File:The mineral content of Illinois waters.. (1909) (14760799226).jpg

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Identifier: mineralcontentof00bart (find matches)
Title: The mineral content of Illinois waters..
Year: 1909 (1900s)
Authors: Bartow, Edward, 1870-1958
Subjects:
Publisher: (n.p.)
Contributing Library: The Library of Congress
Digitizing Sponsor: The Library of Congress

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sure to the air, should not exceed 0.02 parts per million and 0.05parts per million respectively. Nitrogen as Nitrites.—Xitrogen as nitrites should be absent. Nitrogen as Nitrates.—Nitrogen as nitrates should not exceed 2.0parts per million. Alkalinity.—Alkalinity may vary from 150 to 500 parts per million.It should not exceed 300 parts per million. ^Yaiers from Shallow Wells in the Drift. These waters should be clear without color or odor. Residue on Evaporation.—The total residue on evaporation variesfrom 160.5 parts per million, (9.36 grains per gallon) in a well at Poag,to 5331.27 parts per million, (311 grains per gallon) in a well at CrealSprings. The residue should not exceed 500 parts per million. Chlorine.—Chlorine varies from .3 parts per million in a well at Pana,to 310 parts per million in a well at Bloomington. The majority ofthe waters reported are below 15 parts per million, an amount thatshould not l)e exceeded. STATE GEOLOGICAL SURVEY, 41 BI^LL. NO. PLATE 4.
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LEGEND PART5PERMILU0M • O - 5 o 5 - lO + 10-20 A 20-50 ^ 50-100 a 100-500 2<^ 500 + Chlorine in water of springs. 42 MINERAL CONTENT OF WATERS. (bull no. 10. Consumed Oxygen.—^Consiimed oxygen should not exceed 2.0 partsper million. jSitrogen as Free and Alhuminoid Ammonia.—Nitrogen as free andalbuminoid ammonia should not exceed 0.02 and 0.05 parts per millionrespectively. Nitrogen as Nitrites.—Nitrogen as nitrites should be absent. Nitrogen as Nitrates.—Nitrogen as nitrates should not exceed 2.0parts per million. All-alinity.—Alkalinity varies from 200 to 500 parts per million, withexceptional cases above or beloAV these limits. The alkalinity shouldnot exceed 300 parts per million. Waters From Deep Drift Wells. Turbidity.—The well waters in the drift are clear when first drawn,but almost invariably become turbid on exposure to the air, due to ox-idation of the iron salts, and to the loss of carbon dioxide. Color.—These waters are colorless when first drawn, but m

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Author Bartow, Edward, 1870-1958
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  • bookid:mineralcontentof00bart
  • bookyear:1909
  • bookdecade:1900
  • bookcentury:1900
  • bookauthor:Bartow__Edward__1870_1958
  • bookpublisher:_n_p__
  • bookcontributor:The_Library_of_Congress
  • booksponsor:The_Library_of_Congress
  • bookleafnumber:52
  • bookcollection:library_of_congress
  • bookcollection:americana
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30 July 2014



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