Evaluation of Juvenile Fall Chinook Salmon Stranding on the Hanford Reach in the Columbia River, 1998 Interim Report.

2001 ◽  
Author(s):  
John Nugent ◽  
Todd Newsome ◽  
Michael Nugent
Keyword(s):  
Chinook Salmon ◽  
Columbia River ◽  
Interim Report ◽  
Hanford Reach

Suitability criteria analyzed at the spatial scale of redd clusters improved estimates of fall chinook salmon (Oncorhynchus tshawytscha) spawning habitat use in the Hanford Reach, Columbia River

2000 ◽  
Vol 57 (8) ◽  
pp. 1636-1646 ◽  
Author(s):  
David R Geist ◽  
Julia Jones ◽  
Christopher J Murray ◽  
Dennis D Dauble
Keyword(s):  
Habitat Use ◽  
Spatial Scale ◽  
Chinook Salmon ◽  
Oncorhynchus Tshawytscha ◽  
Columbia River ◽  
Water Velocity ◽  
Point Pattern ◽  
Spawning Habitat ◽  
Cluster Location ◽  
Hanford Reach

We improved our predictions of fall chinook salmon (Oncorhynchus tshawytscha) habitat use by analyzing spawning habitat at the spatial scale of redd clusters. Spatial point pattern analyses indicated that redd clusters in the Hanford Reach, Columbia River, were consistent in their location from 1994 to 1995. Redd densities were 16.1 and 8.9 redds·ha-1 in 1994 and 1995, respectively, and individual redds within clusters were usually less than 30 m apart. Pattern analysis also showed strong evidence that redds were uniformly distributed within the clusters where interredd distances ranged from 2 to 5 m. Redd clusters were found to occur predominantly where water velocity was between 1.4 and 2 m·s-1, water depth was 2-4 m, and lateral slope of the riverbed was less than 4%. This habitat use represented a narrower range of use than previously reported for adult fall chinook salmon. Logistic regression analysis determined that water velocity and lateral slope were the most significant predictors of redd cluster location over a range of river discharges. Overestimates of available spawning habitat lead to nonachievable goals for protecting and restoring critical salmonid habitat. Better predictions of spawning habitat may be possible if cluster-specific characteristics are used.

Variables Influencing the Presence of Subyearling Fall Chinook Salmon in Shoreline Habitats of the Hanford Reach, Columbia River

2006 ◽  
Vol 26 (2) ◽  
pp. 351-360 ◽  
Author(s):  
Kenneth F. Tiffan ◽  
Loreley O. Clark ◽  
Rodney D. Garland ◽  
Dennis W. Rondorf
Keyword(s):  
Chinook Salmon ◽  
Columbia River ◽  
Hanford Reach

Hyporheic discharge of river water into fall chinook salmon (Oncorhynchus tshawytscha) spawning areas in the Hanford Reach, Columbia River

2000 ◽  
Vol 57 (8) ◽  
pp. 1647-1656 ◽  
Author(s):  
David R Geist
Keyword(s):  
Dissolved Oxygen ◽  
River Water ◽  
Chinook Salmon ◽  
Hyporheic Zone ◽  
Oncorhynchus Tshawytscha ◽  
Columbia River ◽  
Specific Conductance ◽  
Chemical Gradients ◽  
Spawning Areas ◽  
Hanford Reach

Fall chinook salmon (Oncorhynchus tshawytscha) spawned predominantly in areas of the Hanford Reach of the Columbia River where hyporheic water discharged into the river channel. This upwelling water had a dissolved solids content (i.e., specific conductance) indicative of river water and was presumed to have entered highly permeable riverbed substrate at locations upstream of the spawning areas. Hyporheic discharge zones composed of undiluted ground water or areas with little or no upwelling were not used by spawning salmon. Rates of upwelling into spawning areas averaged 1200 L·m-2·day-1 (95% CI = 784-1665 L·m-2·day-1) as compared with approximately 500 L·m-2·day-1 (95% CI = 303-1159 L·m-2·day-1) in nonspawning areas. Dissolved oxygen content of the hyporheic discharge near salmon spawning areas was about 9 mg·L-1 (±0.4 mg·L-1) whereas in nonspawning areas, dissolved oxygen values were 7 mg·L-1 (±0.9 mg·L-1) or lower. In both cases, dissolved oxygen of the river water was higher (11.3 ± 0.3 mg·L-1). Physical and chemical gradients between the hyporheic zone and the river may provide cues for adult salmon to locate suitable spawning areas. This information will help fisheries managers to describe the suitability of salmon spawning habitat in large rivers.

TIMING OF REDD CONSTRUCTION BY FALL CHINOOK SALMON IN THE HANFORD REACH OF THE COLUMBIA RIVER

2013 ◽  
Vol 30 (9) ◽  
pp. 1110-1119 ◽  
Author(s):  
D. B. Hayes ◽  
B. J. Bellgraph ◽  
B. M. Roth ◽  
D. D. Dauble ◽  
R. P. Mueller
Keyword(s):  
Chinook Salmon ◽  
Columbia River ◽  
Hanford Reach
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