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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.

Great Canadian Oil Sands dyke discharge water. Summary report of the Scientific Enquiry Committee

Authors
Year of Publication: 1976

Abstract:
The Scientific Enquiry Committee was appointed by the Hon. D.J. Russell, Minister of the Environment, to investigate factors associated with the discharge of effluents from the Great Canadian Oil Sands (GCOS) tailings pond dyke to the Athabasca River. The terms of reference of the Enquiry were to evaluate the impact of the discharges on the Athabasca River, and to provide recommendations on any necessary action to be taken by Alberta Environment and Great Canadian Oi1 Sands Limited. The general nature of the terms of reference has permitted an independent and unrestricted enquiry.

Great Canadian Oil Sands experience in the commercial processing of Athabasca tar sands

Year of Publication: 1968

Abstract:
A brief review is given of the history of the Great Canadian Oil Sands (G.CØS.) project to recover 45,000 bpd of synthetic crude oil from the Athabasca Tar Sands by open pit mining, hot water extraction, coking, and hydrorefining. This paper then discusses the startup and initial operation of the G.CØS. plant. Emphasis is directed toward actual vs. design performance and a general discussion of operating problems. Included in the technical discussion are geological and mechanical problems encountered in mining tar sand, performance of the hot water extraction process, coking of Athabasca bitumen, hydrorefining of coker distillate produced from bitumen, and properties of the finished synthetic crude oil.

Greener social constructions: Marie Lake Fort Chipewyan and the Alberta oil sands

Authors Brodie, S.
Year of Publication: 2014

Abstract:
There is considerable debate in the green criminological and environmental sociological literature regarding achieving environmental reform. This dissertation contributes to the discussion through a qualitative constructivist interpretation of regional/national news media depictions of two environmental/industrial controversies. The embroiled controversies pit concerned social actors from the Alberta communities of Marie Lake and Fort Chipewyan against Canadian oil sands proponents. Using grounded theory methods and NVivo 10 software, media depictions of the controversies were examined as indicative of the dominant voices at the intersection of a public conversation about the harms caused by the oil sands industry. Very few issue entrepreneur efforts resulted in meaningful environmental reforms, but several key findings emerged. First, we must provide empowering eco-solutions for government, appreciating that politicians are particularly adept at avoiding the negativity accompanying symbolically charged environmental issues. Second, there is value in embracing human interests as a means to save nature, recognizing that social actors can appear self- serving when they affix conventional environmental concerns to anthropocentric (human- centered) causes. Third, sensationalizing isolated aspects of an environmental issue can allow attention to be diverted from fundamental environmental considerations. Fourth, issue entrepreneurs must remain cognizant of the ways in which ideology can defile science during an environmental controversy. Fifth, issue entrepreneurs must acknowledge that scientists are frequently ill prepared to portray their environmental findings against political ideology, and in the media where suspenseful stories routinely take precedence to nuanced and contextualized environmental portrayals. Sixth, it is important to depict environmental controversies in ways that cast science as only one part of a broader landscape of environmental decision-making that also acknowledges localized/first-hand experiences, and the precautionary principle. Lastly, official “truth- seeking” investigations by authoritative governmental agencies often subjugate other important avenues for understanding environmental realities. These key findings are placed in a constructivist framework entitled greener social constructions. The framework contributes to an evolving body of environmental social constructivist literature critical of ways in which journalists, policymakers, environmentalists, criminologists, and concerned publics include the environment and environmentalism in their communications. Ultimately, greener social constructions are synonymous with conceiving more compelling ways to remake the planet’s future.

Greenhouse gases: How does heavy oil stack up?

Year of Publication: 1991

Abstract:
Life-cycle emissions of direct greenhouse gases (GHG) have been calculated to elucidate the global warming impacts of various fossil fuel feedstocks. Calculations were made for the transportation sector using five fossil fuel sources: natural gas, light crude oil, conventional heavy oil, crude bitumen recovered through in-situ steam stimulation, and crude bitumen recovered through mining. Results suggest that fuels sourced from light crude oil have the lowest GHG emissions, while conventional heavy oil has the highest GHG emission levels for this application. Emissions of methane can constitute a significant portion of the life-cycle GHG emissions of a fossil fuel. For all the fossil fuels examined, except conventional heavy oil, GHG emissions associated with their production, transport, processing, and distribution are less than one third of their total life-cycle emissions. The remainder is associated with end use. This confirms that consumers of fossil fuel products, rather than fossil fuel producers, have the most leverage to reduce GHG emissions. 2 figs

Greenhouse pot studies dealing with amendation of oil sands tailings: Effects of peat sewage sludge and fertilizer on plant growth mycorrhizae and microbial activity

Authors Parkinson, D.
Year of Publication: 1984

Abstract:
Carex and feather moss peats from northern Alberta were used as growth media for jack pine and slender wheatgrass and their microbiological properties assessed. Differences between the two peats were minimal. Following this assessment, mixtures of the two peats were used to amend oil sand tailings (55% peat, V/V) and either mineral fertilizers or sewage sludge were added at different rates. Slender wheatgrass and jack pine were grown in the greenhouse in the various growth media, and plant growth, microbial activity and mycorrhizal development were measured. Growth of both species was poor without the addition of either fertilizer or sewage. Fertilization up to the equivalent of 112:49:72 kg N:P:K ha-1 substantially increased shoot and root growth of slender wheatgrass. Shoot growth of jack pine reached a maximum at the 28:12:18 kg ha-1 rate, and pine roots weights were depressed when more than 56:24:36 kg ha-1 were applied. Maximum shoot growth of slender wheatgrass and jack pine occurred with the equivalent of 46 and 23 mT ha-1 sewage respectively. The addition of 92 mT ha-1 strongly depressed the growth of jack pine while slender wheatgrass was unaffected. In the absence of peat, slender wheatgrass was much more sensitive to sewage. VA mycorrhizal inoculum in the peat was sparse and high levels of fertilizer or the lowest level of sewage completely inhibited VA mycorrhizal infection. Ectomycorrhizal inoculum was abundant but infections were nil when more than 56:24:36 kg N:P:K ha-1 was applied and very strongly reduced when 23 mT ha-1 or more of sewage was applied. In the presence of slender wheatgrass, fertilizer increased microbial biomass but had no effect when no plants were present, i.e. fertilizer did not affect the decomposition of peat. Microbial activity (C02 efflux) was unaffected by the addition of fertilizer but decomposition of grass litter was reduced by high rates of fertilizer. When sewage was added to the growing medium, microbial activity and microbial biomass were increased and the decomposition potential was decreased. The presence of the fibrous rooted slender wheatgrass consistently inhibited the decay of grass litter as compared to unplanted systems.

Greening the oil sands

Authors Dembicki, G.
Year of Publication: 2013

Gregoire Lake monitoring program: Six month report April to September 1979

Authors Murray, W. A.
Year of Publication: 1981

Abstract:
This report presents a summary of the meteorological data collected by the meteorological tower network in the Gregoire Lake region of northeast Alberta during the spring and summer of 1979. The network was established to help monitor the impact on the environment by the Amoco Canada Co. Ltd. pilot plant. A previous report, prepared by Athabasca Research Corporation (Ferguson 1979), presented an analysis of the winter 1978-79 data. A discussion is presented of the theoretical meteorological background including synoptic and mesoscale influences on the dispersion of effluents emitted into the atmosphere. Field dispersion experiments in the oil sands area are reviewed briefly. The statistics of the various weather elements are discussed. Wind velocity was measured at the 30 m tower level at Anzac, the Gregoire Lake Provincial Park, the Amoco pilot plant, and Stoney Mountain. Temperature, relative humidity, vertical velocity, precipitation, barometric pressure, and solar radiation were to be monitored at the pilot plant. The system for recording these data was not completely debugged by the end of the summer so data are not available yet. The meteorological statistics and the case studies indicated that when the air is stable or neutral, the regional airflow is deflected to follow the contours of the ridge, which is south of Gregoire Lake, and parallel to the Athabasca and Clearwater rivers. Under convectively unstable conditions, air flow tended to be upslope at the plant site and on Stoney Mountain, but similar to the regional flow at the valley stations. Wind speeds were generally light in agreement with long-term records in the oil sands area. Temperatures also followed the longterm trends. Examination of local meteorological and upper air data from Edmonton and Fort Smith indicated that the high concentrations of nitric oxide recorded on 27 September 1979 may have been related to low mixing heights. The source was probably not the pilot plant because the wind had been from the northwest for several hours prior to the incident. It is recommended that the reliability of data acquisition be improved. A study such as this one depends on valid, complete data it is of little value to collect data which has uncertainties as to time, calibration, or scale zeroes.

Gross N transformations were little affected by 4 years of simulated N and S depositions in an aspen-white spruce dominated boreal forest in Alberta, Canada

Year of Publication: 2011

Abstract:
The effects of 4 years of simulated nitrogen (N) and sulfur (S) depositions on gross N transformations in a boreal forest soil in the Athabasca oil sands region (AOSR) in Alberta, Canada, were investigated using the 15N pool dilution method. Gross NH4+ transformation rates in the organic layer tended to decline (P < 0.10, marginal statistical significance, same below) in the order of control (CK, i.e., no N or S addition), +N (30 kg N ha−1 yr−1), +S (30 kg S ha−1 yr−1), and +NS treatments, with an opposite trend in the mineral soil. Gross NH4+ immobilization rates were generally higher than gross N mineralization rates across the treatments, suggesting that the studied soil still had potential for microbial immobilization of NH4+, even after 4 years of elevated levels of simulated N and S depositions. For both soil layers, N addition tended to increase (P < 0.10) the gross nitrification and NO3− immobilization rates. In contrast, S addition reduced (P < 0.001) and increased (P < 0.001) gross nitrification as well as tended (P < 0.10) to reduce and increase gross NO3− immobilization rates in the organic and mineral soils, respectively. Gross nitrification and gross NO3− immobilization rates were tightly coupled in both soil layers. The combination of rapid NH4+ cycling, negligible net nitrification rates and the small NO3− pool size after 4 years of elevated N and S depositions observed here suggest that the risk of NO3− leaching would be low in the studied boreal forest soil, consistent with N leaching measurements in other concurrent studies at the site that are reported elsewhere.

Groundwater control for tailings dams built on large Pleistocene Channel deposits. A case study of integrated systems at Suncor's South Tailings Pond

Year of Publication: 2011

Abstract:
This paper provides a review of the engineered systems implemented at the south tailings pond (STP) for seepage mitigation and pressure relief, and the continued advancement in understanding the hydrogeological systems being managed. A brief recap of the project, the site hydrogeology and pertinent design criteria are provided, together with information on the design, installation, functionality and performance of the engineered groundwater control systems. The STP, an oil sands external tailings storage facility was commissioned in July 2006. Three of four principal seepage mitigation and pressure relief design elements have been installed in the Wood Creek Sand Channel (WCSC) aquifer. These are the Northwest Wellfield, the Southwest Cut-off Wall and the passive relief well system. Following the design basis, an observational approach was adopted, and the requirements for additional seepage mitigation design elements are assessed through ongoing performance monitoring for the tailings structure and the groundwater control systems, and using improved hydrogeological understanding gained from the application of geophysical technology.

Groundwater in harmony with oil sands development: A blueprint

Year of Publication: 2010

Abstract:
A Canadian-oriented paradigm shift is needed in how groundwater regimes are characterized and, thereby, optimally managed in the Fort McMurray oil sands theatre. Encouragingly, an issues-driven incipient shift is to some extent already taking place at the regional level within the domain of the regulatory agencies. At the local level, high quality groundwater characterization programs already are commonly initiated by mining proponents. Conversely, local scale efforts tend to focus on the proposed mine footprint, which inherently promotes somewhat fragmented coverage at a region scale. Paradoxically it would seem, although Canadian universities turn out strong graduate, masters and PhD level hydrogeologists, there is nevertheless a disconnect with how hydrogeology is actually practiced in Canada. In fact, there are two disconnects and, unfortunately for the insightful-level practice of hydrogeology, they are both of a fundamental nature. Firstly, universities, regulatory agencies at the provincial and federal levels, consultants and the actual oil sands players tend to operate to a deleterious extent in mutual isolation. That is not at all to say that these institutions are entirely disparate or that they otherwise operate in a vacuum, but they are missing cross-over subcomponents that are quite subtle. Secondly, hydrogeology, owing to the demands and rewards of the contaminated-groundwater industry has, to an unbalanced extent, resulted in a generation of contaminant hydrogeologists. A review of groundwater literature topics in leading journals will show that the research studies and case histories in the past two to three decades tend to favour projects at a local scale commensurate with high profile, high strength point sources, such as gasoline stations and dry cleaning stores. By way of contrast, however, some of the water issues in the Fort McMurray theatre are more of a sub-regional to regional scale. The hydrogeologic perspectives required are therefore more analogous to regional groundwater resources development rather than the comparatively localized nature of point-source contaminant hydrogeology. Indeed, the issues-driven nature of the incipient shift is in itself analogous to the proper versus random nature of regional groundwater resources exploitation. Specifically, proper development of groundwater resources tends to occur reactively when the groundwater regime is already failing in some way (e.g. classically, localized overpumping), which can lead to failure-driven recourse to insufficiently- informed decision making. Now, this is not to say that contaminant hydrogeology does not have an important role to play in oil sands development. To the contrary, contaminant hydrogeology remains an absolutely essential and integral consideration in regards to scenario predictions surrounding conceptual leaks from tank farms, landfills and tailings disposal areas. In parallel, however, a regional level of groundwater assessment skills, such as those that are analogous to regional groundwater resources development, are needed.

Groundwater instrumentation for mining projects

Authors Patton, F. D.
Year of Publication: 1979

Abstract:
Groundwater measurements enter into many phases of the mining industry. Recently, Westbay Instruments has developed new equipment for groundwater monitoring and sampling. This paper presents a brief summary of some of these developments, particularly as they affect the quality of technical data collected and the cost and scheduling of groundwater instrumentation programs.

Groundwater temperatures in the Athabasca oil sands area, Alberta

Year of Publication: 1978

Abstract:
Bottom-hole temperatures were measured in groundwater observation wells in the Athabasca Oil Sands area of Alberta. Depth of observation varies from 6–581 m in rocks of Holocene, Cretaceous, and Devonian age. Observations of temperature at various depths at a particular location were made in individual wells.At depths of 300 and 400 m, a correlation of both hydraulic head-loss and temperature with the elevation of the land surface at the observation well indicates that groundwater flow is the dominant parameter controlling subsurface temperatures. The control of groundwater flow on temperature and the location of observation wells in different positions in the groundwater flow system means that temperatures are not well correlated with depth.Bottom-hole temperatures from geophysical logs made in the area are significantly higher than values observed nearby at similar depths during this study. Published thermal gradient maps based upon information from geophysical logs give values which are about twice as high as those calculated with the present data.At depths less than about 60 m temperatures varied widely and at many well sites declined with depth. The average temperature of shallow groundwater was 5.9 °C at an average depth of 12.7 m. This fact indicated that the mean annual air temperature of −0.6 °C should not be used to approximate the temperature of shallow groundwater.

Growing season energy and water exchange from an oil sands overburden reclamation soil cover Fort McMurray, Alberta, Canada

Authors Carey, S. K.
Year of Publication: 2008

Abstract:
The oil sands mining industry in Canada is required to return mining areas to a land capability equivalent to that which existed prior to mining. During the reclamation process, ecosystems are created that bear little similarity to boreal forests that existed prior to mining. Quantifying the water balance of reclaimed ecosystems is critical in establishing whether there is sufficient moisture for vegetation growth and in the fate of salts, which can be toxic when drawn to the surface or leached out of the covers. At Syncrude Canada Ltd's Mildred Lake mine north of Fort McMurray, Alberta, the surface energy balance was measured atop a reclaimed saline-sodic overburden pile during three growing seasons using eddy covariance. At the onset of the study, the dominant vegetation was foxtail barley, which changed to sweet clover in 2004, and a low-density species mix in 2005, including some aspen and white spruce seedlings. The 2005 growing season was cooler and wetter than 2003 and 2004, and there were seasonal differences in the delivery of precipitation among years. There were distinct differences in the surface energy balance among the study years related to weather, soil moisture, vegetation and stage of growth. Latent heat was the largest consumer of energy in 2003, and mid-day fluxes of sensible and latent heat were approximately equal. In 2004, sensible heat became the dominant flux, primarily due to prolonged dry periods, whereas the wet 2005 season had the greatest latent heat flux density of any year. Ground heat flux declined throughout the growing season and ranged between 3 and 17% of net radiation. Total evapotranspiration was 246, 224 and 283 mm for 2003, 2004 and 2005, respectively. A total derivative analysis of the Penman-Monteith equation reveals the influence of available energy, vapour pressure deficit and surface conductance in controlling evapotranspiration.

Growth and elemental composition of jack pine (Pinus banksiana) seedlings treated with sodium chloride and sodium sulfate

Year of Publication: 2002

Abstract:
Mining activities in the boreal regions can increase levels of Na+, Cl– and SO4 2– in the forest soil. In the present study, we compared the effects of NaCl and Na2SO4 on the nutrient status of jack pine (Pinus banksiana). Germinated seedlings were grown in sand culture for 28 weeks before adding salts over a period of 3 days to treatment concentrations of 60 mM NaCl and 60 mM Na2SO4, which were maintained for 10 weeks. Salt treatments decreased shoot dry weights and shoot elongation rates. Growth and injury of seedlings were more affected by NaCl than equimolar Na2SO4. Plants treated with NaCl exhibited a delay in flushing of the terminal buds, reduced carotenoid content, extensive needle necrosis, and elevated levels of K, Mg, Mn, N and P in the shoot. Treatment with Na2SO4 resulted in reduced shoot Ca and K concentrations, while those of N and P increased. Necrosis was correlated with tissue Na only in NaCl-treated plants, and no relationship was found between growth or necrosis, and tissue levels of Cl or nutritional elements. We conclude that the greater toxicity of NaCl in jack pine is not due to nutrient deficiency.

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