ANALYSIS OF SOILS. 329 



quantity. If nnj- tiling, silica plnys a more important part in vegetation than any oilier 

 element, notwithstanding it is so inert to our senses. It exists, it is true, in greater pro- 

 portion in those parls of grain which are rarely consunu-d by man, as the straw of the 

 cereals ; \'et the seed, the part used l>y us as food, is perfected only when the silica of the 

 straw is in due proportion. Hence it may be, that, in many soils, ilie very want of soluble 

 silica is the only reason why the cereals arc not raised and cultivated successfully. If so, 

 it is at once suggested that here is a case to which Lieliig's manures woidd be specially 

 adapted. 



Silica is rendered soluble by the action of potash and the alkalies : if it is fused with 

 them, it becomes perfectly soluble in water. We may suppose, however, that the mere 

 addition of ashes to a soil wanting in soluble silica, would secure the attainment of the 

 object sought : they would dissolve, or, in other words, enter into combination with the 

 silica of the soil, and thus supply the great desideratmn. 



If we look carefully over the many analyses of grains and other vegetable products, we 

 can scarcely fail to be convinced that none of the elements which appear in the foregoing 

 analyses are unimportant : they are wanted by different vegetables in different proportions ; 

 but all are wanted, and all are consumed. It may be that the quantity in which some of 

 them appear is inconsiderable, and, to a superficial observer, sucli an element may not 

 appear to be essential ; but this opinion is inadmissible, and we are obliged to accede to the 

 view which maintains that a minute proportion of one element is as essential to the com- 

 position of a grain in its perfect state, as the more ample abundance of another. 



In making our analyses, the amount of potash and soda should have been determined 

 more frequently, had time permitted. It is true, many of the analyses might have been 

 omitted, and the process in the remaining instances carried to its ultimatum. In expla- 

 nation of our course of proceeding, it seemed quite desirable to increase the number even 

 of partial analyses. We had very clearly six districts, the character of whose soils were 

 to be determined ; and this required many analyses, carried at least so far as to determine 

 the amount of lime and magnesia, two great elements in the constitution of soils. Another 

 reason for the omission in regard to soda and potash, is that we were not fully convinced 

 of the utility of the analyses we were engaged in. A variety of opinions prevailed, and do 

 still prevail, in regard to this part of the work ; and hence in consequence of the doubt 

 which brooded over us, we did not commence in earnest at a period sufficiently early to 

 enable us to execute what we now wish ; and even now we shall not be disappointed if a 

 contrariety of opinion exists as to the usefulness of our work. Some valuable facts have 

 been elicited by the questionings we have put to the soils of the several districts ; and we 

 believe we have prepared the way for more, or for an advance in this inode of procedure. 



We lay more stress, however, upon the matter, v/hen applied to the soils of this State, 

 than when applied to those of New-England. The soils of tiiis State are far more uniform 

 in their composition ; and hence a single analysis is worth more, for the purpose of de- 

 termining what the soil is for a wide extent of territory, than elsewhere. This is quite 



[Agricultural Report.] 42 



