FREE BOOKS

Author's List




PREV.   NEXT  
|<   69   70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   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   >>   >|  
re A represents the surface-soil; B, the impervious subsoil of clay; C, the bed of sandy-clay or gravel; and D, the lower bed of clay, resting upon the rocky strata beneath. [Illustration: Fig. 10.] "Springs sometimes communicate with lakes or pools, at higher levels. In such cases, the quantity of water discharged is generally so great, as to form at once a brook or stream of some magnitude. These, therefore, hardly come under the ordinary cognizance of the land-drainer, and are, therefore, here merely referred to." THE WATER OF PRESSURE. Water that issues from the land, either constantly, periodically, or even intermittently, may, perhaps, be properly termed a _spring_. But there is often much water in the soil which did not fall in rain upon that particular field, and which does not issue from it in any defined stream, but which is slowly passing through it by percolation from a higher source, to ooze out into some stream, or to pass off by evaporation; or, perhaps, farther on, to fall into crevices in the soil, and eventually form springs. As we find it in our field, it is neither rain-water, which has there fallen, nor spring-water, in any sense. It has been appropriately termed the _water of pressure_, to distinguish it from both rain and spring-water; and the recognition of this term will certainly be found convenient to all who are engaged in the discussion of drainage. The distinction is important in a legal point of view, as relating to the right of the land-owner to divert the sources of supply to mill-streams, or to adjacent lower lands. It often happens that an owner of land on a slope may desire to drain his field, while the adjacent owner below, may not only refuse to join in the drainage, but may believe that he derives an advantage from the surface-washing or the percolation from his higher neighbor. He may believe that, by deep drainage above, his land will be dried up and rendered worthless; or, he may desire to collect the water which thus percolates, into his land, and use it for irrigation, or for a water-ram, or for the supply of his barn-yard. May the upper owner legally proceed with the drainage of his own land, if he thus interfere with the interests of the man below? Again: wherever drains have been opened, we already hear complaints of their effects upon wells. In our good town of Exeter, there seems to be a general impression on one
PREV.   NEXT  
|<   69   70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   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   >>   >|  



Top keywords:
drainage
 

stream

 

spring

 
higher
 

adjacent

 
termed
 

surface

 

desire

 

supply

 

percolation


relating

 
streams
 

engaged

 

divert

 

important

 

discussion

 

distinction

 

sources

 

convenient

 
drains

opened

 

interests

 
proceed
 

interfere

 

Exeter

 

general

 

impression

 
complaints
 

effects

 
legally

neighbor

 

washing

 

advantage

 

derives

 
refuse
 

irrigation

 

rendered

 
worthless
 

collect

 

percolates


generally

 
discharged
 

quantity

 

levels

 

magnitude

 

cognizance

 

drainer

 

ordinary

 

subsoil

 

gravel