EXPBRIMKNTS ON (LOVER-SOILS. 155 



First Sirtwif Third 

 sixinclus. six iiiclus. six inches. 



lbs. Il>s. lbs. 



Phosphoric arid S/JT") 4,15() 3,500 



Nitrogen 4,725 3.;J.'>0 2:125 



Kqual to ariimoiiia 5,?^ 4,a5(< 2,700 



" Here, again, as migLit naturally be expected, the proportion of 

 nitrogen is largest in the surface, where all the decaying leaves 

 driipped during llie growth of the clover for seed are found, and 

 wherein root-tihres are more abundant than in the lower strata. 

 TIjc hrst six inches of soil, it will be seen, contained in round 

 nunibirs, 2i tons of nitrogen per acre, that is, considerably more 

 tiuin was found in the same section of the soil where the clover 

 was mown twice for hay ; showing plainly, that during the ripening 

 of the clover seid, the surface is niucii enriched Ijy the nitrogen- 

 ous matter in the dropping h-aves of the i^lover-plant. 



" Clover-roots. — The roots from one square foot of this soil, freed 

 as much as possible from adhering soil, were dried at 212', and 

 when weighed and rcchiceil to a line powder, gave, on analysis, the 

 following results: 



Oganic matter* 64.76 



Mineral matterf _ 35.24 



100.6(3 



•Containing nitrogen 1.702 



Equal to ammonia 2.066 



t Including clay and sand (insoluble silicious matter) 26.04 



*' A .square foot of this soil jiroduced 582 grains of dried clover- 

 roots, consequently- an acre yielded 3,622 lbs. of roots, or more 

 than twice the weight of roots ol)tain(Hl from the soil of the same 

 field where the clover was twice mown for hay. 



" In round numbers, the 3,622 lbs. of clover-roots from the land 

 mown once, and afterwards left for seed, contained 51^ lbs. of 

 nitrogen. 



" The roots from the soil after clover-seed, it will be noticed, 

 were not so clean as the preceding sample, nevertheless, they 

 jielded more nitrogen. In 64.76 of organic matter, we have here 

 1.702 of nitrogen, whereas, in the case of the roots from the part 

 of the field where the clover was twice mown for hay, we have in 

 81.33 parts, that is, much m-^re organic matter, and 1.635, or rather 

 less of nitrogen. It is evident, therefore, that the organic matter 

 in the soil after clover seed, occurs in a more advanced stage of 

 decomposition, than found in the clover-roots from the part of the 

 field twice mown. In the manure, in which the decay of such 

 and similar organic remains proceeds, much of the non-nitrogen- 

 ous, or carbonaceous matters, of which these remains chiefly, 



