Effects of Urbanization on Stream Ecosystems in the Willamette River Basin and Surrounding Area, Oregon and Washington PDF Download
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Author:
Publisher:
ISBN:
Category : Stream ecology
Languages : en
Pages : 62
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Book Description
Author:
Publisher:
ISBN:
Category : Stream ecology
Languages : en
Pages : 62
Get Book Here
Book Description
Author:
Publisher:
ISBN:
Category : Stream ecology
Languages : en
Pages : 62
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Book Description
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 58
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Book Description
Author:
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ISBN:
Category :
Languages : en
Pages : 498
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Book Description
Author: United States. Office of the Assistant Secretary of the Army (Civil Works)
Publisher:
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Category : Environmental impact analysis
Languages : en
Pages : 1308
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Book Description
Author: David A. Rickert
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 44
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Book Description
Author: Mark A. Uhrich
Publisher:
ISBN:
Category : Sandy River Watershed (Or.)
Languages : en
Pages : 34
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Author:
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Category : Hydroelectric power plants
Languages : en
Pages : 20
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Author:
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ISBN:
Category : Water quality
Languages : en
Pages : 180
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Book Description
Author: James O. Shearman
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ISBN:
Category : Geology
Languages : en
Pages : 32
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Book Description
For nearly half a century the Willamette River in Oregon experienced severe dissolved-oxygen problems related to large loads of organically rich waste waters from industries and municipalities. Since the mid-1950 's dissolved oxygen quality has gradually improved owing to low-flow augmentation, the achievement of basinwide secondary treatment, and the use of other waste-management practices. As a result, summer dissolved-oxygen levels have increased, salmon runs have returned, and the overall effort is widely regarded as a singular water-quality success. To document the improved dissolved-oxygen regimen, the U.S. Geological Survey conducted intensive studies of the Willamette during the summer low-flow seasons of 1973 and 1974. During each summer the mean daily dissolved-oxygen levels were found to be higher than 5 milligrams per liter throughout the river. Because of the basinwide secondary treatment, carbonaceous deoxygenation rates were low. In addition, almost half of the biochemical oxygen demand entering the Willamette was from diffuse (nonpoint) sources rather than outfalls. These results indicated that point-source biochemical oxygen demand was no longer the primary cause of dissolved-oxygen depletion. Instead, the major causes of deoxygenation were nitrification in a shallow ' surface active ' reach below Salem and an anomalous oxygen demand (believed to be primarily of benthal origin) in Portland Harbor.
