Use the squared three-dimensional endpoint displacements, not their arithmetic mean. The mean squared displacement estimate and corresponding diffusion coefficient are
The factor six is for three-dimensional Brownian motion. For an isolated no-slip sphere, the Stokes–Einstein relation gives the Brownian radius estimate from endpoint displacements:
Here room temperature is taken as ; choosing gives , a much smaller difference than the sampling uncertainty. Under independent increments with a normal distribution, for . The sampling uncertainty of an endpoint diffusivity estimate therefore makes this a rough radius estimate. It assumes negligible drift and hydrodynamic coupling between probes, the supplied bulk viscosity, and actual three-dimensional tracking. Localization noise adds to the squared displacements and would bias this inferred radius downward if uncorrected.
For the three-dimensional worm-like chain, define the bending coefficient by . Its persistence length is . Holding that coefficient and the polymer contour length fixed gives
The temperatures must be absolute. The end-to-end distance of a worm-like chain obeys
For a long flexible chain, , the typical size is , so warming contracts the chain, with . The finite-length formula also decreases as decreases, but the rod limit changes very little. A large segment count alone does not guarantee . If the material's bending coefficient itself depends on temperature, replace the first ratio by ; the sign then needs that additional material information. This calculation concerns a generic physical filament, with no biomolecular application.
For monovalent mobile ions, the linearized Debye–Hückel screening length is
Here is a number density in , not a molarity. Use the question's idealized neutral-water convention, , and . Both ion species contribute:
For added salt concentration in , the ionic strength in this model is . With the numerical molarity ,
The water contribution is negligible at that salt level. The factor converts molarity into ; omitting it or counting only one ion species gives a wrong screening length. Exact water autoionization and activities vary with temperature, so the first estimate uses the simplified neutral concentrations implied by the question. At the higher salt level, ion-size effects, nonideal activities and changes in permittivity limit the numerical accuracy of this continuum estimate.

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