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Traditional land use and occupancy study: Anzac, Gregoire Lake Reserve, and Fort McMurray; Janvier and Chipewyan Prairie; and Conklin Settlement: Final Report. Volume 1


Year: 1993

Abstract:
The Traditional Land Use and Occupancy Study (TLUOS) grew out of the Parallel Aboriginal Process to Participate in Alberta Pacific's Forest Management Task Force, which was signed by senior representatives of the Athabasca Native Development Corporation (ANDC), Alberta Pacific Industries Inc. (AlPac), and the Alberta Department of Environmental Protection. The Aboriginal forum process detailed in the above document commits to: assessment of previous and current levels and extent of utilization of wildlife by Aboriginal people in the target region of the FMA land base; and assessment and discussion of traditional aboriginal land use in each compartment so that this information may be considered in the Detailed Forest Management Plan and during the Public Involvement Action Plan. Timber harvest plans will be reviewed under the Parallel Aboriginal Process prior to their approval. This report is to be used in conjunction with "Mapping How We Use Our Land: Using Participatory Action Research"

Traditional land use and traditional ecological knowledge


Year: 2004

Abstract:
The objectives of this study were to "integrate information on historical and current traditional land use in the Sunrise Project area with traditional ecological knowledge preserved within affected Aboriginal communities." The authors of this assessment consulted recent environmental impact assessments, traditional land use studies and traditional plant lists prepared by Fort McKay and Athabasca Chipewyan First Nations, interview transcripts from previously completed environmental impact assessments, documentary information provided by the Fort McKay First Nation Industrial Relations Corporation, as well as information gathered at ongoing consultation with Fort McKay, Athabasca Chipewyan, and Mikisew Cree First Nations. Additionally, there were two rounds of interviews in the spring of 2004 with the holders of the four registered traplines that would be affected by the development. The interviews aimed to gather traditional knowledge on land use of the area before oil sands development, in the early stages of development (Syncrude, Great Canadian Oil Sands, now Suncor), and during the current stage of oil sands expansion. Field visits were also conducted. The historical context and a summary of the traditional economy of each Nation, as well as a detailed table on flora and fauna use, are provided. The authors include background information on the four traplines, their holders and families, and detail what the project-specific and cumulative impacts to those traplines would be. Mitigation efforts by Husky are summarized at the end of the document. Expected impacts are reported from consultant's point of view. A short list of Fort McKay First Nation concerns is included.

Traditional use mapping of the lower Athabasca River: Phase 1 study


Year: 2009

Abstract:
This Phase 1 report describes the First Nations and M tis communities in the Lower Athabasca River area and discusses the traditional use activities that occur in the region. Impact hypotheses and pathways are described for the potential effects of water level changes in the Athabasca system. Substantial sections of the report are devoted to identifying gaps in traditional use information presently available, particularly information that could support testing of impact hypotheses and pathways.

Treasure in the sand: An overview of Alberta's oil sands resources


Author(s): Hirsch, T.

Year: 2005

Abstract:
From humble beginnings in the 1960s, development of Alberta’s oil sands has grown into a major driver of the provincial economy and a significant contributor to Canada’s crude oil supply. With an estimated 2.5 trillion barrels of oil in the ground, it is one of the largest deposits of oil on earth. But there is one major problem – the oil trapped in the oil sands is much more difficult and expensive to extract than is conventional crude oil. Nonetheless, oil companies have made tremendous headway in developing ways to extract the oil from the oil sands. Already, more than 1 million barrels of oil are produced each day from the oil sands – about a third of current total Canadian crude oil production. This figure is expected to double to 2 million barrels a day by 2010 when it will account for 57% of all oil production in the country. To date, over $34 billion has been invested in the oil sands – more than the total annual GDP of neighbouring Saskatchewan. According to the Canadian Association of Petroleum Producers (CAPP), close to $38 billion in investments are planned over the next ten years – a number that changes almost daily as more and more projects are announced. These projects are having a massive impact on investment activity, exports, and employment. Despite the massive scope of oil sands development, few of us have taken the time to understand what it all means to Alberta and to Canada. How do we get oil from oil sands? Who owns the oil? How much oil is there? What do these projects mean for our environment, the economy and the global supply of oil? This report seeks to provide an accessible primer on the oil sands, its importance to the economy, and the core public policy issues to which they give rise. A key goal here is to expand awareness of Alberta’s oil sands outside the province and the energy sector.

Understanding traditional use studies: Aboriginal traditions and knowledge. People of the boreal forest photo gallery.


Year: 2009

Abstract:
This gallery of photographs taken by Terry Garvin over a period of 50 years is a dynamic part of the People of the Boreal Forest Website, which is part of the Alberta Online Encyclopedia. The site was developed as an Aboriginal Centennial project by the Heritage Community Foundation in partnership with Terry Garvin and the Aseniwuche Winewak First Nation. Funding support was provided by Alberta Aboriginal Affairs and Northern Development (now Alberta Aboriginal Relations).

Use of traditional ecological knowledge in environmental assessment of uranium mining in Saskatchewan


Year: 1999

Abstract:
Use of traditional ecological knowledge (TEK) is now a requirement of many environmental review panels. It was in the remit for investigation into uranium mining in northern Saskatchewan, but there was a mismatch between the narrow, often technical treatment of TEK and the broader, more cultural comments of the Dene Aboriginal intervenors. It is essential to recognize when a development proposal's planning needs and social issues exceed the scope of environmental assessment (EA). TEK can relate to EA on three levels; detailed information from local people on the environment and wildlife; gaining insight in to socio-cultural effects of a project; and changes to a landscape or a people's relationship with it that may threaten deep identification with their environment. The last may not be a part of an ordinary EA.

Use of traditional ecological knowledge in environmental assessment of uranium mining in the Athabasca Saskatchewan


Year: 1999

Abstract:
Use of traditional ecological knowledge (TEK) is now a requirement of many environmental review panels. It was in the remit for the investigation into uranium mining in northern Saskatchewan, but there was a mismatch between the narrow, often technical, treatment of TEK and the broader, more cultural comments of the Dene Aboriginal intervenors. It is essential to recognize when a development proposal's planning needs and social issues exceed the scope of environmental assessment (EA). TEK can relate to EA on three levels: detailed information from localpeople on the environment and wildlife; gaining insight in to socio-cultural effects of a project; and changes to a landscape or a people's relationship with it that may threaten their deep identification with their environment. The last may not be a part of an ordinary EA.

Vanadium and nickel complexes in the Alberta oil sands (asphaltenes, porphyrins, Canada)


Author(s): Strong, D.

Year: 1986

Abstract:
The nature, distribution and mode of association of vanadium and nickel complexes in the Alberta oil-sand bitumens were investigated using neutron activation analysis (NAA), ultra-violet spectroscopy (UV), liquid chromatography, and mass spectrometry (EI-MS). The Athabasca, Peace River and Cold Lake bitumens were fractionated into three soluble extracts and an asphaltene solid. Vanadium and nickel were distributed between the different components of the bitumen. All the vanadium in the extracts was present as vanadyl porphyrin but only a small fraction of the nickel is porphyrinic. The vanadyl porphyrin content of the Athabasca bitumen is 9.52 (mu)g/g (Peace River: 92 (mu)g/g; Cold Lake 77 (mu)g/g) corresponding to 47% of the total vanadium in the bitumen (51% and 40% of Peace River and Cold Lake respectively) the remaining still associated strongly in the asphaltenes. All five types of porphyrins were present as homologous series with carbon numbers ranging from C(,27)-C(,40). The maxima occur at C(,32) for DPEP series, C(,29)-C(,32) for etio and C(,28) for the diDPEP, rhodo etio and rhodo DPEP. The relative abundance was in the following order: DPEP > etio > diDPEP > rhodo-etio > rhodo-DPEP. The DPEP/other porphyrin ratios (etio, di-DPEP, etc.), in the bitumen extracts are similar and decrease in the order: Athabasca > Peace River > Cold Lake. The results confirm that biodegradation has no effect on porphyrin distributions and that the bitumens are related geochemically. The porphyrins distribute in the bitumen extracts as shown by the porphyrin ratios: DPEP/etio ratio; maltenes < pentane extract < methanol-acetone extract. The DPEP/other porphyrin ratios decrease from maltenes to methanol-acetone extract confirming the fractionation of metal complexes in the bitumen which is governed by the relative polarities of the different types of porphyrins.

Vegetation communities of Marguerite Crag and Tail Wildland Provincial Park


Author(s): Meijer, M.

Year: 2002

Abstract:
This park straddles the Central Mixedwood and Athabasca Plain Natural Subregions transitional area. The terrain in the park is defined by the crag and tail topography created through the actions of glacial ice and meltwater. Crags refer to the knobs or areas of exposed bedrock located on the up-ice side of the landform, while the tails are the trailing elongate bodies on the lee side of the landform and generally consist of erodible bedrock (American Geological Institute 1984 in Alberta Natural Heritage Information Centre 1998). The bedrock patches in this area are generally quite small; however they are very distinct, and do provide defining character for the park landscape This park is located in a relatively remote region of the province and little documented information is currently available for this area. Much of the information currently used to describe this area has been extrapolated from more intensively studied areas near Lake Athabasca to the north and the Athabasca Sand Dunes Ecological Reserve to the northwest. This vegetation study was one component of a multi-disciplinary project, which was conducted to develop a preliminary inventory of the natural components of the area. The objective of this vegetation study was to define some of the more commonly occurring plant communities found within the park and to identify the site conditions with which these communities are associated.

Walleye and goldeye fisheries investigations in the Peace-Athabasca Delta - 1975


Year: 1976

Abstract:
The following report presents the results of- investigations on walleye and goldeye in the Peace-Athabasca Delta in 1975. The report is divided into four main sections that concern the following topics: (1) walleye in the Richardson Lake – Lake Athabasca system; (2) goldeye in the Lake Claire – Mamawi Lake system; (3) field observations of the completed Little Rapids weir on Riviere des Rochers; (4) assessment of field trials of the feasibility of marking fish with acrylic dye. Spawning success, movement, distribution, age structure, and several other biological characteristics of walleye and goldeye in the Peace-Athabasca Delta are discussed. The results of fisheries investigations in 1975 were generally incomplete because of the late initiation (mid-July) of the field work, and must therefore be interpreted carefully. BACKGROUND AND PERSPECTIVE The study on walleye and goldeye in the Peace-Athabasca Delta was sponsored by the Aquatic Fauna Technical Research Committee of AOSERP, in cooperation with the Peace Athabasca Delta Monitoring Group. This group is a multidisciplinary committee composed of representatives from governments of Alberta. Saskatchewan and Canada, and charged with the responsibility of monitoring the effects of remedial measures taken to restore water levels in the delta region. AOSERP funded the investigation in order to gain insight into baseline conditions with respect to walleye and goldeye in the Peace-Athabasca Delta. Walleye Investigations The primary objectives of this study were to delimit fry production in Richardson Lake during 1975 and to obtain the current age structure of the Lake Athabasca walleye population. A secondary objective was to obtain length-weight, age-length relationships and to determine sex ratios for the Lake Athabasca walleye. Studies on walleye fry numbers in the Delta region, surveys of some Saskatchewan streams along the south shore of Lake Athabasca and studies on life history and population dynamics of walleye in the delta have provided evidence that Richardson Lake is a major spawning ground for walleye arid that spawning in Richardson Lake provides most of the annual recruitment to the Lake Athabasca walleye population. Although all areas in the delta have not been surveyed, no other region in the delta has been identified as a major walleye spawning area. Much of Richardson Lake, and its outlet stream, Jackfish Creek, freeze to the bottom during winter. Walleye migrate from Lake Athabasca to the Athabasca River by Big Point Channel during March. Due to ice thickness and the lack of flowing water, walleye cannot enter Richardson Lake until flood waters from the Athabasca River flow into Richardson Lake via Jackfish Creek. These flood waters normally lift the ice in late April, or soon thereafter, and the spawning migration proceeds into Richardson Lake. It is possible that unusually low waters in the spring could cause conditions which would prevent or delay walleye from spawning in Richardson Lake. In view of the present situation, it appears that Richardson Lake is critical to the recruitment of walleye in Lake Athabasca and that the spawning success of this species could be seriously disrupted by unusually low water, during the spring. Goldeye Investigations The major objectives of this study were to determine the age structure of the goldeye population in the Claire-Mamawi Lakes system; and to estimate spawning success of goldeye in the system. A secondary objective was to collect information concerning seasonal movements of goldeye. Results from past studies indicate that goldeye migrate into waters of the Peace-Athabasca Delta in the spring to spawn and move back into the Peace River during summer and autumn. These studies suggest that the Chenal des Quatre Fourches is a major spring migration route for adult and juvenile goldeye as well as a major summer and autumn migration route for goldeye adults, juveniles and fry. Concern has arisen that water level control structures may block) this migration route. It was not possible to absolutely assess the spawning success of goldeye in 1975 because the number of spawners was unknown. In relative terms spawning in 1975 appeared to be less successful than in previous years. Little Rapids Weir On the basis of data gathered during ground and aerial inspections, several sites close to and on both sides of the weir and fishway have been identified as being suitable for setting gillnets. Nets cannot be set close to the weir or fishway due to strong turbulence. The dam constructed across the Flett bypass channel of Riviere des Rochers was also inspected. Water in this channel can flow through the rockfill dam, but fish cannot pass through this structure. Acrylic Dye Marking of Fish A total of 38 walleye were marked during September 1975, in Lake Athabasca near Fort Chipewyan. Most walleye were injected in the operculum (gill cover) and several were injected in the lower jaw. Injection was accomplished more easily in the operculum than in the lower jaw but because pigmentation in the lower jaw is lighter, the dye was more visible. During October 1975, 47 goldeye were marked above the weir at Little Rapids. They were injected at the origin of the anal fin. Between 30 and 40 northern pike and lake whitefish respectively were also marked. The most suitable injection site of a northern pike was at the base of either pelvic fin. Blue dye was easily visible anywhere on the ventral surface of lake whitefish, but was most visible at the base of the adipose fin. ASSESSMENT In depth investigations of spawning success, movement, distribution, age structure and other biological characteristics of walleye and goldeye populations in Peace-Athabasca Delta were conducted for the Aquatic Fauna Technical Research Committee of AOSERP. The study provides baseline information on walleye and goldeye populations with respect to the “before conditions” faced by the Athabasca Delta fisheries in view of the prospect of present and increased levels of oil sands development. This “before condition” is in the context of the “after condition” produced by remedial measures implemented after the Peace-Athabasca Delta Project Investigations into the effects of the Bennett Dam constructed on the Peace River in 1968. The report has been reviewed extensively by Research Secretariat of Alberta Environment and the Aquatic Fauna Research Committee and has been approved for publication. The content of this report does not necessarily reflect the views of Alberta Environment, Environment Canada or the Oil Sands Environmental Study Group. The mention of trade names for commercial products does not constitute an endorsement or recommendation for use. The Aquatic Fauna Committee acknowledges the importance of this report with respect to future fisheries studies in the Peace-Athabasca Delta. It will serve as the basis for studies into the effects of other manmade, structures in, the Athabasca River basin. Such basic investigations: are important since the Peace-Athabasca Delta is one of the most productive regions in Alberta. It is recognized by the Oil Sands Environmental Study Group that although innovative research methodology was not employed in the study, changes in methodology are difficult to accommodate during or after completion of a field project. The OSESG does acknowledge that the research objectives have been met and compliments the researchers on addressing themselves directly to the research subjects. The Aquatic Fauna Technical Research Committee of the Alberta Oil Sands Environmental Research Program accepts \"Walleye and Goldeye Investigations in the Peace-Athabasca Delta - 1975\" as an important and valid research document, and thanks the researchers for their scientific contributions.

Water quality and aquatic resources of the Beaver Creek diversion, 1977


Author(s): Noton, L. R., & Chymko N. R.

Year: 1978

Abstract:
The Beaver Creek Diversion System was investigated from March to November, 1977, to describe post-diversion conditions in Beaver Creek, Ruth Lake and Poplar Creek and to characterize the two newly created water bodies in the system. Ten sites in the system were sampled regularly for physical-chemical parameters, phytoplankton, zooplankton and benthic macroinvertebrates. Additional surveys were done for fish, aquatic macrophytes, stream drift and stream habitat.

Water quality issues in the oil sands region of the lower Athabasca River, Alberta


Author(s): Schindler, D. W.

Year: 2013

Abstract:
I summarize the controversies about industrial pollutants in freshwaters near the oil sands industrial area of Alberta, the inadequacies in environmental monitoring that have led to widespread misconceptions, and recent attempts to correct the problems. Adequate data are available to show that mercury, other trace metals, and polycyclic aromatic compounds are being added by industry to the Athabasca river system and its watershed, although the relative contributions of industrial development and natural sources remain in question. Recent improvements in water monitoring by Environment Canada show promise of resolving the controversies, although independent governance for Canada's and Alberta's water monitoring programs in the lower Athabasca River will be necessary to rebuild public confidence in the data and their interpretation by government and industry. I document one success story in the Athabasca River: the elimination of dioxins from pulp mills in the mid-1990s has caused a consumption advisory for fish in the river to be repealed.

Water quality overview of Athabasca River Basin


Year: 1985

Abstract:
This report overviews major water quality patterns and trends for the Athabasca River and its major tributaries. In doing so it compares water quality data with surface water quality objectives, identifies spatial and temporal patterns, defines major factors affecting water quality, characterizes the relationship between basin hydrology and water quality and identifies river reaches with similar water quality characteristics. The data analyzed for this overview assessment include historical water quality records collected since 1970 at three fixed station network locations (Jasper, Town of Athabasca and Ft. McMurray), and the results of six basin wide synoptic sampling surveys done seasonally during 1984 and early 1985. The historical data define long term trends, whereas the synoptic surveys provide information on spatial patterns. Results indicate that except for the St. Regis Pulp Mill at Hinton, point source effluents from municipal and industrial plants have no broadly based influence on river water quality. In almost all instances, tributary streams account for 90% or more of all measured constituent 1oadings. At low river flows the Hinton Pulp Mill does affect river water quality for a distance of 50 to 75 km. Many of the Alberta Surface Water Quality Objectives (ASWQUO) are regularly exceeded, however most of these exceedances are not attributable to point or nonpoint source impacts. These provincial objectives do not account for regional variations in natural water quality. Comparison with Environment Canada's use specific water quality objectives indicate Athabasca River water can be used for all beneficial uses except contact recreation, which is 1imited much of the year by low water temperatures and high turbidity. Certain objectives for aquatic life and wildlife are occasionally exceeded, however, these violations are due to natural causes and pending further investigation are not thought to be significant. Three water quality zones can be defined for the Athabasca River. The Foothills Reach, between Jasper Park boundary and Ft. Assiniboine, is characterized by fast flow and good overall water quality conditions. Alkalinity and hardness 1evels are elevated, reflecting the mountain origin of the water; yet the suspended solids, organic carbon and nutrient contents are low. The Hinton pulp mill is the only significant anthropogenic impact. Coal mining activity in the upper tributaries has no broad based effect on the mainstem river system. In contrast, very different water quality conditions are experienced in the river reach situated between Ft. McMurray and Lake Athabasca. Suspended solid 1evels are high much of the year, as are associated parameters like organic carbon, particulate nutrients and metals. These constituents are derived from upstream tributaries and channel re-suspension, rather than municipal or industrial effluents. The lower reach al so has a unique major ion chemistry created by loadings from the Clearwater River. The intermediate reach between Ft. Assiniboine and Ft. McMurray is a transition zone. Along this stretch, alkalinity and hardness levels decrease, while most other constituent concentrations increase due to tributary loadings. Based upon statistical analysis of the historical water quality database three distinct water quality seasons are defined. These include the ice cover interval, and two open water periods, from ice off to July 31 and August 1 to freeze-up. Water quality in the early openwater season is controlled by local and mountain snowmelt runoff and a rising hydrograph. The 1ate openwater season is affected by a falling hydrograph, summer rainstorms in the Interior Plains and maximum instream biological activity. Except for some tributaries the existing database adequately defines baseline water quality conditions throughout the basin. Future work should emphasize expansion of the fixed station water quality monitoring network, definition of river assimilation processes, development of basin specific water quality objectives, further work on trace organic compounds and more detailed definition of parameter inter-correlation and discharge dependence.

Water use in Canada's oil-sands industry: The facts


Author(s): Lunn, S.

Year: 2013

Abstract:
Canada's oil-sands industry is often perceived as having poor environmental performance. One focus area is the use of water for oil-sands production. Bitumen from oil sands is produced by surface mining or by in-situ thermal extraction. Both technologies are water-based. The oil-sands deposits are situated in northern Alberta, where the river basins have 87% of the provincial average annual water supply but only have 13% of the demand. Oil-sands operators have made significant progress in improving freshwater use productivity (intensity), and water use represents a small percentage of natural supply. For in-situ production, the 2010 freshwater use productivity for the industry was 0.43 units of freshwater per unit of bitumen produced. As an example of continuous improvement, the Imperial Oil Cold Lake in-situ oil-sands operation has improved freshwater use productivity by 90% since 1985 through produced-water recycling and the use of deep saline groundwater. The in-situ oil-sands industry will remain a relatively small water user into the future (2030) using an estimated 0.04 to 0.09% of available supply from the three river basins where it is situated. For oil-sands mining, most of the source water comes from the Athabasca River. The average water-use productivity for oil-sands production between 2006 and 2011 was 2.5 units of Athabasca River water per unit of bitumen and synthetic crude oil produced (3.6 for all freshwater sources). In 2011, the oil-sands mining industry used 0.54% of the annual Athabasca River flow and 3% of the lowest 2011-2012 winter weekly flow. For growth forecasts to 2030, it is estimated that the oil-sands mining industry will require 1.4% of the average annual flow of the Athabasca River. Overall, by 2030, it is projected that the entire oil-sands industry will use less than 0.4% of Alberta's average annual water supply to produce 80% of Canada's total oil production.

We can no longer be sacrificed


Author(s): Waller, L.

Year: 2008

Abstract:
Many suspect that Fort Chipewyan's health problems have something to do with the fact that it sits less than 200 kilometres downriver from the biggest industrial project on Earth-the wringing of oil from Alberta's tar sands. It's an endeavour that threatens to devastate not only the people of Fort Chipewyan, but dozens of indigenous communities throughout northern Alberta-and perhaps Canada's entire Northwest. THE TAR SANDS DEPOSITS underlie 149,000 square kilometres of land in three regions: Athabasca, Peace River, and Cold Lake. That's an area larger than the state of Florida, and nearly one third of it, 54,000 square kilometres, has already been leased for development in Alberta. On top of or adjacent to those lands are more than two dozen First Nations, some already touched by tar sands extraction. Most are covered by Treaty Eight, which was signed in 1899, on the heels of a previous mining frenzy-the gold rush. Treaty Eight affirmed the Metis and First Nations' rights not only to reserve lands and monetary compensation, but also to the continued pursuit of traditional hunting, trapping, and fishing practices. These rights have been steadily eroded by the expansion of the tar sands development. In 1986, the Fort McKay Band Council formed the Fort McKay Group of Companies, which now pulls in millions of dollars of revenue each year from businesses that service oil companies with everything from heavy equipment to workers' camps. The band council is also in discussion with oil companies about extracting the 600 million barrels of bitumen that lie under their reserve. Fort McKay is rumoured to be the richest First Nation in Canada. "This community's success is completely dependent on oil sands development," says [Jim Boucher]. "That's the only option.

Citation:

Western woods Cree


Author(s): Smith, J. G. E.

Year: 1981

Abstract:
Smith breaks down "Western Woods Cree" into three major divisions: the Rocky Cree, the Western Swampy Cree, and Strongwoods or Fort Bois Cree. It is the latter that he places the Cree residing in the northern Alberta/Fort Chipewyan region. He also suggests the possibility of a fourth group, the Athabasca Cree, due to the presence of a distinct r-dialect south of Lake Athabasca in the eighteenth and nineteenth centuries. He does not expand upon this, but refers to the works of Pond, LaCombe and Pentland to back up this theory. Although Smith provides interesting information on the language; territory; history; traditional culture; and socio-culture of both the Rocky and Western Swampy Cree, any substantial information on the Strongwoods Cree is desperately lacking. In lieu of this, Smith's article tends to be lopsided and incomplete.

What investors need to know about reclamation risks in the oil sands.


Author(s): Barrios, P.

Year: 2010

Abstract:
The development of Canada’s oil sands has attracted considerable attention in Canada and elsewhere in the last few years, mainly due to the impact of oil sands projects on the local environment, and the fact that they constitute an important source of Canada's greenhouse gas emissions.1 Among the impacts of oil sands projects on the local environment, land reclamation deserves special attention by investors, as there are many uncertainties regarding the effectiveness of current approaches to reclamation (in particular of wetlands and of tailings, the waste stream that results from oil sands mining), and new technologies remain unproven. These uncertainties indicate that reclamation may prove much more costly and difficult to achieve than anticipated. Oil sands operators are required to reclaim disturbed land to an “equivalent land capability,” which is defined as the ability of the land to support uses that are similar but not necessarily identical to those that existed before mining.2 Despite companies’ assurances that disturbed lands will be reclaimed to viable ecosystems, after nearly fifty years of mining, only 0.2% of disturbed land has been certified as reclaimed by the government of Alberta (companies claim to have reclaimed 13.6% of the disturbed land, but it is unclear whether they meet regulatory requirements to obtain a reclamation certificate), and no tailings pond has been reclaimed to date.3 Suncor projects to finalise the reclamation of Pond 1 in 2010, but the process will consume virtually no “mature fine tailings,” the portion of the mining waste stream that has proven most difficult to reclaim (see section 2.1 for details). In an effort to help our clients assess the risks associated with land reclamation, in May 2009 SHARE initiated a dialogue with five Canadian companies involved in mining projects in Alberta’s oil sands region. Considering the specific features of different projects, we inquired about each company’s success in the area of tailings and land reclamation, and steps taken to mitigate key risks associated with reclamation. This briefing note summarizes those discussions, highlighting areas where greater information will be required if shareholders are to be able to thoroughly assess the value of their investments. While most questions are relevant to mining operations (notably, in situ projects do not create tailings), the issue of wetland restoration and compensation may be relevant to all projects, and therefore merits consideration by all investors.

Wildlife movement traditional environmental knowledge workshops: Wildlife movement in the regional municipality of Wood Buffalo


Year: 2005

Abstract:
The intention of this report is to summarize the traditional environmental knowledge information gathered during workshops with Aboriginal communities in the fall of 2005. The overall project objective was "to collect information from selected traditional environmental knowledge holders on wildlife "corridors' for seven animal species" (black bear, moose, woodland caribou, wolf, lynx, fisher, and marten). The report would then be used by the Wildlife Movement Task Group of the Cumulative Environmental Management Association's Sustainable Ecosystems Working Group to develop management strategies to help "ensure maintenance of effective habitat connectivity in order to sustain wildlife populations." One-day workshops were held with Athabasca Chipewyan First Nation, Métis Local #125, Fort McKay First Nation, Fort McKay Métis Local #63, Fort McMurray First Nation, Anzac Willow Lake Métis Local #780, Fort McMurray Métis Local #2020, Chard Métis Local #214, and Métis Local #193. The number of Elder participants for each workshop varied between one and six; workshops lasted on average three hours. Discussions began with the seven selected indicator species and distinguished between past movement patterns (pre-1960) and current ones (post-1960). The results of the workshops are presented by five community areas: Fort Chipewyan, Fort McKay, Anzac, Chard, and Conklin. The TEK information is then further organized by indicator species, with traditional environmental knowledge on other species presented in the appendix. In addition to movement patterns, information is also provided on habitat, behaviour, seasonality, sex, population levels, and changes to these components over time. Following this, there is a brief section on "areas that are "still good'" for animals and/or hunting, where there is little or no industrial or recreational development, clean water and air, no pollution, and abundant, healthy wildlife and vegetation. Finally, there is also a substantial section of the report on "survival areas," that is, areas that are essential for the survival of both the animal species and Aboriginal traditional lifeways. It is recommended that these areas be preserved.

Wind-wave-induced suspension of mine tailings in disposal ponds - a case study


Year: 1991

Abstract:
Linear wave theory and wave hindcasting are applied to derive an expression for the depth of water needed to prevent the wind-wave-induced suspension of sediments in mine tailings ponds. The depth is expressed as a function of four factors: the threshold velocity, the wind velocity, the fetch over which the wind blows, and a factor based on the statistical distribution of wave heights. This study was motivated by the need to determine the thickness of water required to prevent the suspension of sludge solids in existing and proposed tailings ponds at Syncrude Canada Ltd.'s oil sands plant. Although data relevant to this problem are used to provide a specific example, the results are applicable whenever sediment suspension is caused by fetch-limited, deep water, wind waves. The results should be of particular use when the available data set is limited, e.g., for proposed tailings ponds. Key words: linear wave theory, wave hindcasting, wind-wave-induced suspension, threshold velocity, sludge capping, reclamation ponds, mine tailings ponds.

Winter and summer hydrometric surveys and modeling in the Athabasca Delta - hydrodynamic & habitat modeling report


Year: 2009

Abstract:
AMEC was retained by CEMA in February 2008 as the prime consultant on a team with Northwest Hydraulic Consultants to execute a detailed bathymetric and hydrometric survey at key locations in the Athabasca River delta. The summer survey was conducted in the 2008 open water season (AMEC-nhc, 2008a) while the winter survey was conducted in February 2008 (AMEC-nhc, 2008b). The surveys focused on four sites within the delta. This report presents the results of a hydrodynamic and fish habitat modeling exercise for Site 2 and Site 4 using the River2D hydrodynamic model. HYDRODYNAMIC MODELING Model boundaries were selected which encompassed all the topographic data in each segment which typically included the top of bank line and one additional survey point taken approximately 10 m inland from the top of bank. The upstream boundary at Site 4 was extended about 400 m upstream of the survey data to allow the model to simulate the velocity distribution measured at Section 4-1Q. The final open water simulations were carried out with bed roughness values of 50, 80, 100 and 120 mm with a bed roughness of 80 mm providing the best overall fit to the observed water surface elevation data. The final under ice simulations were carried out for ice roughness values of 80, 120, 160, 200 and 240 mm with an ice roughness of 160 mm providing the best overall fit to the observed water surface elevation data. Under both open water and under ice conditions, the modeled water surface elevations were found to be insensitive to the roughness values selected but were sensitive to the water level assigned to the downstream boundary. The simulated velocities matched the measured velocities reasonably well under both open water and under ice conditions. FISH HABITAT MODELING Outflow boundary rating curves at Site 2 and Site 4 were developed using an average Lake Athabasca water level computed based on lake level records between 1998 and 2006. Using the open water outflow rating curves, a total of 116 different river discharges at Site 2 and 112 different river discharges at Site 4 were selected to represent both extreme low flow conditions and extreme high (but confined within the channel) flow conditions. Using the under ice outflow rating curves, a total of 20 different river discharges each at Site 2 and Site 4 were selected to represent both extreme low flow conditions and extreme high (but confined within the channel) flow conditions. River2D models were generated for each of the above open water and under ice modeling conditions. For each open water River2D model, the total available wetted area was computed as were the weighted useable area (WUA) values for a total of ten different fish species/life stage combinations. For each under ice River2D model, the total available wetted area was computed as were the weighted useable area (WUA) values for a total of three different fish species/life stage combinations.

Winter Flows in the Mackenzie Drainage System


Author(s): Woo, M. - K., & Thorne R.

Year: 2014

Abstract:
Winter low flow of northern rivers refers to the diminished discharge between the time of rapid flow reduction in the freeze-up period and the arrival of spring freshet, when the flow makes a quick rise. For the Mackenzie River in Canada, the duration of the winter low-flow season so defined varies considerably within the river’s large basin (1.8 million km2); therefore, to give a common time frame that enables between-basin comparison we consider 1 November to 31 March as the winter flow season. Several hydroclimatic conditions influence winter flows to varying degrees. Lengthy periods of sub-freezing temper­atures inhibit rain events and prevent snowmelt, while the formation of river ice increases channel storage at the expense of discharge. Groundwater sustains baseflow, and the flow amount at most stations is related to autumnal discharge, which reflects groundwater storage status in the pre-winter season. Large reservoirs and lakes provide substantially higher winter flows than their neighboring non-lake areas. Winter flow increases downstream as more water is gathered from the expanded drainage network, but flow contribution varies: larger baseflow is delivered from uplands than from lowlands, and discharge from the Williston Lake reservoir, regulated for hydropower production, provides about half of the total winter flow of the Mackenzie. Monotonic linear trends in winter flow are detected statistically for some tributaries, but the effect of short-term flow variability and the confounding influence of managed flow should be evaluated when considering long-term tendencies and their causative factors.

Wood bison and the early fur trade


Author(s): Ferguson, T. A.

Year: 1993

Abstract:
The intent of this paper is to present data from fur trade records documenting the depletion of the northern Alberta wood bison, or buffalo, as perceived by fur traders prior to 1840 and to consider the implications of these data for temporary game management strategies, especially involving Aboriginal harvesters.

Zooplankton communities are good indicators of potential impacts of Athabasca oil sands operations on downwind boreal lakes


Year: 2014

Abstract:
We used zooplankton communities as indicators to evaluate the potential influence of acidifying–eutrophying emissions from the Athabasca oil sands region (AOSR) on 244 downwind lakes in northwest Saskatchewan. The impacts of regional environmental change on zooplankton communities are determined by responses of resident species to altered local environmental conditions as well as changes in composition due to dispersal processes. To test and quantify the relative importance of these individual processes, we conducted ordination analyses, spatial modeling, and variation partitioning. Local environmental factors were the dominant determinants of community structure, including two major environmental gradients susceptible to atmospheric emissions (i.e., acid–base status and productivity). Spatial structuring of these factors induced similar spatial structures in zooplankton distribution across the region. However, disentangling any impacts of the AOSR on these environment–spatial–species relationships from the underlying natural variability was precluded by unavailability of baseline data. Nevertheless, as our findings indicate that dispersal of zooplankton was not strongly limiting across this broad geographic region, zooplankton indicators can be crucial to detect future environmental changes in lakes across northwest Saskatchewan.

[Diary of a trip from Montreal to Lake Athabasca in 1811]


Author(s): LeHaiye

Year: 1813

Abstract:
A private collector of Canadiana visited my office about 1967 and described a rare volume which he said he possessed. In Paris he had picked up a French book describing a journey with the Nor'West fur brigade taken by a Frenchman in 1811. It was my intention to verify this entry some time when in my informant's city by arranging to see the book. Finally, I made enquiries and learned that the collector had died unexpectedly and his collection had been dispersed. The discovery and verification of this book remains a challenge.

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