊆ ℕ S and a reaction relation R ⊆ ℛ C = C × C × ℙ.
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Despite the American reaction, relations between the sides are not expected to be damaged.
We first tried to determine the reaction relations from the four-component system but were unable to get proper reaction relations.
The SVD analysis gives linear dependence among these minerals, corresponding to the stoichiometry in reaction relations.
The four-component CaO SiO2 AF FM system does not yield proper reaction relations.
This constraint is critical in subsequent discussions on reaction relations forming the reaction zone as derived by the SVD method.
We then examined linear combinations of these reactions, which can also give reaction relations among these minerals.
The SVD method is a type of least square method that systematically surveys reaction relations among minerals.
We then attempted to find reaction relations that hold the conservation of pseudoternary components SiO2 AF FM for the same mineral assemblage.
To conclude, we have successfully derived reaction relations in the rodingite serpentinite system under constant solid volume conditions.
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