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Persistent organic contaminants in sediments and biota of Great Slave Lake, Canada: Slave River and long-range atmospheric source influences


Author(s): Evans, M. S., & Muir D. C. G.

Year: 2016

Abstract:
Over 1993–1996, we conducted a series of studies to investigate the distributions of legacy persistent organic pollutants (POPs) in the West Basin and East Arm of Great Slave Lake with a focus on sediments and fish species common in traditional diets; lesser attention was paid to polynuclear aromatic hydrocarbons (PAHs) and chemicals associated with pulp and paper mill activity. The Slave River, formed by the confluence of the Peace and Athabasca Rivers, profoundly affects the limnology of the West Basin by transporting large quantities of water and suspended sediments into the lake. Most POPs occurred in substantially higher concentrations in sediments offshore of the Slave River inflow than in the remote East Arm where long-range atmospheric transport was inferred to be the primary source. POP concentrations tended to be higher in East Arm than the West Basin fish possibly because the low productivity of the East Arm provides less opportunity for contaminant dilution through fish growth and the adsorption onto organic particulates in the water column. Overall, POP concentrations were relatively low in plankton, lake trout fillet and burbot liver from both regions of the lake and generally comparable to other lakes located at similar latitudes. Since 1998, we have been monitoring POPs, mercury and other contaminants in lake trout and burbot under the Northern Contaminants Program in which we are contributing to national and international reporting and to the global understanding of contaminants and climate change on northern and other environments.

Pit lake modelling Phase II


Author(s): Mackenzie, I.

Year: 2007

Abstract:
This report presents results of Phase II modelling studies aimed at optimizing the performance of pit lakes in treating reclamation waters in the oil sands region.

Planning for Canada's future oil sands pit lakes: An overview of the COSIA demonstration pit lakes project


Author(s): Vandenberg, J. A.

Year: 2014

Abstract:
Pit lakes are one of the most visible legacies of open pit mining that result from permanent modifications to pre-mining topography, hydrology and hydrogeology. The extraction of the non-traditional hydrocarbon resource bitumen from Alberta’s Athabasca Oil Sands using truck-and-shovel techniques will result in the development of 35 pit lakes within the next 50 years. These will be large permanent basins with surface areas ranging from 0.2 to 35 km2 and depths ranging from 5 to 42 m. Only one lake, Syncrude’s Base Mine Lake, presently exists. Stakeholders and regulators are concerned that concentrations of constituents such as naphthenic acids, PAHs, ammonia and chloride in lake water will impair the environmental function and social utility of these lakes. However, numerical models have predicted that, within a decade or two of filling, these lakes will become relatively benign systems with the capacity to sustain aquatic ecosystems and to be fully integrated within the Athabasca watershed. To improve our understanding of oil sands pit lake functions, a consortium of oil sands producers called Canada’s Oil Sands Innovation Alliance (COSIA) is considering developing a state-of-the-art research facility with three to four demonstration pit lakes, a dozen experimental ponds, and a smaller mesocosm and microcosm facility. The proposed demonstration pit lakes will be approximately 200 m in diameter and 20 m deep, will be constructed using oil sands waste materials and process waters representing proposed closure strategies, and will be monitored regularly for at least a decade. The DPL Project will include funding for external researchers (both Canadian and international) to conduct publishable research on specific knowledge gaps. On a global scale, this will be one of the first research initiatives from the petroleum-, metals-, coal-, uranium-, diamond-, or aggregate-mining sectors to physically test pit lake predictions on this scale in advance of lake formation. This presentation will review the content and status of the COSIA Demonstration Pit Lakes Project, and will highlight potential research opportunities.

Polycyclic aromatic hydrocarbons increase in Athabasca River Delta sediment: Temporal trends and environmental correlates


Author(s): Timoney, K. P., & Lee P.

Year: 2011

Abstract:
The Athabasca River in Alberta, Canada, flows north through an area undergoing extensive bitumen resource extraction and processing before discharging its water and sediments into the Athabasca Delta and Lake Athabasca. Polycyclic aromatic hydrocarbons (PAHs) have been identified as an environmental concern in the region. We analyzed environmental data collected by the Regional Aquatics Monitoring Program and government agencies to determine whether temporal trends exist in the concentration of sediment PAHs in the Athabasca River Delta. We then determined what environmental factors related to the trends in sediment PAH concentrations. Total PAH concentrations in the sediment of the Athabasca River Delta increased between 1999 and 2009 at a rate of 0.05 mg/kg/yr ± 0.02 s.e. Annual bitumen production and mined sand volume, extent of landscape disturbance, and particulate emissions were correlated with sediment PAH concentrations as were total organic carbon in sediment and discharge of the Clearwater River, a major tributary of the Athabasca River. Within four tributaries of the Athabasca River, only the Clearwater River showed a significant correlation between discharge and sediment PAH concentration at their river mouths. Carefully designed studies are required to further investigate which factors best explain variability in sediment PAH concentrations.

Population Distribution, Alberta Economic Regions


Year: 2009

Abstract:
This Alberta Official Statistic provides the distribution of Alberta’s population within the 8 economic regions of Alberta for 2011. Alberta is divided into eight economic regions as follows: Lethbridge – Medicine -Hat; Camrose-Drumheller; Calgary; Banff – Jasper – Rocky Mountain House; Red Deer; Edmonton; Athabasca – Grande Prairie – Peace River; and Wood Buffalo – Cold Lake. The economic regions of Calgary and Edmonton account for the largest proportion (69.0%) of Alberta’s population. The remaining six economic regions each accounted for less than 10% of the population.

Population Growth, Alberta Economic Regions


Year: 2009

Abstract:
This Alberta Official Statistic describes the growth of Alberta’s population by Economic Regions between the 2006 Census and the 2011 Census. Alberta is divided into eight economic regions as follows: Lethbridge – Medicine Hat; Camrose-Drumheller; Calgary; Banff – Jasper – Rocky Mountain House; Red Deer; Edmonton; Athabasca – Grande Prairie – Peace River; and Wood Buffalo – Cold Lake.

Potential impacts of beaver on oil sands reclamation success–an analysis of available literature


Year: 2013

Abstract:
The North American beaver (Castor canadensis) is a large semi-aquatic rodent that has played acentral role in shaping the Canadian boreal landscape, and colonial Canadian history. Exploitation of North American beaver populations to supply the European hat industry spurred the westward expansion of European explorers and traders into the continental interior. With intensive unregulated harvest, beavers virtually disappeared across much of their range; though populations are recovering, the species is only about 10% as abundant as it was before the furtrade took its toll. As a result, much of the recent ecological history of the Canadian boreal forest has occurred in the absence of this keystone ecosystem engineer, and the ecological state that we perceive as natural is in many regions quite different than it was a century ago. Beavers, while playing an important role in structuring streams and wetlands by altering vegetation communities and water flow patterns, may also affect human structures. In the mineable oil sands region of northeastern Alberta, much of the landscape will be impacted by mining. Mine sites will have to be reclaimed, and those reclaimed sites will consist of engineered landforms (including water bodies and waterways); the long-term hydrological and ecological function of those sites may be vulnerable to beaver activity. In an effort to determine if approaches exist that could manage the risk of beavers colonizing and negatively impactingreclaimed sites, we performed an extensive literature search and analysis. Our objective was to examine characteristics of beaver ecology that might potentially impact reclamation plans, and to identify possible methods to mitigate those impacts. We also include information on traditional use, historical abundance, and current abundance in the mineable oil sands region to provide important historical and ecological context. Although beavers inhabit a range of aquatic habitats,the focus of our review is on watercourses that could be dammed by beavers. Of the aquatic habitats which will be constructed during reclamation, these systems are probably the most vulnerable to impacts from beaver activity. Note, however, that inlet and outflow streams fromlakes may be vulnerable to beaver activity, which could impact the performance of constructed lakes in a variety of ways. Beavers alter stream form and function, create wetlands, and change vegetation patterns. The most important predictor of beaver occurrence is stream gradient, with low gradients being associated with higher beaver activity. Stream depth and width, soil drainage, and stream substrate are also important. Although beavers may also respond to vegetation factors, such astree or shrub species and density, hydrological factors are more important predictors of beaver occupancy of a site.The primary forage preferred by beavers includes deciduous tree and shrub species. Aspen(Populous tremuloides) is the species most preferred by beaver, and is a common component of reclamation plantings and natural recolonization of reclamation sites in the oil sands region. Beavers are central-place foragers, meaning foraging is concentrated around a central home base. They typically harvest deciduous trees and shrubs up to 60 m or more from the water, but mostharvest occurs less than 30 to 40 m from the water’s edge. Predation (and predation risk) restricts the size of beavers’ foraging areas, and may also regulate their population size. Management of wolf populations to limit predation on caribou in northeastern Alberta may have significant indirect effects on beaver abundance and distribution by releasing them frompredation pressure.The boreal forest ecosystem of Canada evolved over millennia with the beaver as a keystone species altering hydrological systems, creating vast areas of wetlands and beaver meadows,changing vegetation communities and modifying geomorphological processes. Reclamation offunctional ecosystems in the region must therefore integrate beavers and their engineered structures. The most ecologically- and cost-effective approach is to design reclaimed areas withthe objective of including beaver, but directing beaver activity to areas away from vulnerablereclamation structures. Ecological function requires the presence of beaver on the post-reclamation landscape, and the species is important to First Nations peoples and other trappers in the area. Although beaver abundance can be expected to increase in the area after reclamation, their activities will result in the replacement of existing vegetation with species of lower nutritional quality to beaver (conifer trees). This is expected to result in a beaver population decline and then stabilization over time. With beavers an integral component of the functional landscape, it is important to create “beaver exclusion zones” to ensure that the impact of thespecies is diverted to areas where beaver activity does not damage reclamation structures.There are very few existing studies of beaver impacts to reclaimed areas. Incorporating ecologically-based strategies for keeping beaver density low in sensitive areas at the outset of a reclamation project, and then monitoring the effectiveness of that strategy, is the best advice thatcan be derived from our analysis of the existing literature. Beavers could be discouraged from settling at a site by creating streams with steep gradients (>10%) that are wide and deep enoughto ensure substantial water flows, are armoured with rock or cobble bottoms, and are bordered byconiferous tree species and/or grass and sedge species. Trees should be planted at high density to prevent growth of shrubs and deciduous trees in the understory, as these are preferred by beaver. Deciduous vegetation should not be planted during reclamation near sites where beavers are to be excluded, and it may be necessary to remove existing deciduous trees and shrubs and replace them with conifers, grasses and sedges in these areas. Although planting specific typesof vegetation may be used to discourage beavers from settling a certain area in the short term,natural succession could eventually result in other vegetation communities attractive to beavers. Therefore, unless long-term vegetation management is envisioned, reclamation plans should notrely on using vegetation to dissuade beaver activity in sensitive areas alone, though this approachmay be used in combination with other methods, especially in the few decades immediately following reclamation. Note that the goal is to plan for a maintenance-free environment in whichongoing beaver control is unnecessary, and the use of multiple strategies in tandem to guidebeaver activity is more likely to achieve this goal. More active, maintenance-intensive techniques could be used to limit the damage caused bybeaver dams to sensitive areas. These techniques include lethal (e.g., kill trapping or shooting)and nonlethal (e.g., relocation) methods to reduce population density. However, these methodsrequire constant effort, and can be expensive. Another approach is to manipulate water flowthrough existing beaver dams using pipe drainage systems; this allows the beaver dam to stay in place, while reducing the risk that it will trap enough water to be dangerous if the dam shouldfail. Again, however, these drainage systems require long-term maintenance.One approach may be more sustainable in the long term and require less maintenance: minimize or maximize water flow through engineered channels, as beavers are less likely to use very low-flow and very high-flow watercourses. Note that beavers may still affect these channels,especially when population densities are high or other habitat is unavailable; however, the probability of beavers affecting very low-flow or high-flow channels is lower than forwatercourses with more moderate flows. Creating several dispersed low-flow channels maymake an area less desirable to beavers compared to a single moderate flow channel. Similarly, multiple low- to moderate-flow channels could be created, with some having characteristics thatattract beavers (“decoys”) and others that do not (“exclusions”), allowing water flow to continuethrough some channels even in the presence of beavers. “Pre-dam” fences can be installed ondecoy streams to create a structure to encourage beavers to occupy a site where damage is not aconcern. Discharge could be controlled by regulating water flow through exclusion streams that are not dammed, or by installing flow devices though dams on decoy streams. A similar approach might be used on culverts that allow streams to flow beneath roadways; flow devices could be used proactively at these sites, and/or oversized culverts could be installed to allowmaintenance of the natural width of the stream channel and reduce the noise of running water,which attracts beaver activity.Although many different landforms on the reclaimed landscape may be vulnerable to beaver activity, a few are considered critical areas where beaver impacts must be controlled, includingthe outlets of lakes, side-hill drainage systems, and constructed peatlands. Beaver activity at the outlet of constructed lakes could cause instability in containment structures, negatively affectlittoral and riparian zones around the lake, and increase the probability of catastrophic outburstflooding. Damming of side-hill drainage systems could cause stream avulsion and routing ofwater flow into a new pathway not engineered for a stream, causing increased erosion. Floodingof constructed peatlands could convert them to open-water systems, thereby subverting theirintended ecological function. These critical areas should be protected from beaver activities,while other areas should be designed to accommodate this important species.In practice, several different approaches – tailored to specific situations and landforms – will benecessary to develop and implement plans that accommodate beavers as a part of the post-reclamation landscape. As so few data exist to inform effective reclamation in the presence ofbeavers, all of the methods we suggest carry an unknown degree of risk. This risk can bedecreased in the future by adapting methods based on observed effectiveness. We recommend implementing a research and adaptive management program on the influence of beavers onreclamation within the context of oil sands reclamation in northeast Alberta. Lack of existing information, particularly in northeast Alberta, illustrates the need to implement research thatdocuments the positive and negative influence of beavers on reclamation sites and testsalternative methods to prevent negative and support positive influences. Otherwise reclamationstrategies will be ad-hoc and tenuous, with a mixed success rate. A research and monitoring program would ideally contribute to a standardized strategic approach to mitigating negativebeaver influences on reclamation of watercourses in the oil sands region. Beavers are, to a certain extent, unpredictable. No single approach will guarantee that a site willbe unaffected by beaver activity. We suggest that multiple management approaches besimultaneously implemented at sites that are particularly vulnerable or critical for the functioning of the reclaimed landscape (e.g., outlet streams from constructed lakes). It is impossible topredict all eventualities, as the character of the reclaimed landscape will change over time due tosuccessional processes, fire, global climate change, and resource extraction. The information weprovide is the best available based on limited current knowledge, and provides the best chancefor minimizing risk while accommodating this keystone species. Ultimately, the presence of beavers on reclaimed oil sands leases will increase biodiversity, enhance ecosystem goods andservices, and assist in developing ecosystems that are consistent with natural systems in the boreal region.

Precambrian Geology of Northeastern Alberta, NTS 74M, 74L and part of 74E (GIS data, polygon features)


Year: 1985

Abstract:
This GIS dataset is part of a digital compilation of the Precambrian geology of the Alberta portion of the Canadian Shield and Athabasca Basin. It is one of the datasets used to produce Alberta Geological Survey (AGS) Map 537. For the Alberta shield, the compilation integrates detailed mapping by both AGS and the Geological Survey of Canada (GSC) at scales ranging between 1:31,680 and 1:250,000. Geochronological data and interpretations also helped prepare this dataset. For the Athabasca Basin, the compilation incorporates the geology of the basin presented in the ExTech IV volume, published in 2007 by the GSC. This dataset tries to present the geological information in a neutral manner, unbiased by the three mutually exclusive, regional tectonic concepts existing at the time of compilation. Users are encouraged to view AGS Map 537, which contains overviews of the geology of the respective areas and a complete reference list. The polygon feature dataset came from existing, though largely unpublished, digital sources. Areas of the shield are mainly from digitized versions of AGS Maps 180 and 25: the shield north of Lake Athabasca and south of the Athabasca Basin, respectively. The selected polygons were from GSC maps, which Alberta Geological Survey digitized, generalized and integrated into the compilation. The author gave new or updated descriptions to the map units and assigned them to the polygon attribute table.

Precambrian Geology of Northeastern Alberta, NTS 74M, 74L and part of 74E, bedrock contacts (GIS data, line features)


Year: 1985

Abstract:
This GIS dataset is part of a digital compilation of the Precambrian geology of the Alberta portion of the Canadian Shield and Athabasca Basin. It is one of the datasets used to produce Alberta Geological Survey (AGS) Map 537. For the Alberta shield, the compilation integrates detailed mapping by both AGS and the Geological Survey of Canada (GSC) at scales ranging between 1:31,680 and 1:250,000. Geochronological data and interpretations also helped prepare this dataset. For the Athabasca Basin, the compilation incorporates the geology of the basin presented in the ExTech IV volume, published in 2007 by the GSC. This dataset tries to present the geological information in a neutral manner, unbiased by the three mutually exclusive, regional tectonic concepts existing at the time of compilation. Users are encouraged to view AGS Map 537, which contains overviews of the geology of the respective areas and a complete reference list. This line feature dataset came from existing, though largely unpublished, digital sources. Areas of the shield are mainly from digitized versions of AGS Maps 180 and 25: the shield north of Lake Athabasca and south of the Athabasca Basin, respectively.

Precambrian Geology of Northeastern Alberta, NTS 74M, 74L and part of 74E, Mylonitized Zones (GIS data, polygon features)


Year: 1985

Abstract:
This GIS dataset is part of a digital compilation of the Precambrian geology of the Alberta portion of the Canadian Shield and Athabasca Basin. It is one of the datasets used to produce Alberta Geological Survey (AGS) Map 537. For the Alberta shield, the compilation integrates detailed mapping by both AGS and the Geological Survey of Canada (GSC) at scales ranging between 1:31,680 and 1:250,000. Geochronological data and interpretations also helped prepare this dataset. For the Athabasca Basin, the compilation incorporates the geology of the basin presented in the ExTech IV volume, published in 2007 by the GSC. This dataset tries to present the geological information in a neutral manner, unbiased by the three mutually exclusive, regional tectonic concepts existing at the time of compilation. Users are encouraged to view AGS Map 537, which contains overviews of the geology of the respective areas and a complete reference list. The polygon feature dataset came from existing, though largely unpublished, digital sources. Areas of the shield are mainly from digitized versions of AGS Maps 180 and 25: the shield north of Lake Athabasca and south of the Athabasca Basin, respectively.

Precambrian Geology of Northeastern Alberta, NTS 74M, 74L and part of 74E, Structures (GIS data, line features)


Year: 1985

Abstract:
This GIS dataset is part of a digital compilation of the Precambrian geology of the Alberta portion of the Canadian Shield and Athabasca Basin. It is one of the datasets used to produce Alberta Geological Survey (AGS) Map 537. For the Alberta shield, the compilation integrates detailed mapping by both AGS and the Geological Survey of Canada (GSC) at scales ranging between 1:31,680 and 1:250,000. Geochronological data and interpretations also helped prepare this dataset. For the Athabasca Basin, the compilation incorporates the geology of the basin presented in the ExTech IV volume, published in 2007 by the GSC. This dataset tries to present the geological information in a neutral manner, unbiased by the three mutually exclusive, regional tectonic concepts existing at the time of compilation. Users are encouraged to view AGS Map 537, which contains overviews of the geology of the respective areas and a complete reference list. The line feature dataset came from existing, though largely unpublished, digital sources. Areas of the shield are mainly from digitized versions of AGS Maps 180 and 25: the shield north of Lake Athabasca and south of the Athabasca Basin, respectively.

Preliminary compatibility studies of G.C.O.S. sand tailings pond water with Athabasca River


Year: 1968

Abstract:
On May 30, 1968 G.C.O.S requested permission to discharge 110 x 106 ft3 of effluent from the sands tailings pond at the Fort McMurray site into the Athabasca River during periods of high river flow. G.C.O.S. outlined the events which made this request necessary in order that an adequate base be developed for a stable 200 foot dike. Samples of the tailings pond water were obtained on June 3, 1968 to assess it’s compatibility with the river water. Samples of the A.P.I. separator retention pond effluent, waste water storage pond, and Lake Athabasca were also obtained. Analytical data suggest that a discharge of 10 x 106 I .G.P.D. from the Tailings Pond would minimize effects on the Athabasca River and yet allow the discharge of 110 x 106 ft3 to occur during a 2 month period when river flows exceed 20,000 c.f.s. Sedimentation of the high solids content could be induced by directing the Tailings Pond water to the retention ponds prior to discharge from the waste water storage pond. Assuming that the regular process waste water discharge is maintained at 10 x 106 I.G.P.D., settling time of the Tailings Pond water (10 x 106 l.G.P.D.) would be 7 hours in the retention ponds and 8.4 days in the waste water storage pond. GCOS requested permission to discharge effluent from the sands tailings pond at the Fort McMurray site into the Athabasca River during periods of high river flow. GCOS outlined the events which made this request necessary in order that an adequate base be developed for a stable 200 foot dike.

Probabilities of emission limitation - Analysis of meteorological data


Year: 1977

Abstract:
Promet Environmental Group Ltd. was retained to perform an analysis of the meteorological data available from the Tar Sands area. The probabilities of occurrence of various meteorological parameters will be used as a basis for estimating the frequencies of occurrence and costs associated with Emission Control at Syncrude's Mildred Lake operation. The minisondings which were carried out at Lease C-17 in the Athabasca Tar Sands from 1974 to 1976 form the data base for this study.

Probable air pathways for long-range transport of air pollutants to Lake Athabasca: Analysis using a Langrangian back trajectory model


Author(s): McDonald, K.

Year: 1996

Abstract:
Long-range transport of air pollutants (or LRTAP) is the mechanism by which atmospheric contaminants are transported very long distances to be deposited and affect the environment thousands of kilometers away from the source of the emissions. From investigation of lake sediments, chemical species are known to be transported into the river basins of northern Alberta via atmospheric pathways. The Atmospheric Environment Service (AES) Lagrangian back trajectory model was used to identify the potential atmospheric routes for airborne contaminants to the basin. Back trajectory analysis indicates that the possible source areas are more wide-spread in the closed- water season than in the open-water season as may be expected from climatology. Although there are subtle differences between the seasons, generally, the greatest frequency of air passages are from the northern Pacific Ocean (30 to 40%)and western North America (50 to 65%). There is no direct transport from Mexico or South America, little transport from Europe (0 to 1%) and central Asia (0.5 to 0.7%) or eastern North America (2 to 3%), but more transport from eastern Asia (3 to 4%) including Japan, China and northern Russia.

Proceedings of Alberta oil sands tailings wastewater treatment technology workshop


Author(s): Baddaloo, E. G. Y.

Year: 1986

Abstract:
Syncrude Canada Limited’s Fort McMurray oi1 sands mining operations has been operating under the concept of zero discharge and total containment of wastewaters since start up in 1978. During this period a considerable volume of contaminated water has been assimulated in a large on-site tailings pond at a substantial costs to the company. This zero discharge philosophy has provided time for a large amount of research to be carried out. Syncrude has requested that Alberta Environment consider controlled (release/reclamation) discharge of treated water as part of the waste control guidelines for the plant; however, as witnessed by recent concerns (i.e., Great Lake Pollution, Edmonton drinking water, etc.), discharge criteria must not only address acute toxicity, but also contaminants that are biologically active in small concentrations over long chronic exposures. This will be necessary for the protection of downstream users (drinking water, sport and commercial fisheries, subsistence fishery, etc.). It is prudent also, that the companies involved should address their major environmental problems while in operation, rather than leaving them for future generations. In response to the formal request from Syncrude to establish discharge criteria for the treatment and release/reclamation of tailings pond water, a departmenta1 committee was formed within Alberta Environment. Meetings have been held and Syncrude has provided an assessment of the treatability of its pond water in relation to the department's \"Wastewater Effluent Guidelines for Alberta Petroleum Refineries\" (1976). In addition to industry research, the federal government’s Panel on Energy Research and Development (PERD) has been funding various projects. Members of the Wastewater Technology Centre in Burlington have also been invited by Syncrude to participate in these studies. To assess the status of collective knowledge and to co-operate/co-ordinate/set priorities for future research, a two-day workshop was planned with industry, public, and various governmental departments and agencies. The goals of the workshop were: 1. To enable free exchange of information and ideas among the various invited groups; 2. To identify priority areas of research and to assist in providing a co-operative effort in order to deal with them; 3. To ensure that research carried out by industry, government, agencies, and the public is well directed and co-ordinated; and 4. To initiate the idea of a co-operative effort with regard to research planning and development to use funds (provided jointly or otherwise) in an efficient manner. The workshop was held on 1985 October 29 and 30 at Mildred Lake Research Station in Fort McMurray, Alberta. It was the first time major issues regarding Alberta oil sands tailings pond had been dealt with by a group comprising industry, federal and provincial governments, agencies, and the public (invited but unable to attend).

Profiling stable isotopes of water signatures to define mass transport mechanisms from water capped fluid fine tailings in the oil sands industry


Author(s): Dompierre, K., & Barbour L.

Year: 2014

Abstract:
Thirty End Pit Lakes (EPLs) are planned for remediation of open pit oil sands mines in the Athabasca Oil Sands region, however their feasibility as a reclamation feature has yet to be fully evaluated. End Pit Lakes are constructed within mined-out pits and many will contain fluid fine tailings (FFT). The main objectives of these lakes are to: (1) provide an effective means of isolating these soft, consolidating tailings within the closure landscape; (2) passively treat mine site water, including expressed FFT pore water; and (3) support the development of a sustainable biological system. Mass transport processes from the FFT to the overlying lake will have considerable influence on EPL performance. Physical mass transport from the FFT to the lake will occur due to diffusion, but will also be affected by advective transport due to tailings self-weight consolidation. Defining physical mass transport mechanisms and rates through the FFT provides insight on geochemical conditions at the FFT – lake water interface, and offers a better understanding of mass balance in the EPL. Syncrude Canada Ltd. has initiated the first full-scale EPL (Base Mine Lake), and established a monitoring program to characterize the physical, geochemical, and biological processes occurring in this new system. The stable isotopes of water (δ2H and δ18O) signature of oil sands process affected water has been shown to be highly distinct from that of freshwater associated with snow melt or rainfall (Baer, 2014). As a result, the isotope composition of the lake water and FFT pore-water can potentially be used as a conservative tracer for mass transport. Samples were collected every 0.1 m across the FFT – lake water interface (2 m above, to 2 m below), at three locations in Base Mine Lake. Water from each sample was analyzed with a Picarro L-2120-i Cavity Ring Down Spectrometer based on the vapour equilibration technique used by Wassenaar et al. (2008) to determine δ2H and δ18O concentrations. These results were compared to δ2H and δ18O concentrations of the lake at multiple locations, as well as inflow and outflow water. Numerical modelling was used to interpret the measured isotope profiles across the FFT – lake water interface and elucidate mass transport mechanisms from the FFT to the lake water.

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