FREE BOOKS

Author's List




PREV.   NEXT  
|<   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   78   79   80   81   82   >>   >|  
lamp chimneys may be used for the experiment by tying the cloth over the tops; then invert them, fill them with soil and set in plates or pans. The sand will take the water in and let it run through quickly; the clay is very slow to take it in and let it run through; the humus soil takes the water in quite readily. Repeat the experiment with one of the soils, packing the soil tightly in one tube and leaving it loose in another. The water will be found to penetrate the loose soil more rapidly than the packed soil. We see then that the power of the soil to take in rainfall depends on its texture or the size and compactness of the particles. If the soil of our farm is largely clay, what happens to the rain that falls on it? The clay takes the water in so slowly that most of it runs off and is lost. Very likely it carries with it some of the surface soil which it has soaked and loosened, and thus leaves the farm washed and gullied. What can we do for our clay soils to help them to absorb the rain more rapidly? For immediate results we can plow them and keep them loose and open with the tillage tools. For more permanent results we may mix sand with them, but sand is not always to be obtained and is expensive to haul. The best method is to mix organic matter with them by plowing in stable manures, or woods soil, or decayed leaves, or by growing crops and turning them under. The organic matter not only loosens the soil but also adds plant food to it, and during its decay produces carbonic acid which helps to dissolve the mineral matter and make available the plant food that is in it. Clay soils can also be made loose and open by applying lime to them. =Experiment.=--Take two bottles or jars, put therein a few spoonsful of clay soil, fill with water, put a little lime in one of them, shake both and set them on the table. It will be noticed that the clay in the bottle containing lime settles in flakes or crumbs, and much faster than in the other bottle. In the same manner, lime applied to a field of clay has a tendency to collect the very fine particles of soil into flakes or crumbs and give it somewhat the open texture of a sandy soil. Lime is applied to soil for this purpose at the rate of twenty bushels per acre once in four or five years. Which soils have the greater power to absorb or pump moisture from below? =Experiment.=--Use the same or a similar set of tubes as in the experiment illustrated in Fig. 23. F
PREV.   NEXT  
|<   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   78   79   80   81   82   >>   >|  



Top keywords:
experiment
 

matter

 

flakes

 
particles
 

applied

 
texture
 

crumbs

 

leaves

 

organic

 

bottle


absorb

 
Experiment
 

results

 

rapidly

 

noticed

 

settles

 

chimneys

 

faster

 

spoonsful

 
applying

dissolve

 

mineral

 
packed
 

bottles

 

manner

 

moisture

 

greater

 
illustrated
 

similar

 
tendency

collect

 

bushels

 

twenty

 

purpose

 
produces
 

Repeat

 

soaked

 
loosened
 

packing

 

surface


carries

 
readily
 

penetrate

 

washed

 

gullied

 

leaving

 

largely

 

compactness

 

slowly

 

tightly