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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.

Regional cumulative effects management framework for Cold Lake, Alberta

Authors Braat, T.
Year of Publication: 2002

Abstract:
The purpose of this Master's Degree Project is to develop a regional cumulative effects management framework for Cold Lake, Alberta to address the environmental impacts of existing and continued development. The framework provides a basis to address cumulative environmental effects that cannot be resolved by a single project proponent or industry acting alone. The framework Is based on current best practice of regional cumulative effects management, as determined by a review and evaluation of seven case studies and interviews conducted with professional practitioners. The framework consists of five components: a Regional Steering Body, EIA Processes, Regional Environmental Monitoring, Regional Information Management, and a Research Body. The Regional Steering Body leads the development and implementation of the framework. EIA Processes contribute to the framework through project-specific efforts and information collected through EIAs that contribute to a regional database. Regional Environmental Monitoring contributes to adaptive management and provides information for a regional database. The Research Body develops specialized knowledge and supports the development of thresholds. Regional Information Management refers to the collection, storage, and sharing of information from environmental monitoring, EIAs, and the Research Body. Sharing data supports comprehensive decision-making. The framework contributes to regional cumulative effects management through a collaborative multi-stakeholder effort that uses cumulative effects management tools, such as regional access management, integrated landscape management, regional information management, and thresholds. The framework provides a model for regional environmental management that may be applicable to other areas. The framework can improve the practice of CEA by facilitating scoping and providing baseline data.

Regional geology and hydrostratigraphy in northeast Alberta

Year of Publication: 1991

Abstract:
The Alberta Oil Sands Technology and Research Authority (AOSTRA) is currently planning to expand the Underground Test Facility (UTF) near Fort McMurray in northeast Alberta to a commercial size operation. As part of this expansion, it is envisaged to dispose of produced residual waters by on-site deep well injection. Selection of a disposal zone is currently under way. The upgrading of the UTF operations provides an opportunity for monitoring possible environmental effects related to the deep disposal of waste water resulting from the in situ extraction of bitumen from oil sands. With this in mind, and the additional objective of developing strategies for similar future activities, Environment Canada and the Alberta Research Council initiated a collaborative study of the effects of deep waste injection at the UTF site, with data support and cooperation from AOSTRA. The evaluation of the effects of deep injection of waste water is based on predictive modelling, which requires knowledge of the initial baseline hydrogeological conditions. Because the data are very scarce and incomplete at the local scale, a regional-scale hydrogeological study is required for the identification and characterization of the hydrostratigraphic units at the UTF site. For this purpose, a regional-scale study area is defined in northeast Alberta between latitudes 55�N and 58�N, and longitudes 110�W to 114�W (Tp 70-103, R 1-26, W4 Mer). The first step in the hydrogeological characterization is the description of the geology and the delineation of the hydrostratigraphy, which form the content of this progress report. The geology and hydrostratigraphy of the Phanerozoic sedimentary rocks in northeast Alberta are extremely complex due to various depositional, salt dissolution and erosional events. The shales interbedded with sandstones, red beds and evaporitic units of the Lower Elk Point Subgroup (Lower Devonian) overlying the impervious crystalline Precambrian basement from a dominantly aquiclude system at the base of the succession. The overlying carbonates of the Winnipegosis aquifer are separated from the mainly carbonate Beaverhill Lake aquifer system by the halite and shale of the Prairie-Watt Mountain aquiclude system. The argillaceous Ireton aquitard separates the Beaverhill Lake and Grosmont-Wabamun aquifer systems. All the Devonian strata have been eroded and subcrop at the sub-Cretaceous unconformity. They are overlain by the succession of the McMurray, Clearwater and Grand Rapids formations of the Lower Cretaceous Mannville Group. These are defined as weak aquifer-aquitards because of a complex combination of interbedded sands, shales and oil sands. The Colorado aquitard system (mainly shales with a few sandy units) lies at the top of the hydrostratigraphic succession. The hydrogeological characterization (porosity and permeability, formation pressure, and chemistry of formation waters) of the hydrostratigraphic units identified in this progress report will form the subject of the next research stage.

Regional groundwater quality study and monitoring network design in the Athabasca oil sands: Phase 1

Authors
Year of Publication: 2010

Abstract:
This report was intended to characterize regional groundwater resources, assess the vulnerability of regional aquifers and recommend locations of monitoring wells for a regional groundwater monitoring network.

Regional habitat evaluation and mapping for key wildlife species in the Athabasca oil sands region

Authors
Year of Publication: 2003

Abstract:
The intent of this project was to provide a regional habitat classification and mapping for key wildlife species in the Athabasca oil sands region. This work was continued under contracts 2002-0005 and 2003-0018.

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

Authors Bennett, K. E.
Year of Publication: 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.

Regional Municipality of Wood Buffalo recreational demand assessment

Authors
Year of Publication: 2003

Abstract:
This report addresses the following tasks: 1) Summarizing current recreational usage rates for various types of activities; 2) Predicting future recreational demands based on projected population increases; 3) Analyzing the number of people engaging in the activity and the projected future number of people likely to engage in these activities under various population size scenarios; 4) Analyzing, where data is available, the current amount of recreational resources available and the projected future demand for recreational resources based on the projected population increase.

Regional water quality of the AOSERP study area. Volume II: Discussion of 1976 and 1977 data

Authors Seidner, R. T.
Year of Publication: 1980

Abstract:
A regular program of water quality sampling has been instituted throughout the region of current oil sands development in northeastern Alberta. The goals of this program were to provide a base of background information on an extensive number of water quality parameters to enable the employment of predictive techniques and at the same time to obtain an understanding of natural water quality loadings and processes. The data collected has been stored under NAQUADAT codes at Alberta Environment, Water Quality Control Branch.

Regional-scale subsurface hydrogeology in northeast Alberta

Year of Publication: 1993

Abstract:
The hydrogeological regime of formation waters in the Phanerozoic sedimentary succession was determined for a region defined as Tp 70-103 W4 Mer (55-58 degrees;N latitude and 110-114 degrees;W longitude) in northeast Alberta, covering most of the Athabasca Oil Sand Deposit. The study was based on information from 12,479 wells, 3187 analyses of formation water, 2531 drillstem tests and 452,030 core analyses. Data management and processing were carried out using the INGRES Data Base Management System and specially designed software developed at the Alberta Geological Survey. The regional geology was synthesized in terms of definable stratigraphic successions, and 26 individual units were characterized by structure top and isopach maps. The hydrostratigraphy was developed through several iterations starting from the stratigraphy and lithology of the strata. Complex groups of aquifers and/or aquitards exhibiting generally common overall characteristics were grouped into hydrostratigraphic systems. Thirteen hydrostratigraphic units were identified in the Phanerozoic succession. The hydrogeological regime in aquifers was described using isopach, salinity distributions and freshwater hydraulic-head distributions. Cross-formational flow was evaluated using plots of pressure variation with depth in selected wells. Because the study area is situated at the feather edge of the Alberta Basin, topography and physiographic features exert a strong influence on the flow regime within most aquifers. In the most general sense, fluid flow is to the northeast toward the edge of the basin. Areas of high topography, such as the Birch and Pelican mountains, act as local recharge areas, introducing fresh meteoric water to aquifers unprotected by significant confining strata. The valleys of the Athabasca River system represent discharge areas for aquifers at outcrop or subcropping near them. The salinity of formation waters generally increases with depth. This is the result of a combination of factors like temperature, hence solubility increase with depth, dissolution of deep Devonian evaporitic beds, and dilution near the surface by meteoric water introduced by local flow systems. In terms of flow regime and overall characteristics, the hydrostratigraphic units can be grouped into pre-Prairie Formation aquifers, Beaverhill Lake-Cooking Lake aquifer system, Grosmont-to-Wabamun aquifers, and Cretaceous aquifers. The aquifers below the Prairie evaporite exhibit regional flow-regime characteristics. Overall high formation water salinity is associated with the proximity of Elk Point Group evaporites. The Beaverhill Lake-Cooking Lake aquifer system has hydrogeological characteristics consistent with an intermediate-to-local flow regime. Within subcrop and outcrop areas, local physiographic influences are superimposed over a regional northeastward flow trend. The Grosmont aquifer and Winterburn-Wabamun aquifer system may act locally as a 'drain' for aquifers in hydraulic continuity above and below. The flow of formation waters is generally to the northwest, towards discharge at outcrop along the Peace River. The Cretaceous aquifers are characterized by low salinity and local flow regime.The synthesis of this vast amount of information on the hydrogeological regime of formation waters in northeast Alberta was carried out under a jointly funded research project by the Alberta Research Council and Environment Canada.

Regulatory enhancement project : Technical report

Authors
Year of Publication: 2010

Abstract:
This Technical Report has been prepared as part of the Regulatory Enhancement Project (REP). The objective of the REP was to examine ways of ensuring Alberta‟s regulatory system for upstream oil and gas is modern, efficient, performance-based and competitive, while maintaining Alberta‟s strong commitment to environmental management, public safety and responsible resource development in the public interest.

Regulatory history of Alberta's industrial land conservation and reclamation program

Year of Publication: 2011

Abstract:
Alberta first legislated the requirement to reclaim land disturbed by industrial activities in 1963 with the enactment of the Surface Reclamation Act. In 1973 the Land Surface Conservation and Reclamation Act introduced the concept of conservation and added new regulated industries and an approvals process. In 1993 the Environmental Protection and Enhancement Act linked reclamation and remediation in a single Act. Alberta's industrial land conservation and reclamation program developed over 48 yr from an initial focus on surface debris removal and safety to increasing emphasis on returning ecological function and minimizing cumulative effects. The program has been influenced by various factors, includingregulatory policies and objectives, education and expectations of stakeholders and the public, educational background and expertise of regulators, advances in science, technology and industry practices, type and scale of land disturbances, intended post-reclamation land use, and working with partners. Vigorous discussion and debates on productivity vs. capability, reclamation vs. restoration, reclamation vs. remediation, conservation vs. reclamation, land vs. water and scientific possibilities vs. practical realities have shaped the program's direction. This review will provide insights for other jurisdictions dealing with the need to balance industrial development and environmental protection in the face of growing public awareness and scrutiny.

Regulatory requirements for nutrient effluent discharges

Authors
Year of Publication: 1994

Abstract:
This review includes both the instream water quality objectives for the nutrients, nitrogen and phosphorus, and the limits for phosphorus and nitrogen (as a nutrient) specified in effluent permits and regulations. The review concentrates on the Peace, Athabasca and Slave Rivers, but the scope also includes Alberta, Canada, and other jurisdictions. Regulatory information pertaining to pulp and paper mill effluents is emphasized.

Reindeer lichen transplant feasibility for reclamation of lichen ecosites on Alberta's Athabasca oil sand mines

Authors Duncan, S.
Year of Publication: 2011

Abstract:
This project is a pilot study to assess the viability of transplantation as a technique to establish reindeer lichens on reclaimed areas of oil sands surface mines in the Athabasca region of Alberta. There were two components to this study: a) a lichen transplant trial, where I investigated which commonly available substrates found in reclaimed forest sites would promote the best lichen fragment survival and vigour for a lichen ‘seeding’ program; and b) a diversity assessment of the reclaimed site to compare the existing cryptogam community with the expected community for the target ecosite based on published descriptions from the surrounding native forests and documented chronosequences for terrestrial lichen communities. In July 2009, Cladonia mitis was transplanted into 54 plots on three sites that were planted with jack pine or spruce 12 or 24 years ago, respectively, on the Suncor Millenium/Steepbank Mine (Suncor Mine) This trial was designed to investigate possible short-term indicators of successful lichen establishment and the effect of substrate (moss, litter, or soil) on the establishment of transplanted lichen thallus fragments. The indicators of lichen establishment evaluated were vigour, movement from plots, photographic areal cover, and microscopic growth (hyphal growth, annual growth and lateral branching). After two growing seasons, the effect of substrate on lichen transplant survival varied by site; there was no significant difference in lichen fragment retention in plots by substrate on the 24-year old sites, but median fragment retention was significantly higher on moss and litter substrates than soil on the 12-year old site. There was also no significant difference in fragment vigour between substrates on each site, except on the south-facing 24-year-old forest site where average vigour was significantly higher on moss plots than on soil plots. Photographic areal measurement is not recommended as a short-term lichen establishment monitoring tool for transplanted fragments based on the difficulties encountered using the method for this trial. Forty-one percent of the fragments collected for microscopic assessment after the first growing season had grown hyphae, 23 percent of the fragments collected during September 2009 and September 2010 had formed apothecia, and 31 percent of the fragments collected in September 2010 had grown lateral branches. The results of the biodiversity assessment were compared with the successional communities previously described for spruce- and pine-lichen boreal forests. There were no lichens found on the 12-year-old site, though the cup lichens were common to abundant on the 24-year-old sites, which is consistent with the cryptogammic community expected for a regenerating natural site of that age. Cladonia mitis was also present but rare to uncommon on the 24-year-old site, while Cladonia stellaris, Cladonia rangiferina and Cladonia stygia that, together with C. mitis, are indicative of the al and c1 ecosites of the Central Mixedwood Boreal forest, were not present.

Reinstatement of biological activity in severely disturbed soils: Effects of mining on the microbiology of three minespoils and the microbial development in the minespoils after amendation and planting

Year of Publication: 1984

Abstract:
The project sought to determine the immediate effects of coal and bitumen mining on a variety of soil microbiological factors; andto provide detailed information on the rates of redevelopment ofbiological activity when various organic and inorganic amendmentsare applied singly to vaious minespoils and subsequently plantedwith different herbaceous and woody plant species.

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