Skip To Content

Long Lake


View Larger Map

Location

Athabasca County No. 12 AB
Canada

Long term prediction of vegetation performance on mined sands


Author(s): Bliss, L. C.

Year: 1977

Abstract:
This project on the \"Long Term Prediction of Vegetation Performance On Mined Sands\" (V.E.6.1) was undertaken to provide management with answers on the predictive ability to maintain different kinds of vegetation on raw sands. The research was designed as an integrated, multi-disciplinary program that would concentrate on the role of water stress in a dynamic soil-plant-atmosphere system of a planted grass cover and a natural Jack pine forest. To date only the latter project has been initiated because of the lack of funding and approval to work on the GCOS dike in 1975. This and the Syncrude dyke represent the worst (driest) environmental situation and therefore revegetation of other sand deposits should be more easily accomplished. The Richardson Fire Tower site was chosen because of the representativeness of its Jack pine - lichen woodland on deep sands, a forest type so characteristic of northeastern Alberta. The results of the first full year show that climatically this southwest-facing sand slope warms more rapidly in spring than do level sites at Mildred Lake and Fort McMurray and that the 1976 summer was above normal for temperature. Precipitation was near normal based upon the 1941 - 1970 period. Of the >60 days of precipitation, over 60% were 4 mm or less and thus little if any water entered the soil due to tree, lichen, and litter interception. Both needle duff and lichens provide a significant barrier to surface evaporation compared with open sand. Resistance to evaporation is 2 to 3 times greater with a lichen cover than with litter. The soils are very porous which is advantageous for water entrance, thus preventing erosion but porosity is a disadvantage in maintaining higher water levels near the soil surface for plant growth. These soils recharge during snowmelt in late March - early April; little runoff occurs and over the summer soil water drawdown takes place. Soil moisture content (volume basis) is generally 8 - 15% near the surface in spring, but by late September is 1 - 3% at all depths. Xylem water potentials, a measure of tree water content, were never very low (mean maximum at dawn -5 to -7 atm. and mean minimum at midday -11 to -14 atm.) which reflect a year of average precipitation with frequent light rains and periodic heavier storms. Transpiration and stomatal closure were controlled largely by vapour pressure deficits. Jack pine avoided spring drought by remaining dormant when air and needle temperatures were above freezing, yet when soils were still frozen. Although Jack pine did not show indications of severe drought in a relatively moist summer, it did develop xylem water potentials of -16 to -18 atm., values which are probably detrimental to many of the species being used in revegetation trials on the dike (Bromus inermis, Phleum pratense, and species of Agropyron). This means that potential species must be drought hardy and tested under laboratory rather than only under field conditions to determine their survival under severe drought conditions that may occur but once in 30 to 50 years. The studies of mycorrhizae show that a large number of species of fungi infect the roots of Jack pine and that the infecting flora from disturbed soils (old burns) is quite different from that of undisturbed forests. Since mycorrhizae are critical for the proper growth and survival of pines, care in innoculating tree seedlings with the proper species is essential. The energy and water balance mathematical model predicts the heat and water status of the Jack pine forest. Examination of the model outputs suggests that late season resistance to water uptake occurs because of increased root resistance in autumn. If this is confirmed with further experimental data, and model runs, it means that fall droughts may be especially critical because of the reduced ability of the trees to absorb water through their roots. A second field season coupled with the laboratory studies to determine lethal and sublethal levels of water stress in Jack pine will provide the added inputs to the models necessary for predicting tree response to severe climatic stress. These data, gathered in a highly integrated manner, will permit the calculation of tree survival on sands, be they dikes or other kinds of mined sand, in terms of soil water content and tree density (including crown extent) in relation to the exceptional dry year that may occur once in 30 to 50 years. Data from field trials of grasses or woody species, without supporting measurements of plant physiological responses to environmental conditions cannot provide this essential predictive tool for management unless the one in 30 to 50 year drought cycle is encountered. It is for this reason that modelling of the data in order to predict plant response to unusual environmental conditions becomes so useful. In summary, this study should be able to provide sufficient data to determine whether or not an open stand of Jack pine or similar conifer is the desired end point in maintaining vegetation at a low maintenance cost on sands, the result of open pit mining of the oil sands.

Methane emissions from oil sand tailings by microbial metabolism of hydrocarbons


Author(s): Siddique, T., & Foght J.

Year: 2011

Abstract:
Enormous volumes of tailings produced during bitumen extraction from oil sands ores are stored in settling basins/tailings ponds. The current inventory of tailings in northern Alberta, Canada exceeds 850 million m3. Biogenic methane emissions have been observed from the surfaces of tailings ponds and about 40 million L of methane day-1 was estimated from a single tailings pond (Mildred Lake Settling Basin) in 1999. This research project was initiated to investigate the source and mechanism of methane emission from the oil sands tailings ponds. The mature fine tailings (MFT) were collected from Syncrude Canada Ltd. and Shell Albian Sands tailings ponds and investigated for methanogenic biodegradation of solvent hydrocarbons that are used in the bitumen extraction process and the residual fractions of these solvents that are present in the tailings deposited in the tailings ponds. Our laboratory experiments have shown that only short-chain n-alkanes (C6-C10) and certain monoaromatics (BTEX) present in C3-C14 range hydrocarbons entrained in Syncrude tailings are readily biodegraded by the indigenous microorganism in the tailings ponds to produce methane. In contrast, a very long acclimation period has been observed for indigenous microbes to degrade long-chain n-alkanes (C14-18) and branched alkanes such as 2-methylpentane. Experiments are in progress to monitor the degradation of these recalcitrant compounds. The molecular analysis of 16S rRNA genes revealed that different microbial communities are involved in the degradation of different groups of petroleum hydrocarbon in oil sands tailings. Understanding the mechanism(s) of biogenic methane production and predicting emissions from oil sands tailings ponds are important objectives for effective management of tailings and greenhouse gas emissions.

Old Fort Point land use study


Year: 2003

Abstract:
The objective of this traditional land use study was to identify and document the traditional lands of Athabasca Chipewyan First Nation (ACFN) in the proposed development zone; evaluate location and condition of sites identified; forecast nature and magnitude of site-specific impacts and to record stories, memories and histories of the people who lived at Old Fort to preserve the knowledge for future generations. Five ACFN members participated in formal and informal interviews over the course of the project. This study begins with a short introduction explaining the study as a by-product of the related Historical Resource Impact Assessment (HRIA) as well as an overview of t he study area and the project objectives. A traditional land use facilitator conducted and interview with one ACFN member and informal interviews with various AFCN members during traditional site visitation as well as incidental site visitations during the HRIA. These interviews produced a number of stories reflecting the long history of Old Fort as well as related places, people and traditional practises and beliefs. Interviews also touched upon on patterns of traditional and modern occupancy and use, location of traditional sites, trails, and past citizens of Old Fort. The report provides a cultural, historical and archaeological context for discussion of the concern faced in the development of the Old Fort area.

Old Fort Point land use study: Athabasca Chipewyan First Nation; Old Fort Point Lake Athabasca, Alberta


Year: 2003

Abstract:
The purpose of the HRIA was to conduct assessment of lands that would be part of a "land swap" that would see the relinquishing of ACFN use of the Chipewyan Reserve 201 at the Athabasca River delta and the creation of a new reserve-based community on the south shore of the lake. As a product of the HRIA, a number of site locations were identified that did not strictly fit the definition of "historical resources", as defined b y the Historical Resources Act (RSA 2000). Often these were areas associated with personal stories and living memories of the members of the Fort Chipewyan community. In an effort to preserve this information, a limited land use study was implemented simultaneously with the HRIA. The purpose of this study was to record the stories, memories and histories of the people who lived at Old Fort, and to preserve a record of these memories for future generations to enjoy. The primary objectives of this land use study were to inventory traditional and modern land use sites within the proposed development zone; to evaluate the location and condition of the individual sites identified; to forecast the nature and magnitude of site-specific impacts; and to present the information in an organized way to permit the ACFN to evaluate the significance of the sites identified in order to make decisions about their long term management. The purpose of the land use recording program conducted was not to provide an exhaustive study of the full history of Old Fort. Rather, it was to provide a local context for not only understanding the historical resource sites identified during the HRIA, but also to preserve some of the stories and memories associated with Old Fort. This was accomplished in cooperation with the members of the Athabasca Chipewyan First Nation. The methods used for the recording of the stories and memories associated with Old Fort Point included three different methods, including a formal interview session with Victoria Mercredi, informal traditional site visitations with Rene Bruno and Charlie Mercredi and incidental visitation that occurred during the HRIA. While the stories of Old Fort were primarily gathered during the first two procedures, the bulk of the reported site locations were noted as the result of the latter field investigation. This investigation was an outgrowth of the work that was being conducted as part of the HRIA for the proposed Old Fort development area.

OPTI Canada Long Lake SAGD Project : Traditional land use study


Year: 2000

Abstract:
The purpose of this Traditional Land Use Study is to ensure that information on traditional land use in the surrounding region is current and relevant so that potential impacts from the Long Lake Project to traditional land use can be reduced or effectively mitigated. The objectives are to document the traditional environmental and historical knowledge of the Fort McMurray No. 468 First nation; present the traditional ecological knowledge in such a way that it can be incorporated into EIAs; to identify and map significant sites such as important medicinal plant and berry-harvesting areas, historical gathering places, graves, cabins, traplines, sweat lodges and salt licks; to identify any concerns that people have about the existing developments, the proposed development, and the potential cumulative impacts; to produce a report and a series of maps that display the Long Lake Project and the traditional uses in the Traditional Land Use Study area; to identify potential ways to reduce or mitigate possible impacts of the proposed Long Lake Project; and to protect confidential or sensitive, site specific information.

Paleohydrologic reconstruction of three shallow basins, Slave River Delta, NWT, using stable isotope methods


Author(s): Mongeon, C.

Year: 2008

Abstract:
The long-term natural hydrological variability of the Slave River Delta (SRD), NWT, is not well documented and needs to be further developed to provide temporal context to understand and evaluate impacts of Slave River (SR) floodwater influence and climate variability and change on contemporary hydro-ecological conditions of the SRD. The SRD has broad ecological and cultural significance, as it provides extensive habitat for wildlife and is important for local First Nations community who have an historical connection with the delta and its resources. Concerns have been raised over recently reported drying trends in the SRD over the past few decades and have largely been attributed to regulation of the Peace River (PR), which supplies the SR with ∼65% of its annual flow. Modern lake water balances (2003 to 2005) of three lakes from different hydrological settings within the SRD were assessed using oxygen (δ 18 O) and hydrogen (δ2 H) stable isotope analyses. Contemporary lake water balance was used to constrain paleohydrological interpretations of cellulose-inferred δ18 O from lake sediment cores. Past hydro-ecological conditions of each lake was also reconstructed using bulk organic carbon and nitrogen elemental and stable isotope analyses. Lead-210 (210 Pb) and caesium-137 (137 Cs) analyses were conducted to establish sediment core chronologies. Results from lake water δ18 O and δ 2 H analyses of SD20, an evaporation-dominated basin, indicate seasonal precipitation, snowmelt runoff and evaporation predominantly control the water balance of this lake. An ∼215-year cellulose-inferred δ18 Olw , δ13 C and δ15 N record of SD20 provides paleoclimatological evidence that recently reported dry conditions in the SRD are not outside of the range of natural variability for the delta. SD20 paleohydrological records follow a similar pattern as PAD5, a climate-driven basin in the Peace-Athabasca Delta (PAD), and align with paleoclimate records reconstructed from tree-ring sequences from the Athabasca River headwaters. Results provide long-term documentation of how hydrological conditions have varied in an area of the SRD that is largely beyond the reach of river flooding. Lake water δ18 O and δ2 H analyses of SD2, a flood-dominated basin, indicate that SR floodwaters control the water balance of SD2. An ∼100 year carbon and nitrogen elemental and isotope record for SD2 documents event-scale flooding on the SR and indicates that regulation of the PR has not decreased flood frequency at this site over the past ∼40 years. The late 1940s and 1950s likely represent the period of lowest river discharge over the past century. The SD2 C/N record is similar to the C/N record of PAD15, an oxbow lake in the PAD, indicating common upstream drivers control flood frequency in both deltas. Lake water δ18 O and δ2 H analyses of SD28, an exchange-dominated basin, suggest that SR flooding and evaporation predominantly control the water balance of SD28. Reconstructed cellulose-inferred δ 18 Olw suggest an increase in river flooding may have occurred over the past ∼40 years. However, reconstructing past hydro-ecological conditions is more difficult at this site due to its long channel connection to the SR, which suppresses the geochemical signals recorded in the lake sediment.

Phytoplankton communities in six eutrophic hardwater lakes in central Alberta and their responses to lime additions


Author(s): Zhang, Y.

Year: 1996

Abstract:
The aim of my study was three-fold: (1) to document natural year-to-year variability in the phytoplankton communities of untreated eutrophic hardwater lakes with relatively low runoffs, (2) to investigate the mechanisms by which Ca(OH)$\sb2$ additions reduce phytoplankton biomass over the short term ($<$20 d), and (3) to identify the effects of treatment on phytoplankton communities in the long term ($>$20 d). The short-term changes in chlorophyll a (chl a), TP and calcium (Ca) concentrations, and pH and turbidity were investigated in four lakes, two dugouts and six limnocorrals after treatment with various Ca(OH)$\sb2$ dosages. Treatments with 250 mg$\rm{\cdot}L\sp{-1}$ of Ca(OH)$\sb2$ in dugouts reduced chl a and TP concentrations in the water by $>$90% and 60%, respectively. Treatment with dosages $\rm{>}75 mg{\cdot}L\sp{-1}$ of Ca(OH)$\sb2$ depressed more chl a and TP concentrations than did dosages $\rm{\le}50 mg{\cdot}L\sp{-1}$ in the limnocorrals. Transitory high pH and turbidity did not reduce phytoplankton biomass in the laboratory. In lakes, treatment with dosages ranging from 25 to 87 mg$\rm{\cdot}L\sp{-1}$ of Ca(OH)$\sb2$ decreased chl a concentrations by 80%, but did not always reduce TP concentration in the water. Effects of lime treatment on phytoplankton communities in the long term were identified by comparing phytoplankton communities in three lime-treated lakes with pre-treatment communities and with communities in three untreated lakes, for the ice-covered period (November to April) and open-water season. Under ice cover, both phytoplankton species composition and biomass fluctuated irregularly from winter-to-winter in all lakes. Treatment effects, if any, on phytoplankton communities were not identified. During the open-water season, mean total phytoplankton biomass and TP concentrations remained unchanged in the year after a single treatment with 72 or 87 mg$\rm\cdot L\sp{-1}\ Ca(OH)\sb2$ in two lakes. In contrast, multiple treatments with dosages ranging from 25 to 75 mg$\rm\cdot L\sp{-1}\ Ca(OH)\sb2$ in Halfmoon Lake reduced mean chl a and TP concentrations by 50% after the first treatment in 1988, and chl a and TP concentrations remained low from 1989 to 1993. Similarly, multiple treatments in Figure Eight Lake, with Ca(OH)$\sb2$ and/or CaCO$\sb3$ at dosages ranging from 5 to 24 mg$\rm\cdot L\sp{-1}$ from 1986 to 1992, reduced mean chl a and TP concentrations from a pre-treatment average (1985 to 1986) of 61 and 161 $\rm\mu g{\cdot}L\sp{-1}$ to 21 and 80 $\rm\mu g{\cdot}L\sp{-1}$ during the repeated treatment years (1987 to 1992). Species diversity decreased in Lofty Lake for up to one year after treatment but was unchanged in N. Halfmoon Lake. Three species of phytoplankton (Gomphosphaeria naegeliana, Lyngbya birgei and Asterionella formosa), which were dominant before treatment, were not recorded for up to two years after lime treatment. More chlorophyte species were found in post- than pre-treatment samples in the three treated lakes. My results suggest that multiple treatments at low to moderate dosages or a single treatment at high dosages are likely required to reduce phytoplankton biomass effectively.

Plains hydrology and reclamation project: Summary report


Year: 1990

Abstract:
Between 1979 and 1988, the Plains Hydrology and Reclamation Project (PHRP) investigated interactions of groundwater, soils, and geology as they affect successful reclamation of surface coal mines in the plains of Alberta. The overall goal of PHRP was: (1) to predict the long-term success and the hydrologic impacts of current reclamation practices; and (2) to develop reclamation technology that will allow modification of current practice to assure long-term success and mitigate deleterious environmental consequences. The first phase of the study, which was completed in 1984, included characterization and instrumentation of two study areas: the Battle River study area, which included Diplomat, Vesta and Paintearth Mines, and the Lake Wabamun study area, which included the Highvale and Whitewood Mines. In the Battle River mining area, the study sites at both Diplomat and Vesta Mines were situated in areas that were mined during the transition from small-scale surface mining to modern, larger scale mining practices. At both mines initial instrumentation, which was installed in 1979 and 1980, was situated in areas of older mining that were reclaimed to pre-modern standards. Later instrumentation, which was installed between 1985 and 1987, was situated in newly reclaimed areas that had been mined using current practice. Paintearth Mine was opened in the early 1980's and all instrumentation was installed in newly reclaimed sites. In the Lake Wabamun mining area, the instrumented areas at both Highvale and Whitewood Mines were located in pits that had been mined during the early to mid-1970's using modern mining and reclamation practices. Active mining continued in other pits of these mines throughout the project. Research from the first phase of study led to the focusing on three problem areas in the second phase of the project: (1) the potential salinization of reconstructed soils from shallow groundwater; (2) the potential deterioration of capability for agriculture as a result of differential subsidence; and (3) the potential changes in the chemical and physical characteristics of reconstructed soils. This report summarizes the results of both phases of PHRP. It brings the project's findings together in one coherent document, and as such exhibits the rationale behind a holistic approach to reclamation research. For a more in-depth treatment of any particular topic, the reader is directed to the project's extensive technical reports and publications (Appendix 1). Mining and reclamation of coal in the plains of Alberta affect two important resources: groundwater resources and agricultural resources (soil and landscape). The most important hydrological impact of surface mining of coal in the plains of Alberta is the reduction in groundwater supply capability within mined areas. Groundwater supplies in areas of potential surface mining of coal are derived almost entirely from either fractured coal beds or sandstone overlying the coal. Surface mining removes these aquifers and replaces them with mine spoil, whose properties, in general, preclude its development as a water supply. The agricultural resources disrupted by mining are replaced by a reconstructed landscape that is not initially in a state of either physical or chemical equilibrium. Depending on reclamation practices, evolution of the reconstructed landscape may result in an agricultural resource that may be better, as good as, or potentially degraded with respect to the pre-mining resource. Groundwater Resources: The hydraulic properties of mine spoil in the plains of Alberta preclude development of water supplies above the base of disturbance within reclaimed mine sites. Cast overburden spoil has values of hydraulic conductivity that are considerably lower than those of the pre-mining coal aquifers, in the range of 10-7 to 10-9 m/s. At these values of hydraulic conductivity, the spoil is not capable of supplying water to wells. In addition, the major ion chemistry of groundwater in mine spoil was found to be considerably degraded relative to pre-mining aquifers. Mean Total Dissolved Solids values are generally 5000 to 7000 mg/L, and the water is generally saturated with respect to calcite, dolomite, and gypsum. At these concentrations, the water is unfit for consumption by both humans and livestock. The brackish nature of groundwater in mine spoil appears to be an inevitable consequence of mining in the plains region of Alberta. There is no known method of materials handling that would alter either the hydraulic conductivity of mine spoil or the chemical make up of the groundwater in mine spoil in this region. We conclude that disruption of shallow groundwater supplies within and above the coal is an unavoidable result of mining in the plains region. The only exception to this generalization would be where extensive, thick sand or gravel deposits lie on the bedrock surface or within the unconsolidated drift overburden. As indicated by Trudell and Moran (1986), it might be possible in such an instance to reconstruct a zone with significantly higher hydraulic conductivity by selectively handling and placing this sand or gravel. There is limited potential to replace the shallow groundwater supplies that are disturbed by mining. Deeper coal or sandstone aquifers that are capable of replacing the shallow coal aquifers removed by mining are present only in some areas. In places where the water quality in these aquifers is acceptable for human consumption, these aquifers offer the best option to replace water supplies lost as a result of mining. AGRICULTURAL RESOURCES The impacts of mining on agricultural resources occur in two time frames: (1) immediate effects, and (2) progressive effects that have long-term implications. Immediate effects focus on the product of the soil reconstruction process. Materials handling associated with mining results in the mixing of the pre-existing soils to produce a reconstructed soil mantle of uniform thickness with properties that are an average of the pre-mining soils. Present requirements for the replacement of up to 1.5 m of subsoil material in addition to topsoil above sodic spoil appear to assure immediate postreclamation capability that is comparable to that prior to mining. There is no evidence to suggest that replacement of greater thicknesses of buffer material would further improve capability. Progressive effects focus on limitations and improvements to agriculture that develop over time; specifically, differential subsidence, which leads to ponding, soil salinization in lowland settings, and leaching in upland settings. Differential subsidence forms depressions that are aligned between the original spoil ridges, and appears to be an unavoidable consequence of dragline mining (Dusseault et al. 1985). These depressions, which typically occupy from five to ten percent of the reclaimed surface, increase infiltration and accelerate differential subsidence by ponding water during spring melt and heavy summer rain storms. As a result, cultivation patterns are disrupted, seeding and/or crop growth is restricted within the ponded depressions, and salinization may occur in the fringe area around the depression. Salinization is a natural phenomenon whose conditions for formation are met in lowland reclaimed settings where ponding occurs, particularly if there is also ponding in the adjacent upland. Ponds in the lowland area cause the water table to persist near the surface. Where there is sufficient ponding in the upland to maintain the water table at levels above that in the adjacent lowland, groundwater will flow toward the lowland. In this setting, the fringe area around ponds in the lowland will become salinized. The flatter the landscape in the lowland, the larger the salinized area will be. The impact of the negative progressive effects of mining and reclamation on agricultural resources can be minimized through modifications of materials placement and grading within existing operations. Grading as much of the upland portion of the reclaimed landscape as feasible into open slopes with integrated drainage can minimize ponding. Pauls et al. (in prep) report that slopes in the range of 1.5 to 3 percent along the long axis of subsidence depressions are sufficient to drain about 90 percent of the water that is ponded on existing reclaimed surfaces. Within the lowland areas, the extent of salinization can be minimized by grading to an undulating to rolling landscape with slopes of 3 percent to 5 percent. This will result in narrower zones around the lowland ponds where the water table is within the critical depth of the surface than when the terrain is more nearly level. There is no known method to prevent the formation of lowland areas where overburden is thinner than the threshold value, other than the expensive process of transporting material from other areas in the mine. These lowland areas can be managed as productive hayland, pasture, or wildlife habitat, which adds much needed variety to the reclaimed landscape. In some cases, it may be desirable to design drainage measures into the materials handling system to facilitate management of the future lowland area.

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


Year: 2013

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

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


Year: 2013

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

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


Author(s): McDonald, K.

Year: 1996

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

Proceedings of Alberta oil sands tailings wastewater treatment technology workshop


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

Year: 1986

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

Professional judgment in mineable oil sands reclamation certification: Workshop summary


Author(s): Creasey, R.

Year: 2012

Abstract:
On June 18, 2012, the Oil Sands Research Information Network (OSRIN) convened a workshop to solicit the expert views from about 50 technical specialists from a variety of disciplines representing about 850 years of experience. The workshop, entitled Information That Professionals Would Look for in Mineable Oil Sands Reclamation Certification sought to document the field experience and “common sense” that a seasoned field specialist brings to the reclamation certification decision process. The workshop was coordinated with the Reclamation Working Group (RWG) of the Cumulative Environmental Management Association (CEMA) to provide additional information in support of their Criteria and Indicators Framework project. With some basic information on the hypothetical lands subject to a reclamation certificate application being considered, the groups were given three different scenarios to analyze from the viewpoint of their professional experience and technical knowledge: Session One: You are going to visit a reclaimed oil sands mine site and decide if a reclamation certificate should be issued. You have only your five senses, experience and common sense to guide your decision. • What positive and negative features do you look for? • How confident (%) would you be that your decision is correct (i.e., mean and range)? Session Two: Next, when you go onto the site you can bring one piece of equipment or one tool. • What would you bring? • What additional information will it provide for your assessment of the site? • How much extra time (and time consuming logistics) would it add to your assessment of the site? • Now how confident are you (%) in your assessment decisions (mean and range)? Session Three: Next, in addition to your senses, experience, and the additional equipment you brought, you can ask for a report(s) regarding the site before the field assessment. • What information would you want to see in the report/documents? • Now, how confident are you (%) in your decision (mean and range)? Session Four: For the final session in the workshop, the groups were asked to provide their comments on one of seven questions: 1. What do we need to know about contamination and remediation? 2. What advice can you give CEMA on criteria and the certification process? 3. Do expectations and process needs change depending on the reclamation goal(s)? 4. Do expectations and process needs change depending on when the site was reclaimed (i.e., older sites, currently reclaimed sites, sites reclaimed in the future)? 5. How long do we monitor for before applying for a reclamation certificate? 6. Do expectations and process needs change based on landform type (e.g., dump, tailings pond, Dedicated Disposal Area, plant site)? 7. What disciplines are missing from the discussion today? The original intent of the workshop was to supplement the science-based reclamation certification criteria and indicators being developed by the Reclamation Working Group of the Cumulative Environmental Management Association with the knowledge and experience used by people with significant field experience. Although valuable suggestions about criteria were received, the discussions seemed to focus more on the information needs and process for assessing certification, suggesting the need for a Guide to the Reclamation Certification Process. The workshop also sought to determine how confidence in decision making is affected by the use of field equipment/tools, and the value of background data and reports in increasing confidence. Given the extensive experience of the workshop participants, it was surprising to see how little confidence they had in using only their knowledge and experience to make reclamation certification decisions. Their confidence in making decisions increased somewhat if they were able to bring a piece of equipment into the field with them. If they were able to review a high quality report and supporting data from the site’s historical file prior to going into the field their confidence increased substantially. This confirms the need for the CEMA RWG Criteria and Indicators work and suggests the need for a Guide to Reclamation Certification Application Content.

Rates of elemental sulphur oxidation and associated oxygen and sulphur isotope fractionation


Author(s): Smith, L. A.

Year: 2009

Abstract:
Elemental sulphur (S0) is removed from sour gas deposits (high H2S) during refinement. The resulting S0 is often stored onsite when the costs of shipping S0 to market exceeds the costs of storing it in large above ground blocks. With the aid of acidiphilic bacteria, atmospheric air and water oxidize S0 to sulphate (SO42-). Long term storage is under consideration; however, oxidation rates and the role of each oxygen source (O2(g) and H2O) is not clear. S0 oxidation experiments were conducted over a range of temperatures (6-32¡ãC) to investigate reaction rates and isotopic fractionation of O and S isotopes during oxidation. The experiments also investigated the effect of integrating S0 oxidizing microorganisms and available nutrients on both the reaction rates and isotope fractionation. Results indicated > 95% of total SO42- generated can be attributed to autotrophic microbial activity. Experiments conducted in a nutrient rich mineral solution showed rates increase with temperature from 0.16 (6¡ãC) to 0.98 (32¡ãC) ¦Ìg S0 cm-2 d-1 (Q10 ¡Ö 1.7 - 1.9). Experiments conducted in a nutrient poor solution (deionized water) showed oxidation rates did not increase with temperature (0.06 to 0.08 ¦Ìg S0 cm-2 d-1) between 12 and 32¡ãC. Oxygen isotope analysis of the generated SO42- indicated essentially all oxygen incorporated into the SO42- originated from H2O. In addition, effluent samples obtained from S0 block effluent at SCL indicated ¦Ä18O(SO4) generally reflected the ¦Ä18O(H2O) in the system at the time of oxidation. While covering the S0 blocks with an impermeable cover would undoubtedly minimize total SO42- accumulation in block effluent, the results of this study suggest ¦Ä18O(SO4) can also be used to track water movement through the block.

Reclamation of boreal forest after oil sands mining: Anticipating novel challenges in novel environments


Year: 2014

Abstract:
Boreal forests in northern Alberta have a growing anthropogenic footprint due to a rapidly growing oil sands mining industry. Although land reclamation is a necessary aspect of responsible industrial development, these activities nearly always affect higher order landscape components such as the broader landform, and its hydrology and biogeochemistry. Recent anthropogenic impacts are then believed to result in new environmental conditions and obstacles under which the boreal forest is developing, potentially leading to irreversibly different environments that could be characterized as novel ecosystems. Reflecting an emerging trend across the field of restoration ecology, these novel ecosystems are not necessarily undesirable. Instead, they are an unavoidable consequence of pervading anthropogenic effects on natural ecosystems. It is our view that successful reclamation outcomes can still be derived so long as policy and regulatory requirements are afforded the necessary scope and economic flexibility to account for the development of hybrid and novel ecosystems among highly disturbed mine sites. Hence, this analysis seeks to situate current and anticipated challenges affecting the reclamation of boreal forest following oil sands mining by describing (i) how regulatory criteria shape reclamation practices and targeted end goals and (ii) how these approaches embody latest trends and priorities in the area of restoration ecology.

Response of confined aquatic biota to mine depressurization water in Beaver Creek Reservoir


Year: 1980

Abstract:
Beaver Creek Reservoir was formed as a result of diverting the natural flow of Beaver Creek away from mine and plant areas and southward to the Athabasca River via Poplar Creek. The diversion was initiated in the fall of 1975 with the closure of the Beaver Creek Dam; filling of the reservoir was completed in the spring of 1976. When it became necessary to remove mine depressurization water from the mining area, Syncrude was granted permission by the Government of Alberta to discharge this effluent into Beaver Creek Reservoir, on the condition that chloride levels in water entering Poplar Creek did not exceed 400 mg/L above ambient levels. The present study was designed to investigate the survival of selected organisms in Beaver Creek Reservoir during 1979. The primary objective was to determine the response of selected species of aquatic biota to saline mine depressurization water after average dilution in the Beaver Creek Reservoir. More specific requirements of the study were: a) the study was to be carried out entirely within the Beaver Creek Reservoir using test organisms held in situ; b) the study must include three sampling locations and three replicates of each test organism at each station; c) test organisms must include: periphyton (on artificial substrates), native species of fish (white sucker and fathead minnow), and native species of invertebrates (either Gammarus or Hyalella); and d) field studies were to be conducted between June and October, 1979 and were to examine both short and long term effects.

Risking rupture: Integral accidents and in/security in Canada's bitumen sands


Author(s): Greaves, W.

Year: 2013

Abstract:
The expansion of unconventional hydrocarbon development in Western Canada is one of the most contentious issues in contemporary Canadian politics. Although widely studied, little attention has been paid to the framing of Alberta's bitumen sands within distinct and incompatible discourses of energy and environmental security. This essay examines these discourses using the tools of securitization analysis, asking the basic questions of what each presents as needing to be secured, from what, and by what means. Presented with two sets of socially constructed in/ security claims related to the bitumen sands and proposed pipeline expansion, the author suggests the social theory of Paul Virilio provides a useful intervention into securitization analysis that allows the material implications of these discourses to be clarified and assessed. Drawing upon Virilio's critical account of technological progress and his theory of accidents, this essay proposes that conventional accounts of "energy security" in the bitumen sands cannot result in meaningful conditions of security because they remain premised upon continued and expanded hydrocarbon consumption in an era of anthropogenic climate change.

Sustainable mine reclamation and landscape engineering


Author(s): McKenna, G. T.

Year: 2002

Abstract:
Since its beginnings thirty years ago, mine reclamation practice continues to evolve. To determine the current state of practice for closure planing, landscape design, and to observe reclaimed landscape performance, 69 mines were visited. Reclamation, though generally well done, seldom satisfied stakeholders or regulators--few sites have received reclamation certification or been returned to the original owner. Until processes for setting realistic goals, multidisciplinary landscape design, and equitable transfer of residual liability are developed, mining companies will not achieve successful reclamation--mining will remain a terminal rather than temporary land use. While most reclaimed areas of most mines exhibit good landscape performance, several shortcomings in the state of practice are clear. The use and rigor of surface-water hydrology design is lacking. Performance of slopes with erodible substrates, the high costs of trafficking soft tailings areas, and errors in predicting end-pit lake filling are particularly troublesome. Designs and regulations that accommodate the dynamic nature of landscapes are uncommon. Poor landscape performance often relates to fluxes (of ions, water, sediment, nutrients, etc) that are unanticipated or outside expected ranges or more commonly, simply fail to achieve unrealistic objectives. Landscape engineering is introduced to help alleviate these shortcomings. It focuses on setting and achieving more realistic goals through inclusions of traditional engineering methods. Work is multidisciplinary and involve teams of specialists. To demonstrate the technical side of landscape engineering, two studies were performed. In the first, the effects of uncertainty in substrate hydraulic conductivity were demonstrated with a database of 800 hydraulic conductivity measurements of oil sand tailings sand. Simple geostatistical tools such as the coefficient of variation, upscaling, and quantifying spatial variability are demonstrated and several design scenarios described. The second study involves predicting erosion rates of fine-grained fills. Results from the laboratory, field, and the literature indicate erosion rate predictions, even under ideal conditions, are generally only accurate to within one order of magnitude. Both the studies highlight the need to estimate common landscape fluxes, their impact on performance, and the need to deliver robust designs and institutional mechanisms that allow for inherent limitations in predicting long term landscape performance for large or complex mining landforms and landscapes.

The geochemical distribution of radium-226 in Cluff Lake uranium mill tailings


Author(s): Goulden, W. D.

Year: 1997

Abstract:
The choice of an input 'source term' for radium concentration into numerical transport models has been a challenge when attempting to predict long term impacts of uranium mill tailings storage. Physical and chemical separation methods were used to establish the geochemical distribution of radium in a fresh Cluff Lake uranium mill tailings sample. Analysis of the experimental data suggested that radium in Cluff Lake uranium mill tailings is present as a barium radium sulfate [(Ba,Ra)S0₄] coprecipitate. Even though radium is known to be strongly adsorptive, only a minor amount of radium absorption was calculated in the presence of competing cations in the Cluff Lake tailings pore fluids. While approximately 80% of the total radium present in the tailings was associated with the < 75μm size fraction (dominated by gypsum, illite, chlorite and iron hydroxide), the data suggests that the common trace mineral barite present in this fraction controls the radium pore fluid concentration. Of the total radium mass present in the tailings, 0.35% was released during deionized water leaching, which removed all of the readily water soluble fraction (11% of the solids mass). Coprecipitation theory using barite as a host mineral for radium adequately predicts equilibrium radium pore fluid concentration. The calculated equilibrium value agrees well with in situ empirical data for Cluff Lake pore fluids, column lysimeter leachates and the empirical experimental data from this study. The results of this study have several environmental implications for stability and transport of ²²⁶Ra associated with sulfuric acid leached and lime neutralized uranium mill tailings. If the barium and radium solids concentrations are known, the equilibrium radium pore fluid concentration can be predicted using coprecipitation theory. The majority of the radium mass (>99%) will be highly stable in the solid phase when in contact with deionized water (or by extrapolation, very low ionic strength waters). The radium concentration in solution is sensitive to sample disturbance; therefore, sampling should be performed with care not to agitate the tailings solids during liquid recovery.

The impact of beaver dams on the design and construction of reclaimed mine sites


Year: 2000

Abstract:
The 1990 failure of the Matachewan Consolidated Gold tailings dam in Ontario should have been a wake-up call to the mining industry. Beavers blocked the spillway of this abandoned tailings darn causing the reservoir to overtop, and toxic tailings to be released into the Ottawa River. Almost ten years later, most miners remain unaware of the risk of beaver darns to post-closure landscapes. There is little guidance about how to assess the risk of beaver dams and how to design reclaimed landscapes to endure beaver activity. As part of its investigations into creating sustainable landscapes at its oils sands mining operations, Syncrude Canada Ltd. conducted an interdisciplinary study of beaver dams in northeastern Alberta. The program included observations from visits to over 70 beaver dams and 29 lake outlets, cataloguing of 784 dams from aerial photographs, and review of over 350 books and articles on beaver behaviour. The program confirmed that beaver activity, especially dam building, has a profound effect on the natural landscape. Beaver dams block streams and lake outlets, attenuate flows, divert streams, flood large areas, trap sediment, create beaver meadows, trigger landslides, and significantly alter the boreal forest ecology. Beaver dams can reach three to four metres high and be over a kilometer long - no stream is too small to dam and few rivers are too large. Large dams can be constructed in just a few days and can be repaired overnight. Beaver colonies can consume up to a hectare of deciduous forest per year and a beaver pond can affect tens of hectares of forest. Outburst flooding of abandoned beaver dams has caused numerous cases of damage to infrastructure. Proceedings of the 24th Annual British Columbia Mine Reclamation Symposium in Williams Lake, BC, 2000. The Technical and Research Committee on Reclamation. Reclaimed landscapes must be designed to encourage, discourage, or, in most cases, accommodate beaver behaviour. The cost of building landscapes to accommodate beavers can be significant, although retrofitting previously reclaimed areas is even more expensive. Even given the best design and construction, residual risks remain owing to extreme beaver behaviour and the prohibitive cost of designing for all risks. Because beaver behaviour varies geographically, a local study of dams would be required to adapt landscape design parameters for mines in other regions.

The role of sulphur in the carbon balance of boreal peatlands


Author(s): Vile, M. A.

Year: 2001

Abstract:
With the exception of photosynthesis, carbon dioxide (CO2 ) emissions from soils exceed all other terrestrial-atmospheric carbon fluxes. Due to the magnitude of this soil-to-atmosphere CO2 flux, and the great mineralization capabilities associated with this large soil carbon pool, any increases in soil carbon fluxes have the potential to provide a large positive feedback to global warming. This dissertation examines the role of atmospheric sulfur deposition on anaerobic carbon fluxes from peatland soils, which contain one-third of the world's soil carbon pool. The first objective of this dissertation was to determine the contribution of sulfate reduction to anaerobic carbon mineralization in peatlands across a regional atmospheric sulfur deposition gradient. The second objective was to determine the fate of currently retained sulfur in peatlands under changing atmospheric sulfur depositional regimes, using stable sulfur isotopes as a tool. We determined the relationship between rates of sulfate reduction, and CO2 and CH4 production in peatlands spanning a wide atmospheric sulfur gradient in central Alberta, Canada and Cervené Blato and Oceán bog, The Czech Republic. Results from this study suggest that although peatlands are important global sources of CH4 , methanogenesis is responsible for a small proportion of anaerobic carbon cycling in these ecosystems. We further tested the hypothesis that in peatlands receiving low sulfate inputs, methane production will predominate during anaerobic carbon mineralization. We hypothesized that with sulfate amendments, anaerobic carbon mineralization at Bleak Lake Bog would be governed by sulfate reduction. In opposition to our hypotheses, sulfate amendments did not increase rates of sulfate reduction, increase CO 2 production, or decrease CH4 production. We conducted a peat transplant experiment to evaluate the impact of atmospheric sulfur deposition on sulfur cycling processes in soil under alternate scenarios of increasing and decreasing atmospheric sulfur deposition. We found that a substantial fraction of the sulfur that enters a peatland via atmospheric deposition is retained in the peat, and this fraction increases with a concomitant increase in rates of atmospheric sulfur deposition. Implications for total sulfur pools, extrapolated to the long term, may be a gain of total sulfur under a scenario of both increasing and decreasing rates of sulfate reduction.

Traditional land use setting report for the Suncor Voyageur South Project


Author(s): Goodjohn, M.

Year: 2007

Abstract:
This traditional land use setting report compliments and extends information collected for the Suncor Steepbank Mine Project, Millennium Project, South Tailings Project and the Voyageur project. Senior and, in some cases, junior trapline holders of RFMA #s 578, 2156, 1790, 2676 were interviewed for the report. Aboriginal participants include members of Fort McKay First Nation and Métis. The report focuses on historic and current traditional land use within the Voyageur South Project Area. Suncor also provided a week long camp-over program where traditionally used plant species were documented by members of Fort McKay First Nation. At the time that this Traditional Land Use Setting Report was released, the report for the camping trip was still being written by Fort McKay First Nation. Likewise, Mikisew Cree First Nation were still in the process of completing their traditional land use study at the time of writing.

Traditional use and traditional ecological knowledge: Long Lake south


Author(s): Wondrasek, R.

Year: 2006

Abstract:
This section of the larger Long Lake South Environmental Impact Assessment is very brief as consultations with First Nations were ongoing at time of release. It is predominantly comprised of a report on baseline conditions, gathered from field surveys of the regional and local study areas, initial meetings with Aboriginal communities, and a limited literature review. The report on baseline conditions note that three categories of issues were raised: plant and animal harvesting areas, traplines, and habitation sites (including trapline cabins). Three hunting sites and six historic sites associated with traditional ecological knowledge were identified. The report notes that none of the sites were within in the project footprint and therefore no impact to the sites was expected.

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.

What if and so what in northwest Canada: Could climate change make a difference to the future of the Mackenzie Basin?


Author(s): Cohen, S. J.

Year: 1997

Abstract:
Global climate change, also known as global warming, is one of the most challenging elements of global environmental change. If atmospheric concentrations of carbon dioxide and other "greenhouse gases" continue to increase, global mean air temperatures are expected to rise 1.5 degrees to 4.5 degrees C within the next several decades. High-latitude regions are projected to experience above-average increases. What effects would such a warming have in the Canadian Arctic? In a recently completed study of the Mackenzie Basin in north-western Canada, regional stakeholders provided their responses to the "what if?" scenario of climate change in their region. This scenario includes more frequent landslides due to permafrost thaw, lower minimum annual river and lake levels, more forest fires, and lower yield from softwoods. These impacts could offset potential benefits from a longer growing and ice-free season. Regional stakeholders, including provincial and territorial governments, aboriginal organizations, and the private sector, felt confident about their abilities to adapt, so long as climate change would be predictable and gradual. Some potential impacts, however, could be very significant for renewable resources and aboriginal communities, and some stakeholders spoke of intervention into national and international policy arenas to raise awareness outside of the Mackenzie Basin.

Enter keywords or search terms and press Search

Search this site


Subscribe to the site

Syndicate content

Bookmark and Share