Estimates your current serum 25-hydroxyvitamin D [25(OH)D] concentration by modelling the depletion of cholecalciferol (vitamin D3) stored in your adipose tissue after the summer UVB season. Uses a two-compartment pharmacokinetic model with a BMI-adjusted terminal half-life of 60–90 days.
End of the effective UVB season at your latitude — for most of the continental US & southern Canada that is late September; for high-latitude sites (> 55° N/S) it is typically mid-August.
≈ 3 nmol/L · 275 days since your summer peak of 20.1 ng/mL
Effective terminal t½
70 d
two-compartment adipose model
Suggested supplement
5,000 IU
cholecalciferol / day for 90 d
Days until insufficiency (<30 ng/mL)
now
Endocrine Society threshold
Days until deficiency (<20 ng/mL)
now
IOM threshold
About this model
Serum 25(OH)D decays with an effective terminal half-life of ~60 days in lean adults and up to ~90 days in obese adults, reflecting the slow release of cholecalciferol from adipose tissue (methodology). This is a modelling estimate, not a substitute for a laboratory 25(OH)D measurement or clinical advice — see the medical disclaimer.
Cholecalciferol (vitamin D3) synthesised in the epidermis from 7-dehydrocholesterol enters the bloodstream bound to vitamin D-binding protein (DBP). In the liver it is 25-hydroxylated by the CYP2R1 enzyme, producing 25-hydroxyvitamin D [25(OH)D] — the metabolite measured clinically because it best reflects overall vitamin D status. A second hydroxylation in the kidney (CYP27B1) yields the biologically active hormone 1,25-dihydroxyvitamin D (calcitriol), which is tightly regulated by parathyroid hormone, calcium, and phosphorus.
Circulating 25(OH)D has an apparent half-life of 15–25 days when studied in short-duration tracer experiments (Jones 2008; Vieth 1999). However, the whole-body terminal half-life is considerably longer — around 60 days in lean adults and 80–90+ days in obese adults — because cholecalciferol partitioned into adipose tissue re-enters the circulation over months. This adipose sequestration explains why obese individuals often show lower serum 25(OH)D at any given UVB dose (Wortsman 2000; Drincic 2012), and why winter decline curves in temperate populations follow an exponential trajectory with a time constant of roughly two months (Kimlin 2007; Webb 2010).
The calculator assumes a first-order elimination process with an effective terminal
half-life scaled to body-mass index. Peak summer serum 25(OH)D is estimated from a
pigmentation-, age-, and dose-adjusted anchor point (Fitzpatrick II, 90 min of near-noon
UVB per week, exposed fraction ≈ 0.28 → 40 ng/mL, per Holick 2007). The model then
projects forward from your entered last-effective-exposure date using
C(t) = Cpeak·e−λt
where λ = ln(2)/t½. Daily supplemental
cholecalciferol asymptotically raises steady-state serum 25(OH)D by ~1 ng/mL per 100 IU/day
in lean adults (Heaney 2003), and this contribution is added with the same time constant.
This is a population-level model and cannot capture individual variability in DBP polymorphisms, CYP2R1 activity, renal function, malabsorption, or medication interactions (e.g., glucocorticoids and anticonvulsants can accelerate 25(OH)D catabolism). If your estimate suggests insufficiency and you have symptoms — bone pain, unexplained fatigue, frequent infections — please seek a serum 25(OH)D measurement from a healthcare provider rather than relying on a modelled projection.