FREE BOOKS

Author's List




PREV.   NEXT  
|<   28   29   30   31   32   33   34   35   36   37   38   39   40   41   42   43   44   45   46   47   48   49   50   51   52  
53   54   55   56   57   58   59   60   61   62   63   64   65   66   67   68   69   70   71   72   73   74   75   76   77   >>   >|  
bstances are dissipated as gas by the decomposition bacteria, others are washed away in the drainage water. These losses are small in poor soils, but they become greater in rich soils, and they set a limit beyond which accumulation of material cannot go. Thus a virgin soil does not become indefinitely rich in nitrogenous and other organic compounds, but reaches an equilibrium level where the annual gains are offset by the annual losses so that no net change results. This equilibrium level depends on the composition of the soil, its position, the climate, etc, and it undergoes a change if any of these factors alter. But for practical purposes it may be regarded as fairly stationary. When, however, the virgin soil is broken up by the plough and brought into cultivation the native vegetation and the crop are alike removed, and therefore the sources of gain are considerably reduced. The losses, on the other hand, are much intensified. Rain water more readily penetrates, carrying dissolved substances with it: biochemical decompositions also proceed. In consequence the soil becomes poorer, and finally it is reduced to the same level as the rate of gain of nitrogenous matter. A new and lower equilibrium level is now reached about which the composition of the soil remains fairly constant; this is determined by the same factors as the first, _i. e._ the composition of the soil, climate, etc. Thus each soil may vary in composition and therefore in fertility between two limits: a higher limit if it is kept permanently covered with vegetation such as grass, and a lower limit if it is kept permanently under the plough. These limits are set by the nature of the soil and the climate, but the cultivator can attain any level he likes between them simply by changing his mode of husbandry. The lower equilibrium level is spoken of as the inherent fertility of the soil because it represents the part of the fertility due to the soil and its surroundings, whilst the level actually reached in any particular case is called its condition or "heart", the land being in "good heart "or "bad heart", according as the cultivator has pushed the actual level up or not; this part of the fertility is due to the cultivator's efforts. The difference between the hi
PREV.   NEXT  
|<   28   29   30   31   32   33   34   35   36   37   38   39   40   41   42   43   44   45   46   47   48   49   50   51   52  
53   54   55   56   57   58   59   60   61   62   63   64   65   66   67   68   69   70   71   72   73   74   75   76   77   >>   >|  



Top keywords:

fertility

 

equilibrium

 
composition
 

cultivator

 

losses

 

climate

 

annual

 

factors

 

limits

 

reduced


reached
 
permanently
 
plough
 

vegetation

 

fairly

 

change

 
virgin
 

nitrogenous

 

determined

 

pushed


represents
 

constant

 

remains

 

efforts

 

difference

 

poorer

 

finally

 

matter

 

actual

 

attain


called
 

simply

 

changing

 

nature

 

higher

 

inherent

 

surroundings

 

spoken

 

husbandry

 

condition


covered
 

whilst

 

offset

 

reaches

 

indefinitely

 
organic
 

compounds

 

depends

 

position

 

undergoes