Skip To Content

Lake Athabasca


View Larger Map

Location

SK
Canada

Genetic population structure of walleye populations in the Athabasca River basin


Author(s): Burke, L.

Year: 2008

Abstract:
This report provides a summary of a field program undertaken to study the population genetic structure of walleye. Samples were collected from Lake Athabasca, a site north of Fort McMurray, McLeod River, Lesser Slave Lake, Calling Lake, and Fawcett Lake.

Geochemical and isotopic investigations of lake sediments from the Athabasca oil sands region


Author(s): Stanners, F. M.

Year: 2014

Abstract:
The Athabasca oil sands region (AOSR) is one of the largest unconventional oil reserves globally, and is projected to become increasingly important as conventional oil resources are depleted. This has lead to increasing concerns about the impact of industrial emissions on surrounding ecosystems. Four sediment cores from three lakes in northeastern Alberta and northwestern Saskatchewan were analyzed to assess the type and quantity of organic matter (OM) in sediments, and whether there had been any impact from industrial emissions originating in the AOSR on lake sediment geochemistry. Analyses showed that sediments in all three lakes are organic-rich, and the OM is dominantly derived from authochthonous primary production of phytoplankton and bacteria. Stable N and S isotope analyses of sediments, deposited between 1850 and 2010 showed no clear impact from industrial emissions in the AOSR.

Geotechnical properties of oil sands and related strata


Author(s): Kosar, K. M.

Year: 1989

Abstract:
The geotechnical response of an oil sands reservoir to in situ heating or to fluid pressure increase results in stresses and deformations which affect hydraulic fracture propagation, formation shearing, well casing performance, the stability of underground openings (uncased wells, tunnels and shafts), and the magnitude of surface heave. The analytical procedures used to model the above mechanisms must simulate fully-coupled thermal-mechanical-fluid flow behaviour (heat consolidation analysis). For these procedures to be utilized for quantitative geotechnical design, material models must be developed and implemented based on an intimate and fundamental understanding of the geotechnical behaviour of the geologically complex and variable reservoir materials. The research documented in this thesis investigates and evaluates the geotechnical behaviour of oil sands and related strata through representative laboratory testing. The geomechanical behaviour of Athabasca and Cold Lake oil sands, as well as that of overlying, underlying and interbedded strata over a range in temperature of 20$\sp\circ$C to 300$\sp\circ$C and effective confining stresses to 7 MPa was investigated. The fundamental influence of temperature, pressure, stress and temperature path, time and history of stress on shear strength, stress-strain and thermal volume change behaviour is examined. The use of geological and geotechnical facies to analyze and interpret laboratory test results is described. The mechanical properties of Athabasca and Cold Lake formation materials were found to be dependent on temperature, pressure and stress path followed during the test. Cold Lake Clearwater Formation oil sands were weaker and more deformable than Athabasca McMurray Formation oil sands and contained minerals which were more susceptible to pressure and temperature induced grain breakage. As a result, the geotechnical properties vary significantly for the two oil sands. The geotechnical behaviour of oil sands was also found to be dependent on the amount of fines present in the specimen. The Clearwater Formation shale properties were strongly affected by temperature. During heating, the shale shows a volume decrease due to structural breakdown. After slow heating, the shales exhibit higher strengths and modulii. The majority of geotechnical properties of oil sands and associated strata vary non-linearly with pressure and temperature.

Gill and liver histopathological changes in yellow perch (Perca flavescens) and goldfish (Carassius auratus) exposed to oil sands process-affected water


Year: 2006

Abstract:
The extraction of bitumen from the Athabasca oil sands (Alberta, Canada) produces significant volumes of process-affected water containing elevated levels of naphthenic acids (NAs), ions, and polycyclic aromatic hydrocarbons (PAHs). The sublethal response of aquatic organisms exposed to oil sands constituents in experimental aquatic environments that represent possible reclamation options has been studied. In this study, the effects of process-affected waters on gill and liver tissues in yellow perch (Perca flavescens) and caged goldfish (Carassius auratus) held in several reclamation ponds at Syncrude's Mildred Lake site have been assessed. Following a 3-week exposure, significant gill (epithelial cell necrosis, mucous cell proliferation) and liver (hepatocellular degeneration, inflammatory cell infiltration) histopathological changes were noted in fish held in waters containing high levels of oil sands process-affected water. In addition, measurements of gill dimensions (gill morphometrical indices) proved sensitive and provided evidence of a physiological disturbance (gas exchange) with exposure to oil sands materials. Due to the complexity of oil sands process-affected water, the cause of the alterations could not be attributed to specific oil sands constituents. However, the histopathological parameters were strong indicators of exposure to oil sands process-affected water and morphometrical data were sensitive indicators of pathological response, which can be used to identify the interactive effects of ionic content, NAs, and PAHs in future laboratory studies

Glacial Lake Agassiz: The northwest outlet and paleoflood spillway, N. W. Saskatchewan and N. E. Alberta


Author(s): Fisher, T. G.

Year: 1993

Abstract:
The Clearwater-lower Athabasca spillway was eroded by a catastrophic flood and extends 233 km from northwestern Saskatchewan into northeast Alberta, ending at the Late Pleistocene Athabasca braid delta, 85 km north of Fort McMurray. At the head of the spillway, an anastomosing complex of erosional channels are separated by streamlined-shaped erosional residual islands (hills). Smaller localized upper scoured zones consisting of channels and erosional residuals are regularly spaced along margins of the spillway. Flood deposits within the spillway are sparse, but are present where the spillway widens or along its upper scoured zones. Representative flood facies consist of (1) boulder lags; (2) poorly sorted boulder gravel; (3) cross-stratified sands and gravels; and, (4) upper flow regime sandy plane beds. The principle depositional feature is the Late Pleistocene Athabasca braid delta which was built into glacial Lake McConnell. Paleohydraulic calculations of the flood from the northwest outlet of glacial Lake Agassiz provide estimates of peak discharges, ranging from 1.2 to $9.1 \times 10\sp6$ m$\sp3$s$\sp{-1}$. The combination of shorelines and glaciolacustrine sediments indicate a lake transgression in the upper Churchill watershed of west-central Saskatchewan. Geomorphic and sedimentological evidence for a transgression, and six radiocarbon ages (average 9869 B.P.) from associated flood deposits strongly supports glacial Lake Agassiz as the source in the upper Churchill river watershed during a high stand of the Emerson high-water phase. Following closure of the eastern outlets at the onset of the Emerson Phase, glacial Lake Agassiz transgressed into the recently deglaciated and isostatically depressed upper Churchill watershed to a present elevation of 490 m at the head of the Clearwater-lower Athabasca spillway, an elevation coincident with the lowest point along the Churchill/Mackenzie drainage divide. The drainage divide consisting of till or the Beaver River moraine, was breached and incised resulting in a lowering of glacial Lake Agassiz by 52 m to a stable elevation of 438 m. In the process, 21,000 km$\sp3$ of water was released to the Arctic Ocean via the Mackenzie River, which raised global sea level by 5.8 cm.

Governance of impacts to land and water resources from oil sands development in Alberta


Author(s): Jordaan, S. M.

Year: 2011

Abstract:
Transitions to unconventional fossil fuels may result in significant impacts to land and water. This review describes the governance challenges and successes related to land and water impacts of oil sands development in Alberta, resulting in four key conclusions. First, the province of Alberta appears to have developed robust systems for governance of impacts that are relatively easy to predict and measure over short timescales, such as water use. However, it has been less successful in developing governance mechanisms that deal with more complicated and subtle tasks such as those concerning cumulative effects, landscape fragmentation and water quality. Second, there are large variations in management on crown and aboriginal lands. Development on land surrounding Aboriginal territory may infringe upon constitutionally protected Aboriginal and Treaty rights and requires consultation with Aboriginal communities. Third, though impacts from oil sands development can be large, it is important to understand them in relative sense, particularly for water use. Looking across the whole province, agricultural water use has resulted in degraded watersheds in the southern portions of the province where water is scarce, leading to the emergence of water markets. By contrast, water withdrawn for oil sands development is from watersheds that do not have similar water constraints. Finally, there is large technological potential for mitigating water impacts. Whether emerging technologies are used will depend on if water policies can keep at the same pace as technological development. This review demonstrates that governance can be challenging where impacts are not easily quantified. One key recommendation is to ensure independent scientific research is undertaken to resolve disputes surrounding the magnitude of impacts, such as changes to water quality. Such research can support the development of governance systems. This review may be used more broadly to develop policies and regulations in other regions that are experiencing similar environmental impacts from growing unconventional fossil fuel production.

Citation:
Jordaan, S. M. (2011).  Governance of impacts to land and water resources from oil sands development in Alberta. Unpublished manuscript, International Relations and Pacific Studies, University of California, San Diego, California. Retrieved from ilar. ucsd. edu. Abstract

Gregoire Lake monitoring program: Six month report April to September 1979


Author(s): Murray, W. A.

Year: 1981

Abstract:
This report presents a summary of the meteorological data collected by the meteorological tower network in the Gregoire Lake region of northeast Alberta during the spring and summer of 1979. The network was established to help monitor the impact on the environment by the Amoco Canada Co. Ltd. pilot plant. A previous report, prepared by Athabasca Research Corporation (Ferguson 1979), presented an analysis of the winter 1978-79 data. A discussion is presented of the theoretical meteorological background including synoptic and mesoscale influences on the dispersion of effluents emitted into the atmosphere. Field dispersion experiments in the oil sands area are reviewed briefly. The statistics of the various weather elements are discussed. Wind velocity was measured at the 30 m tower level at Anzac, the Gregoire Lake Provincial Park, the Amoco pilot plant, and Stoney Mountain. Temperature, relative humidity, vertical velocity, precipitation, barometric pressure, and solar radiation were to be monitored at the pilot plant. The system for recording these data was not completely debugged by the end of the summer so data are not available yet. The meteorological statistics and the case studies indicated that when the air is stable or neutral, the regional airflow is deflected to follow the contours of the ridge, which is south of Gregoire Lake, and parallel to the Athabasca and Clearwater rivers. Under convectively unstable conditions, air flow tended to be upslope at the plant site and on Stoney Mountain, but similar to the regional flow at the valley stations. Wind speeds were generally light in agreement with long-term records in the oil sands area. Temperatures also followed the longterm trends. Examination of local meteorological and upper air data from Edmonton and Fort Smith indicated that the high concentrations of nitric oxide recorded on 27 September 1979 may have been related to low mixing heights. The source was probably not the pilot plant because the wind had been from the northwest for several hours prior to the incident. It is recommended that the reliability of data acquisition be improved. A study such as this one depends on valid, complete data it is of little value to collect data which has uncertainties as to time, calibration, or scale zeroes.

Guide to the Athabasca oil sands area


Year: 1973

Abstract:
The oil sands area is located in northeastern Alberta adjacent to the Canadian Shield (Fig. 1). The main drainage of the area is provided by the Athabasca-Clearwater system, the valleys of which are incised into a broad, muskeg-covered interior plain to depths of 200 to 300 feet. The tributary streams originate in three highland areas (Fig. 2): the Birch Mountains to the west of the Athabasca River which rise to about 2,700 feet, Stony Mountain south of Fort McMurray which reaches an elevation of 2,500 feet, and Muskeg Mountain to the east of the Athabasca River which rises gradually to 1,900 feet. To the southwest of the area, between Birch Mountain and Stony Mountain and north of the eastward flowing Athabasca River, is a subdued highland area with gentle slopes called the Thickwood Hills. These hills give rise to northward flowing tributaries of the MacKay River, and a few short streams flowing southward to the Athabasca. A number of shallow lakes are located in the area, the largest and most numerous of which are located on the top of the Birch Mountains and form an interconnected chain of lakes, which flow into the Ells River. These are called Eaglenest, Gardiner, and Namur Lakes. The only lakes of any size south of Fort McMurray are Algar and Gregoire Lakes. McClelland Lake, which is located in the lowlands northeast of Bitumount, is an area of internal drainage.

Has Alberta oil sands development altered delivery of polycyclic aromatic compounds to the Peace-Athabasca Delta?


Year: 2012

Abstract:
BACKGROUND: The extent to which Alberta oil sands mining and upgrading operations have enhanced delivery of bitumen-derived contaminants via the Athabasca River and atmosphere to the Peace-Athabasca Delta (200 km to the north) is a pivotal question that has generated national and international concern. Accounts of rare health disorders in residents of Fort Chipewyan and deformed fish in downstream ecosystems provided impetus for several recent expert-panel assessments regarding the societal and environmental consequences of this multi-billion-dollar industry. Deciphering relative contributions of natural versus industrial processes on downstream supply of polycyclic aromatic compounds (PACs) has been identified as a critical knowledge gap. But, this remains a formidable scientific challenge because loading from natural processes remains unknown. And, industrial activity occurs in the same locations as the natural bitumen deposits, which potentially confounds contemporary upstream-downstream comparisons of contaminant levels. METHODS/PRINCIPAL FINDINGS: Based on analyses of lake sediment cores, we provide evidence that the Athabasca Delta has been a natural repository of PACs carried by the Athabasca River for at least the past two centuries. We detect no measureable increase in the concentration and proportion of river-transported bitumen-associated indicator PACs in sediments deposited in a flood-prone lake since onset of oil sands development. Results also reveal no evidence that industrial activity has contributed measurably to sedimentary concentration of PACs supplied by atmospheric transport. CONCLUSIONS/SIGNIFICANCE: Findings suggest that natural erosion of exposed bitumen in banks of the Athabasca River and its tributaries is a major process delivering PACs to the Athabasca Delta, and the spring freshet is a key period for contaminant mobilization and transport. This baseline environmental information is essential for informed management of natural resources and human-health concerns by provincial and federal regulatory agencies and industry, and for designing effective long-term monitoring programs for the lower Athabasca River watershed.

Has Alberta oil sands development altered delivery of polycyclic aromatic compounds to the Peace-Athabasca Delta?


Year: 2012

Abstract:
BACKGROUND: The extent to which Alberta oil sands mining and upgrading operations have enhanced delivery of bitumen-derived contaminants via the Athabasca River and atmosphere to the Peace-Athabasca Delta (200 km to the north) is a pivotal question that has generated national and international concern. Accounts of rare health disorders in residents of Fort Chipewyan and deformed fish in downstream ecosystems provided impetus for several recent expert-panel assessments regarding the societal and environmental consequences of this multi-billion-dollar industry. Deciphering relative contributions of natural versus industrial processes on downstream supply of polycyclic aromatic compounds (PACs) has been identified as a critical knowledge gap. But, this remains a formidable scientific challenge because loading from natural processes remains unknown. And, industrial activity occurs in the same locations as the natural bitumen deposits, which potentially confounds contemporary upstream-downstream comparisons of contaminant levels. METHODS/PRINCIPAL FINDINGS: Based on analyses of lake sediment cores, we provide evidence that the Athabasca Delta has been a natural repository of PACs carried by the Athabasca River for at least the past two centuries. We detect no measureable increase in the concentration and proportion of river-transported bitumen-associated indicator PACs in sediments deposited in a flood-prone lake since onset of oil sands development. Results also reveal no evidence that industrial activity has contributed measurably to sedimentary concentration of PACs supplied by atmospheric transport. CONCLUSIONS/SIGNIFICANCE: Findings suggest that natural erosion of exposed bitumen in banks of the Athabasca River and its tributaries is a major process delivering PACs to the Athabasca Delta, and the spring freshet is a key period for contaminant mobilization and transport. This baseline environmental information is essential for informed management of natural resources and human-health concerns by provincial and federal regulatory agencies and industry, and for designing effective long-term monitoring programs for the lower Athabasca River watershed.

Has Alberta oil sands development increased far-field delivery of airborne contaminants to the Peace-Athabasca Delta?


Year: 2012

Abstract:
Identifying potential regional contamination by Alberta oil sands industrial emissions on sensitive ecosystems like the Peace–Athabasca Delta, ~ 200 km to the north, requires knowledge of historical contaminant levels and trends. Here we provide some of these critically-needed data, based on analysis of metals in a sediment core from an upland precipitation-fed lake in the delta. The lake is well-situated to record the anthropogenic history of airborne contaminant deposition for this region. Sediment records of metals of concern (Pb, Sb, As, Hg) reflect early to mid-20th century increases in North American industrial emissions, followed by reduced emissions due to improved industrial practices after 1950–70. Notably, Pb, Sb, As and Hg have declined since the onset of Alberta oil sands production, belying concerns that this activity has enhanced far-field atmospheric delivery of these contaminants to the delta.

Have atmospheric emissions from the Athabasca oil sands impacted lakes in northeastern Alberta, Canada?


Year: 2008

Abstract:
The rate of bitumen extraction in northeastern Alberta, Canada, is outpacing the state of ecological understanding of the region, so that the extent of potential disturbances caused by atmospheric deposition remains largely unknown. Atmospheric SO2 emissions from the Fort McMurray region of Alberta (∼300 t·day–1) constitute ∼5% of the Canadian total. Combined with an estimated NOx production of ∼300 t·day–1, these emissions have the potential to acidify surface waters. Diatom assemblages in dated sediment cores from eight acid-sensitive lakes were analyzed to assess the effects of acidifying emissions on boreal lake ecosystems. There is no evidence that these lakes have become acidified. Instead, many of the lakes show characteristic changes towards greater productivity and occasionally greater alkalinity. The absence of evidence for acidification does not imply that emissions from the Oil Sands are environmentally benign, but rather suggests that the biogeochemistry of these lakes differs fundamentally from well-studied acidified counterparts in northern Europe and eastern North America. Complex interactions involving in-lake alkalinity production, internal nutrient loading, and climate change appear to be driving these lakes towards the new ecological states reported.

Heavy metal dynamics in the Athabasca River: Sediment concentrations prior to major Alberta oil sands development


Author(s): Allan, R. J., & Jackson T.

Year: 1977

Abstract:
Exploitation of the bituminous sands may elevate heavy metal levels in the sediments of drainage systems of the AOSERP area via waterborne or airborne emissions. One hundred and six dredged sediments and twenty-four sediment cores were collected from the Athabasca River system from just above Fort McMurray to the confluence of Riviere des Rochers with the Slave River. A preliminary sample suite representing all of the drainage units and textural variations was selected for detailed analyses by several total and partial extraction techniques. The objective was to document the natural heavy metal geochemistry of the sediment and to assess cultural influences if any on concentrations. These preliminary analyses indicate that absolute concentrations are low when compared to data for polluted sediments or even for sediments from different natural geological terrains elsewhere. Concentration variations appear to be functions of natural sedimentological, mineralogical and geochemical controls. Highest heavy metal concentrations occurred in the finest grained sediments from Lake Athabasca. Vanadium, the heavy metal most commonly associated with the oil sands, appeared to be present in the drainage sediments in a stable organic compound, which was unextractable by hydrochloric acid, sodium hydroxide, or benzene/mcthanol. Its occurrence in the drainage sediment may be in the same general form as in the original bituminous oil sands. If so, it appears to be unaffected by chemical or bacterial degradation in the bottom sediment. Recommendations for further work, which will require additional funding, are in decreasing order of priority: x-ray diffraction of selected sediments; organic extraction and fractionation of selected sediments; analyses of selected sediment cores; determination of sedimentation rates for selected cores; completion of analyses of the dredged sample suite; analyses of lake sediments from lakes off the mainstream system; detailed grid sediment sampling immediately downstream from extraction plant effluents; collection of a suspended sediment sample suite; and analyses of oil slicks (air-water interface).

Heavy metal warning for Fort Chip residents; Scientists present Athabasca River study


Author(s): Brooymans, H.

Year: Submitted

Abstract:
The oilsands industry is boosting the amount of toxic metals in the Athabasca River, as well as in the area surrounding the plant sites, University of Alberta aquatics ecologist David Schindler told Fort Chipewyan residents on Monday.

High resolution paleolimnology of lakes in the Athabasca oil sands mining region Alberta Canada


Author(s): Neville, L. A.

Year: 2014

Abstract:
The Athabasca oil sands (AOS) represent one of Canada’s most economically important natural resources. Understanding the origin, fate and long-term impact of these industrial operations requires geoscientific knowledge of the potential environmental impacts. To quantify current impact an understanding of long-term environmental drivers is required. Here we utilize arcellaceans (testate lobose amoebae) to identify the long-term peleoecologic history of the area, against which ecological stress associated with anthropogenic activities may be defined. Surface sediment samples were collected from 63 lakes forming a 75 km radius encompassing potential airborne and waterborne contaminate pathways. Total mercury (THg) in lakes close to the AOS were similar to values recorded in lakes farthest away and to values recorded in lakes surrounding coal fire plants in central Alberta. All lakes except one had THg concentrations lower than current CCME guidelines. The spatial extent of arcellacean ecosystem stress did not correlate with THg concentrations. To understand the long-term history of the AOS area a freeze core (ALE) spanning 1,870 cal yr BP - present was used to assess how climate anomalies influence lake hydrology and ecology. Deconvolution of the grain size spectra indicates that populations are likely responding to overarching environmental controls. The coarser bedload material was interpreted to reflect high discharge events that occur during spring melts. A proxy ratio of the coarse:fine fractions demonstrates abrupt oscillations of both high and low frequency and indicates that variation in spring melt volume and velocity was likely forced by climate change. Further ii investigation of the grain size data showed that the hydrologic character of ALE has responded to known ocean-atmosphere cycles, particularly the El Niño Southern Oscillation (ENSO) and that these cycles are underwent abrupt expression shifts every ca. 270-370 years. We attribute the expression shift to movement of the jet stream, which controls air mass distribution at this locality. An investigation of the ecological character of ALE from 1875 AD - present reveals that the arcellacean community was also influenced by climate anomalies and that decreased nutrient input, which is a function of precipitation during the El Niño phase of ENSO, applied stress to benthic ecology in these boreal lakes.

Historical resources study, Athabasca Chipewyan First Nation proposed land swap areas, phase 2 study: Athabasca Delta and south shore of Lake Athabasca


Year: 2004

Abstract:
Athabasca Chipewyan First Nation commissioned a Historical Resources Impact Assessment of the Old Fort area for the purpose of creating an inventory of historical resources sites, as well as devising a plan for the long term management of historical resources in the area. The Nation had the intention of moving from their current location to the Old Fort area. This report deal exclusively with the historical resources side of the side (a land use study was also done), but provides a great deal of information on geologic, and pre-contact history of the area in addition to the archaeological assessment done.

Enter keywords or search terms and press Search

Search this site


Subscribe to the site

Syndicate content

Bookmark and Share