THE MINERAL SPRINGS OF SARATOGA 



37 



When statistics are prepared of these analyses, the following 



results become apparent. There are 66 analyses : 



^Maximum Minimum 



NaCl 87. 21.2 



Ca(HC03)2 40.6 1.4 



MgCHCOg)^ 27.9 2.3 



NaHCOg 67.3 .6 



KCl II. 2 .4 



GsxE R.A L Range 

 45-60 



15-30 

 5-20 



1-15 

 1-5 



IIQ. 



USl 



chA nd l.e r 



SER 



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arts p =r M 



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IT) 



TZ 



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OO 



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lio 



VP 



^C^ 



0^ 



:o? 



^y 



01 



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^y 



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r& 



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Figure 6 Diagrams of the rarer ions on an exaggerated scale as compared with figure S 



The extremely high values of NaCl are probably due to artificial 

 strengthening. The minimum is due to the artificial addition of 

 NaHCOg, which relatively decreased the NaCl. NaCl above 60 per 

 cent is an object of suspicion. The maximum, 40.6 of Ca(HC03)o 

 is from a recent analysis of the High Rock. The next value is 40.4. 

 of the Red spring. Then follow, 40.3 of the Magnetic and 38.6 of 

 the Flat rock. All these have low total grains in the gallon, l>eing 

 respectively 129.4, 249.3, 214.7, and 253.8. All are from springs in 



