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Friday, August 7, 2020 | History

3 edition of Water and sediment reconnaissance of the Hanford shoreline found in the catalog.

Water and sediment reconnaissance of the Hanford shoreline

Norm Buske

Water and sediment reconnaissance of the Hanford shoreline

Hanford Reach Project, data report 4, fall 1988

by Norm Buske

  • 248 Want to read
  • 7 Currently reading

Published by Hanford Education Action League in Spokane, WA .
Written in English

    Subjects:
  • Radioactive substances in rivers, lakes, etc. -- Washington (State) -- Hanford Reach,
  • Groundwater -- Pollution -- Washington (State) -- Hanford Reach,
  • Groundwater -- Sampling -- Washington (State) -- Hanford Reach,
  • River sediments -- Sampling -- Washington (State) -- Hanford Reach

  • Edition Notes

    Statementby Norm Buske, Linda Josephson.
    ContributionsJosephson, Linda., Hanford Education Action League., SEARCH Technical Services.
    Classifications
    LC ClassificationsTD224.W2 B87 1988
    The Physical Object
    Pagination30, [35] p. :
    Number of Pages35
    ID Numbers
    Open LibraryOL16336140M
    ISBN 100032975038
    LC Control Number88084103
    OCLC/WorldCa50450237

    radiation levels attributable to natural causes, worldwide fallout, and Hanford operations. Data were also collected to monitor several chemicals and metals in Columbia River water, sediment, and wildlife. For more information regarding the sampling schedule for the Surface Environmental Surveillance.   Columbia River, Hanford Site ponds, and off-site irrigation sources (Figure ). Aquatic sediment monitoring was conducted for the Columbia River and one Hanford Site pond. Tables and summarize the sampling locations, types, frequencies, and sample analyses included in surface-water and sediment monitoring.

    If all the sediment, including the “fixed bed sediment”, is moving down river at the same rate as the water, equation (1) of the draft report is an adequate representation, and changing the suspended-sediment concentration is straightforward. Sedimentation is one of several methods for application prior to filtration: other options include dissolved air flotation and some methods of filtration. Generically, such solids-liquid separation processes are sometimes referred to as clarification processes. There is a variety of methods for applying sedimentation and include: horizontal flow, radial flow, inclined plate.

      Jezero crater, the destination of the Perseverance rover, is a promising place to look for evidence of extinct Martian life. An image obtained by the Mars Reconnaissance Orbiter in .   Documenting the sedimentary characteristics of recent tsunami deposits is an important tool used for the identification of paleotsunami in the geologic record (Goff et al., , Peters and Jaffe, , Chagué-Goff and al., in press).The primary goal of this study is to identify and characterize the September tsunami deposits and to further the development of geologic criteria for.


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Water and sediment reconnaissance of the Hanford shoreline by Norm Buske Download PDF EPUB FB2

Water and sediment reconnaissance of the Hanford shoreline: Hanford Reach Project, data report 4, fall [Buske, Norm] on *FREE* shipping on qualifying offers. Water and sediment reconnaissance of the Hanford shoreline: Hanford Reach Project, data report 4, fall Author: Norm Buske.

RECONNAISSANCE INVESTIGATION OF WATER QUALITY, BOTTOM SEDIMENT, AND BIOTA ASSOCIATED WITH IRRIGATION DRAINAGE IN THE SALTON SEA AREA, CALIFORNIA, By James G.

Setmire U.S. GEOLOGICAL SURVEY and John Cs Wolfe and Richard K. Stroud U.S. FISH AND WILDLIFE SERVICE U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 89 Cited by: Water, bottom sediment, and biota were sampled during and in the Salton Sea area to determine concentrations of trace elements and pesticides as part of the Department of Interior Irrigation Drainage Program.

The sampling sites (12 water, 15 bottom sediment, and 5 biota) were located in the Coachella and Imperial Valleys. The focus of sampling was to determine the current or.

Environmental surveillance at the Hanford Site collects data that provides a historical record of radionuclide and radiation levels attributable to natural causes, worldwide fallout, and Hanford operations. Data are also collected to monitor several chemicals and metals in Columbia River Water and Sediment.

Shoreline changes were analyzed using two metrics: (1) shoreline mobility and induced coastal area change over time, and (2) conversion of coastal land into water, or conversion of adjacent coastal water into land. Data on shoreline mobility and area change were obtained from 47 digitized LANDSAT satellite images (60–30 m pixel size) from Cited by: 2.

water, bottom sediment, and biota were moderately to considerably larger than established criteria and standards.

The largest selenium concentra­ tions in water and bottom sediment were from seeps that surround Benton Lake, with maximum concentrations of micrograms per liter in water and micrograms per gram in bottom sediment. " World Environmental and Water Resources Congress Online publication date: May Habersack Helmut Kreisler Andrea "Sediment Transport Processes.

" Dating Torrential Processes on Fans and Cones /, Viparelli Enrica Wesley Lauer J. Belmont Patrick Parker Gary " A numerical model to develop long-term.

As river water passes along the northern and eastern boundary of Hanford, groundwater from beneath the site enters through shoreline springs and direct discharge. Downstream of Hanford, an average of 11 curies of natural and human-made radioactivity flow in the river each day.

Manual measurements of water levels and temperatures provided calibration and quality control. Synoptic manual shoreline sediment temperatures also were logged periodically 10 cm offshore at depths of 1 and 15 cm into the lake sediments. Streamflow Measurements.

Water & Shorelines. We improve and protect water quality, manage and conserve water resources, and effectively manage coastal and inland shorelines to assure our state has sufficient supplies of clean water for communities and the natural environment. Deep-water sediment waves can be classified using a combination of grain size and wave-forming process, although in some cases one or other of these criteria may be indeterminable.

Sediment waves are generated beneath currents flowing across the seabed, in the form of either downslope-flowing turbidity currents or alongslope-flowing bottom. @article{osti_, title = {Study of the relationship between water quality and sediment transport: A guide for the collection and interpretation of sediment quality data}, author = {Golterman, H.L.

and Sly, P.G. and Thomas, R.L.}, abstractNote = {This guidebook takes the reader from a description of the nature and properties of sediments, to an explanation of how to plan a sediment. @article{osti_, title = { Area Columbia River sediment sampling}, author = {Weiss, S G}, abstractNote = {Forty-four sediment samples were collected from 28 locations in the Hanford Reach of the Columbia River to assess the presence of metals and man-made radionuclides in the near shore and shoreline settings of the Hanford Site.

@article{osti_, title = { Hanford riverbank springs characterization report}, author = {Dirkes, R L}, abstractNote = {This reports presents the results of a special study undertaken to characterize the riverbank springs (i.e., ground-water seepage) entering the Columbia River along the Hanford Site.

Radiological and nonradiological analyses were performed. Many USGS reports on water resources are now being served online. Most publications located at this site and other USGS sites can be located by subject, author, date, USGS series or publication series number by using the reports and thematic maps electronic Publications Warehouse.

The Publications Warehouse will eventually be taking the place of this page. The summary categories are based on descriptive observational oiling metrics (e.g.

thickness, areal distribution, across-shore width) with wide inherent uncertainty. Shoreline oil itself often consisted of oil–water emulsions, or oil-sediment aggregations with widely varying oil content (Michel et al.,Urbano et al., ).

A bottom-contacting probe for measuring electrical conductivity at the sediment-water interface was used to scan the bed of the Columbia River adjacent to the Hanford Site in southeast Washington State during a day investigation.

Four river-sections, each about a kilometer in length, were scanned for variations in electrical conductivity. The probe was towed along the riverbed at a speed of.

Storms, of course, deliver large amounts of water to a river, but did you know they also bring along lots of eroded soil and debris from the surrounding landscape?Rocks as small as tiny clay particles and larger that are moved by the water are called sediment.

Fast-moving water can pick up, suspend, and move larger particles more easily than slow-moving waters. We made improvements to this page.

Please tell us how they work for you. Ecology provides the high-quality science that is the foundation of Washington state environmental policy. Our monitoring, assessment, and modeling services provide a data-rich understanding of our state’s land, air, and. Contents Notice ii Disclaimer iii List of Figures vii List of Tables vii INTRODUCTION 1 Objective and Scope 1 Characteristics of Surface Water and Sediment 1 Surface Water 1 Sediment 3 Representative Sampling 4 Conceptual Site Model 4 Representative Sampling Objectives 6 Determine Hazard and Identify Contaminant 6 Establish Imminent.

The mean water discharge of the Mekong at Kratie, in Cambodia (Fig. 1b) is 14, m 3 /s annual hydrological regime is seasonal (Fig. 2b) with a southwest Monsoon flood season (May-October) during which river-borne sediment is delivered to the delta and coastal ocean through several distributary mouths associated with the two main branches, the Bassac and the Mekong (Fig.

1a).Create a new account. Are you an ASCE Member? We recommend that you register using the same email address you use to maintain your ASCE Member account.Sedimentation 1 Sedimentation.

Sedimentation, or clarification, is the processes of letting suspended material settle by gravity. Suspended material may be particles, such as clay or silts, originally present in the source water.