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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.

The assimilative capacity of the Athabasca River for organic compounds

Year of Publication: 1980

Abstract:
Understanding the functioning of the aquatic ecosystem within the mainstem Athabasca River is of paramount importance if protection against the input of contaminants from oil sands developments is to be afforded to the Athabasca River itself, the Peace-Athabasca Delta, and Lake Athabasca. The term assimilative capacity has been applied to denote the dynamic ability of aquatic ecosystems to remain viable and productive in the face of external factors (natural or anthropogenic). An implicit assumption within this definition is the fact that aquatic ecosystems possess the ability to change in response to external factors while maintaining their productivity and diversity. The rate and extent of this adaptive capability is the underlying process of assimilative capacity which must be understood and therefore examined.

The Athabasca oil sands

Authors Govier, G. W.
Year of Publication: 1965

Abstract:
This paper is to be presented at the AIME Annual Meeting in Chicago, Illinois, on Feb. 14-18, 1965, and is considered the property of the Society of Petroleum Engineers of AIME. Permission to publish is hereby restricted to an abstract of not more 300 words, with no illustrations, unless the paper is specifically released to the press by the Editor of Journal of Petroleum Technology or the Executive Secretary. Such abstract should contain conspicuous acknowledgment of where and by whom the paper is presented. Publication elsewhere after publication in Journal of Petroleum Technology or Society of Petroleum Engineers Journal is granted on request, providing proper credit is given that publication and the original presentation of the paper. Discussion of this paper is invited. Three copies of any discussion should be sent to the Society of Petroleum Engineers office. Such discussion may be presented at the above meeting and considered for publication in one of the two SPE Magazine with the paper. Introduction In accepting Mr. Ward C. Pearl's invitation to speak to you on the subject of the Athabasca Oil Sands I was cognizant of the fact that a number of talks have recently been given on the subject and none too sure that I could add much of interest. It did seem, however, that some of you at least might be interested in a broad review of the subject with some emphasis on the current situation and the future outlook. This is what I plan to give. To those of you who heard or have read the excellent review of Mr. L. A. Bellows and Mr. V. E. Bohme presented in Dallas two years ago, my apologies for the necessary repetition. The Athabasca oil sands of north-eastern Alberta contain one of the worlds largest reserves of economically recoverable oil. The deposit extends over an area of 10,000 square miles and outcrops for a distance of more than 100 miles along the valleys of the Athabasca River and its tributaries. Fort McMurray, a small town in the heart of the oil sands, is approximately 235 air miles north-east of Edmonton. The town is served by railway and air lines, and the Provincial highway system is presently being extended into the area. There are virtually no all-weather secondary roads in this wilderness of muskeg and forest. Peter Pond, a Northwest Company fur trader and explorer who ventured into the Athabasca River system in 1778, was probably the first white man to see the oil sand outcrops. The tarry oil sands were also referred to in the journals of such famous explorers as Alexander Mackenzie, David Thomson, Sir Johns Franklin and Sir John Richardson between the years 1792 and 1848. Technical study of the oil sands began in 1875 when a member of the Geological Survey of Canada travelled the Athabasca River on a reconnaissance geological survey. Other geologists followed. After a survey in 1888, R. G. McConnell expressed the belief that the bitumen in the oil sand formation was the residue of a petroleum that entered from the Devonian limes tone below, and that oil might be found in normal fluid form at locations remote from exposures. As a result of his views, several wells were drilled in 1897-98 at Pelican Rapids on the Athabasca River, about 100 miles upstream from Fort McMurray. The oil sand was encountered at a depth of 740 feet and was found to contain the same heavy oil that is observed in the cutbanks near McMurray.

The Athabasca oil sands - a regional geological perspective Fort McMurray area, Alberta, Canada

Year of Publication: 2006

Abstract:
Most of the bitumen in the Athabasca deposit is hosted within fluvial, estuarine, and marginal marine deposits of the Lower Cretaceous Wabiskaw-McMurray succession. The present study is an integration of recent outcrop and subsurface studies, mainly focused in the Fort McMurray area of northeastern Alberta. The basis of the regional geologic framework includes outcrop sections (78), detailed core descriptions (165), and a net of subsurface wire-line log sections (14), all framed within modern concepts of regional correlation and sequence-stratigraphy. The paleogeographic evolution of the Athabasca Wabiskaw-McMurray succession includes five main phases: (1) Lower McMurray fluvial as lowstand deposits; (2) the lower part of the Upper McMurray fluvio-estuarine channel complexes which formed during early transgressive conditions; (3) the upper part of the Upper McMurray A sequences as relict bay-fill and marginal marine deposits formed during early and middle transgressive phases; (4) Wabiskaw D valley-fill developed during a relative sea-level drop at the end of McMurray time (valley-incision phase), which was backfilled during the ensuing transgression; (5) Wabiskaw D regional marine shale, deposited during widespread flooding of the main McMurray-Wabiskaw transgression; and (6) Wabiskaw C deposits formed during continued transgression or early regressive pulses. The regional geological framework has both economic and academic significance, providing better documentation and understanding of the compartmentalization of the oil sands mainly the result of the inherent geological heterogeneity of the Wabiskaw-McMurray succession. Such regional correlation and framework will aid in predicting subsurface and surface reservoir quality and in increased understanding of marginal marine and non-marine sequence stratigraphy.

The battle over oil sands access to tidewater: A political risk analysis of pipeline alternatives

Authors Hoberg, G.
Year of Publication: 2013

Abstract:
A massive, high-stakes political conflict has erupted over oil sands pipelines -- Keystone XL to the Gulf Coast, two pipeline proposals to the Pacific Coast, and new proposals for alternative routes to Eastern Canada. Alberta’s fossil fuel wealth is virtually landlocked, and as the growth of US demand for Canadian oil has stagnated, the sector’s profitability and future growth have been jeopardized. Environmentalists, recognizing the strategic importance of these pipelines to the growth of the sector, have aggressively sought to block their approval in an effort to limit the expansion of the oil sands. The conflict has spilled over into federal Canadian politics, interprovincial politics, and Canadian-American relations. This paper will examine this political controversy from a perspective that focuses on two core factors: the operation of institutional veto points and the distribution of risks and benefits across jurisdictions. The political risk to major infrastructure projects is a function of five factors: the number of institutional veto points; whether opposition groups have access to veto points; whether the project can take advantage of existing infrastructure; the salience of place-based, concentrated environmental risks; and the jurisdictional separation of risks and benefits We will see that each of the projects faces formidable political risks, but that these risks vary in type and magnitude by project. The key question is whether sufficient political pressure can be mounted to overcome these obstacles.

The Beaver Creek site: A prehistoric stone quarry on Syncrude Lease #22

Authors
Year of Publication: 1974

Abstract:
The significance of the Beaver Creek Quarry site and the kinds of information we may expect to glean from it may now be enumerated. With reference to the recently published results of archaeological reconnaissance conducted on the Tar Sands Syncrude Lease #17, it was noted that over 67% of the total stone assemblage recovered from 28 localities consists of quartzite derived from the Beaver Creek Quarry. It was also shown that the majority of the artifacts produced from Beaver Creek quartzite consists of flakes and detritus as opposed to finished tools. This in turn suggests that while the production of preforms at the quarry remains to be established, a significant amount of subsequent tool manufacture probably took place within a certain radius of quarry locale. The quartzite exposed along the banks of Beaver Creek may represent a unique deposit in the region. Little, indeed, is known of potential aboriginal stone sources in northern Alberta. In the central region of the province, water-rolled quartzite pebbles and cobbles found along streams and river beds is the ubiquitous stone type. North of the Tar Sands region lies the Canadian Shield which offers a variety of quartz minerals but in difficult to extract seams and veins. Some beds of chert are known to occur in the Paleozoic formations which border the pre-cambrian platform. To the west, near Peace River, Alberta dark volcanics are found in sites and en cache that were apparently traded in from aboriginal British Columbia. Should the Beaver Creek quartzite turn out to be a unique deposit in the Athabasca region, it offers an ideal opportunity to trace its dispersion and perhaps aboriginal trade networks as well. The value of being able to reconstruct a total technological process with an eye to defining an archaeological tradition has already been discussed. The potential of the Beaver Creek Quarry in this respect should be obvious. It is most opportune that this site exists and that it was located early in the archaeological research of the region. Once we have been able to define the technological tradition(s) contained in the Beaver Creek Quarry Site, attention may be turned to details regarding specific subsistence activities, seasonal cycles of food-getting, and the temporal aspects of technological traditions defined within the quarry deposit. The quarry site may constitute the basic reference from which interpretation of adjacent satellite sites will proceed. Thus adequate excavation and proper analysis of materials at the Beaver Creek Quarry may well play a key role in unraveling the prehistory of the Tar Sands region of northeastern Alberta.

The Canadian oil boom

Authors Kunzig, R.
Year of Publication: 2009

Citation:

The Canadian oil sands industry under carbon constraints

Year of Publication: 2012

Abstract:
We investigate the impact of climate policies on Canada’s oil sands industry, the largest of its kind in the world. Deriving petroleum products such as gasoline and diesel from oils sands involves significant amounts of energy, and that contributes to a high level of CO2 emissions. We apply the MIT Emissions Prediction and Policy Analysis (EPPA) model, a computable general equilibrium model of the world economy, augmented to include detail on the oil sands production processes, including the possibility of carbon capture and storage (CCS). We find: (1) without climate policy, annual Canadian bitumen production increases almost 4-fold from 2010 to 2050; (2) with climate policies implemented in developed countries, Canadian bitumen production drops by 32% to 68% from the reference 4-fold increase, depending on the viability of large-scale CCS implementation, and bitumen upgrading capacity moves to the developing countries; (3) with climate policies implemented worldwide, the Canadian bitumen production is significantly reduced even with CCS technology, which lowers CO2 emissions at an added cost. This is mainly because upgrading bitumen abroad is no longer economic with the global climate policies.

The Canadian oil sands: Energy security vs. climate change

Authors Levi, M. A.
Year of Publication: 2009

Abstract:
This report explores both the energy security and climate change implications of expanded oil sands production. It assesses current and future trends in the oil sands, including in the scale and cost of production and in the oil sands' impact on world oil markets, and evaluates the potential impacts of a range of policy options. The report concludes that the oil sands are neither critical to U.S. energy security nor catastrophic for climate change.

The changing boreal forest: Incorporating ecological theory into restoration planning

Year of Publication: 2012

Abstract:
Boreal ecosystems contain one-third of the world's forests and stored carbon, but these regions are under increasing threat from both natural and anthropogenic disturbances. Written by leaders from the forefront of private, public and academic sectors Reclamation and restoration of boreal ecosystems emphasizes a broad, conceptual approach to the specific application of empirical research into development planning, restoration and modelling of these ecosystems, the importance of which is highlighted at a time of global climate change as they act as carbon sinks. There is a focus on the reclamation of exploited ecosystems from a holistic standpoint, ranging from environmental and edaphic variables to the restoration of keystone flora. Recent advances in quantification of ecosystem services, such as habitat suitability and carbon storage modelling are also detailed. The book contains case-studies which address how both historical and novel assemblages can provide ecosystem stability under projected climatic and land-use scenarios.

The characterization analyses and biodegradation of naphthenic acids

Authors Clemente, J. S.
Year of Publication: 2004

Abstract:
I examined vegetation community development of reclaimed oil sands wetlands. Soil transfers from reference wetlands accelerated plant colonisation rates in a consolidated/composite tailings (CT) wetland. Hydrologic regimes differed between reference and CT wetlands making it difficult to explain observed differences in species composition. CT was a hospitable environment for plants, indicated by rapid colonization of isolated CT plots in reference wetlands. Wetland soil seed banks were more similar in species-relative abundances than composition. CT subsoils reduced emergence from seed banks (species composition and relative abundance). Salinity (surface waters, subsoils), wetland isolation and northern climates may slow or alter species replacement sequences for Reclaimed wetland plant communities. Seed bank analyses overestimated species richness, compared to field observations of wetland vegetation communities, except for Newly Constructed wetlands. Adding a CT subsoil treatment increased the accuracy of the seed bank analyses to predict initial vegetation establishment in a Newly Constructed CT wetland.

The characterization and distribution of inorganic chemicals in tributary waters of the lower Athabasca river oil sands region, Canada

Year of Publication: 2005

Abstract:
At present, there are two large industrial plants recovering oil from the lower Athabasca oil sands area and there are plans for several more mines in the area. There are environmental concerns for aquatic life in areas downstream of current and future oil sands activities. To assess and predict potential impacts of industrial activities, it is important to separate impacts from those produced by naturally occurring oil sands deposit. Studies were therefore conducted to determine whether the water quality of tributaries to the Athabasca River, which have not been impacted by anthropogenic activities, is affected by inorganic constituents resulting from flowing through reaches with natural oilsands deposit. Three tributaries, Steepbank River, Mackay River, and Ells River at upstream and downstream locations on each stream were investigated during four surveys from 1998 to 2000. In addition to some physical parameters such as pH, conductance and hardness and the major ions (calcium, magnesium, sodium, potassium, bicarbonate, chloride, sulfate, and silicates), seventeen trace metals were investigated. Some of these metals, especially iron and manganese, were of high concentrations and in some instances, particularly in a survey conducted during the spring freshets in April 1999, exceeded guidelines for the protection of aquatic life. The observed concentrations of metals seem to be of natural origin and can be used as base-line data for future assessment of anthropogenic activities in the oil sand region.

The chemical and biological evolution of mature fine tailings in oil sands end-pit lakes (PO)

Year of Publication: 2011

Abstract:
This presentation described an innovative bench-scale technique to characterize oil sand tailings and their impact on sediment oxygen demand (SOD) for future end-pit lake model behaviour. SOD is a dominant contributor to oxygen depletion in wetlands. The function and sustainability of a wetland ecosystem depends on the biochemical processes occurring at the sediment-water interface. The biochemical reactions associated with natural sediment can change with the addition of oil sands processed material (OSPM), which can affect SOD and ecosystem viability. It is important to establishing the biotic and abiotic controls of SOD. In order to evaluate the effectiveness of current wetland reclamation designs, it is important to establish the biotic and abiotic controls of SOD. The REDOX chemistry of fresh tailings sediment (MFT) was measured in this laboratory microcosm to determine the chemical and biological influences, and to study the role of developing microbial communities as new mature fine tailings (MFT) age. The study evaluated the changes in the main chemical, physical and biological populations of the MFT in both aerobic and anaerobic microcosms. A combination of microelectrode arrays and DNA profiling at the tailings water interface was used in the study.

The chemical and mineralogical composition of soil parent materials in northeast Alberta

Year of Publication: 1989

Abstract:
Seven major parent materials from the Athabasca oil sands area were investigated for detailed mineralogy and chemistry. The clay mineral species identified and quantified were mica, smectite, kaolinite, chlorite and vermiculite. The fine (50-250 pm) sand mineralogical suite was dominated by quartz, with lesser amounts of Na-, K-, and Ca-feldspars, and minor amounts of individual heavy mineral species. Electronoptical examination indicated that the feldspar grains in the parent materials have undergone extensive preglacial weathering. Regional mean levels of all analyzed elements (.A1, Ca, Fe, K, Mg, Na, Mn, P, Cr, Co, Cu, Ni, Pb, Sr, Y, ard Zn), with the exception of Ca, are related to textural variability. The variability of Ca levels within the study area is related to the occurrence ofcalcareous parent materials. The highest levels of all major, minor, and trace elements were associated with either the Legend unit derived largely from Cretaceous bedrcrck or with the modern sediments of the Athabasca delta.

The climatology of the Alberta Oil Sands Environmental Research Program study area

Authors Longley, R. W., & Janz B.
Year of Publication: 1978

Abstract:
In many respects, the climate of northeastern Alberta resembles that of the central portions of the province. It is generally somewhat cooler, especially In winter, and precipitation is slightly less. The area has a very definite continental climate and its distance from the Pacific Ocean and the mountains result in the almost complete absence of winter chinooks which are often thought of as an integral part of Alberta climate. Winters are cold with relatively little snow. Heavy snowfalls such as are common in the mountains and foothills are rare. Intense cold outbreaks can last from several days to a few weeks. Summers are relatively short and cool, although the occasional warm spell can cause temperatures to rise above 30°C. About two-thirds of the precipitation falls in the summer months with several major rainstorms generally accounting for much of the seasonal rain. Northeastern Alberta cannot be considered windy. High winds do occur but they are infrequent and rarely last longer than 12 to 24 hours. Although the topography does not have a major impact on the weather patterns, certain terrain features are significant in establishing windflow patterns that must be understood and considered In assessing the impact of climate on the development of the Athabasca Oil Sands.

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