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| 006 | m o d f |
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| 008 | 110127s2009 vauab ob f000 0 eng d |
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| 019 | | . |
‡a1037507707 |
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‡a(OCoLC)698478958 |
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| 037 | | . |
‡agovdocs.govdocse |
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‡aGPO
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‡bJ37 2009 |
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| 074 | | . |
‡a0624-B-02 (online) |
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| 082 | 1 | 4. |
‡a19.42/4-4:2009-5165 |
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| 086 | 0 | . |
‡aI 19.42/4-4:2009-5165 |
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| 100 | 1 | . |
‡aJastram, John D.
‡eauthor |
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| 245 | 1 | 2. |
‡aA comparison of turbidity-based and streamflow-based estimates of suspended-sediment concentrations in three Chesapeake Bay tributaries
‡h[electronic resource] /
‡cby John D. Jastram, Douglas L. Moyer, and Kenneth E. Hyer ; prepared in cooperation with the U.S. Environmental Protection Agency Chesapeake Bay Program and the Virginia Department of Environmental Quality. |
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| 264 | | 1. |
‡aReston, Va. :
‡bU.S. Dept, of the Interior, U.S. Geological Survey,
‡c2009. |
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| 300 | | . |
‡a1 online resource (vi, 37 pages) :
‡billustrations (some color). |
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| 336 | | . |
‡atext
‡btxt
‡2rdacontent |
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| 337 | | . |
‡acomputer
‡bc
‡2rdamedia |
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| 338 | | . |
‡aonline resource
‡bcr
‡2rdacarrier |
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| 347 | | . |
‡adata file
‡2rda |
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| 490 | 1 | . |
‡aScientific investigations report ;
‡v2009-5165 |
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| 500 | | . |
‡aTitle from PDF title screen (viewed on Jan. 27, 2011). |
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| 504 | | . |
‡aIncludes bibliographical references (pages 35-37). |
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| 650 | | 0. |
‡aTurbidity
‡zChesapeake Bay Watershed. |
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| 650 | | 0. |
‡aSuspended sediments
‡zChesapeake Bay Watershed. |
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| 700 | 1 | . |
‡aMoyer, Douglas L. |
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| 700 | 1 | . |
‡aHyer, Kenneth E.
‡q(Kenneth Edward) |
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| 710 | 1 | . |
‡aVirginia.
‡bDepartment of Environmental Quality.
‡0(CARDINAL)218263 |
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| 710 | 2 | . |
‡aChesapeake Bay Program (U.S.)
‡0(CARDINAL)221047 |
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| 710 | 2 | . |
‡aGeological Survey (U.S.)
‡0(CARDINAL)154385 |
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| 776 | 0 | 8. |
‡iPrint version:
‡aJastram, John D.
‡tA comparison of turbidity-based and streamflow-based estimates of suspended-sediment concentrations in three Chesapeake Bay tributaries
‡hvi, 37 p.
‡w(DLC) 2009438996
‡w(OCoLC)475437156 |
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| 830 | | 0. |
‡aScientific investigations report ;
‡v2009-5165.
‡0(CARDINAL)271380 |
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| 856 | 4 | 0. |
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