THE SOIL 85 



(a) The amount of water entering the soil ; 

 (&) The character of the water ; and 

 (c) The power of the soil to retain it. 



(a) The Amount o! Water entering the Soil depends 

 upon — 



1. The amount of water received from above — i.e., 

 upon the rainfall, and upon the percolation of water from 

 rivers and lakes, springs, and adjacent sheets of water. 



2. The amount of water sucked up from below. This 

 depends upon the size of soil-particles, the presence or 

 absence of ground-water, and its depth below the surface 

 of the soU during the vegetative season. 



(6) The Availability of this Water to Plants depends, as 

 we have already shown, upon its chemical nature. The 

 roots of plants can only absorb very weak alkaline solu- 

 tions. For this reason, if the proportion of material in 

 solution in the water is greater than a certain smaU amount 

 (1 to 3 per cent.), or if souring acids be present, the soil, 

 though it may be physically wet, is physiologically dry, 

 and little water is absorbed. The soil also must be well 

 aerated, otherwise the water present is useless. 



(c) The Amount of Water retained by the Soil depends 

 upon its physical properties, and the physical properties 

 are all directly or indirectly coimected with the size of 

 the particles formiag the soil. 



The Physical Properties of the Soil, and their Relations 

 to Water. — ^The rock-fragments forming the soil vary in 

 size from large stones to an impalpable dust, which, when 

 dry, remains for a long time suspended in water, and 

 which, when wet, becomes compacted into a greasy, heavy 

 clay. The particles, however, touch one another at a 

 few points only, leaving between them pores, or spaces, 

 which are normally filled with water and air. In ordinary 

 soils the water forms a fihn of varying thickness round 

 the particles, air occupying the rest of the pore-space. 

 As the particles are in contact, the water-films surround- 

 ing them are everywhere in continuity with one another. 

 These films are elastic, and the withdrawal of water at 

 any point sets up a flow of water along the adjacent 

 films untU equilibrium is restored. If a section of some 

 coarse-grained soil containing water be examined, it wUl 

 be seen that the water-films increase in thickness as we 



