154 ROOTS 



that it can not be driven off except by the application^ heat. 

 The driest of "air dry" soils still contain considerable hygroscopic 

 water, as shown by their loss in weight when they are further 

 dried in an oven. 



Plants depend mainly upon capillary water, although in some 

 cases, especially in soils with high hygroscopic power, some hygro- 

 scopic water may be available to the plant. When soils are satu- 

 rated, as after heavy rains or in bogs and swamps, there is more 

 water present than the plant needs, and, besides, the air which 

 roots must have is driven from the soil pores. Experiments have 

 shown that, in general, a soil is best adapted to plant growth 

 when the water present is not more than 60 per cent of the amount 

 required for saturation, or, in other words, when about two-fifths 

 of the pores are open for the circulation of air. 



The forces which resist the pulling away of hygroscopic and 

 capillary water from the soil particles tend to keep the water 

 equally distributed. Thus as water is lost from the pores in the 

 surface soil, either by evaporation or root absorption, it is replaced 

 by water moving up from below through the force of capillarity. 

 Consequently, as a root absorbs, the movement of water toward 

 it from all around enables it to obtain water from regions several 

 feet away. In fact, capillarity has been known to raise water to 

 a height of 10 feet in one kind of soil. Again, in hygroscopic 

 water the thin films, which are like stretched rubber around the 

 soil particles, are connected where the soil particles touch, agd to 

 compensate the greater water loss one film may have over others, 

 there is such a movement of water between the films that all for 

 a considerable distance around share in the loss. Thus, due to 

 the forces of capillarity and the surface tension of hygroscopic 

 films, soil water tends to move to the point where it is being 

 absorbed. It is now clear why the soil becomes so evenly dry 

 around a plant. 



Air in the soil is necessary for the respiration of roots and 

 micro-organisms. It is also of use in oxidizing poisonous sub- 

 stances which result from the decay of organic matter in the soil, 

 so that their poisonous effects on roots are destroyed. 



Humus consists of organic matter in a state of decomposition. 

 When only partially decayed as in some bogs where it accumu- 

 lates in large quantities, it forms peat. It gives to soils the dark 

 color which is characteristic of good soils, such as loams where it 



