Northern River Basins Study and the Athabasca River: The Value of Experimental Approaches in a Weight-of-Evidence Assessment

Author(s):  
Alexa Alexander ◽  
Patricia Chambers ◽  
Robert Brua ◽  
Joseph Culp
1979 ◽  
Vol 25 (9) ◽  
pp. 1058-1062 ◽  
Author(s):  
G. G. Geesey ◽  
J. W. Costerton

Epifluorescent microscopy showed as many as 4 × 106 bacteria/mL in the turbid waters of the Athabasca River near the tar sand deposits in northeastern Alberta. The numbers were usually similar upstream and downstream (60 km) from pilot-mining operations. The majority of bacteria existed as free-living cells in spite of the fact there were high concentrations of suspended sediment present (average 220 mg/L) during the ice-free period. Fluctuations in bacterial concentration were positively correlated (r = 0.86, P < 0.05) with total organic carbon concentrations in the river water.


2019 ◽  
Author(s):  
Emma K. T. Carroll ◽  
Steven M. Vamosi

AbstractAcross its native range, Bull Trout (Salvelinus confluentus) extent and abundance are in decline due to historic overharvest and habitat degradation. Because Bull Trout are dependent on extensively connected, cold, clean headwater habitats, fragmentation from land use changes causes difficulty when determining the true extent and health of their populations, with Bull Trout of Alberta’s Eastern Slope region being no exception. Across this region, 431 Bull Trout from 20 sites were sampled from the Athabasca and Saskatchewan River basins and compared using 10 microsatellite loci to characterize within- and among-population genetic variation. The Saskatchewan and Athabasca River basins contained similar levels of heterozygosity but were differentiated from one another. Within the Athabasca River basin, five genetically differentiated clusters were found. Additionally, no isolation-by-distance pattern was observed between these sites. These results suggest these populations have ample genetic diversity, but genetic differentiation should be considered when deciding whether and how to alter connectivity between populations.


River Systems ◽  
2002 ◽  
Vol 13 (3-4) ◽  
pp. 189-194
Author(s):  
Juha Kämäri ◽  
Erkki Alasaarela ◽  
Jouko Inkeröinen ◽  
Satu-Maaria Karjalainen ◽  
Kaisa Heikkinen
Keyword(s):  

2014 ◽  
Vol 62 (3) ◽  
pp. 197-208 ◽  
Author(s):  
Yeugeniy M. Gusev ◽  
Olga N. Nasonova

Abstract The scenario forecasting technique for assessing changes of water balance components of the northern river basins due to possible climate change was developed. Three IPCC global emission scenarios corresponding to different possible scenarios for economic, technological, political and demographic development of the human civilization in the 21st century were chosen for generating climate change projections by an ensemble of 16 General Circulation Models with a high spatial resolution. The projections representing increments of monthly values of meteorological characteristics were used for creating 3-hour meteorological time series up to 2063 for the Northern Dvina River basin, which belongs to the pan-Arctic basin and locates at the north of the European part of Russia. The obtained time series were applied as forcing data to drive the land surface model SWAP to simulate possible changes in the water balance components due to different scenarios of climate change for the Northern Dvina River basin


River Systems ◽  
2002 ◽  
Vol 13 (3-4) ◽  
pp. 353-370 ◽  
Author(s):  
S. Hellsten ◽  
M. Marttunen ◽  
M. Visuri ◽  
A. Keto ◽  
S. Partanen ◽  
...  

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