Abstract
The two-dimensional form of the equation of diffusionuχx=zAzχz(z>0),under steady mean conditions in a fluid moving with mean velocityuis discussed in the ease where u andAzvary aszmandz1-mrespectively (0 <m< 1). Integrals are constructed which satisfy boundary conditions of the types arising in physical problems, and the results are applied to the theory of evaporation into a turbulent atmosphere.

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