. 1
Mineral lVaters 63 p  
zmd magnesium carbonate and traces of iron, silica and potassium I `
_ sulfate. -  
m` It is strongly- alkaline, due to the sodium carbonate pres-  
m` ent, It would be classed as an alkaline saline water and should  
A 1 · have some medicinal value. p  
  _ Lanonarony No. 50300-No. 2. From a well 50 ft. deep on  
gu railroad station platform. Sample clear and colorless.  
fg ANi\IiYSIS——O]1€ gallon contains 36.7 grains of solid matter  
lr- I A (.629 gram per- liter) composed of calcium sulfate, calcium car-  
bonate, magnesium carbonate, a small amount of· sodium chlorid aa
_ _ and traces of iron and silica.  
W6 X The analysis indicates an ordinary well water. }·j;i
. LIVINGSTON COUNTY.  
th, - Linonxrour No. G 3G76—}.Iineral water from a well SO ft. p  
Of deep in Livingston County, sent by J. I3. Iloeing. State Geolo—  
DIC gist, l)e<·einber 21, ltllel. Sample clear and colorless.  
ut. ) AN.\LYSlS—Tl1C water contains 0265 gram total solids per  
liter, equivalent to 15.5 grains per gallon, composed of calcium  
mi carbonate. calcium sulfate, sodium clilorid, magnesium sulfate  
Vid and a little iron.  
lm It is a weak clialybeale water. the amount of mineral matter  
Im ‘· present being only about as much as is usual in spring and well  
Ht, waters of a limestone region.   `
 Pit
l j
ble p LOGAN COUNTY.  
· Iiixnonyronv No. 50573»~\Vell water sent by Dr. Jesse L.  
Russell, Adairville. Sample clear and colorless. Received Aug.  
15, 1915. » ,  
20, . AN.\li\'SlS—OllC gallon contains 117.5 grains of solid matter  
(2.014 grams per liter) composed of calcium sulfate and mag- A  
at Ilesium sulfate, small quantities of calcium carbonate, magnesium  
1 Carbonate and sodium ehlorid, with traces of iron, silica and   ·
ter 5 potassium sulfate.  
,nd   It would be classed as a magnesian water and would doubt-  
ate _. less have a laxative effect.  
= .i.