If Q is expressed in terms of this unit in equation (I), it is necessary to divide by c, or to replace k on the right-hand side by the ratio k/c. This ratio determines the rate of diffusion of temperature, and is called the thermometric conductivity or, more shortly, the **diffusivity**.

The velocity of propagation of temperature waves will be the same under similar conditions in two substances which possess the same **diffusivity**, although they may differ in conductivity.

No calorimetric observations are required, but the results are obtained in terms of the thermal capacity of unit volume c, and the measurements give the **diffusivity** klc, instead of the calorimetric conductivity k.

We thus obtain the simple equation k'(de'/dx') - k"(de"/dx") =c (area between curves)/(T - T'), (4) by means of which the average value of the **diffusivity** klc can be found for any convenient interval of time, at different seasons of the year, in different states of the soil.

For the particular soil in question it was found that the **diffusivity** varied enormously with the degree of moisture, falling as low as ooio C.G.S.