The one formula that I use above all others in my research is that for the diffusion constant of a dilute species in a fluid, called the Stokes-Einstein (or sometimes Stokes-Einstein-Sutherland) equation:
DSE = kT/(6 π η RH)
The diffusion constant DSE of something with a size (hydrodynamic radius) RH is just the thermal energy kT divided by 6π times the product of the viscosity of the fluid, η, and the hydrodynamic radius, RH. All it tells you is that large species in viscous fluids diffuse more slowly than small species in less viscous fluids.
This is a simple formula but whenever I want to calculate a diffusion constant I usually have to get Python running and use it like a calculator. This takes less than a minute, but even so this is irritating.
So (together with LLMs Google Gemini and MS Copilot) I have done a simple Streamlit app that calculates the diffusion constant, given the hydrodynamic radius as input – for water at room temperature. It runs on Streamlit Community Cloud which is a doodle to do as it just pulls the Python/Streamlit code from a GitHub repository.
It is very basic and only does this one thing: compute a diffusion constant. But because of this it is very easy to use. If I find it useful may be I will make it fancier but we will see. If you find it useful or feel that a fancier version (eg where you can vary the temperature, viscosity etc), just let me know.