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Lakeland County AB
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Experimental and numerical investigation of the Fast-SAGD process


Author(s): Shin, H.

Year: 2006

Abstract:
The SAGD process has been tested in the field, and is now in a commercial stage in Western Canadian oil sands areas. The Fast-SAGD method can partly solve the drilling difficulty and reduce costs in a SAGD operation requiring paired parallel wells one above the other. This method also enhances the thermal efficiency in the reservoir. In this research, the reservoir parameters and operating conditions for the SAGD and Fast-SAGD processes are investigated by numerical simulation in the three Alberta oil sands areas. Scaled physical model experiments, which are operated by an automated process control system, are conducted under high temperature and high pressure conditions. The results of the study indicate that the shallow Athabasca-type reservoir, which is thick with high permeability (high k×h), is a good candidate for SAGD application, whereas Cold Lake- and Peace River-type reservoirs, which are thin with low permeability, are not as good candidates for conventional SAGD implementation. The simulation results indicate improved energy efficiency and productivity in most cases for the Fast-SAGD process; in those cases, the project economics were enhanced compared to the SAGD process. Both Cold Lake- and Peace River-type reservoirs are good candidates for a Fast-SAGD application rather than a conventional SAGD application. This new process demonstrates improved efficiency and lower costs for extracting heavy oil from these important reservoirs. A new economic indicator, called simple thermal efficiency parameter (STEP), was developed and validated to evaluate the performance of a SAGD project. STEP is based on cumulative steam-oil ratio (CSOR), calendar day oil rate (CDOR) and recovery factor (RF) for the time prior to the steam-oil ratio (SOR) attaining 4. STEP can be used as a financial metric quantitatively as well as qualitatively for this type of thermal project. An automated process control system was set-up and validated, and has the capability of controlling and handling steam injection processes like the steam-assisted gravity drainage process. The results of these preliminary experiments showed the overall cumulative oil production to be larger in the Fast-SAGD case, but end-point CSOR to be lower in the SAGD case. History matching results indicated that the steam quality was as low as 0.3 in the SAGD experiments, and even lower in the Fast-SAGD experiments after starting the CSS.

Citation:

Field evaluation of an erosion hazard assessment system in west central Alberta


Year: 1987

Abstract:
This thesis examines the environmental history of the industrial transformation on the large lakes of Northwest Canada, Winnipeg, Athabasca, Great Slave, and Great Bear between 1921 and 1960. Using corporate and personal records, government documents, published scientific reports and oral history collections, it reconstructs patterns of industrial activity, relationships between these activities and local ecosystems, and environmental consequences. Touching on the history of the north, ecological colonization, the politics of resource development, and relationships between Natives and Newcomers the argument builds on two main threads of historiography: the place of industrial humans in nature and the role of twentieth-century science in shaping engagements with the natural world. This study traces the development of mining, fishing, and transportation industries on the large lakes and their surrounding environment. This Subarctic development was a Canadian manifestation of international industrial transformations that sought increasingly remote resources for the production of goods destined to capitalist markets. I examined this transformation by asking what happens to nature (organisms, including humans, in relationship with their environment) as a result of twentieth-century industrialization (high-energy fuels, especially fossil fuels, and mechanical technologies applied to production)? I argue that industrialization remained embedded in and dependent upon local ecosystems. Mining, elsewhere seen to exemplify the destructive and inorganic character of industry, integrated its operations with the physical world, extended habitable environments underground, and modelled its work on natural and human metabolism. Where ties to the physical world weakened in this period, it was as a direct result of the commodification of natural resources and how these were processed into goods for distant markets. Scientists played a major role in guiding industrial mining and fishing operations, with provincial and federal governments granting scientists authority to ensure fisheries conservation. The industrial transformation in this period carries the imprint of how these scientists imagined the natural world and the unintended consequences to lake ecosystems of these models.

Genetic population structure of walleye populations in the Athabasca River basin


Author(s): Burke, L.

Year: 2008

Abstract:
This report provides a summary of a field program undertaken to study the population genetic structure of walleye. Samples were collected from Lake Athabasca, a site north of Fort McMurray, McLeod River, Lesser Slave Lake, Calling Lake, and Fawcett Lake.

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


Author(s): Murray, W. A.

Year: 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.

Ground penetrating data radar (GPR): A new geophysical methodology used to investigate the internal structure of sedimentary deposits (field experiments on lacustrine deltas)


Author(s): Jol, H. M.

Year: 1993

Abstract:
Although in its infancy, ground penetrating radar (GPR) is rapidly emerging as a geophysical technology with many possible applications. To assess whether GPR could become a useful tool to investigate internal sedimentary structures, GPR field experiments were conducted on several modern, Holocene and Pleistocene lacustrine deltas to better understand the internal stratigraphy. A pulseEKKO$\sp{\rm TM}$ IV radar system was used with 25, 50, 100 and 200 MHz frequency antennae and 400 and 1000 V transmitter power levels. For most surveys one metre steps (station spacing) were used to provide detailed horizontal resolution of the sedimentologic structures. The profiles were processed and plotted (wiggle trace format) using pulseEKKO$\sp{\rm TM}$ IV software. Depth of reflections was determined from using the common midpoint (CMP) method. Experiments with different antennae frequencies and transmitter powers showed significant variations in vertical resolution, depth of penetration and continuity of reflections. Radar stratigraphic (facies) analysis of GPR profiles, evolved as a secondary development in this dissertation, provided identification of three deltaic types: (1) fan-foreset, (2) wave, and (3) braid. These deltaic types are in general agreement with existing concepts. Fan-foreset deltas are dominated by steeply dipping (25$\sp\circ$) reflections, sandwiched by surface and basal radar facies which have slightly inclined or horizontal reflections. Wave deltas have low-angle inclined reflections capped by discontinuous, wavy reflections. Braid deltas have distinct, continuous and semi-continuous, wavy reflections, often overlying a basal, horizontally continuous reflection, below which an abrupt signal loss occurs. As well, two post depositional features found in deltaic environments were investigated: (1) a potential failure plane and (2) a peatland. The insights gained from the radar stratigraphic analysis of deltaic environments may be extended to the interpretation of seismic records and ancient deltaic systems. More importantly, this information will provide a better understanding of the internal structure which will aid earth scientists in the interpretation of deltaic sequences from drill cores. GPR was found to be most effective (resolution and depth of penetration) in dry and/or wet (freshwater), quartzose-rich, clean (no clay) sand and gravel deposits. The technique does not work well in sediments with silt, clay, caliche (CaCO$\sb3$, calcrete), or saline ground water which attenuate the electromagnetic signal.

Hydrogeologic characterization of a newly constructed saline-sodic clay overburden hill


Author(s): Chapman, D. E.

Year: 2008

Abstract:
Syncrude Canada Ltd (Syncrude) Mildred Lake operation is the largest producer of crude oil from oil sands mining in Canada. A saline-sodic clay-shale overburden known as the Clearwater Formation (Kc) must be removed in order to access the oil-bearing McMurray Formation (Km). The potential concerns associated with the reclamation of overburden structures include shale weathering and salt release and migration, resulting in salinization of groundwater, surface water, and reclamation soil covers. South Bison Hill (SBH) is one example of a Kc overburden structure located at the Syncrude Mildred Lake Operation. The general objective of this study is to develop a preliminary conceptual/interpretative model of the hydrogeology of the newly reclaimed SBH at the Syncrude mine site. A number of tasks were undertaken to meet this general objective. The first, and most important aspect of this study was to develop a geological model of SBH including pile geometry and depositional history of the hill. Secondly, to gain an understanding of the field conditions, a program was carried out over 2002 and 2003 to obtain pile physical characteristics. The geological model revealed that there are four main geological sections of SBH of different materials using different construction methods. The field data were used to verify the geological model, which illustrated the differences in hydraulic conductivities and geochemical signatures between the different sections. All information was used to develop a simple steady-state numerical seepage model of SBH to be used as a tool to investigate the response of the water levels of SBH to variations in the model parameters. The model illustrated that groundwater flow is largely controlled by a more permeable section on the south side of SBH and an unstructured Kc fill at the base of the pile. A sensitivity analysis was conducted on the model changing the flux into the pile, the permeability of the materials, and most importantly the head value of the tailings facility located on the north side both showing to be influential on the elevation of the water table through SBH.

Interim report of soil research related to revegetation of the oil sands area


Year: 1980

Abstract:
Monitoring was continued at instrumented sites which were selected in spring 1976, at Mildred Lake, Supertest Hill, the GCOS dike, and near Richardson Tower. Because of budget limitations, sites at Richardson were only monitored occasionally. However, information was obtained at a number of temporary 'outlying sites', which showed that conditions at the instrumented sites are fairly representative of those under similar vegetation in the surrounding area. Special emphasis in 1977, was placed on obtaining detailed information on moisture tensions using thermocouple psychrometers, and in acquiring accurate information on changes in moisture distribution during spring thaw. Growth of grasses and legumes in tailings sand, and the effect of adding materials such as peat and glacial till to tailings sand, were studied using lysimeters both indoors and in the field, and by establishing small plots, all of which were instrumented for gathering of physical and chemical information. Aspects of nutrient cycling such as nutrient inputs and outputs at forest sites, nitrogen mineralization and immobilization, retention of nitrogen by soil mixes, and decomposition of plant materials, were investigated with 15N and 14C. Laboratory studies were carried out on nitrogen and carbon cycling in tailings sand and two overburden materials. Much interpretation of information gathered over the year is still to be done and will be included in the next report.

Isotope tracing of water yield and chemical loadings in the Alberta oil sands region for evaluating acid sensitivity to acid deposition


Year: 2009

Abstract:
A field-based study was carried out by researchers and students from the Geography Department, University of Victoria to improve upon existing knowledge of water cycling, biogeochemical processes and acid sensitivity of lakes in complex, ungauged areas of the Boreal Forest in the Oil Sands region NE Alberta. Sponsored by the Cumulative Environmental Management Association and the Natural Sciences and Engineering Research Council of Canada, the research involved detailed studies at two lake/watershed sites near Fort McMurray (NE07 and SM08) during 2005 to 2009, supported by regional water surveys of 48 additional lakes/watersheds monitored during 2000-2009 as part of the Regional Aquatics Monitoring Program. The research program utilized an array of physical, geochemical, and isotopic techniques aimed at providing information required to assess present and future trends in critical acid loadings to aquatic ecosystems in areas broadly affected by NOxSOx emissions from the bitumen refining operations. Overall the study has confirmed that site-specific estimates of water yield (a.k.a. runoff) are necessary when applying critical loads models to lakes in the region. This study has also tested and identified a number of practical local- and regional-scale approaches for characterization of water yield to lakes, critical loads of acidity, and for determining relative importance of various pathways of water flow to lakes. These are important variables required to predict acidification using dynamic models such as the Model for Acidification of Groundwater In Catchments (MAGIC). Together with wetland classification mapping by CEMA collaborators, this study also has provided a broader understanding of hydrologic organization of watersheds in wetland-dominated areas, and has uncovered the existence of a systematic relationship between land cover types, permafrost distribution, and water yield to lakes. These findings contribute to a sharper focus on potential impacts of acid deposition from oil sands operations and establish and test new tools for site-specific, regional-scale critical loads assessment in complex wetland-dominated terrain.

Labour Force Estimates by Industry and by Occupation (2 and 3 Digits) for Selected Alberta Economic Regions (Annual Average) (1987 - 2011)


Year: 2015

Abstract:
(StatCan Product) Customization details:  This information product has been customized to present information on labour force estimates by industry and by occupation (2 and 3 digits) for Alberta’s Economic Regions (excluding Edmonton and Calgary) from 1987 to 2011 (annual averages).  The LFS characteristics presented are:  - Labour Force     - Employment  The Economic Regions presented are:  - Lethbridge – Medicine Hat - Camrose – Drumheller - Banff- Jasper – Rocky Mountain House - Red Deer - Athabasca – Grande Prairie – Peace River - Wood Buffalo – Cold Lake   Labour Force Survey  The Canadian Labour Force Survey was developed following the Second World War to satisfy a need for reliable and timely data on the labour market. Information was urgently required on the massive labour market changes involved in the transition from a war to a peace-time economy. The main objective of the LFS is to divide the working-age population into three mutually exclusive classifications - employed, unemployed, and not in the labour force - and to provide descriptive and explanatory data on each of these.  Target population  The LFS covers the civilian, non-institutionalized population 15 years of age and over. It is conducted nationwide, in both the provinces and the territories. Excluded from the survey's coverage are: persons living on reserves and other Aboriginal settlements in the provinces; full-time members of the Canadian Armed Forces and the institutionalized population. These groups together represent an exclusion of less than 2% of the Canadian population aged 15 and over. National Labour Force Survey estimates are derived using the results of the LFS in the provinces. Territorial LFS results are not included in the national estimates, but are published separately.  Instrument design  The current LFS questionnaire was introduced in 1997. At that time, significant changes were made to the questionnaire in order to address existing data gaps, improve data quality and make more use of the power of Computer Assisted Interviewing (CAI). The changes incorporated included the addition of many new questions. For example, questions were added to collect information about wage rates, union status, job permanency and workplace size for the main job of currently employed employees. Other additions included new questions to collect information about hirings and separations, and expanded response category lists that split existing codes into more detailed categories.  Sampling  This is a sample survey with a cross-sectional design.  Data sources  Responding to this survey is mandatory. Data are collected directly from survey respondents. Data collection for the LFS is carried out each month during the week following the LFS reference week. The reference week is normally the week containing the 15th day of the month. LFS interviews are conducted by telephone by interviewers working out of a regional office CATI (Computer Assisted Telephone Interviews) site or by personal visit from a field interviewer. Since 2004, dwellings new to the sample in urban areas are contacted by telephone if the telephone number is available from administrative files, otherwise the dwelling is contacted by a field interviewer. The interviewer first obtains socio-demographic information for each household member and then obtains labour force information for all members aged 15 and over who are not members of the regular armed forces. The majority of subsequent interviews are conducted by telephone. In subsequent monthly interviews the interviewer confirms the socio-demographic information collected in the first month and collects the labour force information for the current month. Persons aged 70 and over are not asked the labour force questions in subsequent interviews, but rather their labour force information is carried over from their first interview. In each dwelling, information about all household members is usually obtained from one knowledgeable household member. Such 'proxy' reporting, which accounts for approximately 65% of the information collected, is used to avoid the high cost and extended time requirements that would be involved in repeat visits or calls necessary to obtain information directly from each respondent.  Error detection  The LFS CAI questionnaire incorporates many features that serve to maximize the quality of the data collected. There are many edits built into the CAI questionnaire to compare the entered data against unusual values, as well as to check for logical inconsistencies. Whenever an edit fails, the interviewer is prompted to correct the information (with the help of the respondent when necessary). For most edit failures the interviewer has the ability to override the edit failure if they cannot resolve the apparent discrepancy. As well, for most questions the interviewer has the ability to enter a response of Don't Know or Refused if the respondent does not answer the question. Once the data is received back at head office an extensive series of processing steps is undertaken to thoroughly verify each record received. This includes the coding of industry and occupation information and the review of interviewer entered notes. The editing and imputation phases of processing involve the identification of logically inconsistent or missing information items, and the correction of such conditions. Since the true value of each entry on the questionnaire is not known, the identification of errors can be done only through recognition of obvious inconsistencies (for example, a 15 year-old respondent who is recorded as having last worked in 1940).  Estimation  The final step in the processing of LFS data is the assignment of a weight to each individual record. This process involves several steps. Each record has an initial weight that corresponds to the inverse of the probability of selection. Adjustments are made to this weight to account for non-response that cannot be handled through imputation. In the final weighting step all of the record weights are adjusted so that the aggregate totals will match with independently derived population estimates for various age-sex groups by province and major sub-provincial areas. One feature of the LFS weighting process is that all individuals within a dwelling are assigned the same weight. In January 2000, the LFS introduced a new estimation method called Regression Composite Estimation. This new method was used to re-base all historical LFS data. It is described in the research paper ""Improvements to the Labour Force Survey (LFS)"", Catalogue no. 71F0031X. Additional improvements are introduced over time; they are described in different issues of the same publication.  Data accuracy  Since the LFS is a sample survey, all LFS estimates are subject to both sampling error and non-sampling errors. Non-sampling errors can arise at any stage of the collection and processing of the survey data. These include coverage errors, non-response errors, response errors, interviewer errors, coding errors and other types of processing errors. Non-response to the LFS tends to average about 10% of eligible households. Interviews are instructed to make all reasonable attempts to obtain LFS interviews with members of eligible households. Each month, after all attempts to obtain interviews have been made, a small number of non-responding households remain. For households non-responding to the LFS, a weight adjustment is applied to account for non-responding households. Sampling errors associated with survey estimates are measured using coefficients of variation for LFS estimates as a function of the size of the estimate and the geographic area.

Labour Force Estimates by Industry and by Occupation (2 and 3 digits) for Selected Alberta Economic Regions (Annual Average) (2000-2013)


Year: 2015

Abstract:
(StatCan Product) Customization details:  This information product has been customized to present information on labour force estimates by industry and by occupation (2 and 3 digits) for Alberta’s Economic Regions (excluding Edmonton and Calgary) from 2000 to 2013 using annual averages.  The LFS characteristics presented are:  - Labour Force     - Employment  The economic regions presented are:  - Lethbridge – Medicine Hat - Camrose – Drumheller - Banff- Jasper – Rocky Mountain House - Red Deer - Athabasca – Grande Prairie – Peace River - Wood Buffalo – Cold Lake   For more information about the occupations and industries presented, contact OSI.Support@gov.ab.ca  Labour Force Survey  The Canadian Labour Force Survey was developed following the Second World War to satisfy a need for reliable and timely data on the labour market. Information was urgently required on the massive labour market changes involved in the transition from a war to a peace-time economy. The main objective of the LFS is to divide the working-age population into three mutually exclusive classifications - employed, unemployed, and not in the labour force - and to provide descriptive and explanatory data on each of these.  Target population  The LFS covers the civilian, non-institutionalized population 15 years of age and over. It is conducted nationwide, in both the provinces and the territories. Excluded from the survey's coverage are: persons living on reserves and other Aboriginal settlements in the provinces; full-time members of the Canadian Armed Forces and the institutionalized population. These groups together represent an exclusion of less than 2% of the Canadian population aged 15 and over. National Labour Force Survey estimates are derived using the results of the LFS in the provinces. Territorial LFS results are not included in the national estimates, but are published separately.  Documentation – Labour Force Survey  Instrument design  The current LFS questionnaire was introduced in 1997. At that time, significant changes were made to the questionnaire in order to address existing data gaps, improve data quality and make more use of the power of Computer Assisted Interviewing (CAI). The changes incorporated included the addition of many new questions. For example, questions were added to collect information about wage rates, union status, job permanency and workplace size for the main job of currently employed employees. Other additions included new questions to collect information about hirings and separations, and expanded response category lists that split existing codes into more detailed categories.  Sampling  This is a sample survey with a cross-sectional design.  Data sources  Responding to this survey is mandatory. Data are collected directly from survey respondents. Data collection for the LFS is carried out each month during the week following the LFS reference week. The reference week is normally the week containing the 15th day of the month. LFS interviews are conducted by telephone by interviewers working out of a regional office CATI (Computer Assisted Telephone Interviews) site or by personal visit from a field interviewer. Since 2004, dwellings new to the sample in urban areas are contacted by telephone if the telephone number is available from administrative files, otherwise the dwelling is contacted by a field interviewer. The interviewer first obtains socio-demographic information for each household member and then obtains labour force information for all members aged 15 and over who are not members of the regular armed forces. The majority of subsequent interviews are conducted by telephone. In subsequent monthly interviews the interviewer confirms the socio-demographic information collected in the first month and collects the labour force information for the current month. Persons aged 70 and over are not asked the labour force questions in subsequent interviews, but rather their labour force information is carried over from their first interview. In each dwelling, information about all household members is usually obtained from one knowledgeable household member. Such 'proxy' reporting, which accounts for approximately 65% of the information collected, is used to avoid the high cost and extended time requirements that would be involved in repeat visits or calls necessary to obtain information directly from each respondent.  Error detection  The LFS CAI questionnaire incorporates many features that serve to maximize the quality of the data collected. There are many edits built into the CAI questionnaire to compare the entered data against unusual values, as well as to check for logical inconsistencies. Whenever an edit fails, the interviewer is prompted to correct the information (with the help of the respondent when necessary). For most edit failures the interviewer has the ability to override the edit failure if they cannot resolve the apparent discrepancy. As well, for most questions the interviewer has the ability to enter a response of Don't Know or Refused if the respondent does not answer the question. Once the data is received back at head office an extensive series of processing steps is undertaken to thoroughly verify each record received. This includes the coding of industry and occupation information and the review of interviewer entered notes. The editing and imputation phases of processing involve the identification of logically inconsistent or missing information items, and the correction of such conditions. Since the true value of each entry on the questionnaire is not known, the identification of errors can be done only through recognition of obvious inconsistencies (for example, a 15 year-old respondent who is recorded as having last worked in 1940).  Estimation  The final step in the processing of LFS data is the assignment of a weight to each individual record. This process involves several steps. Each record has an initial weight that corresponds to the inverse of the probability of selection. Adjustments are made to this weight to account for non-response that cannot be handled through imputation. In the final weighting step all of the record weights are adjusted so that the aggregate totals will match with independently derived population estimates for various age-sex groups by province and major sub-provincial areas. One feature of the LFS weighting process is that all individuals within a dwelling are assigned the same weight. In January 2000, the LFS introduced a new estimation method called Regression Composite Estimation. This new method was used to re-base all historical LFS data. It is described in the research paper ""Improvements to the Labour Force Survey (LFS)"", Catalogue no. 71F0031X. Additional improvements are introduced over time; they are described in different issues of the same publication.  Data accuracy  Since the LFS is a sample survey, all LFS estimates are subject to both sampling error and non-sampling errors. Non-sampling errors can arise at any stage of the collection and processing of the survey data. These include coverage errors, non-response errors, response errors, interviewer errors, coding errors and other types of processing errors. Non-response to the LFS tends to average about 10% of eligible households. Interviews are instructed to make all reasonable attempts to obtain LFS interviews with members of eligible households. Each month, after all attempts to obtain interviews have been made, a small number of non-responding households remain. For households non-responding to the LFS, a weight adjustment is applied to account for non-responding households. Sampling errors associated with survey estimates are measured using coefficients of variation for LFS estimates as a function of the size of the estimate and the geographic area.

Long term prediction of vegetation performance on mined sands


Author(s): Bliss, L. C.

Year: 1977

Abstract:
This project on the \"Long Term Prediction of Vegetation Performance On Mined Sands\" (V.E.6.1) was undertaken to provide management with answers on the predictive ability to maintain different kinds of vegetation on raw sands. The research was designed as an integrated, multi-disciplinary program that would concentrate on the role of water stress in a dynamic soil-plant-atmosphere system of a planted grass cover and a natural Jack pine forest. To date only the latter project has been initiated because of the lack of funding and approval to work on the GCOS dike in 1975. This and the Syncrude dyke represent the worst (driest) environmental situation and therefore revegetation of other sand deposits should be more easily accomplished. The Richardson Fire Tower site was chosen because of the representativeness of its Jack pine - lichen woodland on deep sands, a forest type so characteristic of northeastern Alberta. The results of the first full year show that climatically this southwest-facing sand slope warms more rapidly in spring than do level sites at Mildred Lake and Fort McMurray and that the 1976 summer was above normal for temperature. Precipitation was near normal based upon the 1941 - 1970 period. Of the >60 days of precipitation, over 60% were 4 mm or less and thus little if any water entered the soil due to tree, lichen, and litter interception. Both needle duff and lichens provide a significant barrier to surface evaporation compared with open sand. Resistance to evaporation is 2 to 3 times greater with a lichen cover than with litter. The soils are very porous which is advantageous for water entrance, thus preventing erosion but porosity is a disadvantage in maintaining higher water levels near the soil surface for plant growth. These soils recharge during snowmelt in late March - early April; little runoff occurs and over the summer soil water drawdown takes place. Soil moisture content (volume basis) is generally 8 - 15% near the surface in spring, but by late September is 1 - 3% at all depths. Xylem water potentials, a measure of tree water content, were never very low (mean maximum at dawn -5 to -7 atm. and mean minimum at midday -11 to -14 atm.) which reflect a year of average precipitation with frequent light rains and periodic heavier storms. Transpiration and stomatal closure were controlled largely by vapour pressure deficits. Jack pine avoided spring drought by remaining dormant when air and needle temperatures were above freezing, yet when soils were still frozen. Although Jack pine did not show indications of severe drought in a relatively moist summer, it did develop xylem water potentials of -16 to -18 atm., values which are probably detrimental to many of the species being used in revegetation trials on the dike (Bromus inermis, Phleum pratense, and species of Agropyron). This means that potential species must be drought hardy and tested under laboratory rather than only under field conditions to determine their survival under severe drought conditions that may occur but once in 30 to 50 years. The studies of mycorrhizae show that a large number of species of fungi infect the roots of Jack pine and that the infecting flora from disturbed soils (old burns) is quite different from that of undisturbed forests. Since mycorrhizae are critical for the proper growth and survival of pines, care in innoculating tree seedlings with the proper species is essential. The energy and water balance mathematical model predicts the heat and water status of the Jack pine forest. Examination of the model outputs suggests that late season resistance to water uptake occurs because of increased root resistance in autumn. If this is confirmed with further experimental data, and model runs, it means that fall droughts may be especially critical because of the reduced ability of the trees to absorb water through their roots. A second field season coupled with the laboratory studies to determine lethal and sublethal levels of water stress in Jack pine will provide the added inputs to the models necessary for predicting tree response to severe climatic stress. These data, gathered in a highly integrated manner, will permit the calculation of tree survival on sands, be they dikes or other kinds of mined sand, in terms of soil water content and tree density (including crown extent) in relation to the exceptional dry year that may occur once in 30 to 50 years. Data from field trials of grasses or woody species, without supporting measurements of plant physiological responses to environmental conditions cannot provide this essential predictive tool for management unless the one in 30 to 50 year drought cycle is encountered. It is for this reason that modelling of the data in order to predict plant response to unusual environmental conditions becomes so useful. In summary, this study should be able to provide sufficient data to determine whether or not an open stand of Jack pine or similar conifer is the desired end point in maintaining vegetation at a low maintenance cost on sands, the result of open pit mining of the oil sands.

Mercury in the lower Athabasca River and its watershed


Author(s): Radmanovich, R.

Year: 2013

Abstract:
This study assessed the geographic distribution of mercury in water, and biota of the Athabasca River, and in snow and vegetation in its watershed. Mercury in the snowpack was significantly elevated within 46km of oil sands development relative to greater distances. Mercury was significantly higher in tributaries more disturbed by oil sands development relative to less disturbed watersheds. Mercury in vegetation was elevated near development, but was higher at moderate distances from development, likely due to differences in atmospheric speciation within upgrader plumes compared to speciation within the downwind atmosphere. Mercury concentrations were significantly higher in Walleye, Northern Pike, and Goldeye compared to Lake Whitefish. A large percentage (72-80%) of Northern Pike, Goldeye, and Walleye exceeded the Health Canada fish consumption guideline for frequent consumers. The spatial distribution of mercury within the Athabasca River and its watershed indicates oil sands development is a significant source of mercury within the region.

Meteorology and air quality winter field study in the AOSERP study area March 1976


Author(s): Fanaki, F.

Year: 1978

Abstract:
In March 1976, the first in a series of intensive field studies was carried out in the Alberta Oil Sands Environmental Research Program study area in northeastern Alberta to examine the fine structure of the atmosphere and dispersion characteristics under winter conditions. The study comprised several co-ordinated sets of measurements over a two week period. These included: minisonde flights, tethersonde vertical profiles, acoustic sounder and delta-T sonde profiles, correlation spectrometer and ground level sulphur dioxide measurements, plume rise photography and background air and precipitation chemistry. Plume dispersion measurements made by aircraft were co-ordinated with the study and are reported in a separate publication. All measurements, except those for background air chemistry, were made within 20 km of Mildred Lake taking in the present oil sands processing facility of Great Canadian Oil Sands Ltd. and the future production site of Syncrude Canada Ltd. The study was successful in identifying unique features of the winter environment of the area such as diurnal formation and breakup of inversion layers, the effects of the river valley on circulation patterns, plume characteristics, pollutant deposition patterns in the snowpack and background levels of gases and particulates.

Microbial S biogeochemistry of oil sands composite tailings


Year: 2014

Abstract:
Oil sands tailings are important, globally relevant, S reservoirs, known to contain active and diverse microbial communities. However, the potential for S bigeochemical cycling occurring within composite tailings (CT), a mixture of fluid fine tailings, post-processed sand and gypsum (flocculant) used in dry reclamation approaches, has not been examined prior to this study. Biogeochemical characterization of CT solid and porewater samples taken from 5 depths over a 40 meter CT deposit (Mildred Lake, Syncrude Ltd, Fort McMurray, AB, CANADA) revealed distinct depth dependent zones of surficial iron reducing and more extensive sulphate reducing microbial activity. Porewater H2S was detected below 6 meters in the deposit ranging in concentration from 14–300 µM, while much lower concentrations, 1-40 µM, of porewater Fe2+ were restricted to surficial CT samples. Metagenomic (454 pyrosequencing) characterization revealed highly diverse CT microbial communities, with 21 different phyla encountered overall. However, consistent with the porewater geochemical profiles, two depth dependent, structurally distinct communities emerged from multivariate statistical analyses of phylogenetic data (UniFrac http://bmf.colorado.edu/unifrac): a surficial CT zone of Fe3+ reduction and an underlying, more extensive zone of SO42- reduction. These microbial zones were linked to DOC, redox and salinity conditions within the CT deposit. Consistent with the notion that accessible organic carbon was limiting IRB and SRB activity, available SO42- and Fe3+ sources were evident and abundant throughout the deposit. Pilot reclamation is currently focusing on capping CT with a freshwater wetland, reflecting the original boreal forest landscape. However a wetland may provide a more labile organic carbon source for underlying CT associated bacteria, which may stimulate greater H2S generation and/or aid sequestration through IRB driven FeS formation. Recent field and laboratory results from the adjacent CT pilot fen reclamation site suggest that stimulation of H2S generation associated with downwelling fen organic carbon inputs is occurring. These results identify the need to consider the potential for microbial biogeochemical transformations of waste materials to hinder the efficacy of proposed reclamation scenarios.

Modelling the circulation and sediment distribution in the Athabasca Delta area


Author(s): Harrington, A. R.

Year: 1982

Abstract:
This project undertook an assessment of the potential for using satellite imagery to determine water quality parameters in the southwest end of Lake Athab8sca and to provide a mathematical model capable of simulating the circulation patterns in this area of the lake. A substantial amount of field data was collected for calibration purposes and served to ellucidate some of the hydraulic characteristics of the study area. The results indicated that water from the Athabasca River and its distributary channels could reach the north shore of the lake under conditions of moderately large inflow. It had been previously assumed that penetration of river water so far into the lake was unlikely. In addition, river water was found to extend up to at least 20 km northeast of the distributary channels. Water from the Embarras River and Fletcher Channel generally leaves the lake via the Chenal des Quatres Fourches while water from Big Point Channel generally discharges through the Riviere des Rochers. Correlation of LANDSAT imagery with contemporaneous water quality data yielded a high correlation between suspended sediment concentrations and band 6 digital response values. No other water quality parameters were correlated with the raw LANDSAT data. Principal component analysis of the satellite data indicated a high correlation between suspended sediment and the first principal component, which emphasized the infrared bands. In addition, conductivity was well correlated with the third principal component, which emphasized the difference between the visible bands. This result could prove beneficial in analysing satellite imagery since conductivity is a useful parameter for differentiating between lake and river water. A finite element model was developed which solves the vertically integrated momentum and continuity equations. Based on an implicit time stepping algorithm, the model was used to generate circulation patterns for an idealized representation of the study area.

Molecular identification of a yellow perch viral disease associated with exposure to oil sands process affected waters (PO)


Year: 2011

Abstract:
Large volumes of tailings and process affected water are generated as a result of oil sand mining processes. This presentation discussed the safe incorporation of these wastes into the terrestrial and aquatic landscape. A study was conducted in which yellow perch were stocked into experimental ponds, namely Demonstration Pond and South Bison Pond, during the periods of 1995-1997 and 2008-2010. Demonstration Pond was comprised of mature fine tailings capped with natural surface water, while South Bison Pond was formed at a site surrounded by overburden or lean oil sands. Disease surveys were conducted at these experimental ponds and also at Mildred, Sucker, and Kimowin Lakes. External white nodular lesions, characteristic of lymphocystis disease were observed on perch at all sites except Kimowin Lake. The identity of the virus was confirmed by DNA extraction and PCR with genotype generic major capsid protein gene primers. The presence of lymphocystis disease virus in perch was confirmed through sequencing of PCR results. The viral genotype appeared to be different from any previously isolated viral genotype. During the course of the study, there was an increasing incidence of the disease at Demonstration Pond and a decreasing incidence at the South Bison Pond. The intensity of the disease was found to be proportional to the incidence, which was positively correlated with changes in naphthenic acid concentration.

Monitoring ice cover characteristics and behaviour along the Slave River


Year: 2015

Abstract:
For communities along the Slave River, ice is an important component of the traditional way of life. During the winter, a stable ice cover provides local residents with safe access to traditional hunting, trapping, and fishing areas along the river. In recent years, however, local communities have observed changes in ice cover characteristics (e.g. air pocket formation, double layer ice), that have increased the risks associated with travel on the ice. Research to date has focused in the impact of flow regulations, but very little is known about the Slave River ice cover characteristics and behaviour. Remote sensing and field surveys were used to gain an understanding of the ice cover progression along the river during the 2013 – 2014 and 2014 – 2015 winters. RADARSAT- 2 satellite imagery captured changes in the ice cover and identified different types of ice during the entire course of each winter season. The results show that flow regime and meteorological conditions are the main parameters influencing the ice regime along the Slave River.

Old Fort Point land use study: Athabasca Chipewyan First Nation; Old Fort Point Lake Athabasca, Alberta


Year: 2003

Abstract:
The purpose of the HRIA was to conduct assessment of lands that would be part of a "land swap" that would see the relinquishing of ACFN use of the Chipewyan Reserve 201 at the Athabasca River delta and the creation of a new reserve-based community on the south shore of the lake. As a product of the HRIA, a number of site locations were identified that did not strictly fit the definition of "historical resources", as defined b y the Historical Resources Act (RSA 2000). Often these were areas associated with personal stories and living memories of the members of the Fort Chipewyan community. In an effort to preserve this information, a limited land use study was implemented simultaneously with the HRIA. The purpose of this study was to record the stories, memories and histories of the people who lived at Old Fort, and to preserve a record of these memories for future generations to enjoy. The primary objectives of this land use study were to inventory traditional and modern land use sites within the proposed development zone; to evaluate the location and condition of the individual sites identified; to forecast the nature and magnitude of site-specific impacts; and to present the information in an organized way to permit the ACFN to evaluate the significance of the sites identified in order to make decisions about their long term management. The purpose of the land use recording program conducted was not to provide an exhaustive study of the full history of Old Fort. Rather, it was to provide a local context for not only understanding the historical resource sites identified during the HRIA, but also to preserve some of the stories and memories associated with Old Fort. This was accomplished in cooperation with the members of the Athabasca Chipewyan First Nation. The methods used for the recording of the stories and memories associated with Old Fort Point included three different methods, including a formal interview session with Victoria Mercredi, informal traditional site visitations with Rene Bruno and Charlie Mercredi and incidental visitation that occurred during the HRIA. While the stories of Old Fort were primarily gathered during the first two procedures, the bulk of the reported site locations were noted as the result of the latter field investigation. This investigation was an outgrowth of the work that was being conducted as part of the HRIA for the proposed Old Fort development area.

Patterns of riparian disturbance in Alberta's boreal mixedwood forest: Beavers, roads, and buffers


Author(s): Martell, K. A.

Year: 2004

Abstract:
Road-crossings at streams in Alberta's boreal mixedwood forest may act as human analogues of beaver dams by blocking flow, raising water tables upstream and lowering water tables downstream. I compared riparian vegetation on low-order streams with paired road crossings and beaver dams, to explore the idea that roads form a permanent, human-created beaver dam. My results indicate that water levels are raised upstream of road crossings but extensive interaction between road crossings and beavers confounded my analyses. Detailed field surveys of the beaver dams provided valuable data on beaver habitat use in boreal mixedwood forests. A 50-year chronosequence of air photos suggests that beavers may be the primary disturbance agent structuring riparian zones on low-order streams in the study area. Current forestry operating ground rules in Alberta require 30-60 m unharvested buffer strips on permanent streams but this study showed that beavers could be removing forest cover from entire buffer strips.

Performance of grasses shrubs and trees on disturbed soil at the AOSERP Mildred Lake camp experimental area


Year: 1980

Abstract:
The plants referred to in this report were initially established on the AOSERP Mildred Lake Camp area in 1977. The objectives of the program were to establish grass, shrub and tree species for evaluation of their response, particularly their reproduction response, to the climatic and edaphic conditions north of Fort McMurray. Over the 1977 growing season, 50 species and/or sources of grasses were spring seeded, 47 species and/or sources were started in containers and transplanted to the field and 24 species and/or sources were fall seeded. In addition, 12 woody plant species and/or sources were also planted in the field after growth in the greenhouse in containers. This report discusses the results of an evaluation of the plants conducted in late August and September, 1979.

Planning for Canada's future oil sands pit lakes: An overview of the COSIA demonstration pit lakes project


Author(s): Vandenberg, J. A.

Year: 2014

Abstract:
Pit lakes are one of the most visible legacies of open pit mining that result from permanent modifications to pre-mining topography, hydrology and hydrogeology. The extraction of the non-traditional hydrocarbon resource bitumen from Alberta’s Athabasca Oil Sands using truck-and-shovel techniques will result in the development of 35 pit lakes within the next 50 years. These will be large permanent basins with surface areas ranging from 0.2 to 35 km2 and depths ranging from 5 to 42 m. Only one lake, Syncrude’s Base Mine Lake, presently exists. Stakeholders and regulators are concerned that concentrations of constituents such as naphthenic acids, PAHs, ammonia and chloride in lake water will impair the environmental function and social utility of these lakes. However, numerical models have predicted that, within a decade or two of filling, these lakes will become relatively benign systems with the capacity to sustain aquatic ecosystems and to be fully integrated within the Athabasca watershed. To improve our understanding of oil sands pit lake functions, a consortium of oil sands producers called Canada’s Oil Sands Innovation Alliance (COSIA) is considering developing a state-of-the-art research facility with three to four demonstration pit lakes, a dozen experimental ponds, and a smaller mesocosm and microcosm facility. The proposed demonstration pit lakes will be approximately 200 m in diameter and 20 m deep, will be constructed using oil sands waste materials and process waters representing proposed closure strategies, and will be monitored regularly for at least a decade. The DPL Project will include funding for external researchers (both Canadian and international) to conduct publishable research on specific knowledge gaps. On a global scale, this will be one of the first research initiatives from the petroleum-, metals-, coal-, uranium-, diamond-, or aggregate-mining sectors to physically test pit lake predictions on this scale in advance of lake formation. This presentation will review the content and status of the COSIA Demonstration Pit Lakes Project, and will highlight potential research opportunities.

Plants and habitats — a consideration of Dene ethnoecology in northwestern Canada


Author(s): Johnson, L. M.

Year: 2008

Abstract:
This paper discusses local understanding of plants and habitats, based on the linguistic evidence [terms for plants and (or) habitats] gathered from ethnobotanical and ethnoecological field work conducted with several Dene Nations of the Canadian northwestern boreal forest and adjacent regions. Nations involved in the study include (Mackenzie Delta Region), Sahtú’otine’ (Great Bear Lake), Kaska Dena (southern Yukon), and Witsuwit’en (northwest British Columbia). Key plant-related habitats include meadow, “swamp”, forest, “willows”, and “brush”. The ethnobotanical classification of willows is explored in conjunction with the explanation of the Dene habitat concept. In local classifications, ‘willow’ is not co-extensive with the genus Salix, but includes a variety of medium to tall woody shrubs that lack either conspicuous flowers, ‘berries’, or thorns; these may include shrubby species of Salix, Alnus, Cornus, and Betula. Shoreline and alpine environments are also discussed as plant habitats. Dene use of alpine environments and resources is ancient, according to the results of recent alpine ice patch research in the Yukon region. The Human dimensions of habitat knowledge are presented. Indigenous concepts of plant taxa and of landscape associations or habitats may differ substantially from those of scientific botany and ecology, and are based in a holistic and interactive ethnoecology. [ABSTRACT FROM AUTHOR]

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