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Robertson Model


The Robertson model is a three-species mass-action system used as a test problem for solvers for stiff differential equations (Robertson 1966, Baumgartner and Szmolyan 2025). If x, y, and z are the concentrations, its ordinary differential equations are

x^'=-k_1x+k_3yz
(1)
y^'=k_1x-k_2y^2-k_3yz
(2)
z^'=k_2y^2,
(3)

where x(t), y(t), and z(t) are functions of time, primes denote derivatives with respect to t, and k_1, k_2, and k_3 are positive rate constants. The usual benchmark uses k_1=0.04, k_2=3×10^7, and k_3=10^4, with initial state (1,0,0).

Adding the equations gives the conserved total M=x+y+z. The nonnegative concentrations with fixed M>0 form an invariant simplex, so any concentration can be eliminated to obtain a planar system. Every solution in this simplex tends to the equilibrium point (0,0,M) (Baumgartner and Szmolyan 2025). The widely separated rate constants make the approach take place on different time scales.


See also

Mass-Action System, Singular Perturbation, Stiff Differential Equation

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References

Baumgartner, L. and Szmolyan, P. "A Multiparameter Singular Perturbation Analysis of the Robertson Model." Stud. Appl. Math. 154, e70020, 2025. https://doi.org/10.1111/sapm.70020.Robertson, H. H. "The Solution of a Set of Reaction Rate Equations." In Numerical Analysis: An Introduction (Ed. J. Walsh). London: Academic Press, pp. 178-182, 1966.

Cite this as:

Weisstein, Eric W. "Robertson Model." From MathWorld--A Wolfram Resource. https://mathworld.wolfram.com/RobertsonModel.html

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