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  50 Department of Chemistry
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  L Bunnrrr COUNTY.
  l LABoRA·roRY No. 50025—Mineral water from a well 1600 ft. · -
  deep, bored at Lebanon Junction. Thought to be from the same  
  formation as the water of St. Patriek’s well, Louisville (Labora-  .2
  tory No. 36616). Probably from the calciferous formation.
  Sent by George D. Morrison, 924 South Third St., Louisville,
 ,‘ December 16, 1914. Sample contained some reddish brown, fer-
  ruginous sediment.
  Analysis gave 17.27 grams total solids, dried at 1000 C. I
  to the liter, equivalent to 1007 .3 grains to the gallon. Q
  = Qualitative tests showed very*1nuch chlorid, considerable
  sulfate, much calcium, considerable magnesium, a little iron and
  some calcium carbonate. . ‘
  ,  These tests indicate that the mineral matter is mainly sodium .
  chlorid with sulfates and chlorids of calcium and magnesium,  V
  some calcium carbonate and iron carbonate. ·
  The amount of total solids found is about the same as in —
 b y S the water of St. Patrick’s well and the qualitative tests show
  I a similarity in the character of the mineral matter. It should be  `
  just 3S gO0Cl as the St. Patrick’s water for drinking or bathing.  
  CHRISTIAN COUNTY.  
  L.xBoR.vro1zY No. 50703—Wate1· sent by D. C. Bell, Gracey,  
  from a well 60 ft. deep. Sample colorless with a little sediment.  V;
  Received November 16, 1915.  
  ANALYs1s——One gallon contains 29.0 grains of solid matter ’ 
  (.462 gram per liter) composed of calcium carbonate, sodium ' 
    chlorid, magnesium carbonate, a small amount of calcium sulfate,  
  distinct traces of iron, and traces of silica and potassium sulfate. A 
  omni; country  ;
  Laisoiuroizr No. 50661—Watcr sent by W. S. Duty & Co.,  ·
    \Vinchester. Sample colorless with very little sediment. Received ,1 
 it about October 27, 1915.  
  ANM·YSIS—One gallon contains 11.7 grains of Solid matter li 
  gl ( .20 gram per liter) composed mainly of calcium carbonate,  _~
  , . 
1*-;*