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   >>   >|  
Trial-holes. _b_ Clay-banks of lias or of boulder-clay. _c_ A more porous warp-drift filling furrows between the clay-banks.] "The next object is to connect these furrows by drains laid across them. The result is, that as the furrows and ridges here run along the fall of the ground, which I have observed to be the case generally elsewhere, the sub-mains follow the fall, and the parallel drains cross it obliquely. "The intervals between the parallel drains are irregular, varying, in the same field, from 14 to 21, 31, and 59 feet. The distances are determined by opening the diagonal drains at the greatest distance from the trial-holes at which experience has taught the practicability of its draining the hole. If it does not succeed in accomplishing the object, another drain is opened in the interval. It has been found, in many cases, that a drain crossing the clay-banks and furrows takes the water from holes lying lower down the hill; that is to say, it intercepts the water flowing to them through these subterranean channels. The parallel drains, however, are not invariably laid across the fall. The exceptions are on ground where the fall is very slight, in which case they are laid along the line of greatest descent. On such grounds there are few or no clay-banks and furrows." It would seem highly probable that the mode of drainage adopted at Keythorpe, is indebted for its success at that place, to a geological formation not often met with. At a public discussion in England, Mr. T. Scott, a gentleman of large experience in draining, stated that "he never, in his practice, had met with such a geological formation as was said to exist at Keythorpe, except in such large areas as to admit of their being drained in the usual _gridiron_ or parallel fashion." It is claimed for this system by its advocates, that it is far cheaper than any other, because drains are only laid in the places where, by careful examination beforehand, by opening pits, they are found to be necessary; and that is a great saving of expense, when compared with the system of laying the drains at equal distances and depths over the field. Against what is urged as the Keythorpe system, several allegations are brought. In the first place, that it is in fact _no system_. Mr. Denton, having carefully examined the Keythorpe e
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:

drains

 

furrows

 

Keythorpe

 

system

 

parallel

 

draining

 

experience

 

distances

 

opening

 
greatest

geological
 

formation

 

object

 
ground
 

stated

 

gentleman

 
carefully
 

practice

 
public
 

success


Against
 

indebted

 

drainage

 

adopted

 

depths

 

discussion

 

examined

 

laying

 

England

 

compared


probable

 

cheaper

 

advocates

 
allegations
 

examination

 

careful

 

places

 
brought
 

drained

 
expense

Denton
 
saving
 

claimed

 

fashion

 

gridiron

 

follow

 

obliquely

 

intervals

 
observed
 

generally