FREE BOOKS

Author's List




PREV.   NEXT  
|<   90   91   92   93   94   95   96   97   98   99   100   101   102   103   104   105   106   107   108   109   110   111   112   113   114  
115   116   117   118   119   120   121   122   123   124   125   126   127   128   129   130   131   132   133   134   135   136   137   138   139   >>   >|  
nts of sand, silt, clay and humus contained in the soil. The power of admitting a free circulation of air through its pores is also an important property of a fertile soil, for air is necessary to the life and growth of the roots. This property is dependent also on texture. Two other important properties of a fertile soil are power to absorb and power to hold heat. These depend upon the power of the soil to take in warm rain and warm air, and also upon density and color. The denser or more compact soil and the darker soil having greater power to absorb heat. The compactness of the soil which gives it greater powers to absorb heat weakens its powers to hold it, because the compactness allows more rapid conduction of heat to the surface, where it is lost by radiation. The more moisture a soil holds, the weaker is its heat-holding power, because the heat is used in warming and evaporating water from the surface of the soil. These important properties or conditions of moisture, heat and air, are, as we have seen, dependent on soil texture and color, which in turn are dependent upon the relative amounts of sand, clay and humus in the soil. We are able to control soil texture and therefore these physical properties to a certain degree by means of tillage and the addition of organic matter or humus (see Chapter IV). BIOLOGICAL PROPERTIES OF A FERTILE SOIL Biology is the story or science of life; and the biological properties of the soil have to do with living organisms in the soil. The soil of every fertile field is full of very small or microscopic plants called bacteria or germs. They are said to be microscopic because they are so small that they cannot be seen without the aid of a powerful magnifying glass or microscope. They are so small that it would take about 10,000 average-sized soil bacteria or soil germs placed side by side to measure one inch. A knowledge of three classes of these soil germs is of great importance to the farmer. These three classes of germs are: Nitrogen-fixing germs. Nitrifying germs. Denitrifying germs. NITROGEN-FIXING GERMS We learned in Chapter VIII that nitrogen is one of the necessary elements of plant food, and that although the air is four-fifths nitrogen, most plants must take their nitrogen from the soil. There is, however, a class of plants called legumes which can use the nitrogen of the air. Clover, alfalfa, lucern, cowpea, soy bean, snap bean, vet
PREV.   NEXT  
|<   90   91   92   93   94   95   96   97   98   99   100   101   102   103   104   105   106   107   108   109   110   111   112   113   114  
115   116   117   118   119   120   121   122   123   124   125   126   127   128   129   130   131   132   133   134   135   136   137   138   139   >>   >|  



Top keywords:
properties
 

nitrogen

 

plants

 
texture
 
dependent
 
fertile
 

absorb

 

important

 

compactness

 

surface


moisture
 
powers
 

bacteria

 

classes

 

Chapter

 

microscopic

 

greater

 

called

 

property

 

average


admitting
 

knowledge

 

contained

 
measure
 

circulation

 
importance
 
microscope
 

powerful

 

magnifying

 

Nitrifying


legumes

 

Clover

 
alfalfa
 
lucern
 

cowpea

 
FIXING
 

NITROGEN

 

Denitrifying

 

Nitrogen

 

fixing


learned

 

fifths

 
elements
 

farmer

 
growth
 
depend
 

conditions

 

evaporating

 
warming
 

control