174 University Geological Survey of Kansas. 
Council Grove Magnesium Well. 
This well ison the property of A.W. Simcock, four and one-half 
miles from the town of Council Grove and 100 yards from a 
running creek. It is twenty-five feet deep and ordinarily con- 
tains about eight feet of water. Council Grove is at the junc- 
tion of the M. K. & T. and Mo. Pac. railroads. The water has 
been used locally with considerable success. 
The partiai analysis is as follows: 
COUNCIL GROVE (PARTIAL ANALYSIS). 
Grams per liter. 
IONS. RADICALS. 
Sworn NIE). oo00 0006 DS ee L006 i Sodiumpoxids(Nas®) paneer .0082 
Oblate (CB). 6 000500000000000 .4375 | Calcium oxid (Ca®).......... . 6690 
Magnesium (Mg)............. .2931 | Magnesium oxid (MgO)....... .4890 
Proni(He)esewe ices Sane OMS | Ibo odie! (E@XOR). coco occb000e .0225 
Olakoyatin (OM)..6o0000vcncc0000n0 tracem | a©@hloriny (Clee trace 
Sulfuric acid ion (SOx)........ 2.3730 | Sulfuric anhydrid (SOs)....... 1.9775 
Silicic acid ion (SiOs)......... .1868 | Silicic anhydrid (SiOg)........ .1475 
Total! oss ks ee ee 3.3137 
Hypothetically combined as follows: 
Grams Grains 
per liter. per gallon. 
Sodium sulfate (NaoSO,)................ .0187 1.092 
Sodium chlorid (NaCl).............. eetrace trace 
Calcium sulfate (CaSO,)................ 1.6245 94.887 
Magnesium sulfate (MgSOu,)............. 1.4670 85.687 
Ferric sulfate (Feo(SO4)s)................ .0560 DorsUdl 
Silicat(Si@s\ tec. ee ee .1475 8.615 
Totalscet eect Oe EE Doousyy 193 .552 
Analysis by E. H. S. Bailey and H. P. Cady. 
