Introduction & Context

The Noyes–Whitney equation is the classical mass-transfer model for dissolution of a solid into a well-stirred liquid. In pharmaceutical and chemical process engineering, it is used to predict the instantaneous in-vitro dissolution rate of tablets, granules, or powders under controlled hydrodynamic conditions (USP paddle/basket apparatus, flow-through cells, etc.). Accurate rate estimates are required for:

  • Formulation screening and excipient selection
  • Scaling from lab to production (equipment similarity)
  • Justifying biowaiver requests via in-vitro–in-vivo correlations (IVIVC)
  • Detecting possible mass-transfer limitations in crystallisation or reactive systems

Methodology & Formulas

The model treats the solid–liquid interface as a planar surface bathed by a stagnant diffusion film of thickness h. Solute molecules migrate across this film under the influence of the concentration gradient. The process is assumed to be:

  • Isothermal and isobaric
  • Sink or near-sink (bulk concentration CbCs)
  • Film-controlled (surface reaction much faster than diffusion)

Step 1 – Convert film thickness to centimetres

\[ h_{\text{cm}} = h_{\mu m} \times 10^{-4} \]

Step 2 – Impose a minimum gradient to avoid division by zero

\[ \Delta C = \max(C_s - C_b,\; 10^{-9}\ \text{mg cm}^{-3}) \]

Step 3 – Compute the film mass-transfer coefficient

\[ k = \frac{D}{h_{\text{cm}}} \qquad \text{with}\quad k \ge \frac{D}{10^{-9}} \]

Step 4 – Instantaneous dissolution rate

\[ \frac{dm}{dt} = A\ k\ \Delta C \]

Step 5 – Convert to desired time units

\[ \left.\frac{dm}{dt}\right|_{\text{min}} = \left.\frac{dm}{dt}\right|_{\text{s}} \times 60 \]
Recommended hydrodynamic regime for standard USP II apparatus
Parameter Range Interpretation
Film thickness h 30–100 µm Corresponds to 50–150 rpm paddle speed
Sink index Cb ≤ 0.3 Cs Ensures gradient remains essentially Cs

Outside these intervals, the assumptions of a single stagnant film and/or constant gradient may no longer hold; experimental calibration or more elaborate mass-transfer correlations (e.g., Levich, Ranz–Marshall) should be used instead.