I. ANALYSES OF FERTILIZERS— FALL SEASON, 1911. 



Bx B. W. KILGORE, 

 W. G. HAYWOOD, J. M. PICKEL, J. Q. JACKSON and W. H. STROWD. 



The analyses presented in this Bulletin are of samples collected by 

 the fertilizer inspectors of the Department, under the direction of the 

 Commissioner of Agriculture, during the fall months of 1911. They 

 should receive the careful study of every farmer in the State vs^ho uses 

 fertilizers, as by comparing the analyses in the Bulletin with the 

 claims made for the fertilizers actually used, the farmer can know by 

 or before the time fertilizers are put in the ground whether or not they . 

 contain the fertilizing constituents in the amounts they were claimed to 

 be present. 



^ TERMS USED IN ANALYSES. 



Water-soluhle Phosphoric Acid. — Phosphate rock, as dug from the 

 mines, mainly in South Carolina, Florida, and Tennessee, is the chief 

 source of phosphoric acid in fertilizers. 



In its raw, or natural state, the phosphate has three parts of lime 

 united to the phosphoric acid (called by chemists tri-calcium phosphate). 

 This is very insoluble in water and is not in condition to be taken up 

 readily by plants. In order to render it soluble in water and fit for 

 plant food, the rock is finely ground and treated with sulphuric acid, 

 which acts upon it in such a way as to take from the three-lime phos- 

 phate two parts of its lime, thus leaving only one part of lime united 

 to the phosphoric acid. This one-lime phosphate is what is known as 

 water-soluble phosphoric acid. 



Reverted Phosphoric Acid. — On long standing some of this water- 

 soluble phosphoric acid has a tendency to take lime from other sub- 

 stances in contact with it, and to become somewhat less soluble. This 

 latter is known as reverted or gone-back phosphoric acid. This is 

 thought to contain two parts of lime in combination with the phos- 

 phoric acid, and is thus an intermediate product between water-soluble 

 and the original rock. 



Water-soluble phosphoric acid is considered somewhat more valuable 

 than reverted, because it becomes better distributed in the soil as a con- 

 sequence of its solubility in water. 



Available Phosphoric Acid is made up of the water-soluble and re- 

 verted ; it is the sum of these two. 



Water-soliihle Ammonia. — The main materials furnishing ammonia 

 in fertilizers are nitrate of soda, sulphate of ammonia, cotton-seed meal, 

 dried blood, tankage, and fish scrap. The first two of these (nitrate 

 of soda and sulphate of ammonia) are easily soluble in water and be- 

 come well distributed in the soil where plant roots can get at them. 



