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Friday, May 15, 2020 | History

3 edition of Sediment oxygen demand in Upper Klamath and Agency Lakes, Oregon, 1999 found in the catalog.

Sediment oxygen demand in Upper Klamath and Agency Lakes, Oregon, 1999

Tamara M. Wood

Sediment oxygen demand in Upper Klamath and Agency Lakes, Oregon, 1999

by Tamara M. Wood

  • 387 Want to read
  • 28 Currently reading

Published by U.S. Dept. of the Interior, U.S. Geological Survey, USGS Information Services [distributor] in Portland, Or, Denver, CO .
Written in English

    Places:
  • Oregon,
  • Upper Klamath Lake.
    • Subjects:
    • Water -- Dissolved oxygen -- Oregon -- Upper Klamath Lake.,
    • Lake sediments -- Oregon -- Upper Klamath Lake.

    • Edition Notes

      Statementby Tamara M. Wood ; prepared in cooperation with the Bureau of Reclamation.
      SeriesWater-resources investigations report ;, 01-4080
      Classifications
      LC ClassificationsGB701 .W375 no. 01-4080
      The Physical Object
      Paginationiv, 13 p. :
      Number of Pages13
      ID Numbers
      Open LibraryOL4016704M
      LC Control Number2001387600
      OCLC/WorldCa47361902

      UPPER KLAMATH LAKE Description Upper Klamath Lake is the largest body of water in the Klamath basin anti is one of the largest lakes in the western United States (about mid. The lake anti its drainage lie on volcanic deposits clerivecI in part from the nearby Crater Lake calclera, which took its present form as a result of the eruption of. Lower Klamath Lake By William G. Robbins Before human engineering altered the upper Klamath Basin, water flowed from Upper Klamath Lake into Link River, a short stream that emptied into Lake Ewauna, the true headwaters of the Project, which straddled the Oregon-California state line. The Klamath enterprise involved an elaborate scheme of.

      In the U.S. Fish and Wildlife Service listed two endemic fishes of the upper Klamath River basin of Oregon and California, the sucker and the Lost River sucker, as endangered under the federal Endangered Species Act (ESA). USGS Reports Low Dissolved Oxygen Events in Lake Linked to Wind and Currents. Fish die-offs in Upper Klamath Lake, Oregon, have been preceded in recent years first by high pH and ammonia levels, then by widespread conditions of low dissolved oxygen, according to a .

      Action Plan for the Klamath River Total Maximum Daily Loads Addressing Temperature, Dissolved Oxygen, Nutrient, and Microcystin Impairments in the Klamath River in California. and Lost River Implementation Plan1. The Klamath River basin in California, including all tributaries, comprises approximat square miles. The Northern lakes guide [electronic resource]: to lakes Simcoe and Couchiching, the lakes of Muskoka, the Georgian Bay and Great Manitoulin Channel, and Lake Superior: giving a description of the lakes and river scenery with the [b]est spots for waterside summer resorts, hotels, camping outfit, fishing and shooting, distances and cost of travel.


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Sediment oxygen demand in Upper Klamath and Agency Lakes, Oregon, 1999 by Tamara M. Wood Download PDF EPUB FB2

Sediment Oxygen Demand in Upper Klamath and Agency Lakes, Oregon, By Tamara M. Wood SIGNIFICANT FINDINGS • The distribution ofSOD20 values (measured sediment oxygen demand values corrected to 20oC [degrees Celsius]) had a median value of g/m2/day (grams per square meter per day) in the spring and g/m2/day in the late by: Get this from a library.

Sediment oxygen demand in Upper Klamath and Agency lakes, Oregon, [Tamara M Wood; Geological Survey (U.S.); United States. Bureau of Reclamation.].

Upper Klamath and Agency Lakes, Oregon, June – Relation of daily minimum dissolved oxygen concentration from hourly records to lake Sediment oxygen demand also may be enhanced at lower lake levels because it is concentrated over a smaller vol-ume of water. Some compensation 1999 book by: 8.

Upper Klamath Lake is a large ( square-mile), shallow (mean depth about 8 ft) lake in south-central Oregon that the historical record indicates has been eutrophic since its discovery by non-Native Americans. In recent decades, however, the lake has had annual occurrences of near- monoculture blooms of the blue-green alga Aphanizomenon flos-aquae.

The sediment samples will be sent to the Cascade Volcano Observatory sediment laboratory in Vancouver, Washington, for analysis. Reports. Doyle, M.C., and Lynch, D.D.,Sediment Oxygen Demand in Lake Ewauna and the Klamath River, Oregon, June U.S.

Geological Survey Sientific Investigations Report14 p. Sediment oxygen demand in Upper Klamath and Agency Lakes, Oregon,by Tamara M. Wood. SIR Water quality conditions in Upper Klamath Lake, Oregon,by Tamara M. Wood, Gene R. Hoilman, and Mary K.

Lindenberg. SIR DOI: /wri Corpus ID: Sediment oxygen demand in the lower Willamette River, Oregon, @inproceedings{CaldwellSedimentOD, title={Sediment oxygen demand in the lower Willamette River, Oregon, }, author={James M. Caldwell and Micelis C. Doyle}, year={} }. Wind Control on Water Quality in Shallow, Hypereutrophic Upper Klamath Lake, Oregon Article (PDF Available) in Lake and reservoir management 21(2) June with 46 Reads.

FIELD STUDIES ON SEDIMENT-WATER ALGAL NUTRIENT INTERCHANGE PROCESSES AND WATER QUALITY OF UPPER KLAMATH AND AGENCY LAKES July March A. Gahler Working Paper No. 66 United States Department of the Interior Federal Water Pollution Control Administration, Northwest Region Pacific Northwest Water Laboratory Southwest Thirty-fifth.

Rounds joined the U.S. Geological Survey in and worked on a wide variety of studies, with a focus on water-quality monitoring and modeling of rivers and lakes around Oregon. InStewart retired and continues to volunteer with USGS as a Scientist Emeritus.

Sediment-phosphorus release rates as a function of pH were determined in laboratory experiments for sediment and water samples collected from Shoalwater Bay in Upper Klamath Lake, Oregon, in Sediment oxygen demand in Lake Ewauna and the Klamath River, Oregon, June USGS Scientific Investigations Report [Micelis C.

Doyle, Dennis D. Lynch] on *FREE* shipping on qualifying offers. The United States Geological Survey (USGS) is a scientific organization created inand is part of the U.S. : Dennis D. Lynch. PORTLAND, Ore. — The United States Geological Survey, in cooperation with several Klamath Basin stakeholders, has developed hydrologic datasets for the upper Klamath Basin of south-central Oregon that can help water managers identify and prioritize water uses that could be voluntarily set aside and reallocated to yield an additio acre feet of water to Upper Klamath Lake.

During June-Octoberwater quality data were collected from Upper Klamath and Agency Lakes in Oregon, and meteorological data were collected around and within Upper Klamath Lake.

Data recorded at two continuous water quality monitors in Agency Lake showed similar temperature patterns throughout the field season, but data recorded at the northern site showed more day-to-day variability for.

The Wood River Valley occupies about 5% of the land area of the upper Klamath Basin but provides about 25–35% of the water input to Agency and Upper Klamath lakes (U.S. Bureau of Reclamation ). The Wood River Wetland area was diked and drained for agriculture in two stages: the higher elevation northern area in and the southern area Cited by: Upper Klamath Lake, filling a broad valley at the foot of the eastern slope of the southern High Cascades, is the source of the Klamath lake is fed by the Williamson River, which originates in the Winema National Forest, and the Wood River, which rises near Crater Lake National Klamath River issues from Klamath Lake at Klamath Falls as a short 1-mile ( km) stream known as Country: United States.

Sediment oxygen demand was calculated from known volumes, sediment surface areas, and rate of DO loss. Final Report: Canyon Lake Nutrient Flux and In-Lake Alternatives 25 June (Rydin and Welch, ). Results Forms of Phosphorus in the Sediments The sediment in Canyon Lake was found to be dominated by a reducible iron.

Sediment oxygen demand in the lower Willamette River, Oregon, [Caldwell, James M.] on *FREE* shipping on qualifying offers. Sediment oxygen demand in the lower Willamette River, Oregon, Author: James M.

Caldwell. Abstract. A combination of tephrochronology and 14 C, Pb, and Cs measurements provides a robust chronology for sedimentation in Upper Klamath Lake during the last 45 years.

Mixing of surficial sediments and possible mobility of the radio-isotopes limit the usefulness of the Cs and Pb data, but Pb profiles provide reasonable average sediment accumulation rates for the Cited by: Similar Items. A review of possible causes of nutrient enrichment and decline of endangered sucker populations in Upper Klamath Lake, Oregon / by: Bortleson, Gilbert Carl, Published: () Water velocity and suspended solids measurements by in-situ instruments in upper Klamath Lake, Oregon Published: ().

The Klamath River flows about mi ( km) through southern Oregon and northern California to the Pacific Ocean. The river begins at Link River Dam at the outlet of Upper Klamath Lake (); the dam regulates lake level, controls downstream flow, and diverts water for hydropower or first mile of the river downstream of Link River Dam is named Link by: USGS () Upper Klamath Lake Basin Nutrient-Loading Study—Assessment of Historic Flows in the Williamson and Sprague Rivers.

Water-Resources Investigations Cited by: 1.The Klamath River is located in northern California and southern Oregon on the Pacific owned by PacifiCorp, consists of six generating developments along the mainstem of the Upper Klamath River.

The project also includes a re-regulation dam with no generation facilities, Klamath River Dam and Sediment Investigation GEC.