414 



Journal of Agricultural Research 



Vol. X, No. 8 



Table XIII. — Change in the moistened layer of the ratio of the water content to the hygro- 

 scopic coefficient and the proportion of the total distance of penetration covered during 

 successive intervals following the application of i inch of water to the surface of the 

 soil columns — Continued 



SOIL M (hygroscopic C0EFFICIENT=3.3) 



