62 The Sugar-Beet in America 



and thawing, (4) alternate wetting and drying, (5) or- 

 ganic matter, (6) soluble salts, (7) animal life, and (8) 

 storms. The tilth of the soil is the result of a combined 

 action of a number of these factors, all of which improve 

 it, except certain kinds of storms and certain soluble salts 

 like sodium carbonate. 



AIR IN THE SOIL 



Oxj'gen is as necessary for the growth of plants as it is 

 for that of animals. It is, therefore, impossible to have a 

 fertile soil unless there are spaces through which air can 

 circulate. Seeds in germinating, and roots in growing, 

 require oxj^gen which is absorbed while carbon dioxid is 

 given off. The decay of organic matter uses oxygen 

 and forms carbon dioxid which accumulates in the soil 

 air. If conditions in the soil do not favor a free move- 

 ment of air, the oxygen supply soon becomes reduced to 

 a point at which plant growth is retarded. The aeration 

 of the soil is dependent on texture, structure, drainage, 

 and a number of other factors. In a coarse sand, air 

 moves readily, but in a clay, especially if it is compact, 

 the movement is slow. Puddling greatly reduces aeration, 

 whereas flocculating the soil particles into groups pro- 

 motes the ready movement of air. 



A water-logged soil, on accoimt of the lack of oxj-gen, 

 usually has a low crop-producing power. A free circu- 

 lation of air, resulting from placing drains under such a 

 soil, is in part responsible for the increased yields that 

 follow drainage. The beneficial nitrifying and nitrogen- 

 fixing bacteria require an abundant supply of oxygen for 



