. ;;»—.. .
_ _A   p
Mineral Waters. U 599 4 l
  carbonate and traces of magnesium carbonate, silica, potas- . l
  sium and lithium. Q
`  It is a weak chalybeate water and should have some . _
  medicinal value. ‘ » ‘  
, LABORATORY No. 43300—Water sent by W. O. Tucker,   ·
  Marion, Ky. Sample contained a good dealof ferruginous ‘ Q c
  sediment. Received October 22, 1913.   ,  
  ANALYsIs——One gallon contains 160.9 grains of solid matter _   I ?i  
Y (2.768 grams per liter) composed of calcium sulfate, sodium   Q i
  chlorid, magnesium sulfate, calcium carbonate, a small   ’ ·  
2, quantity of ferrous carbonate and traces of_ silica, potassium   _‘
 i sulfate and lithium carbonate.   _ { [
  It is a saline, sulfated water such as is found in many deep ;· ‘}   J
3 wells. · i
  FAYETTE COUNTY.     K
  LABORATORY NO. 36991~Water brought by F. F. Wilson,  iQ!Y:j..
·. Lexington, Ky., from a bored well 57 feet deep, located   ....  
4 miles out on the Nicholasville pike. Sample very slightly gi,-Qii  A
  turbid with a slight whitish, flocculent sediment. Received  
  April 18, 1913.  j;
  ANALYsIs—One gallon contains 21.5 grains of solid matter  {1
- (.37 gram per liter) composed of sodium chlorid, calcium r1j;fg;,{’:*_i,.
J carbonate, magnesium carbonate, a small amount of calcium  
{ sulfate and traces of iron, silica, potassium, lithium and  
iT strontium. `Q ·    
  It contains very little more mineral matter than the  
¥ average well water of this region.  
  LABORATORY NO. 43199~Water from an old bored well 147 , 
I feet deep, on the property formerly owned by the Lexing-  
  ton Brick Company. Sample brought in August, 1913,  
  by Mr. Thos. Warren, Lexington. See 43261 for a later  
`* ‘ sample from this well.  
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