SOILS. I 



. \ xntuJy Awwi have- from <>7) to 00 por rout, ol' and 

 and 



"0. A sa ml y Mull contains no more than 10 percent, of 

 pure cla\ . 



''The mode of examining with the view of naming soils, 

 as above, is ver\ >imp!c. It !,- only necessary to spread a 

 weighed quantity of the soil in a thin layer upon writing 

 pap-.T, and, to dry il for an hour or two in an oven or upon a 

 hot plate, the heat of which is not sufficient to discolor tin- 

 paper tin; loss of weight gives the water it contained. 

 While this is drying, a second weighed portion may he 

 boiled or otherwise thoroughly incorporated with water, and 

 the whole then poured into a vessel, in which the heavy sandy 

 parts are allowed to subside until the fine clay is beginning 

 to settle also. This point, must be carefully watched, the 

 liquid then poured oft", the sand collected, dried as before 

 upon paper, and again weighed. This weight is the quan- 

 tity of sand in the known weight of moist, soil, which by the 

 previous experiment has been found to contain a certain 

 quantify of water. 



" Thus, suppose two portions, each 200 grs., are weighed, 

 and the one in the oven loses !">0 grs. of water, and the other 

 leaves (il) grs. of sand, then, the '200 grs. of moist are equal 

 to 150 of j/v/, and this 150 of dry soil contain 60 of sand, or 

 40 in 100 (40 per cent.). It would, therefore, be properly 

 called a loam, or Jnaniy soil. 



" But the above classification has reference only to the clay 

 and sand, while we know that lime is an important, constituent 

 of soils, of which thev are seldom entirely destitute. We 

 have, therefore, 



" 7". Marly so/7.v, in which the proportion of lime is more 

 than "> but docs not exceed 20 per cent, of the whole weight 

 of the dry soil. The marl is a sandy, loamy, or clay marl, 

 according as the proportion of clay it contains would place it 

 under the one or other denomination, supposing it to be 

 entirely free from lime, or not to contain more than 5 per 

 cent., and 



'* s". Calcareous soils, in which the lime exceeding 20 per 

 cent, becomes the distinguishing constituent. These are 

 also calcareous clays, calcareous loams, or calcareous sands, 

 according to the proportion of clay and sand which are 

 present in them. 



"The determination of the lime also, when it exceeds 5 

 per cent., is attended with no difficulty. 



