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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.

Soil microbial communities in early ecosystems

Authors Hahn, A. S.
Year of Publication: 2012

Abstract:
Microbial communities are responsible for biogeochemical processes in soils such as nutrient cycling and organic matter formation, which are essential to the establishment of vegetation and ecosystem sustainability. Phospholipid fatty acid analysis, microbial respiration and enzymatic activities were used to assess the development of soil microbial communities in two early ecosystems: along a 99 year glacial chronosequence, and in reconstructed soils in the Canadian boreal forest following open-pit mining. In the glacial environment, microbial biomass, respiration and enzymatic activity increased along the chronosequence and became more similar to the reference stand as vegetation developed. Further, in mid-successional stage soils, microbial biomass in plant rhizospheres was double that measured in bulk soil. In the reconstructed soils the use of organic amendments originating from the target ecosystem placed both the vegetation and soil microbial community on a faster trajectory towards ecosystem recovery than did the use of alternative amendments.

Soil moisture regime and salinity on a tailings sand storage facility

Year of Publication: 2003

Abstract:
The Southwest Sand Storage Facility (SWSS) is a 25 km2 tailings sand facility in Alberta's Athabasca oil sands. Revegetation of this structure has been delayed due to concerns of waterlogging and increasing salinity. This study involved monitoring soil moisture and chemistry on one section of the SWSS to examine the variability in soil moisture (spatial, temporal) and the degree of salinization in the topsoil. The root zone is not currently threatened by saturation or salinity/sodicity. Dry areas were more prominent than wet areas on site. The soil profile, topsoil directly over tailings sand, contains a textural discontinuity that acts as somewhat of a barrier to water flow. This caused moisture above the interface to gradually increase and moisture in the tailings sand to stay consistently low over time. Salinity coincided with soil moisture on site, with greater moisture and salinity at depth in the tailings sand.

Soil nitrogen indicators for land reclamation policy development for forest ecosystems

Authors Chang, S. X., Yan E., & Hu Y.
Year of Publication: 2011

Abstract:
The lack of understanding of possible relationships between soil nitrogen (N) availability indices and forest productivity in the oil sands region of Alberta may adversely affect reclamation practices and the development of reclamation policy for the region. This project was designed to investigate the foregoing relationships on natural, undisturbed stands and to recommend the best soil N availability indicators to use to evaluate soil N for achieving the maximum site productivity and for long-term monitoring of soil and vegetation performance in the region. Soil N availability indices evaluated in this project included several common field-based methods (available mineral N concentrations, in-situ N mineralization rates, potential N availability measured using the plant root simulator (PRS) probes) and laboratory-based measurements (extractable N, aerobic and anaerobic N mineralization rates). We attempted to correlate the above soil N availability indices with several forest productivity indices of three of the most common native tree species in this region. The measured forest productivity characteristics include foliar size of trees, annual tree growth ring width, and aboveground net primary productivity (ANPP). The results of our research showed that most N availability indices were correlated with productivity measurements in jack pine (Pinus banksiana) stands, while few N availability indices were correlated with productivity indices in trembling aspen (Populus tremuloides) and white spruce (Picea glauca) stands. Based on those results, we conclude that jack pine forest productivity is most likely limited by N availability and thus there are tight relationships between many soil N availability indices and forest productivity; while for aspen and white spruce stands, factors controlling forest productivity may be more complex (such as co-limitation of water availability) and thus there are poor N availability-productivity relationships. We recommend that for jack pine stands, laboratory based aerobic and anaerobic mineralization rates are the most cost effective methods for measuring N availability while for aspen and white spruce stands the in-situ N mineralization rate is likely the most appropriate method to determine soil N availability, as that index gave the best relationship with stand productivity. While this study helps to determine which method of measuring nitrogen availability is most appropriate for potential input to the land capability classification system (LCCS) for soil nutrient regime assessment, further research is need to evaluate the relationship between N availability indices and LCCS classes or reclamation performance, as the current project was conducted in natural forests and extrapolating into reclamation areas will be difficult without calibration between natural and reclamation sites; the natural sites in this study were used as an analog for future developed forest stands in the reclaimed area in the oil sands region.

Soil physical properties in reclamation

Year of Publication: 1991

Abstract:
To provide coordinated direction for reclamation research in Alberta, the need to review the current understanding and the role of soil physical properties in soil disturbance related activities was identified. Surface coal mining, pipeline and wellhead construction, oil sands extraction, timber harvesting, and agricultural production activities alter the landscape to some degree and their cumulative effect has changed, and will continue to change, the soil resources of the province of Alberta. The nature and severity of these alterations are dependent upon inherent soil properties as affected by disturbance type and the success of reclamation and management practices. Doll (1987) believed, \"the goal of reclamation should be the establishment of a permanently stable landscape, aesthetically and environmentally compatible with the surrounding undisturbed land\". Restoration of the productivity of reconstructed soil is a complicated problem. Nielsen et al. (1983) stated \"In the past, management has been judged on annual measurements of crop productivity, and not on measurements taken below the soil surface that could be used to signal the long term consequences of management of present-day soil and water resources\". The emphasis on chemical fertility has often resulted in neglect of soil physical properties that combine with chemical properties for optimum, sustainable, soil productivity. However, it is often soil physical properties that present the main limitations to reclamation of disturbed lands (Albrecht and Thompson 1982; King and Evans 1989; McSweeney and Jansen 1984). The over-emphasis on chemical fertility is attributable, to some extent, to the lack of reliable, quantitative descriptions of soil physical properties in the field. While studying soil physical properties in the laboratory using soil cores and repacked samples has yielded much information on core and repacked samples, there are limited guarantees that such information can be applied to the landscape (White 1988). In spite of soil physical properties being recognized as one of the critical productivity limiting factors in reclamation, soil chemical properties are still often used as the only criteria of reclamation success because of difficulties in characterizing soil physical properties (Omodt et al. 1975). Often soil scientists, reclamation specialists, and agrologists concerned with management of disturbed lands are forced to seek answers to their questions regarding soil physical properties in a style once described by Oscar Wilde as \"Chaos, illumined by flashes of lightning\". Measurement of soil physical properties in the field is difficult; subject to spatial and temporal variability, time and length scales, and nonsteady, multidimensional velocity fields in a three phase system. Every soil physical property and process is also modified by weather phenomena (rainfall, frost, solar radiation, and drought), erosion, and human manipulation (management). Often the inability to characterize spatial variability prevents researchers from accurately matching soil use requirements to soil characteristics and, therefore, from predicting soil performance and behaviour. Soil physical properties and processes are closely interconnected, further complicating their measurement. It is also easy to understand why field measurement of soil physical properties has been described as a \"challenge that few have ever accepted\" (Nielsen and Biggar 1967). While that challenge is still evident in the measurement of many soil physical properties, the current challenge is related to selection of those soil physical property measurements that will best answer our questions, and the measurement techniques that will best provide that information. We must simplify a complex system by concentrating on the factors which appear to have the greatest and most direct bearing upon the problem at hand. In the view of White (1988) \"What properties we need to know and how we measure them are related directly to the questions we are attempting to answer\". Through a Soil Physical Properties Workshop held in November 1990 for people in Alberta working with soil physical properties, and an extensive literature review, the authors have attempted to identify what questions have been answered, what questions remain unanswered, and what soil physical properties and measurement techniques are best suited to meeting information needs within Alberta. The objective of this review is not to provide a methodology manual or theoretical treatise on soil physics, but rather to assess the various properties and composite parameters and processes in a manner that hopefully will clarify, not confound. The report contains a brief overview of field related measurement methodology and spatial and temporal variability for each soil physical property, followed by a review of soil physical property interrelationships, the effects of development management activities on these properties, and the prevention/amelioration/remediation/acceptance strategies employed in dealing with changes in the physical property. Recommendations for future research follow a summary of physical properties most affected by reclamation activities and differences by disturbance type.

Soil physics

Authors Maclean, A. H.
Year of Publication: 1976

Citation:

Soil quality criteria relative to disturbance and reclamation

Authors
Year of Publication: 1987

Abstract:
Land disturbances due to resource extraction and transport are intended to be only temporary disruptions to the normal use of land for food and fiber production or for recreation. Although no two sites are identical, many disturbances cause similar types of problems and concerns but in varying degrees of intensity. Assurance such disturbances are temporary is possible only if information concerning the site is well documented and an appropriate reclamation program planned prior to disturbance. Evaluation of the nature of materials at hand prior to disturbance and subsequent to reclamation, however, requires criteria by which to assess the quality of those materials. To this end a Soil Quality Criteria Subcommittee of the Alberta Soils Advisory Committee was formed in 1978 with the terms of reference being to develop criteria relative to: 1. soil mapping and sampling for baseline and post disturbance activity; 2. overburden sampling; 3. analytical requirements; 4. physical, chemical, and biological criteria for evaluating the suitability of soil materials for revegetation; and 5. utilization of soil as a medium for waste disposal including materials such as sewage sludge, animal wastes, and fly ash. The following responsibilities became part of the purview of the subcommittee: 1. preparation of a glossary of soil terms and a bibliography relevant to the above subject matter; 2. delineation of the province into broad ecological zones so relevant guidelines 3. development of recommendations for future action and research. A report was prepared, reviewed by the Alberta Soils Advisory Committee, and published in 1981 under the title "Proposed Soil Quality Criteria in Relation to Disturbance and Reclamation". During the intervening four years, it has received considerable attention and many constructive suggestions for revision. Where new information, or more complete interpretations of earlier data have been available, revisions have been made. The report that follows deals with the first four terms of reference, and has benefited from consultation with many Soil Scientists, Pedologists, and others involved in reclamation. The subcommittee did not address the term of reference dealing with soil quality for waste utilization, as provincial guidelines governing wastewater and sludge application to soil presently exist. The subcommittee is aware that a number of government agencies are involved in regulating the selection and operation of landfill sites and other waste disposal emplacements.

Soil reclamation amendments affect long term growth of jack pine following oil sands mining

Year of Publication: 2013

Abstract:
A retrospective study of reclamation soil properties and associated tree growth was conducted on a former tailings pond site containing a 21-year old jack pine stand. The purpose of the study was to explore possible causes of observed variations in mean tree heights in various portions of the stand. An expected link to total depth of the fine textured glaciolacustrine reclamation capping material was not found. Instead, a strong relationship was found between tree height and organic matter (OM) content (by % dry weight), where OM is in the form of predominantly mesic peat mixed with the capping material at the time of placement. Possible OM-related causes of the height growth effect could include (a) contributions to water holding capacity of the soil and (b) contributions to soil nutrition. Contributions to water holding capacity could not be evaluated in this study, but the lack of correlations to total capping depth suggests that moisture may be of lesser importance as a growth limiting factor on this site. Nitrogen supply was identified as the most likely nutritional deficiency. For current soil OM content, substantial increases in tree heights were measured with OM increases to approximately 8 %, followed by marginal increases in tree height with OM greater than 8 %. This study offers a relatively inexpensive methodology through which oil sands operators can test for similar relationships over a broad range of site and stand conditions, and evaluate the benefits of varying their allocation of OM resources to achieve optimum tree growth benefits at the landscape scale.

Soil reconstruction design for the reclamation of oil sands tailings

Authors
Year of Publication: 1983

Abstract:
This report contains the result of a study jointly financed by Alberta Environment, Petro Canada, Suncor Inc., Alsands Project Group, Syncrude Canada Ltd. and the Oil Sands Environmental Study Group. The objective of the study was the definition of physical and chemical soil properties required to support the forest ecosystems which are the targets of oil sands tailings reclamation research in the Athabasca region, Alberta. We wish to thank Dr. K.A. Armson of the Ontario Ministry of Natural Resources and Dr. T.M. Ballard, Faculty of Forestry, University of British Columbia for their review of the Manuscript and their valuable suggestions.

Soil research related to revegetation of the oil sands area: Sub-project VE 4

Authors Cook, F. D.
Year of Publication: 1977

Abstract:
3 reports available - Studies of physical properties of soils and mined materials in relation to reclamation - Studies of chemical properties of soils and methods of improving mined material for plant growth - Sulphur deposition and acidification of soils in the oil sands area

Soil resources of Syncrude Lease 22

Year of Publication: 1984

Abstract:
This inventory of the soils of Syncrude Lease 22 has been prepared as part of an environmental baseline data collection program conducted by Syncrude Canada Ltd. The soil inventory is presented in report and map form. Intensive sampling and mapping was conducted during the summer of 1984, which was supplemented by analysis of key soil properties in the laboratory. The following points summarize the distribution and characteristics of the soils on Lease 22: 1. Poorly drained mineral soils and peat wetlands constitute slightly more than half (54 percent) of the lease area. The poorly drained mineral soils occupy 25 percent of the soil landscape and Organic soils, which have greater than 40 cm of peat, occupy 29 percent. 2. Freely drained mineral soils make up only 37 percent of the lease surface. This land area includes well, moderately well, and imperfectly drained soils, developed on glaciolacustrine clays and glaciofluvial sands. 3. River banks, stream channels, and disturbed land constitute nine percent of the land surf ace. 4. The majority of the mineral soils are fine textured Luvisols and Gleysols. These clayey textured soils occur over approximately 35 percent of the lease. Sandy textured soils, including Brunisols and Gleysols, occupy approximately 10 percent of the lease. 5. The peat deposits are seldom thicker than 2 m and are more commonly less than 1 metre thick. Of the estimated total volume of 66 million cubic metres of peat on the lease, approximately 51 percent occurs as deposits within the thickness range of 150 to 250 cm. Approximately 32 percent occurs as deposits of 50 to 150 cm thick, and 17 percent is in the 15 to 50 cm range. 6. Permafrost occurs sporadically in peatlands, with its presence usually coinciding with mounded bog peat landforms. 7. The Soil Map, presented in two halves at 1:20,000 scale, identifies the soils by series name and map unit, which have been correlated with the Alberta Soil Names File and with the names established in the reconnaissance soil survey of the area. 8. Soil patterns in the area are generally quite simple, with large homogeneous soil units. The major criteria for differentiating soils are parent material and drainage conditions. Extrapolation of data within and between soil map units can be done with a fairly high degree of confidence due to this homogeneity.

Soil series information for reclamation planning in Alberta: Volume 1

Authors
Year of Publication: 1993

Abstract:
This RRTAC manual has been published to provide reclamation and conservation planners with information and guidelines to help understand and use soil inventory data. This manual does not replace the need for site-specific 'soil inventory information – it merely provides guidelines for interpreting the maps and reports. The information and interpretations are presented as typical examples - not as rules or regulations. The soil series included in this manual correspond to those in the Generation 2 Alberta Soil Names File (Alberta Soil Series Working Group 1992), which is part of the Alberta Soil Information System (Alta SIS). For access to any published Alberta Soil Survey information contact Publications, Alberta Research Council, Edmonton (Phone 450-5390). Part 1 of this manual is a background and explanatory section that describes the terminology used in soil surveys and presents the assumptions and conventions upon which the interpretations are based. Part 2 presents typical data and interpretations for each soil series in Alberta. The interpretations were made by applying the guidelines presented in Part 1, and checking the results against experience and established practice.

Soil survey of a portion of the Syncrude Lease 17 area Alberta

Authors Twardy, A. G.
Year of Publication: 1978

Abstract:
A soil survey of a portion of Syncrude No. 17 Lease Area, encompassing an area of about 93 square kilometres, was conducted during the period between June 20 and July 8, 1977. The soils were inspected and described at 413 sites and representative soils were sampled for physical and chemical laboratory analyses. The distribution of the soils is presented on the soils map at a scale of 1:24,000. Soils of the Luvisolic, Brunisolic, Gleysolic, Cryosolic and Organic Orders were recognized and characterized. Moderately well drained Orthic Gray Luvisols developed on fine to very fine textured glaciolacustrine materials predominate, occupying about 49 percent of the study area. Organic and Organic Cryosol soils occupy about 35 percent of the area. The depth of peat in the majority of these soils is less than 80 cm. Both bogs and fens were recognized. Bogs have the larger areal extent occupying about 26 percent of the study area. Permafrost was encountered in some of the deep bogs. No permafrost occurs in any of the fens or shallow bogs.

Soil water regimes of reclaimed upland slopes in the oil sands region of Alberta

Year of Publication: 2012

Abstract:
Large oil sands deposits in the Athabasca oil sands region of Alberta, Canada, are recovered through surface mining, creating a large-scale disturbance. Reclamation requires reconstruction of soil profiles to return the land to equivalent land capability and support the required end land use. Soil water regimes must be understood to allow for planting of appropriate vegetation species. This study quantified soil water regimes on reclaimed upland slopes of various reclamation prescriptions and determined whether soil water was affected by slope position. Slope position did not have a consistent effect on soil water. Spatial variability in soil characteristics and vegetation distribution likely had a greater influence on soil water than did slope position. The upper slope soil profiles had highly dynamic water regimes and a greater response to precipitation events than the lower soil profiles. Differences in water-holding capacity among sites were attributed to differences in clay, sand and organic matter content. Overwinter soil water recharge varied dramatically by site. Capillary barriers resulting from the textural discontinuities created by the reclamation prescriptions enhanced soil water retention within the profiles in at least two sites, and hence are desirable in reclamation scenarios, especially where reclamation material is coarse textured.

Soils inventory of the Alberta Oil Sands Environmental Research Program study area

Year of Publication: 1982

Abstract:
A soil survey of the Alberta Oil Sands Environmental Research Program (AOSERP) study area was initiated in 1976 as part of the program objective to establish a data base for the area. The purpose of this report and accompanying soil maps is to provide data on the kinds, characteristics, location, and areal distribution of soils in the AOSERP study area. The soil maps indicate types of soils and landforms within delineated areas. The mapping approach used is similar to the ecological method of classification in which land areas are mapped rapidly and at a small or reconnaissance scale by means of air photo interpretation and supporting field checks on 1:50,000 airphotos. Recurring patterns of soils, landforms, and vegetation were delineated. The information was transferred first to 1:50,000 preliminary maps and then to eight 1:126,720 maps which accompany this report. General characteristics of vegetation are provided in this report, but more detailed information must be derived from AOSERP vegetation maps. In addition to airphoto interpretation, the information on soil maps is based on about four field checks per township and on analyses of samples from 130 soil profiles. The predominant upland soils in the study area are Gray Luvisols, developed on loamy to clayey, morainal and glaciolacustrine deposits; and Dystric Brunisols, developed on sandy glaciofluvial and eolian materials. Gleysolic soils occupy a significant proportion of the landscape in many areas. Gleysols and Regosols occur on recently deposited fluvial materials, which occur in stream channel, fan and apron, and delta landforms. Solonetzic soils are associated with Luvisols on some of the clayey glaciolacustrine plains. Soils of low-lying, poorly drained areas are mainly Organic. These soils, formed in and fen peats, occupy a considerable portion of the area, and vary from less than 1 m to several metres in thickness. Soil formed in peat and which have permafrost layers in them, the Organic Cryosols, are extensive in the Birch Mountains Upland and occur sporadically elsewhere. Miscellaneous land types mapped include Rock, Rough Broken, and Disturbed lands. This report outlines methodology and systems of classification used in this soils inventory. This is followed by descriptions of ecological units and soils. The last part of the report outlines soil survey interpretations relating to forestry, agriculture, engineering, wildlife and recreational uses, and soil sensitivity to acidic deposition. Data for representative soil profiles are presented in RMD Report L-80, \"Soils Inventory of the Alberta Oil Sands Environmental Research Study Area: Appendix 9.4\".

Soils inventory of the Alberta Oil Sands Environmental Research Program study area: Appendix 9.4 to AOSERP report 122

Year of Publication: 1982

Abstract:
Soil morphology, site descriptions, and physical and chemical data for 130 soil profiles from the AOSERP study area are presented in this section. Except for some miscellaneous land units, each of the soil groups are represented by at least one profile description. For many of the soil groups, several profile descriptions are given. A list or index of the profiles described has not been provided, but a search for data about a specific soil group is facilitated by the alphabetical arrangement of soil groups. The soil descriptions consist of three parts - a general site description, the profile description, and analytical data for the profile.

Soils of permanent sample plots in the Athabasca oil sands area

Year of Publication: 1982

Abstract:
Soils of permanent sample plots were investigated to provide baseline data for research related to monitoring of terrestrial ecosystems. More specifically, the objective of this project was to provide information on the kinds, characteristics, and distribution of soils in 16 permanent sample plots, each of about 5 ha area, established during 1981. The background and general purpose of the project are outlined in the Terms of Reference appended to this report. General information about distribution and characteristics of soils in the oil sands area is provided in a report on the soils inventory of the Alberta Oil Sands Environmental Research Program study area (Turchenek and Lindsay 1982). Emphasis in 1981 was placed on selecting permanent sample plots with jack pine vegetation communities on Eluviated Dystric Brunisols. These soils are members of the Mildred and Heart soil groups which are described in the report of Turchenek and Lindsay (1982). Both of these soils groups are composed predominantly of Eluviated Dystric Brunisols. The Heart soils have developed in eolian sands while Mildred soils have formed in sandy glaciofluvial materials. Both soil groups are very sandy and usually contain less than 5% fine materials (clays and silt). The Mildred soils normally have a variable content of coarse fragments (larger than 2 mm) while Heart soils have no coarse materials. Two permanent sample plots were established in the Richardson Hills Upland. Soils in this area belong to the Firebag soil group; they have developed on sandy, gravelly and stony glaciofluvial ice-contact deposits, but are otherwise similar to the Mildred and Heart soil groups. In this project, samples for laboratory analysis were taken from one or two sites within each permanent sample plot. For additional data and for making comparisons, analytical data for Heart, Mildred, and Firebag soils can be found in Volume 2 of the report by Turchenek and Lindsay (1982). Other soil surveys conducted in the general area are those of Hardy Associates Ltd. (1980) for the Alsands lease, and Twardy (1978) for portions of the Syncrude lease. Information about general properties, moisture movement and retention, and nutrient cycling in soils near the AOSERP Mildred Lake research facility can be found in the report of McGill et al. (1980).

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