Page 196 - 1915, Springs of CA.
P. 196

180                  SPRINGS  OF  CALIFORNIA.

           as  containing  sulphureted-carbonated  springs.  The  twelfth  spring
           seeps  from, massive sandstone two-fifths of a mile up the ravine from
           the hotel.  Iron-stained lime  carbonate is dpposited by it on the rock
           face  and  indicates  that  the  spring  is  similar  in  chemical  character
           to the springs of  the main group.
             The following analyses of  four springs  at  Saratoga show the water
           to be primary and secondary alkaline.  The prominence of magnesium
           is  an interesting chemical  feature  of  the water.
                     Analyses of water from Saratoga Springs,  Lake  County,  Col.
            [Analyst, Selby Smelting Co.  Authority, advertising matter.  Constituents are in parts per million.]

                                   1          2          3           4
           Properties of reaction:
                                       3           3          3           2
                                       0           0          0           0
                                       0           0          0           0
                                       11          7         11          12
              SecoHdary alkalinity. ....   86     90         86          86
              Tertiary alkalinity ......  117    120         147         166
                                    React-     React-      React-     React-
                               By          By         By          By
                Constituents.  weight.  ing   weight.  ing   weight.  ing   weight.  ing
                                    values.    values.     values.    values.
           Sodium (Na).. . ..............  180  7.84  113  4.90  Ill  4.83  75  3.27
                                 5.1  .13   4.3  .11    3.0  .08   3.3   .08
           Calcium (Ca).. . ..............  270  13.48  216  10.78  147  7.34  117  5.86
                                458  37.68  421  34.63  291  23.54  180  14.82
           Iron(Fe)... .................  5.8  .21  5.1  .18  3.6  .13  3.6  .13
                                 2.7  .30   2.8  .31    2.0  .22   1.6   .18
           Sulphate (SO<). ..............      Trace.   4.1  .09   5.3   .11
           Chloride (Cl)...... ...........  55  1.54  47  1.33  28  .79  16  .45
           Carbonate (CO3) .............  1,734  57.80  1,478  49.27  1,063  35.44  708  23.60
           Silica (SiOs)... ...............  105  3.48  101  3.34  93  3.10  84  2.79
                              2,815.6     2,388.2    1,745.7     1,193.8
           Carbon dioxide (CO2) ........  1,439  65.40  1,250  56.80  1,101  50.00  812  36.91
            1,2, 3, 4.  Separate springs, names not given.
             CARBONATED  SPRING  NEAR  NORTHWEST  EDGE  OF  CLEAR  LAKE
                                      (LAKE  21).
             About 3  miles south of the town of Upper Lake a small carbonated
           spring rises  in the  alluvium near the  lake  edge,  but it has  not  been
           improved and is little used.  It forms a small, iron-stained pool that
           may be occasionally visited by a hunter or fisherman.
                   CARBONATED  WELL  NEAR  TIPPER  LAKE  (LAKE  19).
             In  connection  with  the  existence  of  the  carbonated  spring  just
           described,  two  flowing  wells  in  the  locality,  which  yield  noticeably
           carbonated water, may be mentioned.  One of these is near the north-
           ernmost extension of Clear Lake, north of the carbonated spring,  and
           is one-half mile south of  the  town of Upper Lake.  It is situated on
           the Taylor place,  is 2| inches in diameter,  and was sunk about  1905
           to  a depth of  108  feet.  In 1910  it yielded  about 5  gallons  a minute
           of  cool,  slightly  carbonated  water.  It was  used  only  for  domestic
           purposes.
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