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Lakeland County AB
Canada

Probabilistic approach for design and hydrologic performance assessment of reconstructed watersheds


Year: 2007

Abstract:
The oil sands mining industry in Canada has made a commitment to reclaim mining areas to an equivalent capability to that which existed prior to mining. An essential requirement in the design of reclamation covers to meet this objective is that all covers must have a sufficient available water holding capacity AWHC in order to supply sufficient moisture for vegetation over the summer moisture deficit typical in the region. AWHC is currently based on static evaluations of wilting point and field capacity under a constant annual evapotranspiration demand. This paper presents an alternative probabilistic approach by which the hydrologic performance of these reclamation soil covers can be assessed. A field-calibrated water balance model is used along with the available historical meteorological record to estimate the maximum soil moisture deficit that a soil cover is able to sustain over the growing season. Frequency curves of the maximum annual moisture deficit are used to assess the probability that a cover is able to provide any particular threshold of moisture demand. The method also allows for a quantification of the predictive uncertainty of the model. The predictive uncertainty is used as a margin of safety to estimate a design value of moisture deficit for various alternative cover designs. This paper recommends procedures for a frequency-based assessment and design of reclamation soil covers in the oil sands industry. This method takes into account climatic variability as well as parameter uncertainty in estimating the soil moisture deficit.

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.

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


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

Year: 2014

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

Rapid densification of the oil sands mature fine tailings (MFT) by microbial activity


Author(s): Guo, C.

Year: 2009

Abstract:
The Mildred Lake Settling Basin (MLSB) is the largest disposal site for mature fine tailings (MFT) at the Syncrude Canada Ltd oil sands plant. Since 1996, MFT densification in the MLSB has significantly accelerated due to microbial activity. Methane-producing microorganisms, known as methanogens, have become very active. A field and laboratory research program has been performed to study the mechanisms leading to the rapid densification. This research program consisted of historical monitoring data analyses, field investigations, small-scale column tests, and gas MFT densification tests. The field investigations have shown that the rapid densification of the MFT has occurred in the southern part of the pond ranging from 8 m to 15 m below the water surface. A connection existed between the rapid densification zone and the zone with intense microbial activity at the pond. The small-scale column tests demonstrated that, with increases of biogas generation, water drainage from the MFT was enhanced. Gas MFT densification tests showed that, stress histories and total pressure affected MFT densification property during microbial activity. Under high total pressure (6-7 m below pond surface) gas bubbles had difficulty to release. For MFT without pre-consolidation or under a preloading, during rapid gas generation, water was rapidly drained out. For over-consolidated MFT, water flowed back into MFT quickly during intense biogas generation. The concept of operative stress, the difference between the total stress and pore water pressure for the soil with large gas bubbles, was introduced to analyze the densification behavior of gassy MFT. Under high total pressure and under a preloading (1 kPa), excess pore pressure increased and operative stress decreased during rapid gas generation while water drainage from the MFT was accelerated. Total pressure and stress history also affected the structure and permeability of the MFT during microbial activity. Under low total pressure (1 m below pond surface) and without preconsolidation, the MFT permeability increased after intense microbial activity.

Rapid densification of the oil sands mature fine tailings (MFT) by microbial activity


Author(s): Guo, C.

Year: 2010

Abstract:
The Mildred Lake Settling Basin (MLSB) is the largest disposal site for mature fine tailings (MFT) at the Syncrude Canada Ltd oil sands plant. Since 1996, MFT densification in the MLSB has significantly accelerated due to microbial activity. Methane-producing microorganisms, known as methanogens, have become very active. A field and laboratory research program has been performed to study the mechanisms leading to the rapid densification. This research program consisted of historical monitoring data analyses, field investigations, small-scale column tests, and gas MFT densification tests. The field investigations have shown that the rapid densification of the MFT has occurred in the southern part of the pond ranging from 8 m to 15 m below the water surface. A connection existed between the rapid densification zone and the zone with intense microbial activity at the pond. The small-scale column tests demonstrated that, with increases of biogas generation, water drainage from the MFT was enhanced. Gas MFT densification tests showed that, stress histories and total pressure affected MFT densification property during microbial activity. Under high total pressure (6-7 m below pond surface) gas bubbles had difficulty to release. For MFT without pre-consolidation or under a preloading, during rapid gas generation, water was rapidly drained out. For over-consolidated MFT, water flowed back into MFT quickly during intense biogas generation. The concept of operative stress, the difference between the total stress and pore water pressure for the soil with large gas bubbles, was introduced to analyze the densification behavior of gassy MFT. Under high total pressure and under a preloading (1 kPa), excess pore pressure increased and operative stress decreased during rapid gas generation while water drainage from the MFT was accelerated. Total pressure and stress history also affected the structure and permeability of the MFT during microbial activity. Under low total pressure (1 m below pond surface) and without pre-consolidation, the MFT permeability increased after intense microbial activity.

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.

Reclamation with native grasses in Alberta: Field trial results


Year: 1986

Abstract:
Between 1978 and 1981 the Alberta Forest Service established 10 native grass field trials. The general objectives were: (1) to select the most promising native grass species for reclamation of high elevation disturbances in the Eastern Slopes; (2) to design and evaluate native grass seed mixtures; and (3) to develop recommendations for establishing and maintaining native grasses on high elevation disturbances. This report gives the first long-term results from these trials. Species performances were generally poor in the species adaptability trials at Cadomin. The wheatgrasses, especially Agropyron dasystachyum, A. trachycaulum and A. trachycaulum 'Revenue ' performed best overall. Phleum alpinum, Poa interior and Trisetum spicatum were considered failures. Contrastingly, most species performed reasonably well in the species adaptability trial at Mildred Lake. On both trial sites the cultivated species performed equally as well as their native counterparts. The performance of the native grass mixture was poor in the nurse crop x fertilizer rate x seeding rate trials at Cadomin. Fertilization produced a significant increase in plant cover. Neither the nurse crop nor the seeding rate treatments had any significant effect on the performance of the seed mixture. Seed mixtures containing wheatgrass species, especially dasystachyum, performed best in the four seed mixture trials. In contrast, the only seed mixture lacking a wheatgrass generally had the poorest results. The cultivated companion crops had little or no effect on the plant cover of the native grass mixtures. The best native grass mixtures performed equally as well as the best cultivated grass-legume mixtures. In the establishment methods trial at Cadomin the most successful treatments were those that covered and protected the seed. Drill seeding and broadcast seeding followed by application of a mulch produced the highest plant covers. The hydroseeding treatments, in which the seed and mulch were applied together, gave the lowest plant covers. The results from this trial suggested that native grasses, if established properly, can produce adequate cover for erosion control purposes. The revegetation treatments were generally more successful on the native mineral soil than the coarser textured overburden. Most species produced higher plant cover on the mineral soil. Furthermore, the mineral soil supported substantially higher species richness (number of species), indicating the plant communities were more diverse on mineral soil than overburden.

Regional hyrdrologic controls on acid-sensitivity of lakes in boreal Canada: An isotopic perspective


Author(s): Bennett, K. E.

Year: 2006

Abstract:
This study applied the use of a stable isotope mass-balance model to calculate water throughflow, residency and water-yield and to assess acid-sensitivity for 50 lakes in the Athabasca Oil Sands region of northeastern Alberta. The research project was aimed at improving existing regional hydrologic estimates, based on coarse-scale runoff values derived from river gauging stations. Regional isotopic variations measured for components of the water cycle indicated a wide range of hydrologic conditions prevail, from throughflow, high water-yield lakes (186 mm.yr-1) to evaporative, low water-yield systems (23 mm•yr-1). Notably, hydrology is shown to be a controlling factor on acid-sensitivity and may be altering acid-sensitivity via such processes as water flow through peatland dominated catchments or convergence with acidic neutralizing soils, geology or ground waters. At the throughflow end of the hydrologic spectrum at low levels of isotopic enrichment, isotopes in precipitation were sensitive up to 30%. Relative humidity, on the other hand, is sensitive at high levels of enrichment at the evaporative end of the scale on the order of 25%. This application, in conjunction with landscape and chemical analysis, highlighted the over-riding hydrologic processes occurring at lowland and upland systems of the Boreal Plain that may lead to increased acid-sensitivity or buffering capacity. This thesis documents the first ever demonstration of an isotope mass-balance model to estimate water-yields and subsequently assess critical acid loadings in North America. The results of this research project will allow for improved predictive ability and management of acid-sensitive aquatic ecosystems within future planning frameworks.

Report on Lake Athabasca walleye samples for use in the validation of the walleye evaluation criteria


Author(s): Franzin, W. G.

Year: 2011

Abstract:
This document is a summary report on the length, weight data and otoliths for aging of 200 Walleye taken in the June 2011 Fort Chipewyan commercial fishery.

Report on movement and habitat use of fishes in the lower Athabasca River from 2008 -2009


Year: 2009

Abstract:
The objectives of this study were to monitor movements and determine fall and winter habitat use for key target fish species including flathead chub, burbot, lake whitefish and longnose sucker, and collect supplemental information of the location of burbot and lake whitefish spawning and egg incubation areas in the Lower Athabasca River.

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.

Revegetation research : 1976 progress report, sub-projects VE 7.2, 7.3, and 7.4


Year: 1977

Abstract:
Laboratory studies were conducted during 1976 to investigate native grasses and legumes potentially useful for revegetation on various soils. Plant growth was tested in various soils with and without the addition of fertilizer in the greenhouse and ill growth chambers. The Genera tested were: Agropyron Alopecurus, Bromus, Calamagrostis, Festuca, Phalaris, Phleum, Poa, Puccinellia, Astragalus, Hedysarum, Lupinus, Oxytropis, Glycyrrhiza, Lathyrus, Thermopsis, and Vicia. Field studies were conducted at Woodbend Station, Devon. Germination and early establishment were observed on unscarifled, fall-planted and scarified, spring-planted legumes. Work was begun at the Alberta Environment Research Station at Vegreville. Native grasses, naturalized grasses, agricultural varieties of grasses, and native and agricultural varieties of legumes were planted to be evaluated in the uniformity garden. Ft Fort McMurray, research areas were partly established on the Great Canadian Oil Sands Ltd. tailings dike site and the AOSERP Mildred Lake facility. The development of the seed production test sites at Peers, Waskatenau, and High Level were continued. Native species of legumes were seeded at the Peers legume seed-increase nursery. Native grass seed for plants which had been sown the previous year at four different sites in Alberta were harvested. The following tentative conclusions may be used for the planning of Future studies: (i) Plant growth can be established on tailings sand if there is adequate moisture present, but time of planting seems to be a critical factor in establishment; (ii) Native legumes can produce root nodules without the add1tion of inoculum, but capacity to produce nodules on tailings sand varies among species; (iii) Nutrient requirements and soil preferences of native species vary widely. However, it is difficult to establish plant growth on soils with a low pH, a high conductivity (i.e. high salt concentration), or, a high aluminum level; (iv) A high level of available fertilizer may wholly or partially inhibit germination of native legumes and some native grasses. The optimum concentration of fertiIizer is higher for plant growth than for seed germination in some native legumes, but the optimum is determined in part at least by the amount and type of amendment used to ameliorate the tailings sand; and (v) Amendment of tailings sand with silt may cause soil compaction and have subsequent adverse effects on the penetration of the cotyledons through the substrate. In sand amended with peat, the roots of the seedlings tend to remain in the amended layer. The optimum amount of amendment seems to depend to some extent on the species used.

Revegetation research: 1976 progress report. Sub-Projects VE 7.27.3 and 7.4


Year: 1977

Abstract:
Laboratory studies were conducted during 1976 to investigate native grasses and legumes potentially useful for revegetation on various soils. Plant growth was tested in various soils with and without the addition of fertilizer in the greenhouse and ill growth chambers. The Genera tested were: Agropyron Alopecurus, Bromus, Calamagrostis, Festuca, Phalaris, Phleum, Poa, Puccinellia, Astragalus, Hedysarum, Lupinus, Oxytropis, Glycyrrhiza, Lathyrus, Thermopsis, and Vicia. Field studies were conducted at Woodbend Station, Devon. Germination and early establishment were observed on unscarifled, fall-planted and scarified, spring-planted legumes. Work was begun at the Alberta Environment Research Station at Vegreville. Native grasses, naturalized grasses, agricultural varieties of grasses, and native and agricultural varieties of legumes were planted to be evaluated in the uniformity garden. Ft Fort McMurray, research areas were partly established on the Great Canadian Oil Sands Ltd. tailings dike site and the AOSERP Mildred Lake facility. The development of the seed production test sites at Peers, Waskatenau, and High Level were continued. Native species of legumes were seeded at the Peers legume seed-increase nursery. Native grass seed for plants which had been sown the previous year at four different sites in Alberta were harvested. The following tentative conclusions may be used for the planning of Future studies: (i) Plant growth can be established on tailings sand if there is adequate moisture present, but time of planting seems to be a critical factor in establishment; (ii) Native legumes can produce root nodules without the add1tion of inoculum, but capacity to produce nodules on tailings sand varies among species; (iii) Nutrient requirements and soil preferences of native species vary widely. However, it is difficult to establish plant growth on soils with a low pH, a high conductivity (i.e. high salt concentration), or, a high aluminum level; (iv) A high level of available fertilizer may wholly or partially inhibit germination of native legumes and some native grasses. The optimum concentration of fertiIizer is higher for plant growth than for seed germination in some native legumes, but the optimum is determined in part at least by the amount and type of amendment used to ameliorate the tailings sand; and (v) Amendment of tailings sand with silt may cause soil compaction and have subsequent adverse effects on the penetration of the cotyledons through the substrate. In sand amended with peat, the roots of the seedlings tend to remain in the amended layer. The optimum amount of amendment seems to depend to some extent on the species used.

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.

Segmentation analysis and bathymetric surveys of the Athabasca River - Segment 1


Year: 2008

Abstract:
This report provides a review available literature and data sources to determine segment boundaries within the Peace-Athabasca Delta (PAD) for the Athabasca River Delta channels. To support the segmentation analysis, and to determine the overwintering habitat potential within the major Delta channels, mapping grade bathymetric data were collected for several critical sites identified by the Instream Flow Needs Technical Task Group including: the Embarras River; Embarras River breakthrough channel to Mamawi Creek ( may also be known as Cree Creek); Mamawi Creek; Jackfish Creek (conveys Athabasca River water into Richardson Lake during flow reversals); Richardson River (conveys Athabasca River water during flow reversals); Fletcher Channel; Goose Island Channel; Big Point Channel; and, the area known as Big Eddy. The report contains a description of the field survey as well as its results.

Stromatoporoids of the Kaybob Reef, Alberta


Author(s): Fischbuch, N. R.

Year: 1959

Abstract:
From one hundred thin sections of core chips from the Beaverhill Lake formation of the Kaybob area, and also from the Slave Point (?) formation of the North Peace River area of Alberta, twelve species of the genera Actinostroma, Stromatopora, Stachyodes and Amphipora are figured and described. The above named genera are found also in the Lower Cairn formation of the Rocky Mountains, the Waterways formation, and the Swan Hills member of the Beaverhill Lake formation in the nearby Swan Hills field. The correlation suggested by stromatoporoids agrees with a brachiopod correlation. Amphipora are not diagnostic.

Suitability of small fish species for monitoring the effects of pulp mill effluent on fish populations, Athabasca River, 1994 and 1995


Year: 1996

Abstract:
The objectives of this project were addressed by first identifying common sentinel species immediately upstream and downstream of pulp mill effluents at Hinton and Whitecourt. Spoonhead sculpin and lake chub were identified as sentinel species because of their abundance in the Hinton and Whitecourt reaches of the river, respectively. These species are assumed to have limited mobility and a small home range. This project attempted to document the geographic extent of biochemical responses in fish subjected to prolonged exposures during low flow periods (i.e., fall and early spring). This was accomplished by conducting laboratory analyses on the fish tissues collected from the field to determine the potential for the pulp mill effluents to disrupt sex steroid levels and induce liver MFO activity.

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.

System dynamics approach to assess the sustainability of reclamation of disturbed watersheds


Year: 2005

Abstract:
The mining of oil sands in northern Alberta leaves behind large open pits, tailings, and overburden piles in which the surface and subsurface hydrology has been completely disrupted. Extensive reclamation work is required to reconstruct the entire landscape and reestablish the various elements of the hydrologic cycle. Syncrude Canada Ltd. has established a series of small instrumented watersheds in a reclaimed overburden pile at the Mildred Lake mine in northern Alberta, Canada, to test the sustainability of different reclamation strategies. The purpose of these field sites is to assess the performance of different reclamation strategies and track the evolution of the reclaimed landscape with time. The saline-sodic shale overburden has been covered with different (in type and depth) soil layers to provide sufficient moisture storage for vegetation while minimizing runoff and salt transport into the cover from the underlying overburden shale. In this paper, a system dynamics watershed model (SDWM) is developed to simulate one of the reconstructed watersheds and assess its ability to provide common watershed functions. The model is at an early stage, but preliminary results point to the potential of the system dynamics approach in simulating watersheds and testing different scenarios. The tested reclamation strategy seems to be satisfactory within a certain range of hydrologic conditions. Further validation of the SDWM is required, however, before relying on its results for decision support with regard to reclamation strategies.

Test of a bird deterrent device at a tailings pond, Athabasca oil sands, 1974


Year: 1976

Abstract:
Between 26 August and 30 October 1974, a reflector device was tested as a deterrent to birds at a small tailings pond (Lower Camp Tailings Pond) located on Syncrude's lease 17, approximately 40 km (25 mi) north of Fort McMurray, Alberta. This tailings pond provided a situation analogous (though on a smaller scale) to that expected to occur at the Mildred Lake Tailings Pond that will be constructed on lease 17. The discovery of two bitumen-covered ducks and the remains of approximately 25 other birds along the shore of the small tailings pond on 6 August 1974, indicated that birds had died at this pond. Accordingly, the results of this study also provided information on the extent to which this tailings pond was hazardous to water-associated birds. The results of this study indicated that the reflector device did not sufficiently deter shorebirds and passerines from landing along the shoreline of this pond. Few ducks and no geese were observed to land at this pond; consequently, it was not possible to determine the effectiveness of reflectors as a deterrent to these birds. Analysis of the data did indicate that such birds might be deterred by reflectors. Because few ducks or coots and no geese landed at the small tailings pond, the hazard of this pond was considered small to such birds. Evidence did indicate, however, that the risk of contacting bitumen was great for any such birds that did land on the tailings pond. Shorebirds readily landed on the shore of this pond and were observed to pick up bitumen on their feet and legs. The hazard to these birds was considered small – although some shorebirds are known to have died at this pond. The hazard of this pond to passerines was also considered small.

The Athabasca fluting field, Alberta, Canada: Implications for the formation of large-scale fluting (erosional lineations)


Year: 2000

Abstract:
Current drumlin and fluting hypotheses, centred on processes of formation, erosion and deposition by subglacial deformation, accretion by lodgement, glacial erosion, and meltwater erosion and deposition, rarely receive comprehensive field testing. This paper documents the morphology, internal structure, and landscape associations of the Athabasca fluting field, Alberta, and discusses how well these characteristics are explained by postulated fluting forming processes. Fluting hypotheses are comprehensively tested by this approach and their rejection or acceptance are firmly based on field observation and knowledge of processes. Using multiple criteria, fluting is shown to be erosional and not to be a product of pervasive subglacial deformation or accretion by lodgement. Morphology, landscape associations, bed truncation, plus glaciofluvial lags and gravel on fluting ridges are inferred to support erosion by meltwater. Intact primary bedding, synsedimentary faults and injection structures very close to the landsurface, showing no sign of shear deformation, are used to reject erosion by subglacial deformation. Fluting is shown to be closely associated with tunnel channels and indicates that these channels were overtopped by broad floods that formed the fluting field and eroded anabranching tracts over the length of the Alberta Plains. Prior to fluting formation, sequences with melt-out and lodgement till, conduit sediment and boulder lags record net deposition over an extended time period. Diapirism prior to fluting formation marks a period of extreme pressure gradients which are related to bed separation. Following fluting formation, there was only minimal landscape modification, dominated by glaciofluvial and glaciolacustrine deposition, not glacial processes. This progression is presented as evidence for two very different glacial regimes separated by a short period with diapirism and extensive landscape modification by meltwater erosion. We note that the study area was glaciated only once, during the Late Wisconsinian, and it follows that glacial sedimentation and landscape modification were confirmed to this single glacial episode.

The Chipewyan caribou hunting system


Author(s): Irimoto, T.

Year: 1981

Abstract:
This field study in ecological anthropology (man-nature relationships in activities), was done among the Caribou-Eater Chipewyan of northern Saskatchewan, Canada. Direct observation and active participation were used for recording and analyzing their caribou hunting system. The subsistence activities of the Chipewyan are classified in this article and recorded in terms of time-space use and participant involvement. The five major categories of activities are: food getting (FGA), food processing (FPA), sheltering (SHA), hide preparation (HPA) and manufacturing (MA). The three principles for structuring systems of activities on the basis of individual variations, particularly age and sex, are: 1) the temporal sequence of activities; 2) the allocation; and 3) the combination of activities. These various categories of activities are organized into the Chipewyan caribou hunting system.

The contribution of groundwater discharge to the overall water budget of two typical boreal lakes in Alberta/Canada estimated from a radon mass balance


Year: 2010

Abstract:
Radon-222, a naturally-occurring radioisotope with a half-life of 3.8 days, was used to estimate ground- water discharge to small lakes in wetland-dominated basins in the vicinity of Fort McMurray, Canada. This region is un- der significant water development pressure including both oil sands mining and in situ extraction. Field investigations were carried out in March and July 2008 to measure radon-222 distributions in the water column of two lakes as a tracer of groundwater discharge. Radon concentrations in these lakes ranged from 0.5 to 72Bq/m3, while radon concentrations in groundwaters ranged between 2000 and 8000 Bq/m3 . A radon mass balance, used in comparison with stable isotope mass balance, suggested that the two lakes under investigation had quite different proportions of annual groundwater inflow (from 0.5% to about 14% of the total annual water inflow). Lower discharge rates were attributed to a larger drainage area/lake area ratio which promotes greater surface connectivity. Interannual variability in groundwater proportions is expected despite an implied seasonal constancy in groundwater discharge rates. Our results demonstrate that a combination of stable isotope and radon mass balance approaches provides information on flowpath partitioning that is useful for evaluating surface-groundwater connectivity and acid sensitivity of individual water bodies of interest in the Alberta Oil Sands Region.

The design and installation of a field instrumentation program for the evaluation of soil-atmosphere water fluxes in a vegetated cover over saline/sodic shale overburden


Author(s): Boese, C. D.

Year: 2003

Abstract:
The mining of oil sands near Fort McMurray, Alberta, involves the stripping of salinesadie overburden to gain access to the oil-bearing formation. The overburden is placed in mined out pits and surface dumps and is re-contoured before being capped with a mandated 1 m soil cover. The potential for slope instability, subsidence, and salinization resulting from the character of the saline-sodic material and its interaction with fresh water makes it imperative that the amount of precipitation percolating below the root zone be minimised. Syncrude Canada Ltd is conducting a large scale cover trial at the Mildred Lake mine in order to assess the performance of different reclamation strategies. Four 1 hectare prototype covers were placed on an area referred to as the SW30-Dump in order to study the basic mechanisms controlling moisture movement within the cover systems. Three covers were constructed in 1999 with configurations of 1.00 m, 0.50 m and 0.35 m thick and consisted of a thin layer of peat overlying varying thickness of secondary soil. A fourth study site was established on a recently reclaimed watershed capped with a 1.00 m cover of peat/secondary mix in 1996. A field instrumentation program was carried out consisting of detailed monitoring of matric suction, volumetric water content and temperature within the different soil profiles, as well as measurements of runoff, interflow and site-specific meteorological conditions. Generally, all instrumentation performed well and was found to correctly measure the soil-atmosphere fluxes required to assess each cover alternative. Evaluation of the covers revealed that the 1m layered cover was the only one to maintain sufficient soil moisture for all monitored growing seasons. A significant portion of the available soil water was held within the peat layer. The other three covers lacked the required storage during drier periods and on numerous occasions soil suction values exceeded the wilting point

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