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Oil Sands Environmental Management Bibliography

The Cumulative Environmental Management Association (CEMA)partnered with the Oil Sands Research and Information Network (OSRIN) to create the new Oil Sands Environmental Management Bibliography, which includes documents relevant to the environmental management of oil sands development in Alberta. The majority of the documents focus on the mineable oil sands in the Athabasca deposit, though some documents relate to in-situ developments. This bibliography was last updated in November 2014.

Food habits of mink (Mustela vison) and otter (Lutra canadensis) in northeastern Alberta

Authors Gilbert, F. F.
Year of Publication: 1982

Abstract:
Scats of mink (Mustela vison) and otter (Lutra cawdensis) in northeastern Alberta contained different food items in different habitat types according to type of water body. Brook stickleback (Culaea inconstans) was the most frequently encountered food item in scats of both species from a drainage system dominated by lakes and for otter from a second drainage system dominated by streams. However, mink had varying hare (Lepusamericanus) as their primary food item by frequency of occurrencein this latter situation and mammalian items were significantly ( P < 0.01) more frequent. Otter scats contained more fish and invertebrates ( P < 0.01) and fewer mammals ( P < 0.01) and birds ( P < 0.05) than mink scats. Both otters and mink appeared to exploit avian species to a greater degree ( P < 0.01) in the lake-dominated drainage. The frequency of avain remains in otter scats was very high and probably reflected high utilization of breeding and moulting waterfowl.

Food web structure in oil sands reclaimed wetlands

Year of Publication: 2013

Abstract:
Boreal wetlands play an important role in global carbon balance. However, their ecosystem function is threatened by direct anthropogenic disturbance and climate change. Oil sands surface mining in the boreal regions of Western Canada denudes tracts of land of organic materials, leaves large areas in need of reclamation, and generates considerable quantities of extraction process-affected materials. Knowledge and validation of reclamation techniques that lead to self-sustaining wetlands has lagged behind development of protocols for reclaiming terrestrial systems. It is important to know whether wetlands reclaimed with oil sands process materials can be restored to levels equivalent to their original ecosystem function. We approached this question by assessing carbon flows and food web structure in naturally formed and oil sands-affected wetlands constructed in 1970–2004 in the postmining landscape. We evaluated whether a prescribed reclamation strategy, involving organic matter amendment, accelerated reclaimed wetland development, leading to wetlands that were more similar to their natural marsh counterparts than wetlands that were not supplemented with organic matter. We measured compartment standing stocks for bacterioplankton, microbial biofilm, macrophytes, detritus, and zoobenthos; concentrations of dissolved organic carbon and residual naphthenic acids; and microbial production, gas fluxes, and aquatic–terrestrial exports (i.e., aquatic insect emergence). The total biomass of several biotic compartments differed significantly between oil sands and reference wetlands. Submerged macrophyte biomass, macroinvertebrate trophic diversity, and predator biomass and richness were lower in oil sands-affected wetlands than in reference wetlands. There was insufficient evidence to conclude that wetland age and wetland amendment with peat–mineral mix mitigate effects of oil sands waste materials on the fully aquatic biota. Although high variability was observed within most compartments, our data show that 20-year-old wetlands containing oil sands material have not yet reached the same level of function as their reference counterparts.

Forensic source differentiation of petrogenic pyrogenic and biogenic hydrocarbons in Canadian oil sands environmental samples

Year of Publication: 2014

Abstract:
To facilitate monitoring efforts, a forensic chemical fingerprinting methodology has been applied to characterize and differentiate pyrogenic (combustion derived) and biogenic (organism derived) hydrocarbons from petrogenic (petroleum derived) hydrocarbons in environmental samples from the Canadian oil sands region. Between 2009 and 2012, hundreds of oil sands environmental samples including water (snowmelt water, river water, and tailings pond water) and sediments (from river beds and tailings ponds) have been analyzed. These samples were taken from sites where assessments of wild fish health, invertebrate communities, toxicology and detailed chemistry are being conducted as part of the Canada-Alberta Joint Oil Sands Monitoring Plan (JOSMP). This study describes the distribution patterns and potential sources of PAHs from these integrated JOSMP study sites, and findings will be linked to responses in laboratory bioassays and in wild organisms collected from these same sites. It was determined that hydrocarbons in Athabasca River sediments and waters were most likely from four sources: (1) petrogenic heavy oil sands bitumen; (2) biogenic compounds; (3) petrogenic hydrocarbons of other lighter fuel oils; and (4) pyrogenic PAHs. PAHs and biomarkers detected in snowmelt water samples collected near mining operations imply that these materials are derived from oil sands particulates (from open pit mines, stacks and coke piles).

Forest floor as an amendment in oil sand reclamation

Authors McMillan, R. A.
Year of Publication: 2005

Abstract:
Syncrude Canada Inc. and Suncor Energy Ltd. are two oil sand operators in the Athabasca region. Following surface mining, land reclamation entails re-establishment of functioning ecosystems using salvaged mineral soil materials and organic amendments. While traditional reclamation uses peat, benefits from using the forest floor stripped from pre-mining areas were examined. This study investigated the reclamation techniques in terms of nitrogen (N) fluxes. Specifically, net N nitrogen mineralization rates and microbial biomass were measured in an undisturbed forest and several reclaimed sites at Syncrude and Suncor. Results suggested no significant difference in net N mineralization rates between sites. However, there were differences in microbial biomass possibly related to differences in moisture content. A lab experiment manipulating soil moisture content showed a positive relationship between microbial biomass N and moisture content. No relationship with microbial biomass C was found, possibly due to a shift in microbial community structure.

Forest floor development and biochemical properties in reconstructed boreal forest soils

Year of Publication: 2011

Abstract:
Following resource extraction by surface mining in the oil sands region of northeastern Alberta, sites are reclaimed by reconstructing soils using a variety of salvaged organic and mineral materials, and planted to native tree species. This study assessed the influence of three distinct stand types (Populus tremuloides Michx., Pinus banksiana Lamb., and Picea glauca (Moench) Voss) on forest floor development (thickness, morphology, total carbon and nitrogen contents), soil organic matter composition, and associated soil microbial communities. Forest floor and top mineral soil (0–5 cm) samples were collected from 32 sites reclaimed 16–33 years ago. Soil organic matter composition was measured using ramped-cross-polarization 13C nuclear magnetic resonance, and microbial communities were characterized using phospholipid fatty acid analysis. Morphological characteristics indicated little mesofaunal or fungal activities within the forest floors. Stands dominated by P. tremuloides fostered more rapid forest floor development than the coniferous (P. banksiana and P. glauca) stands, and showed a significant increase in forest floor thickness with time since reclamation. Within the P. tremuloides stands, forest floor development was accompanied by temporal changes in soil organic matter composition that reflected inputs from the canopy. Soil microbial community composition differed among reclamation treatments of the reconstructed soils, specifically as a function of their subsoil mineral textures, when canopy cover was below 30%. Above 30%, significant differences became apparent among stand types. Taken together, our results document how canopy cover and stand type were both important factors for the reestablishment of plant–soil relationships at these sites. Furthermore, achieving a canopy cover of 30% emerged as a critical threshold point during soil reclamation.

Forest floor development in reclaimed boreal forest soils of northern Alberta

Authors Sorenson, P.
Year of Publication: 2011

Abstract:
Following oil extraction by surface mining, sites are reclaimed by reconstructing soils using salvaged organic and mineral materials, and planted to native tree species. This study assessed the influence of stand type (Populus tremuloides Michx., Pinus banksiana Lamb, and Picea glauca (Moench) Voss) on forest floor development, soil organic matter composition, and microbial community composition in 32 sites reclaimed 16 to 33 years ago. In three sites, spatial variability in soil nutrients was examined. P. tremuloides stands fostered more rapid forest floor development than coniferous stands, showed changes in soil organic matter composition with time that reflected inputs from the canopy, and was the only stand type with relationships between the canopy, forest floor, and all macronutrients. Furthermore, microbial community composition in reconstructed soils differed among stand types when canopy cover was above 30%. Canopy cover and stand type are important for reestablishment of plant-soil relationships at these reclaimed sites.

Forest floor protection during drilling pad construction and its benefits for natural regeneration of native boreal forest vegetation

Authors Bachmann, S.
Year of Publication: 2014

Abstract:
I tested forest floor protection techniques in the construction and reclamation of temporary drilling pads to restore native boreal canopy and understory cover. By covering and delineating the forest floor I hoped to reduce damage to the vegetative propagule bank, so clonal species such as aspen (Populus tremuloides) can quickly re-establish from root sprouts after being cut on disturbed sites. These were compared to the current soil salvage and replacement operations, assessing density, height and survival of aspen regeneration, as well as associated understory cover and richness. After re-contouring and soil placement, I measured the extent of surface disturbance, slash cover, soil temperature, soil bulk density and nutrient status in the four treatments and control plots. Aspen and understory recovery was prolific in protected sites and exceeded that of salvaged sites. Only little soil compaction from covering and moderate soil surface disturbance in forest floor protection sites were detected.

Forest productivity in naturally saline landscapes of Alberta's boreal forest

Year of Publication: 2007

Abstract:
The effect of salinity on boreal forest plants is of growing concern today because oilsands mining in northern Alberta produces large areas of salt-affected soils that need to be reclaimed. We examined the soil and vegetation characteristics of seven naturally saline forested sites in northern Alberta to better understand the effect of soil salinity on mature boreal forest plants. Soil salinity, sodicity, pH, nutrients, moisture content, and temperature were measured in high, medium, and low salinity soils; salt ions, nutrients, and carbon and nitrogen stable isotope ratios were measured in aspen and white spruce foliage. Both tree height growth and basal area growth were determined. Aspen growth decreased with increasing salinity, but white spruce growth seemed to be more strongly affected by environmental factors other than salinity. Both species appeared to be robust against nutritional toxicities and deficiencies commonly encountered in saline soils, indicating a tolerance for some saline conditions.

Fort Assiniboine Sandhills Wildland Provincial Park : park guide

Authors
Year of Publication: 2012

Abstract:
Fort Assiniboine Sandhills was designated a wildland park in 1997. It covers approximately 66 square kilometres along the north shore of the Athabasca River northeast of the Hamlet of Ft. Assiniboine, roughly 40 kilometres northwest of Barrhead. The Athabasca River forms the eastern boundary of the park.

Fort McMurray Athabasca tar sands development strategy

Authors
Year of Publication: 1972

Abstract:
The basic premise is that the demand for synthetic crude oil is from markets external to Canada, consequently one primary objective and five secondary objectives are suggested: 1. Alberta should regulate and control the Athabasca tar sands development for the socio-economic benefit of Albertans. 2. The social benefits accruing to Albertans should be inherent in the development of the resource and the associated urban development. 3. The rate and direction of the development should be dependent on Canada's ability to participate economically and on Alberta's requirements for economic development. 4. The development should result in a net long term benefit and improvement to Alberta's physical and ecological environment. 5. The evolvement of tar sand technology should be led by Canadian technologists for the benefit of Canadians. 6. The development should be an integration of community, industry and government. In suggesting these objectives there is an explicit recognition of the continuous requirement for balancing the concept of \"investor confidence\" and \"controlled development\". Investor confidence must be maintained if the resource development is to complement and supplement the socio-economic development requirements of Albertans. These objectives are used in projecting a development strategy which envisages a much slower rate of development than suggested by foreign markets. The orderly development rate is regulated by the first and third objective based on the basic premise. The rate of development of one plant in every four years is consistent with present technology and construction requirements.

Four years of simulated N and S depositions did not cause N saturation in a mixedwood boreal forest ecosystem in the oil sands region in northern Alberta Canada

Authors Jung, K., & Chang S. X.
Year of Publication: 2012

Abstract:
We conducted a simulated nitrogen (N) and sulfur (S) deposition experiment in the Athabasca oil sands region (AOSR) where NOx and SO2 have been emitted from oil sands mining/extracting and upgrading activities and then deposited to the surrounding ecosystems for decades. To evaluate changes in tree growth rates, N pool sizes, and nutrient losses by S and N deposition, the following four treatments were applied: control (CK), N addition (+N, 30 kg N ha−1 yr−1), S addition (+S, 30 kg S ha−1 yr−1), and +NS additions (+NS, 30 kg N and 30 kg S ha−1), from 2006 through 2009. Nitrogen addition increased (p < 0.05) tree growth in the +N and +NS treatments, indicating N-limitation in the studied forest, while none of the treatments affected understory growth or soil microbial biomass. The treatments affected inorganic N concentrations in the soil only immediately following N addition. Minimal amounts of NO3- were leached below 45 cm (considered to be below the main rooting zone) of the soil profile in any of the treatments. Decreases in exchangeable Ca2+ and Mg2+ by N and S additions were likely due to increased tree uptake following increased tree growth in the former and increased leaching with sulfate in the latter. Although the lack of significant N leaching indicates that the risk of N saturation was low after 4 yr of elevated N deposition, reduction of exchangeable base cations implies that nutrient imbalance remains a concern in AOSR in the long term.

Fourier transform ion cyclotron resonance mass spectrometry of principal components in oilsands naphthenic acids

Year of Publication: 2004

Abstract:
Naphthenic acids present formidable challenges for the petroleum industry and are a growing concern in the aquatic environment. For example, these acids are responsible for corrosion of refinery equipment, leading to the incurrence of additional costs to the consumer, and are toxic to aquatic wildlife, making disposal and remediation of contaminated waters and sediments a significant problem. The detection and characterization of naphthenic acids is therefore of considerable importance. Fourier transform ion cyclotron resonance mass spectrometry is presented as a technique with inherently ultra-high mass accuracy and resolution, affording unequivocal assignments. The suitability of the technique for environmental applications is demonstrated to characterize two different commercial mixtures of naphthenic acids and one oilsands tailings pond sample.

Fracture-dominated subsurface flow and transport in a sloping reclamation cover

Year of Publication: 2009

Abstract:
The successful performance of reclamation soil covers over saline-sodic overburden associated with oil sands mining in northern Alberta, Canada, depends on the dynamics of water and salt migration within these covers. Subsurface flow exerts a significant control on the distribution of soil moisture and salts within reclaimed landscapes. A conceptual model for fracture-dominated lateral subsurface flow and transport in a sloping clay-rich reclamation soil cover over saline-sodic shale overburden was developed based on an interpretation of field observations. This model was then verified through the use of numerical simulations. The conceptual model assumes that lateral subsurface flow is dominated by a preferential flow system and that chemical equilibration between fresh snowmelt water stored in the macropores and higher concentration pore water stored in the soil matrix is nearly instantaneous. Numerical modeling of subsurface flow indicated that the discharge rate and cumulative volume are controlled by the bulk saturated hydraulic conductivity and drainable fracture porosity, respectively. A drainable fracture porosity ranging from 3 to 4% yielded a simulated cumulative discharge similar to measured values. A pseudo-equivalent porous medium transport model was used to simulate the Na+ concentration of collected subsurface flow with time. General agreement between measured and simulated values demonstrates that discharge concentrations increase as the depth of perched water diminishes with time and water drains through macropores associated with a matrix of higher solute concentrations lower in the cover profile.

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