in Agricultural Chemistry. 



P 3.— SOILS (II.). 



553 



COMPOSITION PER CENT. 



Matter or Ash. 



Rain Water. 



Total Inorganic Matter. 



Abundantly. 



Sparingly, 



Sand and Silica. 













ron. 



si 













Magnesia 



Iron. 





Sulphuric 

 1 Acid. 



Carbonic 

 1 Acid. 



Silica. 1 



Lime. 



Magnesia- 



Sulphuric 

 Acid. 



Carbonic 

 Acid. 



Potash. 



Soda. 



Lime. 



1 



Magnesia. 



Alumina. 



Oxide of I 



o c 



0) til 



if 



Chloride c 

 Sodium. 



Phosphori 

 Acid. 



Sulphuric 

 Acid. 



"c 







i 





1 , 













1 



























salts 

 0'46 











0*02 



J 



? 



J 



p 



81-3 



0*22 



0*09 



1-33 



0'25 



3-0 



G'G8 





trace 



0-07 



0-08 



0-34 

















































salts 

 11'44 











0*08 



? 



? 



? 



p 



84-0 



0-20 



0-07 



1-23 



0-45 



2-4 



4-43 





trace 



1 



0-38 



0*05 



0*09 



salts 

 0'5'J 



salts 

 0-47 











0-33 





? 



p 



? 



83-6 



0-53 



0-13 



0*70 



0-23 



2-5 



5-18 









0-26 



0-15 



trace 













trace 



p 



? 





p 



81-0 



0-55 



trace 



0-85 



0-28 



3-9 



5-61 



_ 





_ 



0*21 



O'lO 



0-18 



salts 



salts 

 0*26 



salts 

 0*47 











— 















salts 

 0-b2 



salts 

 0*20 













1 ^ 



















? 



0-6 



with 

 salts 





0*5 



80*0 



0-6 



with 

 salts 



7-2 



6*0 





with salts 



JL 



COS 



with 



0*5 







— 







— 



? 



0'31 





- 



0*24 



1 78-5 



0-31 





6-5 



6-2 



- 



with salts 

 1 



0- 13 





0*24 























salts 

 0-47 



1*03 







6'3 



- 



with salts 



0*15 





0*81 



salts 

 0*20 







— 



— 



■ 



? 



0-6 



0-1 



- 



0-6 



90*5 



salts 

 0*20 



0-6 



0-1 



1-5 



2-0 





with salts 

 1 



trace 





0*6 



salts 

 0-14 





— 







? 



0-31 



trace 





0-24 



93-6 



salts 

 0-14 



0-31 



trace 



1-2 



1-2 



- 



with salts 

 1 



trace 





0*24 



salts 

 0-48 























































? 



0-28 



0-25 



_ 

 



0-49 



89-0 



sails 



0-28 



0-25 



1-4 



1-6 



- 



with 



salts 



trace 

 



" 



0*49 



- 







- 









- 







- 







p 



1-2G 



? 



0*09 



0-92 



81-3 



0-80 



1-50 



1-28 



1'12 



3-6 



3-4 





», 



trace 



0-38 



0-09 















? 



0-16 



? 



0-16 



0'04 



82-6 



0-60 



1-10 



0-69 





4-5 



3-7 





Chi. 



r2t) 



trace 



0*16 



0*04 







- 







? 



5'7 



0-3 





4-8 



63-1 







6-0 



0-3 



9-0 



6-2 





traces 



j 



0-19 





4*8 













trace 











78-1 



1-08 



0-73 



0-57 



0-43 



5*75 



6-24 









trace 



trace 



























salts 

 0-62 

























3-0 





3-4 





0-13 



0-28 



0*27 



0'2C 



0-41 



75-2 



0-28 



0-27 



0-80 



8-40 





with salts 



0-03 



3-6 



0*41 













? 



0-35 



trace 



0-26 



1 



0*13 j 



83-4 



salts 

 trace 



0*35 



trace 



2-6 



3-0 





trace 





0-26 



0*13 













? 



0-81 



trace 



0-08 



0-16 



88- 2 



sal 

 tra 



ts 

 :e 



0-Sl 



trace 



2-2 



5-1 





1 



trace 



~ 



0-08 



0*16 













0-17 



0'48 



? 





1 



0-38 



80-1 



0*13 



0-12 



0-48 



0-10 



1-2 



e-s 



1 



trace 





trace 



trace 





0*38 



bination or Hvdrate, and is not expelled bv boiling heat. This remark refers to all the other Analyses where water is 

 of Sulphate of Iron present in the soik rf. Called a ' diaf ' soil in Scotland, corrupted from ' dowf,' An-lice ' inert." ^ 



