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Denesoline (Chipewyan) knowledge of Barren-Ground Caribou (Rangifer tarandus groenlandicus) movements


Author(s): Kendrick, A., & Lyver P.

Year: 2005

Abstract:
Semi-directed interviews relating to thetraditional knowledge (TK) of barren-ground caribou (Rangifer tarandus groenlandicus) movements were conducted with elders and hunters from the Denesoline (Chipewyan) community of Luts'l K', Northwest Territories, Canada. The objective was to document Denesoline knowledge of past and present caribou migration patterns and record their explanations for perceived changes in movements. Elders recognized expected and unusual levels of variation in caribou movements. Local narratives show that Denesoline communities have a fundamental awareness of caribou migration cycles. Most elders thought fire frequency and intensity had increased over their lifetimes and that caribou numbers and distribution had been affected. The majority of Lutsel K'e elders thought mining development was affecting caribou movements in some way. Elders believe that disturbance around traditional migration corridors and water crossings and disturbance of "vanguard" animals might be forcing caribou to use less optimal routes and influencing where they overwinter. Elders also believe that a lack of respect for caribou will cause the animals to deviate from their "traditional" migration routes and become unavailable to the people for a period of time. Wildlife management practices may need to further accommodate aboriginal perspectives in the future.

Depositional history of sediment in Great Slave Lake: spatial and temporal patterns in geochronology, bulk parameters, PAHs and chlorinated contaminants


Year: 1996

Abstract:
This report presents the results of August 1993 and March 1994 sediment studies in the West Basin of Great Slave Lake. In August 1993, a series of 10 surficial sediment samples were collected in the vicinity of the Slave River mouth. PCB was the predominant organochlorine (OC) compound detected followed by chlorobenzene, total DDT, HCH, and dieldrin. Concentrations were low and comparable to values reported for other subarctic and arctic lakes. There was no apparent pattern in the distribution of these compounds relative to the Slave River outflow. PAHs were very abundant and were dominated by benzo(g,h,i)perylene, benzo(e)pyrene, and phenathrene: concentrations were slightly higher offshore the river mouth than elsewhere. PCDD and PCDF concentrations were exceedingly low. PCDDs were dominated by DiCDD and OCDD while PCDFs were dominated by DiCDF and TriCDF. The presence of the lower chlorinated forms may be suggestive of a pulp and paper mill influence. Similarly the presence of pentachloroanisole, trichloroveratrole, and tetrachloroveratrole may be suggestive of a pulp and paper mill influence. Two cores were collected in August 1993 on the shelf region immediately west of the Slave River. Station depths were less than 30 m. Both cores were in areas of high erosion and could not be assigned meaningful dates. In March 1994, a series of sediment cores was collected at five sites (Sites 12, 13, 16, 19, and 23) in the West Basin, to the west of the August 1993 surficial sediment and coring studies. A single core from each site was dated at the Freshwater Institute and two additional cores (one each from Sites 13 and 19) were dated at the National Water Research Institute. Cores from four of the sites were in depositional areas while the core collected offshore of the Slave River mouth (Site 23) was in an erosional area. However, sufficient sediment deposition had occurred at this site for the core to be dated. The two cores examined from Site 13, in the central region of the West Basin, gave similar dating estimates. However, the two cores examined from Site 19, further to the east, gave somewhat different estimates from each other. These two cores were collected in a less physically-stable region of the lake with some evidence of postdepositional erosion of older material on top of newer sediments. The core from Site 23 was in the least stable region o f the five sites examined. Sedimentation rate estimates were similar to those for Lake Athabasca and Lakes Ontario and Erie. They were higher than estimates for subarctic and arctic lakes and for Lake Superior. Based on estimates of the suspended sediment loading to Great Slave Lake, we conclude that our cores were not collected in the high-sedimentation regions of Great Slave Lake. The greatest sedimentation may occur offshore of the Slave River mouth. Analysis of cores collected in March 1995 should allow us to confirm this hypothesis. Two cores (Cores 12B and 19B) were analyzed for organochlorine compounds. Concentrations of OCs in Core 12B, collected offshore of Hay River, were relatively high and require verification. Thus, these data are not presented in this report. For Core 19B, there was some evidence of increasing PCB, chlorobenzene, and HCH concentrations over the 1949 - 1994 period investigated. Dieldrin showed a weaker time trend. Based on the analysis of sediment trap material collected in August 1994, we conclude that the Slave River is a significant source of organochlorine compounds to Great Slave Lake. Cores from Sites 12 and 19 were analyzed for PAHs. Although the same number of slices were examined for both cores, slices from Core 12B did not extend as far back in time: thus, the PAH record has not been determined for Core 12B prior to the mid 1960s. Both cores were dominated by naphthalene, 1-methylnaphthalene, and 2-methylnaphthalene suggesting a petrogenic source. Concentrations were higher at Site 19, closer to the Slave River, than Site 12. There was strong evidence that concentrations of these compounds increased since the 1960s suggesting an additional anthropogenic source of these PAHs: temporal patterns of increase differed for Core 12B and Core 19B. Fluorene, phenanthrene, anthracene, fluoranthene, pyrene, benzo(a)anthracene, and chrysene all occurred in higher concentrations in Core 12B than Core 19B. Concentrations varied little over time for Core 19B but showed some evidence of higher concentrations in Core 12B for two periods - the late 1970s and the late 1980s. This is suggestive of a localized input, possibly from Hay River. Higher molecular weight PAHs occurred in similar concentrations in Cores 12B and 19B. There was a suggestion of slightly higher concentrations of these compounds in Core 12B during the late 1970s than earlier and later times. PCCDs and PCDFs concentrations were determined in Cores 19D and 23A. Concentrations of PCDDs were substantially higher during the 1950s through the 1970s than in more recent times. Temporal patterns of increase differed for Core 19D and Core 23A. PCDDs were dominated by HpCDDs and OCDDs with only low concentrations of the lower chlorinated forms being detected. Total PCDFs were less abundant than PCDDs: this is in notable contrast to the surficial samples where PCDDs and PCDFs occurred in similar concentrations to one another. PCDFs (primarily TriCDF and TCDF) showed some evidence of increasing concentrations since the 1950s for Core 23A while this trend was less apparent for Core 19D. These increases in PCDD and PCDF concentrations may be related to increased atmospheric sources and/or paper and pulp mill activities. There was some evidence of a pulp and paper mill signature in Core 19B with pentachloroanisole increasing in concentration from 1949 to the early 1980s and then declining somewhat thereafter: trichloroveratrole and tetrachloroveratrole occurred in low concentrations in the 1950s and in increasing concentrations thereafter. Total organic carbon (TOC) and total organic nitrogen (TON) concentrations were determined in Cores 13C and 19D. Concentrations of both compounds have increased since the early 1900s with the greatest increase occurring since the 1950s. Moreover, the increase was more pronounced in Core 13C than Core 19D. This suggests that the West Basin of Great Slave Lake has undergone a slight increase in productivity, possibly due to land clearing and increased anthropogenic development in the Peace and Athabasca River watersheds. Localized activities, occurring at the towns of Hay River and Yellowknife, may also have been important. While Great Slave Lake is essentially a pristine system, it does show signs of recent anthropogenic contamination. A significant fraction of OCs, PAHs, PCCDs, and PCDFs probably entered the West Basin of Great Slave Lake with Slave River inflow. However, the primaiy source of these compounds is less certain, e.g., localized inputs from industries along the Peace and Athabasca Rivers and/or atmospheric deposition (wet and dry) over the broader watershed with the eventual transport of these compounds into the Peace, Athabasca, and Slave rivers and then into Great Slave Lake.

Depositional history of sediments in Lake Athabasca: Geochronology, bulk parameters, contaminants and biogeochemical markers


Year: 1996

Abstract:
The primary objective of this study was to collect and analyze high quality, well-described sediment cores for use in defining the depositional history of sediment-bound contaminants in Lake Athabasca, including those which have atmospheric or upstream sources.

Developing temporal hydroecological perspectives to inform stewardship of a northern floodplain landscape subject to multiple stressors: Paleolimnological investigations of the Peace–Athabasca Delta


Year: 2012

Abstract:
Effective stewardship of ecologically-significant floodplain landscapes requires knowledge of the relative roles of natural processes and upstream human activities on environmental flows. In these landscapes, hydroecological conditions that develop from potentially competing drivers, such as climate change and industrial development, tend to be expressed at spatial and temporal scales that are often inadequately captured by existing monitoring datasets. Consequently, perceived cause–effect relations may be misunderstood, conflict can escalate among stakeholders, and effectiveness of surveillance systems, policies, and governance may be impaired. This is the context for the Peace–Athabasca Delta (PAD), an internationally-recognized water-rich floodplain landscape located in northern Alberta (Canada) that has been subject to multiple stressors. Here we synthesize evidence from paleolimnological records that have fostered an unparalled window into the natural history of this landscape. Over the past 12 years, we have assembled numerous decadal- to multicentennial-long records of hydrological and ecological variability, including an exceptionally detailed chronicle of Peace River flood frequency and magnitude spanning ~600 years. These efforts recently culminated in a 5200-year reconstruction of Lake Athabasca water-level history. Results have provided the foundation to identify drivers of landscape change and generate insight into the delta’s dynamic and ongoing evolution. Contrary to widespread perceptions that hydroelectric regulation of the Peace River since the late 1960s has reduced the frequency of ice-jam floods and lowered floodplain lake-water levels, results indicate that climate variability exerts the overwhelming influence on the delivery of water to the PAD. We show that impending climate-driven freshwater scarcity of a scale unprecedented in our collective societal memory now poses a significant threat to the ecological integrity of this world-renowned landscape and a major challenge to water resource managers. Also, we propose a hydroecological monitoring program, built upon the knowledge gained from our extensive process studies and paleoenvironmental research, to inform effective ongoing stewardship of the delta.

Development of a bioassay to assess the toxicity of oil sands sediments to pike (Esox lucius) (PO)


Year: 2011

Abstract:
Pike (Esox lucius) are a commercially sought fish species that inhabit the Athabasca River, which flows through the Athabasca oil sands. The fish are exposed to natural sources of bitumen from the McMurray formation. This study was conducted to design and implement a daily-renewal bioassay to assess the toxicity of oil sands to this fish species and to obtain information regarding the development of pike exposed to bitumen. Eggs were collected and fertilized with milt from spawning wild pike captured from Lake Diefenbaker in Saskatchewan. The fertilized eggs were exposed to different concentrations of sediments or culture water only (negative controls) until complete yolk absorption of control fish, approximately 15 days post-hatch. For the rest of the experiment, brine shrimp were fed to the walleye embryos every day after hatching. The developing fish were examined for morphological deformities, survival, hatching success, and changes in weight and length. The research findings indicated that pike is less sensitive than walleye and fathead minnow to the toxicity of oil sands sediments.

Development of a bioassay using walleye (Sander vitreus) to assess the toxicity of oil sands sediments


Year: 2011

Abstract:
This study examined the effects of sediments from the Athabasca oil sands area on fish development and survival. Walleye (Sander vitreus) which inhabit the Athabasca River are exposed to natural sources of bitumen eroding from the McMurray formation. This study described the design and implementation of a daily-renewal bioassay to evaluate the potential effects of toxicants on walleye development. Eggs were collected and fertilized with milt from spawning wild walleye captured from Lake Diefenbaker in Saskatchewan. The fertilized eggs were exposed to different concentrations of sediments or culture water only (negative controls) until complete yolk absorption of control fish. The walleye embryos were fed brine shrimp daily after hatching and the developing fish were examined for morphological deformities, survival, hatching success, and changes in weight and length between treatments. Organics concentrations in fish tissues and water were measured when possible. Fathead minnows and northern pikes will also be exposed to the same sediments in order to compare the relative sensitivity of the three species.

Differential changes in gene expression in rainbow trout hepatocytes exposed to extracts of oil sands process-affected water and the Athabasca River


Year: 2012

Abstract:
The oil sands region of northern Alberta represents the world's largest reserves of bitumen, and the accelerated pace of industrial extraction activity has raised concern about the possible impacts on the Athabasca River and its tributaries. An ecotoxicogenomic study was undertaken on Oncorhynchus mykiss trout hepatocytes exposed to extracts of water samples near the oil sand development area, as well as to oil sands process-affected water (OSPW) extracts using the quantitative reverse transcriptase polymerase chain reaction technique. The expression of the following genes (mRNA) was monitored to track changes in xenobiotic biotransformation (CYP1A1, CYP3A4, glutathione S-transferase, multi-drug resistance transporter), estrogenicity (estrogen receptor and vitellogenin), oxidative stress (superoxide dismutase and metallothionein) and DNA repair activity (DNA ligase). The extent of DNA-aromatic hydrocarbon adducts was also determined in cells by immuno-staining. A comparative analysis of gene expression between the river/lake and OSPW samples revealed that CYP3A4, metallothioneins, DNA ligase and GST genes, were specifically expressed by OSPW. Cells exposed to OSPW, commercial naphthenic acids, and benzo(a)pyrene showed increased polyaromatic hydrocarbon DNA-adducts, as determined by cell immunofluorescence analysis. Other genes were induced by all types of water samples, although the induction potential was stronger in OSPW most of the time (e.g., VTG gene was expressed nearly 15-fold by surface waters from the lake and river samples but increased to a maximum of 31-fold in OSPW). A multivariate discriminant function analysis revealed that the lake and river water samples were well discriminated from the OSPW. The CYP3A4 gene was the most highly expressed gene in cells exposed to OSPW and responded less to the lake or river water in the Athabasca River area. This study identified a suite of gene targets that responded specifically to OSPW extracts, which could serve as toxicogenomic fingerprints of OSPW contamination. Differential changes in gene expression in rainbow trout hepatocytes exposed to extracts of oil sands process-affected water and the Athabasca River (PDF Download Available). Available from: https://www.researchgate.net/publication/221753631_Differential_changes_in_gene_expression_in_rainbow_trout_hepatocytes_exposed_to_extracts_of_oil_sands_process-affected_water_and_the_Athabasca_River [accessed Jan 18, 2016].

Dissipation of naphthenic acids mixtures by lake biofilms


Year: 2010

Abstract:
The dissipation (combined sorption and biodegradation) of naphthenic acids (C(n)H(2n+z)O(2)) by lake biofilms with no previous adaptation to oil sands acids was investigated using rotating annular bioreactors. The dissipation by the biofilm was dependent on the chemical composition of the naphthenic acids mixture. There were 2 distinct groups of Fluka naphthenic acids which dissipated with pseudo first order kinetics: (a) t(1/2)= 7 days, r(2)= 0.984 and (b) components which were less readily dissipated with t(1/2)= 134 days, r(2)= 0.618. In contrast to the results observed for Fluka naphthenic acids, no dissipation was evident for lake biofilm exposed to Athabasca oil sands naphthenic acids. The differences in dissipation observed for the systems investigated are attributed to the combination of 3 key factors: (i) molecular structure and (ii) molecular mass of the naphthenic acids; along with (iii) inhibition by some components (containing elements of S and/or N acids). The later are more prevalent in oil sands naphthenic acids compared to Fluka naphthenic acids.

Distribution and relative abundance of the shortjaw cisco (Coregonus zenithicus) in Alberta


Author(s): Steinhilber, M., & Rhude L.

Year: 2001

Abstract:
Barrow Lake, located about 60 km north of Fort Chipewyan, contains the only verified population of shortjaw cisco in Alberta. A specific search for shortjaw cisco in the area around Barrow Lake was undertaken in an effort to gather additional information on its extent of occurrence in Alberta. Eight lakes in the region north of Lake Athabasca and east of Wood Buffalo National Park were surveyed by gillnetting in July and August 2000. No new populations of shortjaw cisco were found at these sites. Seven other nearby lakes had been sampled in 1996 and 1997 with similar results. Catch-per-unit-effort data from Barrow Lake suggest that this population of shortjaw cisco appears to have been stable over at least the past five years and probably the last 30 years. However, further monitoring is required to determine population trends with a scientifically acceptable level of confidence.

Does the Alberta tar sands industry pollute? The scientific evidence


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

Year: 2009

Abstract:
The extent to which pollution from tar sands industrial activities in northeastern Alberta, Canada affects ecosystem and human health is a matter of growing concern that is exacerbated by uncertainty. In this paper we determine whether physical and ecological changes that result from tar sands industrial activities are detectable. We analyze a diverse set of environmental data on water and sediment chemistry, contaminants in wildlife, air emissions, pollution incidents, traditional ecological observations, human health, and landscape changes from the Athabasca Tar Sands region, Canada.

Dynamic water quality modelling and uncertainty analysis of phytoplankton and nutrient cycles for the upper South Saskatchewan River


Year: 2015

Abstract:
The surface water quality of the upper South Saskatchewan River was modelled using Water Quality Analysis Simulation Program (WASP) 7.52. Model calibration and validation were based on samples taken from four long-term water quality stations during the period 2007–2009. Parametric sensitivities in winter and summer were examined using root mean square error (RMSE) and relative entropy. The calibration and validation results show good agreement between model prediction and observed data. The two sensitivity methods confirmed pronounced parametric sensitivity to model state variables in summer compared to winter. Of the 24 parameters examined, dissolved oxygen (DO) and ammonia (NH3-N) are the most influenced variables in summer. Instream kinetic processes including nitrification, nutrient uptake by algae and algae respiration induce a higher sensitivity on DO in summer than in winter. Moreover, in summer, soluble reactive phosphorus (SRP) and chlorophyll-a (Chla) variables are more sensitive to algal processes (nutrient uptake and algae death). In winter however, there exists some degree of sensitivity of algal processes (algae respiration and nutrient uptake) to DO and NH3-N. Results of this study provide information on the state of the river water quality which impacts Lake Diefenbaker and the need for additional continuous monitoring in the river. The results of the sensitivity analysis also provide guidance on most sensitive parameters and kinetic processes that affect eutrophication for preliminary surface water quality modelling studies in cold regions.

Early successional wildlife monitoring on reclamation plots in the Athabasca oil sands region


Author(s): Hawkes, V. C.

Year: 2011

Abstract:
Assessing the effectiveness of reclamation efforts to create wildlife habitat in the Athabasca Oil Sands Region requires an assessment of wildlife use of reclaimed areas as well as the development of scientifically defensible and repeatable survey methods. The Cumulative Environmental Management Association (CEMA) is mandated to develop guidance documents for assessing reclamation effectiveness on oil sands leases. As part of a pilot study funded by CEMA to assess the use of early successional stands (i.e., those ranging in age from 4 to 17 years) by wildlife (songbirds, small mammals, and ungulates), a wildlife monitoring protocol was developed and field tested in 2010 and 2011. The purpose of this project was to (1) set standards upon which to base longer-term monitoring, and (2) identify wildlife groups that will indicate whether reclaimed ecosystems satisfy land use objectives, including the objective of returning wildlife to reclaimed habitats. The study achieved the following goals: 1) an assessment of the return and re-establishment of early successional wildlife to reclaimed terrestrial systems; 2) an assessment of the feasibility of the recommended protocols for monitoring wildlife on reclaimed terrestrial systems; 3) the development of recommendations for the wildlife appendix of the Guidelines for Reclamation to Forest Vegetation in the Athabasca Oil Sands Region for early successional wildlife monitoring based on the monitoring program results; and 4) the collection of monitoring data to assist in identifying and developing wildlife indicators for reclamation certification. Early indications suggest that the proposed methods are suitable for documenting wildlife use of reclaimed plots; however, the frequency and duration of monitoring needs to be increased to determine patterns of re-establishment and use by wildlife.

Effects of climate variability and change on surface water storage within the hydroclimatic regime of the Athabasca River, Alberta, Canada


Author(s): Walker, G. S.

Year: Submitted

Abstract:
Warmer air temperatures projected for the mid-21st century under climate change are expected to translate to increased evaporation and a re-distribution of precipitation around the world, including in the mid-latitude, continental Athabasca River region in northern Alberta, Canada. This study examines how these projected changes will affect the water balance of various lake sizes. A thermodynamic lake model, MyLake, is used to determine evaporation over three theoretical lake basins – a shallow lake, representative of perched basins in the Peace-Athabasca Delta near Fort Chipewyan; an intermediate-depth lake representative of industrial water storage near Fort McMurray; and a deep lake representative of future off-stream storage of water by industry, also near Fort McMurray. Bias-corrected climate data from an ensemble of Regional Climate Models are incorporated in MyLake, and the water balance is completed by calculating the change in storage as the difference between precipitation and evaporation. Results indicate that evaporation and precipitation are projected to increase in the future by similar magnitudes, thus not significantly changing the long-term water balance of the lakes. However, intra-annual precipitation and evaporation patterns are projected to shift within the year, changing seasonal water level cycles, and the magnitudes and frequencies of extreme 1-, 3- and 5-day weather events are projected to increase. These results demonstrate that future climate change adaptation and mitigation strategies should take into account increases in intra-annual variability and extreme events on water levels of lakes in mid-latitude, interior hydroclimatic regimes.

Effects of oil sands process-affected waters and naphthenic acids on yellow perch (Perca flavescens) and Japanese Medaka (Orizias latipes) embryonic development


Year: 2007

Abstract:
Syncrude Canada Ltd. is currently developing environmentally acceptable oil sands process-affected water management methods as part of their land reclamation strategy. Surface waters of the "wet landscape" reclamation option characteristically have elevated concentrations of sodium sulphate and naphthenic acids (NAs), with low levels of PAHs. The following experiment compared early-life stage responses of yellow perch (Perca flavescens) to those of Japanese medaka (Oryzias latipes) when exposed to Mildred Lake settling basin (MLSB) surface water and a commercial sodium naphthenate (Na-NA) standard. Perch eggs were fertilized and incubated in: 100%, 50%, 20%, 4%, 0.8%, and 0.16% dilutions of MLSB water, as well as 20, 10, 5, 2.5, and 1.25 mg/l solutions of the commercial standard. Medaka embryos were exposed to the same treatments, post-fertilization. Both species demonstrated an increase in the incidence of deformity, and a decrease in length at hatch as NA concentrations increased. MLSB surface water contained higher levels of NAs than the commercial standard, however, showed consistently higher NA threshold effect concentrations for both species. Significant differences between the MLSB water and the Na-NA standard suggest that they contain NA congeners with different toxicity, or other compounds such as PAHs. Species differences in thresholds could be explained by the difference in developmental stage in which the exposures were initiated.

Effects of oil sands related aquatic reclamation on yellow perch (Perca flavescens). I. Water quality characteristics and yellow perch physiological and population responses


Year: 1999

Abstract:
In order to test the viability of oil sands aquatic reclamation techniques, yellow perch (Perca flavescens) were stocked into three experimental ponds. Pond substrates consisted of either oil sands fine tailings or clay and lean oil sands deposited by the mining operations. Yellow perch were stocked immediately postspawning and subsamples were sacrificed at 5 and 11 months to measure indicators of energy storage and utilization. These indicators included survival, age, spawning periodicity, condition factor, gonad size, fecundity, and liver size. Indicators generally showed patterns consistent with improved energy storage and utilization in the experimental pond yellow perch as compared with yellow perch in the lake from which the stocked fish originated. This was evidenced by increased gonad size, condition factor, and liver size and the disappearance of spawning periodicity. The patterns observed in experimental ponds suggest improved resource availability and (or) reduced intra- and interspecific competition. Yellow perch physiological indicators were also compared with those measured at several remote natural lakes in the area. Fisheries parameters measured in yellow perch from the experimental ponds generally fell within the range of those found in natural lakes.

Effects of wastewater from an oil-sand-refining operation on survival hematology gill histology and swimming of fathead minnows


Year: 2004

Abstract:
This study examined the effects of various types of wastewater produced in oil-sand-refining on the survival, hematology, gill morphology, and swimming of caged fathead minnows (Pimephales promelas Rafinesque, 1820). At the reference site, all fish survived a 28-day exposure with unchanged hematocrit, leucocrit, and gill histology. In con- trast, all fish did not survive a 28-day period in any of the wastewaters tested and, in some cases, they had all died within 96 h. In addition, the hematology or gill morphology of fish that had survived shorter exposure durations was found to be significantly altered; the changes included a significant decrease in lymphocytes and significant gill cellular hyperplasia and hypertrophy. The present data suggest that water remediation will be needed before the process wastewater from oil-sand-refining can support fish populations.

Elucidation of ecosystem attributes of two Mackenzie great lakes with trophic network analysis.


Year: 2014

Abstract:
The Mackenzie Basin in northwestern Canada is a high-latitude region, with one of the largest watersheds in the world. The Mackenzie great lakes, consisting of Great Bear Lake, Great Slave Lake and Lake Athabasca form the large lake complex. The human presence in the area is small in terms of population and industry and thus these ecosystems remain comparatively pristine and show no major changes in the fish communities. Ecopath with Ecosim (EwE), the most important and most used ecosystem trophic network modelling tool to study the ecosystem-level responses to changes, and information available in the scientific literature together with traditional knowledge about Great Slave Lake and Great Bear Lake was used to elucidate the ecosystem attributes. Our models give a cohesive view of these two ecosystems that will allow researchers and decision makers to explore questions regarding the stability of fisheries and future ecological change. The moderate trophic level of fish catch along with the small percentage of primary production required to sustain fisheries in both lakes demonstrated that fisheries were sustainable during the time period modelled. The ecosystem indices and attributes of the comparatively pristine Mackenzie great lakes were compared with those of two Laurentian Great Lakes having similar types of Ecopath ecosystem models. The metrics utilized to assess comparatively the ecosystem's maturity, stability and health indicated a decline in ecosystem maturity and stability from pristine Great Bear Lake to transitioning Lake Ontario. [ABSTRACT FROM PUBLISHER]

Emergent plant communities of oxbow lakes in northeastern Alberta: Salinity water-level fluctuation and succession


Author(s): Lieffers, V. J.

Year: 1984

Abstract:
Emergent vegetation was sampled in 15 oxbow lakes in a 50-km segment of the Athabasca River in northeastern Alberta. Cover of individual species was visually assessed in plots at the outer, middle, and (or) inner edge of the emergent zone of each lake ( n , 37 sample units). Detrended correspondence analysis showed two main axes of variation. The first axis related to salinity. Water conductivity ranged from 170to 12200 pS cm-' and community types ranged from freshwater fens to saline wetland communities dominated by Scolochloafestucacea, Scirpus maritirnus, and Triglochin maritima. The second axis of variation related to water-level fluctuations. Half of the lakes had an increase in water level in the recent past (ca. 6-30 years). In these lakes, Typha latifolia was dominant in both grounded and floating substrates subjected to increased water levels. Sedge communities dominated by Carex rostrata, C . aquatilis, and Acorus calanzus were common in sites with stable water levels. In freshwater lakes, floating substrates were established over open water by the lateral growth of floating stems of Calla pal~tstrisand Potentilla palustris. Floating substrates were not in the saline sites probably because these open-water colonizers were not present under saline regimes.

Emporium of the north: Fort Chipewyan and the fur trade to 1835


Author(s): Parker, J. M. P.

Year: 1987

Abstract:
This study examines the establishment of the fur trade at Lake Athabasca, with Fort Chipewyan as its focus. It covers the period from the entry of Peter Pond in 1778, to 1835. By then, the fur trade had recovered from the damaging effects of the competition between the North West Company and the Hudson's Bay Company that preceded their amalgamation in 1821. The study portrays the life of a fort as it was related to the fur trade of a district. Fort Chipewyan, headquarters of both the North West Company's and Hudson's Bay Company's Athabasca enterprises, offers an opportunity to examine the fur trade under the differing conditions prior to and after 1821. Although documents are lacking for the North West period, there are sufficient records to indicate the conditions of the trade. Fort Chipewyan, the first European settlement in Alberta, was ideally situated for the fur trade, located as it is at the hub of a drainage system. The fort was reached from the south by the Athabasca River and the streams running to the north and to the west became highways for expansion of the trade. Lake Athabasca stretches to the east. As a base for extending the trade, Fort Chipewyan ranked second, surpassed only by Fort William on Lake Superior. It was not only the fur trade that benefited from the establishment of Fort Chipewyan, however, because as the "Grand Magazine of the North" it became the base of operations for land explorers. Alexander Mackenzie, John Franklin, George Back, and John Richardson were a few of the men who gained fame after passing through its gates.

End pit lakes technical guidance document


Author(s): Westcott, F., & Watson L.

Year: 2007

Abstract:
This Technical Guidance Document is intended to provide preliminary design and management recommendations for End Pit Lakes (EPLs) in the Athabasca oil sands area. EPLs are an integral component in the management, operation and final reclamation landscape of oil sands development. This Technical Guidance Document will provide managers and oil sands industry representatives with guidelines to help resolve the optimal design and EPL parameters for their respective projects. This Technical Guidance Document is a living document and is meant to be flexible and responsive in its content. The first edition is based on knowledge gathered to date (2007) and will be updated as new information and research results become available. The second edition is expected in about 5 years, or in 2012, and should expand upon the current knowledge base, research results and recommendations for EPL design and management. An EPL will be established in a mined-out pit of an excavated area. It will consist of a bottom substrate capped with water; soft tailings or other process-related materials may be placed on top of the bottom substrate. An EPL will need to be controlled, managed and monitored throughout much of its initial filling and during discharge to downstream aquatic environments. Ultimately, the EPL will become a biologically active, self-sustaining and functional ecosystem. There are uncertainties regarding the construction, maintenance and final success of EPLs. The development of EPLs as a reclamation tool for process-affected waters raises issues of concerns for regional stakeholders. This document summarizes the perspectives and concerns of regulators, environmental and community groups, Aboriginals and the oil sands industry itself. Applicable government legislation, guidelines and policies are summarized. Historical data are insufficient to determine a realistic outcome of the final features of EPLs. Modelling and relevant background studies have been the basis of research, but a fully realized EPL has yet to be constructed. Issues to be considered during the development, implementation and management of EPLs include the design, amounts and inflow/outflow rates of reclamation and natural waters, water quality, stratification and the toxicity and/or concentrations of compounds. EPLs will need to meet water quality guidelines prior to release to adjacent environments. Issues also include potential impacts to aquatic life, the bioaccumulation of compounds within the food web and the development and sustainability of the ecosystem. Ongoing research, monitoring and new technologies will fill in these gaps. This document summarizes the results of historic research on EPLs. Current research directed by the CEMA EPLSG is also summarized. To date, the EPLSG research has focused on the selection and refinement of models best suited to predicting the potential for meromixis in EPLs. Nomographs have been developed that predict the stratification behaviour of lakes over time under various salinity, depth and size features. Future research will focus on further improvement of meromictic modelling, the influence of water quality on meromixis and biophysical modelling. Key physical, chemical and biological components to be considered during the design and management of EPLs are described. Recommended design specifications to attain the goal or desired outcome of these components are also compiled in table format. Monitoring requirements including key parameters and frequency are included. Adaptive management is recommended as a method of incorporating flexibility and responsiveness to ongoing management challenges. The process of designing, managing and operating an EPL is summarized, as is the process for obtaining a reclamation certificate.

Engineering and economics of enhanced oil recovery in the Canadian oil sands


Author(s): Hester III, S. A.

Year: 2014

Abstract:
Canada and Venezuela contain massive unconventional oil deposits accounting for over two thirds of newly discovered proven oil reserves since 2002. Canada, primarily in northern Alberta province, has between 1.75 and 1.84 trillion barrels of hydrocarbon resources that as of 2013 are obtained approximately equally through surface extraction or enhanced oil recovery (EOR) (World Energy Council, 2010). Due to their depth and viscosity, thermal based EOR will increasingly be responsible for producing the vast quantities of bitumen residing in Canada’s Athabasca, Cold Lake, and Peace River formations. Although the internationally accepted 174-180 billion barrels recoverable ranks Canada third globally in oil reserves, it represents only a 9-10% average recovery factor of its very high viscosity deposits (World Energy Council, 2010). As thermal techniques are refined and improved, in conjunction with methods under development and integrating elements of existing but currently separate processes, engineers and geoscientists aim to improve recovery rates and add tens of billions of barrels of oil to Canada’s reserves (Cenovus Energy, 2013). The Government of Canada estimates 315 billion barrels recoverable with the right combination of technological improvements and sustained high oil prices (Government of Canada, 2013). Much uncertainty and skepticism surrounds how this 75% increase is to be accomplished. This document entails a thorough analysis of standard and advanced EOR techniques and their potential incremental impact in Canada’s bitumen deposits. Due to the extraordinary volume of hydrocarbon resources in Canada, a small percentage growth in ultimate recovery satisfies years of increased petroleum demand from the developing world, affects the geopolitics within North America and between it and the rest of the world, and provides material benefits to project economics. This paper details the enhanced oil recovery methods used in the oil sands deposits while exploring new developments and their potential technical and economic effect. CMG Stars reservoir simulation is leveraged to test both the feasible recoveries of and validate the physics behind select advanced techniques. These technological and operational improvements are aggregated and an assessment produced on Canada’s total recoverable petroleum reserves. Canada has, by far, the largest bitumen recovery operation in the world (World Energy Council, 2010). Due to its resource base and political environment, the nation is likely to continue as the focus point for new developments in thermal EOR. Reservoir characteristics and project analysis are thus framed using Canada and its reserves.

Environmental contaminants in fish: Spatial and temporal trends of polychlorinated dibenzo-p-dioxins and dibenzofurans Peace Athabasca and Slave River basins 1992 to 1994


Year: 1997

Abstract:
As part of the work to examine the impact of development on ecosystem health and integrity on the Peace and Athabasca river basins in Alberta, the Northern River Basin Study (NRBS) was required to determine “the contents and nature of the contaminants entering the system ... particular reference to water, sediments and biota" and to determine “... the current concentration of contaminants in water and edible fish tissue and how are these levels changing through time and by location". The Reach Specific Study (RSS) was designed to measure spatial and temporal trends of contaminants including polychlorinated dibenzo-p-dioxins and -dibenzofurans (PCDD/Fs) in sediment, water and and biota (fish and invertebrate) samples collected at six locations on the upper Athabasca River downstream of Hinton (AB) in spring 1992, fall 1992 and spring 1993. The General Fish Collection (spring 1992), the Long nose sucker and Northern pike liver study (fall 1994) and the Special Burbot Collection (fall 1992 and 1994), and the Ft. Chipewyan winter fishery study (1994/95) were also conducted to examine levels in fish tissues within the Athabasca, Peace and Slave River basins. The purpose of this report is to summarize the levels of PCDDs and PCDFs in fish from these various studies and to assess temporal trends of 2,3,7,8-TCDD and 2,3,7,8-TCDF by comparison with previously published data. A second objective was to reexamine pathways of accumulation of 2,3,7,8-TCDD and 2,3,7,8-TCDF from water and suspended sediment to fish, first measured in the upper Athabasca River in 1992 (Pastershank and Muir 1995). The major PCDD/F congeners in muscle (skinless fillet) of mountain whitefish and northern pike samples collected in the upper Athabasca River downstream of Hinton in fall 1992 and spring 1993 were 2,3,7,8-TCDD and -TCDF. Mean concentrations of 2,3,7,8-TCDD in mountain whitefish ranged 0.6 to 7.7 pg-g'1wet wt and from 1.7 to 9.8 pg-g"1for 2,3,7,8-TCDF. Concentrations of other 2,3,7,8- substituted penta- to octachloro- PCDD/F congeners were generally much lower or non-detectable in both species. Two lower chlorinated congeners, 2,7/2,8-dichlorodibenzodioxin and 2,3,8- trichlorodibenzofuran were detected in most samples ofmountain whitefish from fall 1992 at low pg-g'1 concentrations. TCDF was the most frequently detected PCDD/F congener in longnose sucker and northern pike livers collected from the Wapiti/Smoky and Peace Rivers in fall 1994. TCDF concentrations in liver were in the low pg-g'1range similar to levels in muscle of these species. Highest concentrations of TCDF in livers of longnose sucker (9.2 ± 17.8 pg-g"1) were found at a site on the Smoky River (SRI) downstream of the pulp mill effluent near Grande Prairie. Temporal trends in 2,3,7,8-TCDD and -TCDF in mountain whitefish were examined over a four year period by combining the three sampling times in the upper Athabasca River with data from previous studies (DFO National Dioxin Program 1989). There was a definite decline in 2,3,7,8-TCDD and - TCDF concentrations in mountain whitefish downstream of the Hinton but most of the decrease took place in the period 1989 to 1992. The extent of the decline depends to a large extent on which results for spring 1993 are used. If samples from the near-field sites of Weldwood and Obed (mean concentrations of 1.1 and 2.6 pg-g"1wet, for TCDD and TCDF respectively) are used the decline is about five-fold for both TCDD and TCDF over four years. But if the fish from Emerson Lake (48 km downstream) are included (mean concentrations are 3.6 and 7.1 pg-g"1wet, for TCDD and TCDF, respectively) the decline is about 3-fold. In general, concentrations of PCDD/Fs were higher in burbot liver than in muscle or liver of mountain whitefish or northern pike and a greater number of congeners were detected. TCDF was detected i (mean concentrations, 0.30 to 65 pg-g'1) in 86% o f all 203 burbot liver samples analysed, while 2,3,7,8- TCDD was detected in 35% of samples (mean concentrations, <0.3 to 8.5 pg-g'1). Two other 2,3,7,8- substituted- PCDD/F congeners, 1,2,3,6,7,8-HxCDD and the heptachlorodioxin, 1,2,3,4,6,7,8-HpCDD were detected in 37% o f burbot liver samples. OCDD was also detected relatively frequently (17%) while OCDF was found in only 3 of 203 samples. Di and trichloro-CDDs and CDFs were detected infrequently in burbot liver and at low levels relative to tetra- to octachloro congeners. Significantly higher levels (ANCOVA; Tukey’s or least squares means test) of TCDD and TCDF were found in burbot liver downstream of the Hinton BKM than at all other sites. Levels of 2,3,7,8-TCDD and -TCDF in burbot liver were lower in the. fall 1994 collection than in fall 1992 at four sites; downstream of the Grande Prairie pulp mill outlet, PR2 on the Peace River near the mouth ofthe Notikewin River (674 km from confluence ofthe Peace/Slave), and PR3 upstream ofFort Vermillion (396 km). Comparison of concentrations in burbot liver near the BKM at Grande Prairie was problematic because sampling sites were not in the same locations each year. Nevertheless, the results show a decline of 4 to 17-times in the case of 2,3,7,8-TCDF at three sites. No significant decline of TCDD or TCDF concentrations was found in burbot livers from PR2. The burbot liver results, expressed as TCDD TEQ’s, also agreed well with those of Swansonet ak (1995) who found a 5-fold decline in TEQs downstream of the Grande Prairie BKM between summer 1991 and spring 1994. Concentrations of all 2,3,7,8-substituted PCDD/F congeners in composite samples of fish muscle from the Ft. Chipewyan domestic winter fishery in the Peace-Athabasca delta were at or near detection limits (<0.1 to <0.8 pg-g'1). Only 2,3,7,8-TCDF was detectable in most samples (<0.1 to 0.5 pg-g'1). Burbot liver samples from the three sites in the Peace-Athabasca delta had higher levels o f 2,3,7,8-TCDF than burbot muscle (1.7 to 2.9 pg-g'1). These levels were similar to those at other far-field and reference sites located far from BKMs. The bioavailability of TCDD and TCDF to mountain whitefish and northern pike was assessed using biota-sediment (or suspended sediment) accumulation factors (BSAF/BSSAFs). BSAFs for 2,3,7,8- TCDD ranged from 1.1 to 2.0 and for TCDF from 0.19 to 1.63 in mountain whitefish in spring 1992. A similar range of BSAFs was found in 1993. BSSAFs for both 2,3,7,8-TCDD and TCDF were generally lower and showed greater consistency than BSAFs with distance from the BKM. The results suggest that TCDD/TCDF levels in fish can be estimated with an average, site specific, BSAF or BSSAF using concentrations of TCDD/F in bed sediment or suspended sediments. Application of the Thomann and Connolly food chain model (steady-state version) to predict levels of TCDF in the food web downstream of Hinton showed that good agreement between predicted and observed results could be obtained for benthic feeding organisms (and longnose suckers and pike) which were close to equilibrium with sediments or biofilm. The model overpredicted concentrations in filter-feeding invertebrates and mountain whitefish; these organisms are not in equilibrium with TCDF in the water and suspended solids in the river due to the dynamic nature ofthe system. All mean concentrations of TCDD TEQs in fish muscle or liver were below the limit of 20 pg-g'1(wet wt) set by Health Canada for commercial sale and export of fish. A few individual samples, mainly burbot liver from the Athabasca River downstream of Hinton, exceeded the 20 pg-g'1guideline. Assuming TCDD TEQs of 8.3 pg-g'1in mountain whitefish downstream of Hinton a 60 kg individual would have to consume 72 g of mountain whitefish muscle per day to exceed the Health Canada

Environmental contaminants in mink - Peace and Athabasca Rivers, December, 1991 and January 1992


Author(s): Wayland, M.

Year: 1995

Abstract:
Analyses were done on mink that were collected from three sites: 15 km downstream from the Weyerhaeuser Canada pulp mill about 2 km from the Wapiti River on Bear and Olsen Creeks; on Galoot Lake on the Athabasca Delta and on creeks about 5 km from the Athabasca River and approximately 40 km downstream from Hinton

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