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. ~ _ yi 276 (7/iemical Analyses
»`   V\lARR]C*N COUNTY.
  T 17264——Sulphur water from a well at»Hays, Ky., sent by Hons- g,
Z   T ton Bishop, November, 1906.
0   r` if AN.~iLYs1s. "
1 . . . . * TG
. ‘· , One gallon contains 118.7 grains of solid matter (2.036 L Is?
·}. ‘ ‘ grams per liter), composed of sodium chloride, calcium carbon— i CI
. . ate, calcium sulphate, magnesium chloride, sodium sulphide and   Tc
K .j potassium chloride, with traces of iron carbonate, lithium ear- S $6
; V bonate and silica. The total amount of hydrogen sulphide is   C
'     5.34 grains in the gallon (.092 gram per liter), including that { im
V , of the sodium sulphide; ‘  ._
‘ . . t P1
i M g · It is a strong alkaline sulphur water. ,
T   · wniirrnr eounrr. » ’ ‘  GY
T 1 I, 14896—lVater f1·o1n a well 166 feet deep in the town of \Vill—   ha
; , 1 · _ iamsburg, Ky., in a bottom, close to the Oumberland · M
  river. The well is cased to exclude surface water, and g GD
l i _ the water stands in it at 30 feet below the surface of the
ground. The water is thought to resemble that of Ma-  g.
, han Spring, at Waiford. Sample sent by lVilliam Per- _‘—` M
A ,· kins, Williamsburg, Ky. The bottle contained a slight,  
l i reddish sediment. _ `  
pg l Axiuxsis.  ~
_ One gallon contains 1313 grains of solid inatter (0.334 grams j 
per liter), composed of sodium chloride, calcium carbonate, a  
little. magnesium chloride, calcium sulphate, potassium chloride,  
t sodium bromide, iron carbonate and silica and a trace of lithium  
1 carbonate.  
. It is a weak saline chalybeate. 4 .  ;;
. A l WOLFIS COUNTY. V ;  PE
_ lT225—eOhalybeate water` from Swango Springs, Hazel Green, _  m
Ky., sent by Prof. llleury Lloyd, October 1, 1006. -.  ll?
_ Sample from a carboy of the water received by Prof.   (ll
1 liloyd, September   The water of Swango Springs  A bf
, was analyzed in 1003. See Sixteenth Animal Report,   hi
p. 300, No. 11150. Several determinations made on  
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