338 HOW CKOPS GEOW. 



monia-salts gathered by the roots, is united to carbon, hy- 

 drogen, and oxygen, in the formation of albuminoids. 



Besides sugar, malic acid and minute quantities of al- 

 bumin exist in maple sap. Towards the close of the 

 sugar-season the sap appears to contain other organic sub- 

 stances which render the sugar impure, brown in color, 

 and of different flavor. 



It is a matter of observation that maple-sugar is whiter, 

 purer, and " grains " or crystallizes more readily in those 

 years when Sf)ring-rains or thaws are least frequent. This 

 fact would appear to indicate that the brown organic 

 matters which water extracts from leaf-mould may enter 

 the roots of the trees, as is the belief of practical men. 



The spring-sap of many other deciduous trees of tem- 

 perate climates contains sugar, but while it is cane sugar 

 ia the maple, in other trees it consists mostly or entirely 

 of grape sugar. 



Sugar is the chief organic ingredient in the juice of the 

 sugar cane, Indian corn, beet, carrot, turnip, and parsnip. 



The sap that flows from the viae and from many culti- 

 vated herbaceous plants contains little or no sugar; in 

 that of the vine, gum or dextrin is found in its stead. 



What has already been stated makes evident that we 

 cannot infer the quantity of sap in a plant from what may 

 run owt of an incision, for the sap that thus issues is for 

 the most part water forced uj) from the soil. It is equally 

 plain that the sap, thus collected, has not the normal 

 composition of the juices of the plant; it must be diluted, 

 and must be the more diluted the longer and the more rap- 

 idly it flows. 



Ulbricht has made partial analyses of the sap obtained 

 from the stumps of jjotatq, tobacco and sun-flower plants. 

 He found that successive portions, collected separately, 

 exhibited a decreasing concentration. In sunflower sap, 

 gathered in five successive portions, the liter contai)ied 

 the following quantities (grams) of solid matter : 



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