Page 162 - Fundamentals of Computational Geoscience Numerical Methods and Algorithms
P. 162
6.4 Applications of the Proposed Decoupling Procedure 151
Reactant A (t = 500,000 years) Reactant A (t = 800,000 years)
Reactant B (t = 500,000 years) Reactant B (t = 800,000 years)
Product (k =2×10 –11 (1/s), t = 500,000 years) Product (k =2×10 –11 (1/s), t = 800,000 years)
R R
Fig. 6.11 Concentration distributions of the chemical reactants and product at two different time
instants (Type 3)
