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Tuesday, May 5, 2020 | History

4 edition of The abundance of zinc and cadmium in sphalerite-bearing coals in Illinois found in the catalog.

The abundance of zinc and cadmium in sphalerite-bearing coals in Illinois

Illinois State Geological Survey

The abundance of zinc and cadmium in sphalerite-bearing coals in Illinois

by Illinois State Geological Survey

  • 111 Want to read
  • 18 Currently reading

Published by Illinois State Geological Survey in Urbana, IL .
Written in English

    Places:
  • Illinois
    • Subjects:
    • Coal -- Illinois -- Analysis.,
    • Sphalerite -- Illinois -- Analysis.,
    • Zinc -- Analysis.,
    • Cadmium -- Analysis.

    • Edition Notes

      StatementJames C. Cobb ... [et al.].
      SeriesIllinois mineral note ;, 74, Illinois minerals note ;, 74.
      ContributionsCobb, James C.
      Classifications
      LC ClassificationsTN24.I3 I48 no. 74, TP326.U5 I48 no. 74
      The Physical Object
      Pagination28 p. :
      Number of Pages28
      ID Numbers
      Open LibraryOL4242067M
      LC Control Number80622960


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The abundance of zinc and cadmium in sphalerite-bearing coals in Illinois by Illinois State Geological Survey Download PDF EPUB FB2

Abundance of zinc and cadmium in sphalerite-bearing coals in Illinois. Urbana, Ill.: Illinois State Geological Survey, (OCoLC) Material Type: Government publication, State or province government publication: Document Type: Book: All Authors / Contributors: James C Cobb; Illinois State Geological Survey.

The Abundance of Zinc and Cadmium in Sphalerite-bearing Coals in Illinois Paperback – by James C. Cobb (Author) Be the first to review this item. See all formats and editions Hide other formats and editions. Price New from Author: James C.

Cobb. J.C. Cobb, J.D. Steele, C.G. TreworgyThe abundance of zinc and cadmium in sphalerite-bearing coals in Illinois Illinois Geological Survey Illinois Mineral, 74 () Google ScholarCited by:   Arsenic, cadmium, lead, and zinc contents and distributions are discussed in two major Pennsylvanian coal beds in Indiana: the Danville Coal Member and the Springfield Coal Member.

Arsenic contents of the Danville and Springfield coals show similar ranges from to 43 ppm for the Danville Coal and 1 to 50 ppm for the Springfield Coal, with an average of. Abstract. Coal will be a major energy source in the United States and in many other countries well into the 21st century.

Although coal is composed predominantly of organic matter, inorganic constituents in coal commonly attract more attention and Cited by: Abstract. Occurrences of galena and sphalerite associated with coal seams are described. The sources of lead, zinc and sulphur and mechanisms for the formation of galena and sphalerite associated with coals, either dispersed or in cleats and the like, are by: 4.

The Clarke values of lead calculated by Ketris and Yudovich are ± for world brown coals, ± for world hard coals, and for all coals (Ketris and Yudovich ). J.C. Cobb, J.D. Steele, C.G. TreworgyThe abundance of zinc and cadmium in sphalerite-bearing coals in Illinois Illinois Geological Survey Illinois Mineral Note, 74 Cited by: 4.

A suite of high volatile bituminous coals of Pennsylvanian age from Indiana has been studied for their mercury (Hg) concentration and relationship between mercury content and maceral and lithotype composition. The coals ranged in Hg content from in the Danville Coal Member to ppm in the Upper Block Coal Member.

Our study indicates that relationships. Selected References— Revised February These bibliographic references have been compiled as a TSOP project, and organic petrologists. Anthropogenic organic matter in the Great Marsh of the Indiana Dunes National Lakeshore and its implications Article in International Journal of Coal Geology 46().

Full text of "Materials Recycling: An Overview of the Sixth Mineral Waste Utilization Symposium" See other formats. It is commonly found when there is an abundance of arsenic sulfide minerals in a hydrothermal deposit. Hence, native arsenic is a product of low-temperature epithermal mineralization (C) under sulfur-deficient and strongly reducing conditions rather than a weathering product.

A gray or black holocrystalline nepheline monzogabbro or nepheline monzodiorite depending on the ratio of orthoclase to plagioclase and the abundance of nepheline.

Evaporites are sedimentary rocks of water-soluble, minerals that result from the evaporation of bodies of superficial water in continental and marine depositional environments.