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Using transfer functions to explain turbidity in Humboldt Bay, California /Walker, Steven M. January 1900 (has links)
Thesis (M.S.)--Humboldt State University, 2009. / Includes bibliographical references (leaves 107-111). Also available via Humboldt Digital Scholar.
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Treatment of Colorado River water with ozone, ferric chloride and Cat-Floc T-2Di Domizio, Thomas John, January 1990 (has links) (PDF)
Thesis (M.S. - Civil Engineering and Engineering Mechanics)--University of Arizona, 1990. / Includes bibliographical references.
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Depositing and eroding sediment-driven flows turbidity currents /García, Marcelo H., January 1989 (has links)
Thesis (Ph. D.)--University of Minnesota, 1989. / Includes bibliographical references.
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Sedimentation on basin plainsRothwell, Robin Guy January 1994 (has links)
No description available.
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Understanding palynomorph distribution in turbidite systemsPorro, Francesca January 2018 (has links)
No description available.
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An experimental study of atmospheric turbidity using radiometric techniquesShaw, Glenn E. January 1971 (has links)
No description available.
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High-energy sedimentary processes in Kluane Lake, Yukon TerritoryCrookshanks, Sarah 28 May 2008 (has links)
A lacustrine sedimentary process study was undertaken at Kluane Lake, which is a large, glacier-fed, alpine lake in the southwestern corner of Yukon Territory. Data from moored instruments, sediment traps, water column profiling, and high-resolution sub-bottom acoustic surveys were collected over the peak melt seasons of 2006 and 2007 in order to document the spatial and temporal lacustrine sedimentation patterns. A river monitoring station was also established to continuously record the inflow variations of Slims River, which drains meltwater from Kaskawulsh Glacier. Kluane Lake receives sediment-laden (up to 5 g/l) water from Slims River, which varies diurnally in terms of both discharge and suspended sediment concentration. While evidence of seasonal sediment exhaustion is present within the system, the diurnal hysteresis relationship between discharge and suspended sediment is either insignificant or more commonly counterclockwise. The high suspended sediment load delivered by Slims River produces continuous, diurnally fluctuating turbidity currents with maximum velocities in excess of 0.6 m/s at delta-proximal locations, although velocities between 0.2 and 0.4 m/s are more typical. During peak flow conditions, variations in current velocity can be traced to the deepest portion of the lake, over 4 km from the point of inflow. The longitudinal changes in the vertical concentration profiles, suspended sediment load, and mass accumulation rates suggest that the flow structure of the turbidity currents changes rapidly along the first several kilometres of flow. Sedimentation in the Kluane Lake basin is dominated by turbidity currents; overflows occur intermittently and contribute less than 2% to sediment accumulation along the lake bed. The highest rate of deposition occurs approximately 1 km from the delta and is consistent with an accumulation of approximately 0.4 m/a; closer to the delta, high current velocities appear to inhibit sediment deposition. The sediment in Kluane Lake is dominated by silt-size particles and contains virtually no sand except in small amounts very close to the delta. The diurnal pattern of turbidity current activity produces daily rhythmites in sediment traps deployed near the lake bottom, but these laminations do not occur consistently over time or space. / Thesis (Master, Geography) -- Queen's University, 2008-05-22 13:42:20.629
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Effects of turbidity on foraging efficiency and growth of salmonids in natural settings /DeYoung, Chad J. January 1900 (has links)
Thesis (M.S.)--Humboldt State University, 2007. / Includes bibliographical references (leaves 46-51). Also available via Humboldt Digital Scholar.
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Effect of particle size distribution on sediment loading in a mixed-land use watershed in northern Idaho /Ostrowski, Krzysztof Maciej. January 1900 (has links)
Thesis (Ph. D., Biological and Agricultural Engineering)--University of Idaho, June 2007. / Major professor: Jan Boll. Includes bibliographical references. Also available online (PDF file) by subscription or by purchasing the individual file.
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Study of the flow of and deposition from turbidity currentsLakshminarasimhan, Srivatsan, Bonnecaze, R. T. January 2004 (has links) (PDF)
Thesis (Ph. D.)--University of Texas at Austin, 2004. / Supervisor: Roger T. Bonnecaze. Vita. Includes bibliographical references.
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