® T Mineral Waters. 549   p *
  and a small amount of sodium chlorid with traces of potas-   P
  - V sium sulfate and silica. ‘ li  ig [
  The water is strongly acid in reaction due to the aluminum ·  
and ferrous sulfatesi . " 9 L  ji;
_ This is the same water as No. 36653, sampled at a different  
  time and examinedby a different chemist. bij? .e’l’
ll V A WHITLEY COUNTY.  
  . Two samples ofmineral water sent by C. W. Denham,  
  Williamsburg, Ky., with letter of June 18, 1912. Samples in ;     i.‘,
  10-ounce bottles, byvmail. ‘  
  LABORATORY NO. 36618-Labeled "No. 1, from a well about  
  85 feet deep." Contains considerable red sediment.  
  ANALYs1s—One gallon contains 27. grains of solid matter   ..‘,,
  (.464 gram per liter) composed of sodium chlorid, ferrous  
carbonate and calcium sulfate with traces of magnesia and  
silica.   ";:f,$'f€{Q
This is a chalybeate water and should have some medicinal  
W value.  
  LABORATORY No.,36619-Labeled "No. 2 from a well about  
  60 feet deep.". Contains a little black sediment. No smell  
" of hydrogen sulfid when first opened. A  
  ANALYSIS*OH€ gallon contains 14.1 grains of solid matter Q  
  (.242 gram per liter) composed of small quantities of sodium  
  chlorid, ferrous carbonate, calcium sulfate and magnesia with  
  traces of potash and silica.  
  It is a weak chalybeate water.  
  WOODFORD COUNTY.  
l LABORATORY No. 36708—Mineral water brought September  
{ 19, 1912, by Joe Graddy, Versailles, Ky., from a well 142  
, feet deep, bored about 7 years ago, situated on the Lexing- .   
l ton and Frankfort pike about 5% miles west of Versailles.  
[ The well has been cleaned out and the sample was taken  
l fresh this morning with a sand pump. Sample turbid and    
.  
ix  
# a