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Thursday, July 30, 2020 | History

4 edition of Lithologic coring in the lower Anacostia tidal watershed, Washington, D.C., July 2002 found in the catalog.

Lithologic coring in the lower Anacostia tidal watershed, Washington, D.C., July 2002

Frederick J. Tenbus

Lithologic coring in the lower Anacostia tidal watershed, Washington, D.C., July 2002

by Frederick J. Tenbus

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Published by U.S. Dept. of the Interior, U.S. Geological Survey, U.S. Geological Survey, Branch of Information Services [distributor] in Baltimore, Md, Denver, CO .
Written in English

    Places:
  • Anacostia River Watershed (Md. and Washington, D.C.)
    • Subjects:
    • Nonpoint source pollution -- Anacostia River Watershed (Md. and Washington, D.C.),
    • Borings -- Anacostia River Watershed (Md. and Washington, D.C.)

    • Edition Notes

      Includes bibliographical references (p. 12).

      Statementby Frederick J. Tenbus ; in cooperation with the District of Columbia Department of Health, Environmental Health Administration, Bureau of Environmental Quality, Water Quality Division.
      SeriesOpen-file report ;, 03-318, U.S. Geological Survey open-file report ;, 03-318.
      ContributionsGeological Survey (U.S.), District of Columbia. Dept. of Health. Water Quality Division.
      Classifications
      LC ClassificationsTD225.A72 .T46 2003
      The Physical Object
      Paginationiii, 62 p. :
      Number of Pages62
      ID Numbers
      Open LibraryOL3346286M
      LC Control Number2004356187
      OCLC/WorldCa54488877

        Amplitudes of up to m (with a frequency between 5 and 10 days) that are comparable in magnitude to the estuary's tidal range characterise the sub-tidal oscillations (Zaker et al., ). Along the WA coastline, sub-tidal oscillations are associated with the passage of low-pressure systems during summer and winter (Provis and Radok, flow of water through the watershed. For example, if water moves rapidly through the system, the removal of nitrogen through biological uptake and storage and denitrification may be reduced (Howarth et al. ). Thus, there is a strong and inescapable link between water quantity and water quality (Pinay et al. ).

      The northern bay also has lower salinity in general, about ~8 to10 g/kg lower in May-October period (Velinsky et al. a), because of larger fresh water input and . Thirty-three bottom sediments were collected from the Potomac and Anacostia rivers, Tidal Basin, and Washington Ship Channel in June to define the extent of trace metal contamination and to elucidate source areas of sediment contaminants. In addition, twenty-three sediment samples were collected directly in front of and within major storm and combined .

      CSOs. Additionally it is estimated that about 60 percent of the watershed in Washington, DC drains directly to the tidal Anacostia River through sanitary and sewer systems that date as far back as the s. Consequently, constant broken sewage pipes created the problems of sew outflow to area. For Example, there are eleven main. TMDL analysis for the Anacostia watershed addresses the sediment loads during the annual average and growing season (April 1 – October 31) conditions. This technical memorandum Tidal Lower DC Total DC MS4 Loads DC CSO Loads – Tidal Upper DC DC CSO Loads – Tidal Lower.


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Lithologic coring in the lower Anacostia tidal watershed, Washington, D.C., July 2002 by Frederick J. Tenbus Download PDF EPUB FB2

Lithologic Coring in the Lower Anacostia Tidal Watershed, Washington, D.C., July By Frederick J. Tenbus. Abstract. Little is known about the volumetric flux of ground water to the lower tidal Anacostia River, or whether ground-water flow is an important component of the contaminant load in this part of the Anacostia River.

The watershed. Lithologic Coring in the Lower Anacostia Tidal Watershed, Washington, D.C., July Open-File Report [Tenbus, Frederick J., U.S. Department of the Interior, United] on *FREE* shipping on qualifying offers. Lithologic Coring in the Lower Anacostia Tidal Watershed, Washington, D.C., July Open-File Report Author: Frederick J.

Tenbus. |a Lithologic coring in the lower Anacostia tidal watershed, Washington, D.C., July |h [electronic resource] / |c by Frederick J.

Tenbus ; in cooperation with the District of Columbia Department of Health, Environmental Health Administration, Bureau of Environmental Quality, Water Quality Division.

Author Tenbus, Frederick J. Title Lithologic coring in the lower Anacostia tidal watershed, Washington, D.C., July [electronic resource] / by Frederick J. Tenbus ; in cooperation with the District of Columbia Department of Health, Environmental Health Administration, Bureau of Environmental Quality, Water Quality Division.

Get this from a library. Lithologic coring in the lower Anacostia tidal watershed, Washington, D.C., July [Frederick J Tenbus; Geological Survey (U.S.); District of Columbia. Department of Health. Water Quality Division.]. Compre online Lithologic Coring in the Lower Anacostia Tidal Watershed, Washington, D.C., July Open-File Reportde U.S.

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Lithologic coring in the lower Anacostia tidal watershed, Washington, D.C., July Frederick J. Tenbus, Lithologic Coring in the Lower Anacostia Tidal Watershed,Washington, D.C., July62p. OFR Cheryl A. Klohe and Linda M.

Debrewer, Summary of Groundwater-Quality Data in the Anacostia River Watershed, Washington, D.C., September- December74p. OFR Discover our full range of books, gifts, toys, stationery and audiobooks at Buy online with Free UK Delivery on Orders Over £ Amazon配送商品ならLithologic Coring in the Lower Anacostia Tidal Watershed, Washington, D.C., July Open-File Report が通常配送無料。更にAmazonならポイント還元本が多数。Tenbus, Frederick J, U S Department of the Interior, United作品ほか、お急ぎ便対象商品は当日お届けも可能。.

Lithologic Coring in the Lower Anacostia Tidal Watershed, Washington, D.C., July Little is known about the volumetric flux of ground water to the lower tidal Anacostia River, or whether ground-water flow is an important component of the contaminant load in this part of the Anacostia River.

Lithologic Coring in the Lower Anacostia Tidal Watershed, Washington, D.C., July By Frederick J. Tenbus Abstract Little is known about the volumetric flux of ground water to the lower tidal Anacostia River, or whether ground-water flow is an important component of the contaminant load in this part of the Anacostia River.

Lithologic Coring in the Lower Anacostia Tidal Watershed, Washington, D.C., July Open-File Report | Frederick J Tenbus, United U S Department of the Interior | ISBN: | Kostenloser Versand für alle Bücher mit Versand und Verkauf duch : Taschenbuch. Summary of Ground-Water-Quality Data in the Anacostia River Watershed, Washington, DC, September– December Lithologic Coring in the Lower Anacostia Tidal Watershed, Washington, DC, July USGS Ground Water- Quality Data for the District of Columbia.

Lithologic Coring in the Lower Anacostia Tidal Watershed, Washington, D.C., July Open-File Report Frederick J. Tenbus, United U.

Department of the. Frederick J. Tenbus has written: 'Lithologic coring in the lower Anacostia tidal watershed, Washington, D.C., July ' -- subject(s): Borings, Nonpoint source. Tidal freshwater wetlands have been restored to mitigate for wetland losses due to development (roads, buildings), stream channelization, and other hydrologic alterations and to protect shorelines, reduce flooding, control invasive species, and restore the ecosystem functions of converted wetlands (Table ).In the US Pacific Northwest and the Fraser River in British.

USGS CORING LOG 15 Graphic log Lithologic description Project Anacostia Ground Water Date drilled 7/2/ Site name DCHP01 Date described 7/15/ Latitude / Longitude 38o 54’ ” / o 57’ ” Described by Phelan / Tenbus Land-surface elevation ft above sea level Interval to ft Total depth ft below land surface Drilling method Vibracore.

Contact, chat, social media. About. Organization, jobs, budget. levels are expected to lower as the growing season approaches because there is increased water demand from & Drought. 2 of 3 Status of Streams and Wells for February Daily streamflow on the Potomac River near Washington, D.C.Tidal character in local waters.

The source of most of this material is Mofjeld and Larsen (), Tides and tidal currents in the inland waters of western Washington, NOAA Tech. Memorandum ERL PMEL Another good source of information is Rick Thomson’s book Oceanography of the British Columbia Coast.

Tidal elevations.Borings -- Anacostia River Watershed (Md. and Washington, D.C.): Lithologic coring in the lower Anacostia tidal watershed, Washington, D.C., July / by Frederick J.

Tenbus ; in cooperation with the District of Columbia Department of Health, Environmental Health Administration, Bureau of Environmental Quality, Water Quality Division. 1