1 edition of Estimated 1996-97 and long-term average annual loads for suspended sediment and selected trace metals in streamflow of the upper Clark Fork basin from Warm Springs to Missoula, Montana found in the catalog.

Estimated 1996-97 and long-term average annual loads for suspended sediment and selected trace metals in streamflow of the upper Clark Fork basin from Warm Springs to Missoula, Montana

cuenca del Río Camaná-Majes

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Published by Administrator in U.S. Dept. of the Interior, U.S. Geological Survey

    Places:
  • United States
    • Subjects:
    • U.S. Dept. of the Interior, U.S. Geological Survey


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      • Shipping list no.: 98-0352-PAugust 1998--T.p. versoIncludes bibliographical references (p. 34-35)

        StatementU.S. Dept. of the Interior, U.S. Geological Survey
        PublishersU.S. Dept. of the Interior, U.S. Geological Survey
        Classifications
        LC Classifications1998
        The Physical Object
        Paginationxvi, 133 p. :
        Number of Pages84
        ID Numbers
        ISBN 10nodata
        Series
        1
        2Water-resources investigations report -- 98-4137
        3

        nodata File Size: 10MB.


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Estimated 1996-97 and long-term average annual loads for suspended sediment and selected trace metals in streamflow of the upper Clark Fork basin from Warm Springs to Missoula, Montana by U.S. Dept. of the Interior, U.S. Geological Survey Download PDF EPUB FB2


The estimates of fry production potential at sample sites ranged widely 0. 1997 Impacts by Acidic, Metals-Rich Groundwater on the Hyporheic Zone of an Intermontane Stream CASTRO, JAMES M. We tested this assumption by correlating temporal metal trends in sediment between and among stations. Geological Survey Open-File Report 97-552, 91 p. 2001 Sources and Seasonal Variability of Metal and Arsenic Concentrations in the Surface Water of the Clark Fork River Basin, Montana.

:also by Rodger F. Information on data reliability is available at Reference: U. University of Montana Geology Department Theses - Surface and groundwater in the Upper Clark Fork Basin Not available on-line - UM theses can be borrowed from the BROOK, EDWARD J. Furthermore, increased sediment deposition provides additional substrate for colonization by aquatic macrophytes, which serve as forage and habitat for other non-native species.

Most likely these oxygen deficits are a result of allochthonous input of organic matter and subsequent decomposition.

Dilution mixing estimates of trace metal concentrations of suspended sediments (Journal Article)

Chat Now with a Law Librarian• View: 992 LambingJ. The Grove Creek basin includes an area of about 42 sq mi in Duplin County, North Carolina.

Geological Survey Open-File Report 00-370, 102 p.