Skip To Content

Lake Athabasca


View Larger Map

Location

SK
Canada

How one First Nations group in Alberta reaps a windfall from oilsands development


Year: 2015

Abstract:
In 1983 Dorothy MacDonald, chief of the small Fort McKay First Nation, which sits in the middle of the world's richest oilsands deposits, decided to take on the trucks roaring through her community night and day loaded with lumber for construction sites. She mobilized a roadblock that lasted eight days and eventually pushed the Alberta government to intervene. [ABSTRACT FROM PUBLISHER]

Hydraulic modelling of Peace-Athabasca Delta under modified and natural flow conditions


Author(s): Aitken, B., & Sapach R.

Year: 1994

Abstract:
Construction of the Bennett Dam in British Columbia altered natural fluctuations of downstream flows in the Peace River in Alberta, with major implications for the ecosystem of the Peace-Athabasca Delta. In later years, downstream weirs were constructed to restore the water level regime in the Delta. This report presents the results of a modelling exercise undertaken in an attempt to assess the effect of the weirs and the dam on the Delta water levels during 1985-90, at which time Lake Athabasca water levels were low and it was not clear whether the weirs were functioning properly or if the low water levels were caused by low flows coming from the upper Peace and Athabasca river basins. The methodology uses a one-dimensional hydrodynamic model, suitably modified and calibrated. The appendices include numerous plots of water levels indicating the effects of the weirs and dam on natural conditions.

Hydrochemistry of Phanerozoic Strata northeast Alberta


Author(s): Hitchon, B.

Year: 1991

Abstract:
The Northeast Alberta study area is defined as 55� to 58�N, and 110� to 114� W. A total of 2933 formation water analyses from the area were entered into the Alberta Geological Survey Well Data Base, verified, and subjected to a variety of electronic, manual-electronic and manual culling to leave a final data base of 525 analyses on which this study was based. Salinity ranges from freshwater to 325,000 mg/l, and there are corresponding maximum contents of Cl (200,000 mg/l), Ca (40,000 mg/l) and Mg (8000 mg/l). Nine maps illustrate the distribution of salinity, which is essentially depth (temperature) related except where there is incursion of fresher waters from overlying aquifers. Sulfate is high (500-5500 mg/l) in aquifers in which anhydrite is present (Elk Point hydrostratigraphic unit -- Prairie Formation; Beaverhill Lake aquifer -- Fort Vermilion Formation; and Grosmont aquifer -- Hondo Formation). Formation waters in the Elk Point hydrostratigraphic unit from near the updip solution edge of the Prairie aquiclude (halite) are similar to those of saline springs in the valley of the Athabasca River, which have been shown to originate from solution of evaporites by meteoric water. Based on the composition of their formation waters the aquifers can be combined into groups separated by aquitards, as follows: Viking aquifer (weak Joli Fou aquitard); Grand Rapids aquifer (strong, regional Clearwater aquitard); Clearwater, Wabiskaw and McMurray aquifers; Wabamun and Winterburn aquifers (weak Upper Ireton aquitard); Grosmont aquifer (strong Lower Ireton aquitard); Beaverhill Lake aquifer (significant, regional Prairie aquiclude); Elk Point hydrostratigraphic unit (mainly Keg River aquifer); Precambrian aquiclude. In summary, the formation waters of the Northeast Alberta area are an extension of those in the adjacent Peace River Arch area, exhibit similar characteristics, and have similar origins.

Hydroecological responses of the Athabasca Delta, Canada, to changes in river flow and climate during the 20th century


Year: 2008

Abstract:
We employ water-isotope tracers and multi-proxy paleolimnological records to characterize contemporary controls on water balances of floodplain lakes in the Athabasca Delta, Canada, within the context of its hydroecological evolution over the 20th century. The insight gained from these approaches is necessary to gauge the hydroecological resiliency of the Athabasca Delta to past and future changes in Athabasca River flow regime. Results obtained from three lakes located in different regions of the Athabasca Delta indicate that hydroecological conditions were strongly affected by an engineered meander cut-off on the Athabasca River in 1972, intended to maintain flow in the river main stem, and a natural bifurcation of one of the major distributaries (Embarras River) in 1982, in response to progressive overextension of the delta to the east. Climate warming and naturally declining river discharge have also contributed to directional change. Recent drying trends reconstructed from sediment cores at two of the three lakes are likely representative of rapidly evolving hydroecological conditions in the south-eastern sector, based on mapping of a recent high-magnitude ice-jam flood that failed to recharge this portion of the delta, while wetting in the region of the third lake due to increased frequency of river flooding reflects increasing diversion of Athabasca River flow northward. Our findings highlight the hydroecological sensitivity of the Athabasca Delta to changes in the magnitude and timing of discharge in the Athabasca River and heighten the need for informed management strategies to safeguard the integrity of this unique wetland ecosystem. Copyright © 2008 John Wiley & Sons, Ltd.

Hydrological modelling of reconstructed watersheds using system dynamics


Author(s): Elshorbagy, A., & Jutla A.

Year: 2006

Abstract:
The mining of oil sands in the sub-humid region of Northern Alberta, Canada causes large-scale landscape disturbance, which subsequently requires extensive reclamation to re-establish the surface and subsurface hydrology. The reconstructed watersheds examined in this study are located at the Syncrude Canada Limited mine site, 40 km North of Fort McMurray, Alberta, Canada. The three experimental reconstructed watersheds, with nominal soil thicknesses of 1.0 m, 0.50 m and 0.35 m comprised a thin layer of peat (15-20 cm) over varying thicknesses of secondary (till) soil, have been constructed to cover saline sodic overburden and to provide sufficient moisture storage for vegetation while minimizing surface runoff and deep percolation to the underlying shale overburden. In order to replicate the hydrological behavior, assess the sustainability, and trace the evolution over time of the reclaimed watersheds, a suitable modeling tool is needed. In this research, a model is developed using the system dynamics approach to simulate the hydrological processes in the three experimental reconstructed watersheds and to assess their ability to provide the various watershed functions. The model simulates the vertical and lateral water movement, surface runoff and evapotranspiration within each watershed. Actual evapotranspiration, which plays an important role in the hydrology of the Canadian semi-arid regions, is simulated using an indexed soil moisture method. The movement of water within the various soil layers of the cover is based on parametric relationships in conjunction with conceptual infiltration models. The feedback relationships among the various dynamic hydrologic processes in the watershed are captured in the developed System Dynamic Watershed Model (SDWM). Most hydrological models are evaluated using runoff as the determining criterion for model calibration and validation, while accounting for the movement of moisture in the soil as a water loss. Since one of the primary objectives of a reconstructed watershed is to maintain the natural flora and fauna, it is important to recognize that soil moisture plays an important role in assessing the performance of the reconstructed watersheds. In turn, soil moisture becomes an influential factor for quantifying the health of the reconstructed watershed. The developed model has been calibrated and validated with data for two years (2001-2002), upholding the sensitive relationship between soil moisture and runoff. Accurate calibration of the model based on simulations of soil moisture in the various soil layers improves its overall performance. The model was subsequently used to simulate the three sub-watersheds for five years, with changing the calibrated model parameters to use them as indicators of watershed evolution. The simulated results were compared with the observed values. The results of the study illustrate that all three watersheds are still evolving. Failure to identify a unique parameter set for simulating the watershed response supports the hypothesis of watershed evolution. Soil moisture exchange between the till and peat layers changed with time in all of the watersheds. There was also a modest change in the water movement from the till to shale layers in each of the sub-watersheds. Vegetation is increasing in all of watersheds although there is an indication that one of the sub-watersheds may be sustaining deep rooted vegetation. The results demonstrate the successful application of the system dynamics approach and the developed model in simulating the hydrology of reconstructed watersheds and the potential for using this approach in assessing complex hydrologic systems. Degree:

In Conflict


Author(s): Cryderman, K.

Year: 2013

Abstract:
"Any time that we have differences with somebody like [Jim Boucher], it's a cause for concern," he said. "I think he's been a very balanced First Nation leader with respect to the oil sands industry," Mr. [David Collyer] said. "What I would encourage is for all the parties concerned to try to find a constructive way through it."

Citation:

In the shadow of the oilsands


Year: 2011

Abstract:
A young willow branch, stuck intothe mud by a boater, marks the deepest passage from Lake Athabasca into the Athabasca Delta (top left). Fort Chipewyan's band elders are concerned that water being taken from the Athabasca River to process bitumer~ into oil is contributing to declining water levels. Tar sands processing requires almost four barrels of water for every barrel of crude produced; Alberta Energy projects production will reach 3 million barrels of oil per day by 2018. Aside from employment in the oilsands, commercial fishing is one of Fort Chipewyan's last viable means of making a living (top right). Over the last five years, more and more fish with golf-ball-sized tumours, double tails, and other abnormalities have been caught in Lake Athabasca by commercial fishermen. In 2010, fishermen in Fort Chipewyan were unable to sell any fish commercially due to growing concerns over contamination from pollution, according to Lionel Lepine, the traditional environmental knowledge coordinator for the Athabasca Chipewyan First Nation. Most of the fish caught during 2010 were smoked (bottom left) or thrown to sled dogs (bottom right).

Citation:
[Anonymous] (2011).  In the shadow of the oilsands. 44(5), 26-33. Abstract

In-situ recovery process fluids


Author(s): Peake, E., & Maclean M. A.

Year: 1988

Abstract:
The heavy oils produced from the Alberta oil sands contain cyclic organic compounds together with sulphur and nitrogen. Upon thermal treatment they have the potential to form carcinogenic, mutagenic, and toxic compounds. Recovery of oil by in-situ combustion processes, such as the Combination of Forward Combustion and Waterflood (COFCAW) process, may result in the formation of such biologically active compounds with generation dependent upon operating conditions. The objective of the present research program is to evaluate produced oils and accompanying waters from in-situ combustion processes for possible biological activity. This evaluation is based on biological testing, using the Ames test for mutagenicity and the Microtox test for toxicity, and on the chemical analysis of oils and waters for the presence of known carcinogens. For comparison, oils produced by the less thermally rigorous steam injection process, as well as naturally occurring bitumen, and synthetic crude oil and other oils produced from the Athabasca and Peace River oil sands were examined. Analysis of oils produced by in-situ combustion showed the presence of many carcinogenic and mutagenic compounds, among them the well known carcinogen benzo(a)pyrene (BaP). The BaP content of a mixture of bitumen, cracked oil, and diesel fuel produced by the COFCAW process from the Gregoire Lake pilot project contained 14 µg/g BaP. This compares with 1.5 µg/g in unaltered bitumen and 1 to 3 µg/g in most crude oils. Samples obtained from the Suffield Heavy Oil project which had not undergone rigorous thermal treatment contained from 1.5 to 7.5 µg/g benzo(a)pyrene and emulsion produced by steam injection from the Peace River Pilot project. operated by Shell Canada Resources Limited, contained 2.7 µg/g. An oil produced by dry retorting of the Athabasca oil sands contained 16 µg/g BaP. Oils produced from combustion tube experiments with Athabasca oil sand had a similar BaP content, 2.6 and 4.2 µg/g. Some tars and pitches, especially coal tars, may contain 10 to 100 times more BaP than crude petroleum. Refinery residuals, tars, and oils from Sarnia were found to contain 150 to 1050 µg/g. Benzo(a)pyrene is the best known of the carcinogens found in petroleum, but many other known or suspected carcinogens were found in greater quantities than BaP in the oils produced by in-situ combustion and dry retorting. The assessment of any carcinogenic hazard associated with petroleum is difficult. Animal tests are expensive and time consuming; therefore, short term bio-assays for mutagenic properties such as the Ames test, together with chemical analysis, are employed. Positive results in the Ames test are not an absolute indicator of carcinogenic potential. Mutagenicity does not in all cases imply carcinogenicity; however, those polycyclic aromatic hydrocarbons which are carcinogenic are also mutagenic in the Ames test when appropriate enzymes are included. Mutagenic activity was found with the Ames test in oils produced from the Gregoire Lake. Suffield, and Peace River in-situ pilot projects and in vacuum gas oil and pitch from the Peace River diluent recovery unit. The mutagenicity was less than predicted from the amount of carcinogenic aromatic compounds found by chemical analysis. The complex mixture of hydrocarbons which comprises these oils suppressed the activity of the carcinogens in the Ames test. Thus the Ames test was found to be an indicator of mutagenic activity but not a quantitative method for assessing the relative mutagenicity of oils. Synthetic crude oil produced from Athabasca bitumen displayed some mutagenic activity but, despite the presence of BaP, the bitumen itself did not. Waters produced during in-situ recovery of oil by both steam stimulation and combustion processes were toxic to aquatic organisms as determined by the Microtox bioluminescence assay. EC 50 values, the effective concentration of toxicant causing a 50% decrease in the light output of a photoluminescent bacteria, ranged from 0.30 to 11. The toxicity was caused partly by volatile organic compounds, primarily alkyl substituted benzenes, and partly by extractable organic compounds including phenols, organic acids, and hydrocarbons with no single class of compounds solely responsible for the observed toxicity. Wastewaters from the dry retorting process were more toxic than waters produced by in-situ combustion and contained many aromatic hydrocarbons and nitrogen compounds known to be biologically active. The chemical analyses and limited biological testing carried out in this study detected no strong mutagenic or carcinogenic hazard associated with in-situ recovery of heavy oil by combustion and steam injection. The relative hazard is probably marginally greater than that associated with production of conventional light crude oils but far less than might be expected from coal liquefaction processes or from disposal of refinery residuals. The hazard associated with dry retorting is greater than that from in-situ recovery methods and care should be taken in the handling of both products and wastewaters from this process.

Indigenous knowledge of the land and protected areas: Fond du Lac Denesuline Nation and the Athabasca Sand Dunes, Saskatchewan


Author(s): Yantz, J. L.

Year: 2005

Abstract:
Many Aboriginal Nations in Canada seek to be involved in protected areas planning and overall land management. In a partnership study conducted with Fond du Lac Denesuline Nation in northern Saskatchewan, the cultural and ecological uses of land and resources were documented for the Athabasca sand dunes region on the south shore of Lake Athabasca. Denesuline land uses provided a basis to discuss the role of traditional land use and indigenous knowledge in the co-stewardship of protected areas in Saskatchewan. Gathering indigenous knowledge in Fond du Lac Denesuline Nation involved a participatory research design developed through community meetings and study team working groups. Interviews and individual map biographies resulted in a collection of composite maps. The thesis does not include material considered confidential by indigenous knowledge holders. The partnership study was part of a larger project entitled "Respecting and Preserving Fond du Lac Denesuline Indigenous Knowledge: thai gayé, ethedustél túe", published by Fond du Lac Denesuline Nation (2004). (Abstract shortened by UMI.)

Indigenous peoples' rights in Alberta's oil sands : The roles of corporation and the state


Author(s): Fekete, S.

Year: 2009

Abstract:
Corporate actors are increasingly becoming powerful entities in this era of globalization. While the state remains the primary duty bearer in protecting and realizing the rights of its citizens, corporations now have an increased role in this regard. Voluntary mechanisms guiding corporate conduct have emerged to address this fact. In Canada’s Athabasca, Peace River and Cold Lake regions, oil corporations have the increased challenge of operating on the traditional land of indigenous populations, who have been marginalized since colonization. While many indigenous groups seek protect their traditional lifestyle, activities by oil corporations seem to undermine this effort. Human rights and social responsibility norms are increasingly found in corporate policies. Yet the forms which these take are contested and considered unsatisfactory by some. This thesis seeks to identify to what extent corporations have accepted human rights and social responsibility norms, to evaluate whether norm acceptance can be clearly related to performance, to see if actions taken by oil corporations guarantee that indigenous rights are protected and determine what actions the provincial and federal governments can undertake to further complement corporate efforts.

Inter-annual variations in water yield to lakes in northeastern Alberta: Implications for estimating critical loads of acidity


Year: 2010

Abstract:
Stable isotopes of water were applied to estimate water yield to fifty lakes in northeastern Alberta as part of an acid sensitivity study underway since 2002 in the Athabasca Oil Sands Region (AOSR). Herein, we apply site-specific water yields for each lake to calculate critical loads of acidity using water chemistry data and a steady-state water chemistry model. The main goal of this research was to improve site-specific critical load estimates and to understand the sensitivity to hydrologic variability across a Boreal Plains region under significant oil sands development pressure. Overall, catchment water yields were found to vary significantly over the seven year monitoring period, with distinct variations among lakes and between different regions, overprinted by inter-annual climate-driven shifts. Analysis of critical load estimates based on site-specific water yields suggests that caution must be applied to establish hydrologic conditions and define extremes at specific sites in order to protect more sensitive ecosystems. In general, lakes with low (high) water yield tended to be more (less) acid sensitive but were typically less (more) affected by interannual hydrological variations. While it has been customary to use long-term water yields to define a static critical load for lakes, we find that spatial and temporal variability in water yield may limit effectiveness of this type of assessment in areas of the Boreal Plain characterized by heterogeneous runoff and without a long-term lake-gauging network. Implications for predicting acidification risk are discussed for the AOSR.

Interim report on a hydrogeological investigation of the Muskeg River basin, Alberta


Author(s): Schwartz, F. W.

Year: 1979

Abstract:
The Muskeg River in northeast Alberta drains a large highland area east of the Athabasca River. The availability of thick, oil sands deposits at depths less than 30 m in parts of the watershed makes this area an obvious candidate for future mining development. The results of this detailed, chemically-based study of waters from major portions of the hydrologic cycle--precipitation, surface water, and groundwater, in addition to providing descriptive details of pre-mining baseline states has provided useful information about groundwater and surface water processes in the watershed. Baseflow, as it is known in streams in the southern part of the province, probably exists during a few winter months when standing water in muskeg and shallow lakes is frozen and ceases to contribute to streamflow. During times of the year when the muskegs are unfrozen they constitute the bulk of the streamflow. The results of chemically-based hydrograph separation techniques indicate that 12 to 40.% of streamflow during the late spring, summer and fall months consists of groundwater with the remainder coming from lake and muskeg drainage, as well as direct precipitation on the stream channels. This preliminary report will form a basis for more detailed evaluation on systems in the Muskeg River basin.

Interim report on characterization and utilization of peat in the Athabasca oil sands area


Year: 1979

Abstract:
Two sites have been established for the study of stored peat. These are located at Evansburg ; Alberta and on the Syncrude Canada Ltd. lease at Mildred Lake, Alberta. Fibric and mesic moss peat and fen peat have been investigated in terms of their physical, chemical and microbiological properties. Such material will eventually be stored at mining sites in the AOSERP study area, presumably for later use as an amendment to aid reclamation procedures. The main purpose of this research was to quantify the changes in chemical, physical and microbiological properties that are likely to take place in the peat after a period of prolonged storage. A freeze-dry, air-dry, and thaw experiment was initiated to assess the rate of decomposition in stores peat. This indicated that drying affects most physical properties of peat. Drying affects the microbial activity in peat as measured by enzyme activity and CO2 production. Generally freeze-drying appeared less detrimental than air drying. The stored material at Evansburg was essentially composed of peat, whereas at Mildred Lake the material was a heterogeneous mixture of peat and inorganic material (sand, silt and clay). Both sites were instrumented with fiberglass temperature-moisture cells in order to record the annual variation in temperature and moisture in the stored material. Cellulotytic activity was measured by imbedding filter paper in the stored material at both Evansburg and Mildred Lake. Initial results indicate greater cellulose decomposition in the mixed peat material at Mildred Lake than at Evansburg. A higher rate of CO2 evolution from the Mildred Lake samples indicated greater microbiological activity at this site. This increased activity may be attributed to the presence of the inorganic constituents in the pile and to the application of commercial fertilizer. In the investigation of the Mildred Lake stored material, positive correlations have been established between carbon content, and microbiological activity, enzyme activity, and cation exchange capacity. Those samples containing the greatest amount of peat were highest in microbiological and enzyme activity thus indicating a possible greater rate of decomposition. Unlike the stored material, undisturbed peat near Mildred Lake showed little activity. A similar investigation into the activity in the peat storage pile at Evansburg will be undertaken in 1978.

Inventory of selected raptor colonial and sensitive bird species in the Athabasca oil sands area of Alberta


Year: 1980

Abstract:
A three-year inventory of selected rare, endangered and sensitive bird species in the Athabasca Oil Sands area of northeastern Alberta was completed in the late summer of 1977. Aerial and ground surveys of the Alberta Oil Sands Environmental Research Program (AOSERP) study area and selected adjacent areas were conducted. Three major habitat types were investigated: the boreal mixed-wood forest of the Birch Mountains area; the jack pine sandplains south of Lake Athabasca and the Canadian Shield north of Lake Athabasca. Three major groups of birds were surveyed: raptors, colonial birds, and specified sensitive species. Locations of nest sites and colonies were noted and described. No attempt was made to determine the absolute abundance of each species in the AOSERP study area, as the aerial surveillance techniques employed do not justify such an estimation. The exception to this were two species whose total population in the AOSERP study area was restricted to very small areas and therefore could be readily determined: White Pelicans and Peregrine Falcons. Each of these species was investigated in considerable detail and, the data reported in separate publications. Recommendations were made for: 1. Further, more intensive surveys of part of the AOSERP study area in order to determine phenology and numbers of initial breeders more accurately; and 2. Additional surveys of the Canadian Shield area which was incompletely surveyed during this study. Observations of foraging behaviour of a breeding pair of Bald Eagles were conducted in the Birch Mountains, 90 km northwest of Fort McMurray, Alberta, from mid-summer to early fall, 1977. Bald Eagles foraged almost exclusively on fish, although gull wings and a merganser skull were found below nest trees. Nest trees were generally located less than 50 m from water. Active nests were more frequently located on islands and peninsulas. The nest trees were usually tall and broad and included jack pine, spruce, and less frequently trembling aspen. Live trees were preferred over dead trees. In the Birch Mountains, Bald Eagles were relatively sensitive to boat traffic and approaches by humans on foot. Further work is strongly recommended: 1. To further outline critical breeding and foraging habitat criteria; and 2. To assess the potential impact of disturbance on breeding and foraging Bald Eagles.

Investigations of mercury concentrations in walleye and other fish in the Athabasca River ecosystem with increasing oil sands developments


Author(s): Evans, M. S., & Talbot A.

Year: 2012

Abstract:
Recent studies have reported an increasing trend of mercury concentrations in walleye (Sander vitreus) from the Athabasca River, north eastern Alberta (Canada); these studies were based on three years of comparison and attributed the mercury increase to expanding oil sands developments in the region. In order to conduct a more comprehensive analysis of mercury trends in fish, we compiled an extensive database for walleye, lake whitefish (Coregonus clupeaformis), northern pike (Esox lucius) and lake trout (Salvelinus namaycush) using all available data obtained from provincial, federal, and industry-funded monitoring and other programs. Evidence for increasing trends in mercury concentrations were examined for each species by location and year also considering fish weight and length. In the immediate oil sands area of the Athabasca River, mercury concentrations decreased (p < 0.001) in walleye and lake whitefish over 1984-2011. In western Lake Athabasca and its delta, mercury concentrations decreased (p < 0.0001) in northern pike (1981-2009) although no trend was evident for walleye (1981-2005) and lake trout (1978-2009). Mercury concentrations in lake trout from Namur Lake, a small lake west of the oil sands area, were higher in 2007 than 2000 (p < 0.0001); it is difficult to ascribe this increase to an oil sands impact because similar increases in mercury concentrations have been observed in lake trout from similar sized lakes in the Northwest Territories. While mercury emissions rates have increased with oil sands development and the landscape become more disturbed, mercury concentrations remained low in water and sediments in the Athabasca River and its tributaries and similar to concentrations observed outside the development areas and in earlier decades. Our fish database was assembled from a series of studies that differed in study purpose, design, and analytical methods. Future monitoring programs investigating mercury trends in fish should be more rigorous in their design.

Investigations of mercury concentrations in walleye and other fish in the Athabasca River ecosystem with increasing oil sands developments


Author(s): Evans, M. S., & Talbot A.

Year: 2012

Abstract:
Recent studies have reported an increasing trend of mercury concentrations in walleye (Sander vitreus) from the Athabasca River, north eastern Alberta (Canada); these studies were based on three years of comparison and attributed the mercury increase to expanding oil sands developments in the region. In order to conduct a more comprehensive analysis of mercury trends in fish, we compiled an extensive database for walleye, lake whitefish (Coregonus clupeaformis), northern pike (Esox lucius) and lake trout (Salvelinus namaycush) using all available data obtained from provincial, federal, and industry-funded monitoring and other programs. Evidence for increasing trends in mercury concentrations were examined for each species by location and year also considering fish weight and length. In the immediate oil sands area of the Athabasca River, mercury concentrations decreased (p < 0.001) in walleye and lake whitefish over 1984–2011. In western Lake Athabasca and its delta, mercury concentrations decreased (p < 0.0001) in northern pike (1981–2009) although no trend was evident for walleye (1981–2005) and lake trout (1978–2009). Mercury concentrations in lake trout from Namur Lake, a small lake west of the oil sands area, were higher in 2007 than 2000 (p < 0.0001); it is difficult to ascribe this increase to an oil sands impact because similar increases in mercury concentrations have been observed in lake trout from similar sized lakes in the Northwest Territories. While mercury emissions rates have increased with oil sands development and the landscape become more disturbed, mercury concentrations remained low in water and sediments in the Athabasca River and its tributaries and similar to concentrations observed outside the development areas and in earlier decades. Our fish database was assembled from a series of studies that differed in study purpose, design, and analytical methods. Future monitoring programs investigating mercury trends in fish should be more rigorous in their design.

Investigations of poly-chlorinated biphenyls in bottom sediments of the Bear-Wapiti-Smoky-Peace and Upper Athabasca River systems, 1989-2000


Author(s): Hazewinkel, R., & Noton L.

Year: 2004

Abstract:
Studies of contaminant distributions by the Northern River Basins Study (NRBS) revealed high levels of PCBs in fish in the upper Athabasca and in the Wapiti-Smoky rivers, relative to other areas in the basins. In response to recommendations of the NRBS, the purpose of this work was to investigate the source and reasons for the PCB contamination. In co-ordination with other projects under the Northern Rivers Ecosystem Initiative (NREI) on fish, water, and benthos, this project investigated PCBs in river bottom sediments to see if there were spatial or temporal patterns that might identify the source(s) of contamination.

Investigations of the spring spawning fish populations in the Athabasca and Clearwater Rivers upstream from Fort McMurray: Volume I


Author(s): Tripp, D. B., & McCart P. J.

Year: 1979

Abstract:
Fisheries investigations were undertaken in the spring of 1978 (28 April to 25 June) in the Athabasca and Clearwater rivers upstream of Fort McMurray. The major objectives of the studies were to determine what spring spawners utilized these sections of the Athabasca and Clearwater rivers; to locate and describe their spawning grounds; and to describe the timing of spawning, hatching, and emergence in relation to environmental factors such as water temperature, turbidity, dissolved oxygen concentrations, and stream flow. Large numbers of longnose suckers spawned during mid May in the Athabasca River from Fort McMurray upstream to the Cascade Rapids, the same area used by fall spawning lake whitefish. The major concentrations were located just below the Mountain and Cascade rapids. There was no evidence of major spawning concentrations of this species elsewhere in the present study area. Shortly after spawning, longnose suckers left the project study area and presumably returned to the Peace-Athabasca Delta. Northern pike and burbot spawning and rearing areas were identified in the Clearwater River upstream of its junction with the Christina River. There was little or no spawning by either species in the Clearwater River downstream of the Christina River or in the Athabasca River upstream of Fort McMurray. No major concentrations of spawning walleye were located. However, based on the distribution of young-of-the-year, it appears that at least some walleye spawned at various localities in the Athabasca River from the Mountain Rapids to as far upstream as the Grand Rapids. There is no evidence that walleye spawned in the Clearwater River within the AOSERP study area. Lake whitefish young-of-the-year probably emerged and moved downstream out of the present study area before spring breakup. Longnose sucker young-of-the-year emerged at the beginning of June followed by pike, walleye, and white sucker young-of-the year later in June. The Athabasca River, and to a lesser extent the Clearwater River, provide valuable habitat for a number of minor species including flathead chub, longnose dace, and lake chub. Large numbers of juvenile goldeye also use the area as feeding grounds during the open-water period.

Isotopic evidence for oil sands petroleum coke in the Peace–Athabasca Delta


Year: 2015

Abstract:
The continued growth of mining and upgrading activities in Canada’s Athabasca oil sands (AOS) region has led to concerns about emissions of contaminants such as polycyclic aromatic hydrocarbons (PAHs). Whereas a recent increase in PAH emissions has been demonstrated within around 50 km of the main center of surface mining and upgrading operations, the exact nature of the predominant source(s) and the geographical extent of the deposition are still under debate. Here, we report a century-long source apportionment of PAHs using dual (δ2H, δ13C) compound-specific isotope analysis on phenanthrene deposited in a lake from the Athabasca sector of the Peace–Athabasca Delta situated ∼150 km downstream (north) of the main center of mining operations. The isotopic signatures in the core were compared to those of the main potential sources in this region (i.e., unprocessed AOS bitumen, upgrader residual coke, forest fires, coal, gasoline and diesel soot). A significant concurrent increase (∼55.0‰) in δ2H and decrease (∼1.5‰) in δ13C of phenanthrene over the last three decades pointed to an increasingly greater component of petcoke-derived PAHs. This study is the first to quantify long-range (i.e., >100 km) transport of a previously under-considered anthropogenic PAH source in the AOS region.

Enter keywords or search terms and press Search

Search this site


Subscribe to the site

Syndicate content

Bookmark and Share