If you will take a number of glass tubes of different sizes, the largest not more than one-fourth of an inch in diameter, and hold them with one end of each in water or some colored liquid, you will notice that the water rises in the tubes (Fig. 26), and that it rises highest in the smallest tube.  The force which causes the water to rise in these tubes is called the capillary force, from the old Latin word capillum (a hair), because it is most marked in hair-like tubes, the smaller the tube the higher the water will rise.  The water which rises in the tubes is called capillary water.

Another method of illustrating capillary water is to tie or hold together two flat pieces of glass, keeping two of the edges close together and separating the opposite two about one-eighth of an inch with a sliver of wood.  Then set them in a plate of water or colored liquid and notice how the water rises between the pieces of glass, rising higher the smaller the space (Fig. 27).  It is the capillary force which causes water to rise in a piece of cloth or paper dipped in water.

Take a plate and pour onto it a cone-shaped pile of dry sand or fine soil; then pour water around the base of the pile and note how the water is drawn up into the soil by capillary force (Fig. 28).

Capillary water is the other important form of water in the soil.  This is moisture which is drawn by capillary force or soaks into the spaces between the soil particles and covers each particle with a thin film of moisture.

FILM WATER

Take a marble or a pebble, dip it into water and notice the thin layer or film of water that clings to it.  This is a form of capillary water and is sometimes called film water or film moisture.  Take a handful of soil that is moist but not wet, notice that it does not wet the hand, and yet there is moisture all through it; each particle is covered with a very thin film of water.

Now this film water is just the form of water that can supply the very slender root hairs without drowning them, that is, without keeping the air from them.  And the plant grower should see to it that the roots of his plants are well supplied with film water and are not drowned by the presence of free water.  Capillary water may sometimes completely fill the spaces between the soil particles; when this occurs the roots are drowned just as in the case of free water as we saw when cuttings were placed in the puddled clay (see Fig. 18).  Free water is indirectly of use to the plant because it serves as a supply for capillary and film moisture.