Full text: The Elements of economic geology

200 ECONOMIC GEOLOGY 
indispensable for high explosives most nations will probably 
manufacture them, so as to be independent of an imported 
supply. 
PuospuATES 1 
VaLuE anD Use oF ProspaaTes—Phosphate of lime is a 
much scarcer mineral than carbonate of lime; it is of high 
importance as a fertilizer, being especially useful in the 
growth of grain, Burnt bones had long been used in China 
as manure, and their value is explained by Gahn's dis- 
covery in 1769 that bones contain phosphorous; but as bone 
phosphate is insoluble the fertilizing effect of bones was 
attributed to their gelatine, until in 1843 experiments by 
the Duke of Richmond showed that ground bones with and 
without their gelatine were equal in fertilizing value. Normal 
phosphate of lime (CayP,0q) is insoluble; but it was dis- 
covered by Lawes in England and by Liebig in Germany, 
that the action of sulphuric acid on bones and mineral phos- 
phate converts them into superphosphate or acid phosphate 
(CaH4(POy2, H,0) which is soluble and usable as plant 
food. The exhaustion of many wheat fields in North-western 
Europe about that date led to fears of famine. Beds of 
phosphatic nodules occur in the S.E. of England, and their 
conversion into superphosphate rendered them available 
for the refertilization of the European grain-fields. Emerson, 
the American philosopher, suggested that spendthrift agri- 
culture might be saved by agricultural chemistry * offering 
by a teaspoonful of artificial guano to turn a sandbank into 
corn; while Liebig, with generous enthusiasm, declared 
that England had in its mineral phosphates, a source of 
wealth equal to its coal-fields. The supply of English phos- 
phate was disappointingly small, and the industry became 
dependent upon imports from warm temperate and tropical 
cegions. 
The commercial phosphates are due to the concentration 
of phosphoric acid by various processes (Fig. 53). 
The primary source of the phosphorus is the apatite in 
igneous rocks. It is a tricalcic phosphate of lime (Ca,P,04), 
LA general account of the geology of phosphates has been given by 
che author, 77. G. Soc. Glasgow, xvi, 1917, pp. 116-63.
	        
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