Forced convective mass transfer between a solid nonspherical particle and water was studied for 0.1993 < (Dp/Dc) < 0.477 and 50 < WRec < 25000. No effect of (Dp/Dc) was observed in the range studied. The experimental results were correlated by NShNs¿/3 = 0.5844 <,c + 0.006012 /VRec. Mass (or heat) transfer between particles surrounded by a continuous fluid phase is of importance in many engineering operations. Typical examples include absorption, adsorption, aerodynamics, bubble plate distillation column, calcining, catalytic beds, desorption, drying, liquid-liquid and solid-liquid extraction, leaching, nuclear reactors, and spray drying. Although most of these operations involve multiparticle systems, due to simplicity, transfer from single spheres, droplets, etc., has received much attention.Transfer of mass (or heat) between a particle and a surrounding fluid phase can occur by three mechanisms: diffusion (or conduction), natural convection, and forced convection. These mechanisms may act individually or collectively. The actual nature of the combination and interaction of individual mechanisms is still largely unresolved; however, their role may be described by the conventional dimensionless groups used to correlate the overall mass (or heat) transfer rates, i.e., by A/Sh (or NNu) = f[NPe, /sc (or NPr), /VGr]