Basins of Attraction for Third-Order Sigmoid Beverton Holt Difference Equation

The third-order difference equation yn+1=a1yn21+yn2+a2yn−121+yn−12+a3yn−221+yn−22, as a potential discrete time model of population dynamics with three generation involved, is studied. The parts of the basins of attraction of three equilibrium points that this equation admits are described. Some results about period-two and period-three solutions have been established.

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Journal
Mathematics
Published
2025-09-16
DOI
https://doi.org/10.3390/math13182990
Primary Topic
Differential Equations and Numerical Methods
Type
article
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article

Basins of Attraction for Third-Order Sigmoid Beverton Holt Difference Equation

M. R. S. Kulenović, Ryan C. Sullivan
Mathematics
Differential Equations and Numerical Methods
article

Basins of Attraction for Third-Order Sigmoid Beverton Holt Difference Equation

M. R. S. Kulenović, Ryan C. Sullivan
article en

Abstract

The third-order difference equation yn+1=a1yn21+yn2+a2yn−121+yn−12+a3yn−221+yn−22, as a potential discrete time model of population dynamics with three generation involved, is studied. The parts of the basins of attraction of three equilibrium points that this equation admits are described. Some results about period-two and period-three solutions have been established.

MathematicsVol. 13(18)
University of Rhode Island (US)
Openalex Percentile: Top 64%
Differential Equations and Numerical Methods
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Basins of Attraction for Third-Order Sigmoid Beverton Holt Difference Equation — M. R. S. Kulenović, Ryan C. Sullivan · Mathematics (2025) | TGRS Research Map | TGRS