Goal
Approximate the de Bruijn–Newman constant Λ by studying the heat flow of the Riemann zeta function.
Overview
- Define these equations, describing the heat flow of the Riemann Equation
- such that , the zeroes of are real. This is known as the de Bruijn–Newman constant.
- was proved by Brad Rogers & Terence Tau.
- is equivalent to the Riemann Hypothesis.
- was proved as part of the polymath project.
- was later proved by Dave Platt and Tim Trudgian
- is the Fourier representation of
- relates to the zeroes of Riemann’s zeta function
- is the evolution of under the backwards heat equation .
Properties of the Riemann Zeta
- satisfies the functional equation
Plan to bound
- Choose a ( suffices for the time being )
- Take zeroes of
- Computationally estimate how the evolve backwards in time (i.e. towards , getting an estimate of the time at which the trajectories of the various converge to a single point
- Reproduce the above with , obtaining better estimates of .
- If
- , we proved nothing 😢.
- is statistically far from , we have shown that Riemann’s Hypothesis is likely true 🎉
Pre-requisites
Finding zeros
What are the best methods known to find zeroes of the . I have no clue how to find zeroes given the lack of knowledge about the properties of and , namely bounds on the change rate of the function.
- Plot the function for and . Visualise these zeroes. I can do this visually, but I have no confidence this gives me a good approximation of zeroes due to continuity concerns.
Modelling the time evolution of the zeroes
Do we have examples ( in code or books ) of approximating path trajectories using heatflow?Andrea suggested Runge-Kutta. Sounds good
Next steps
Both of the points below follow Andrea’s email suggestion
- Study how to use the Runge-Kutta methodology to solve differential equations. This will be needed to propagate the solution’s of zeroes at backwards in time and find when do the zeroes collapse ( i.e. approximating the defined below )
- Find numerical methods to approximate the zeroes of , for a given large , i.e. .