These calculators turn your human-confirmed field data into the census metrics — all in your browser, no login, no data sent anywhere, and they keep working offline once the page has loaded. The arithmetic is exactly what the course guide specifies; nothing here replaces your judgment about what the numbers mean.
Each capture's density is its count over the disk it sampled, D = N / (π r²), expressed through the ratio r / K so the day's kick-length cancels and dives compare. The site index is the average of the six D̄ = mean of Dᵢ — densities averaged, never counts pooled.
Re-occupy a hub on unchanged structure and the reading still moves a little. That spread is the noise floor — the smallest change the survey can trust. A later reading counts as real change only if it moves by more than the floor.
From the species tally: richness, the abundance-weighted diversity indices as effective numbers of species exp(H′) and 1/λ, Pielou evenness J, and the unified Hill profile at q = 0, 1, 2.
How much the community's composition moved between two visits. Bray–Curtis weighs abundances; Jaccard weighs only presence and absence. Both run 0 (identical) to 1 (nothing shared) — the compositional analog of the noise floor.
The relative rate of change in abundance between two readings a time apart: r = ln(D̄ₜ / D̄ₜ₋₁) / Δt. Like everything here it is a rate of change of the index, honest about the index's own limits.
Assemble everything you've entered and calculated into a clean census report — including the guide's accuracy-and-limitations statement — then use your browser's print dialog to save it as a PDF or send it to a printer.