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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.

Characterization of oil sands process-affected waters by liquid chromatography Orbitrap mass spectrometry

Year of Publication: 2013

Abstract:
Recovery of bitumen from oil sands in northern Alberta, Canada, occurs by surface mining or in situ thermal recovery, and both methods produce toxic oil sands process-affected water (OSPW). A new characterization strategy for surface mining OSPW (sm-OSPW) and in situ OSPW (is-OSPW) was achieved by combining liquid chromatography with orbitrap mass spectrometry (MS). In electrospray positive and negative ionization modes (ESI+/ESI–), mass spectral data were acquired with high resolving power (RP > 100 000–190 000) and mass accuracy (<2 ppm). The additional chromatographic resolution allowed for separation of various isomers and interference-free MSn experiments. Overall, ∼3000 elemental compositions were revealed in each OSPW sample, corresponding to a range of heteroatom-containing homologue classes: Ox (where x = 1–6), NOx (where x = 1–4), SOx (where x = 1–4), NO2S, N, and S. Despite similarities between the OSPW samples at the level of heteroatom class, the two samples were very different when considering isomer patterns and double-bond equivalent profiles. The chromatographic separations also allowed for confirmation that, in both OSPW samples, the O2 species detected in ESI– (i.e., naphthenic acids) were chemically distinct from the corresponding O2 species detected in ESI+. In comparison to model compounds, tandem MS spectra of these new O2 species suggested a group of non-acidic compounds with dihydroxy, diketo, or ketohydroxy functionality. In light of the known endocrine-disrupting potential of sm-OSPW, the toxicity of these O2 species deserves attention and the method should be further applied to environmental forensic analysis of water in the region.

Characterization of oil sands solids closely associated with Athabasca bitumen

Year of Publication: 1988

Abstract:
By means of density fractionation, solids associated with bitumen derived from a variety of oil sand grades, were separated into fractions having different humic matter content. Elemental compositions (daf) and calculated densities of the different fractions were similar suggesting a similarity in the nature of the humic matter. Density fractionated solids having a low and a high (∗>87%) ash content were treated with NaOH for various periods of time to extract the humic acids. For all humic acids analysed the elemental composition and distribution of carbon types in each region of 13C n.m.r. spectra were similar. It has been shown that aromatic carbon was the predominant type of carbon for all samples. On the basis of the aromaticity data, it has been suggested that oil sand humic matter has a significant terrestrial input.

Characterization of oil sands tailings using low field Nuclear Magnetic Resonance (NMR) technique

Year of Publication: 2008

Abstract:
The oil sands mining and extraction processes in Canada produce large volumes of tailings that are a mixture of mainly water, clay, sand, chemicals and bitumen. This mixture is transported to tailings ponds, where gravity segregation occurs. During this process, a stable suspension called mature fine tailings (MFT) is formed, which requires many years to fully consolidate. Therefore, land reclamation and water recirculation become significant environmental issues. For this reason, it is important to understand the tailings content and their settling properties. This study uses the low field Nuclear Magnetic Resonance (NMR) technique to estimate the composition of tailings samples, through a bimodal compositional detection method. Tailings settling characteristics were also studied in the absence and presence of the typical chemical substances used in the industry to accelerate settling. The results show that the NMR technique can be a potential on-site fast measurement of composition and settling characteristics of tailings.

Characterization of organic-rich solids fractions isolated from Athabasca oil sand using a cold water agitation test

Year of Publication: 1988

Abstract:
Using a cold water agitation test (CWAT), different grades of oil-sand solids were separated into three fractions with respect to their insoluble organic carbon content (IOCC). Solids enriched with humic matter (IOCC ~36%) were present in association with bitumen, whereas solids with an IOCC of about 5% occurred suspended in the aqueous phase. The IOCC of the remaining solids was very low (<0.3%). Comparison of and atomic ratios of the different solid fractions rich in organic matter with corresponding results for different types of kerogen indicated that oil-sand organic matter has the same origin as kerogen type III. On the basis of 13C n.m.r. data the oil-sand humic matter was found to be of similar maturity as subbituminous coal. It has been shown that solids associated with bitumen have high concentrations of Ti, Zr and Fe. Solids occurring in the form of an aqueous suspension were enriched with alumina.

Characterization of simple phenols in oil sands extraction-process water

Year of Publication: 1984

Abstract:
An aqueous acetylation method was evaluated for the identification and quantification of simple phenolic compounds in oil sand extraction plant effluents from the Syncrude Canada Ltd plant . Water samples were acetylated by the addition of acetic anhydride and sodium bicarbonate and extracted into methylene chloride. The concentrations were analysed by gas chromatography and mass spectrometry. The method was successfully applied to the analysis of phenols and cresols in tailings pond water, drainage water, groundwater and surface water. Quantitative results for acetate derivatives were reproducible and interference from other constituents was minimal.

Characterization of sol-gel-derived nano-particles separated from oil sands fine tailings

Year of Publication: 2003

Abstract:
Methodology has been developed to separate nano-particles of amorphous material from Syncrude fine tailings. Both, separated finer solids and residual coarser solids, were characterized by elemental analysis, X-ray powder diffraction, XPS, SEM, infrared spectroscopy, solid-state NMR, density, and surface area measurements. Based on the results of infrared and X-ray diffraction, the amorphous minerals identified in finer solids included allophanes, halloysite, ferrihydrite, and amorphous silica. The finer fraction also contained some crystalline material consisting of muscovite and traces of quartz. The residual coarser solids consisted mostly of quartz, muscovite, and kaolinite.

Characterization of solids isolated from different oil sand ores

Year of Publication: 2010

Abstract:
Understanding mineralogy and surface properties of fine solids is vital in oil sands processing and tailings management. Fine solids in oil sands are often contaminated by tightly bound organic matter (OM) originally or during hydrocarbon removal, thereby increasing surface hydrophobicity and making its characterization problematic. The surface properties of solids affect the entire process cycle of obtaining synthetic crude oil from surface-mined oil sands using a water-based extraction process, and managing produced tailings. In this study, low temperature ashing (LTA) was found to be a more suitable method than hydrogen peroxide (H2O2) for OM removal from clay sized minerals (CSM) because of its selectivity for decomposing only organics. The mineralogy and cation exchange capacity of the CSM remained unaffected after treatment with LTA as opposed to H2O2 treatment. To comprehend the organo-mineral interactions in oil sands, solids isolated from weathered and oil sands having low- and high-fine solids content were examined. Low-fines ore possessed the lowest amount of organic coated solids and highest bitumen recovery. The solids in the bitumen froth from these ores were of less quartz, more carbonates, transition metals and carbon than the solids in the corresponding tailings. Infrared spectra showed a likely association between OM and carbonates in the organic coated solids isolated from bitumen froth. Weathered ores were found to contain more organic coated solids which were observed to reduce bitumen recovery from these oil sands ores. A further study of weathered ores was undertaken to understand the reason for its poor processability from a mineralogical perspective. A higher amount of divalent cations was found in weathered ores than in high- and low-fines ores. The low-fines ore was found to exhibit the highest kaolinitic to illitic mineral ratio, while the high-fines ore displayed the lowest ratio. Siderite and pyrite were observed in the solids isolated from weathered and high-fines ores, but were absent in low-fines ores. In addition to wettability, the poor processability of weathered ores appeared to be related to the interactions between the divalent cations and illite, and the cementation effect of the siderite concretions on the oil sand grains, which inhibited bitumen liberation. Corrensite, a mixed-layer chlorite-vermiculite, was detected for the first time in weathered ores.

Characterization of solvent-insoluble organic matter isolated from Alberta oil sands

Year of Publication: 1991

Abstract:
Considerable quantities of organic material, insoluble in common organic solvents, are known to be associated with the inorganic minerals present in oil sands. This insoluble organic matter (IOM) consists of both humic and non-humic components containing numerous oxygen functions. In this investigation IOM was beneficiated from a number of feedstocks using mineral dissolution techniques normally used for the isolation of kerogen concentrate from oil shales. The feedstocks included two different grades of Athabasca oil sand, three tailings stream fractions from oil sand plants in Alberta, and a sample of New Brunswick oil shale. The various fractions were analysed for elemental composition and then characterized by infrared and 13C n.m.r. methods. The elemental analyses have been discussed in terms of a van Krevelen diagram by plotting atomic ratios against atomic ratios. N.m.r. data have been used to calculate the aromaticities of various fractions.

Characterization of stored peat in the Alberta oil sands area

Year of Publication: 1980

Abstract:
Properties of stored peat were studied at sites near Evansburg, Alberta, and on the lease of Syncrude Canada Ltd. at Mildred Lake, Alberta. Physical, chemical, and microbiological properties of stored materials were compared with those of fibric moss peat, mesic moss peat, and mesic fen peat samples from undisturbed sites. Environmentally induced changes in peat properties were simulated in' the laboratory by freeze-drying, air-drying, and thawing peat samples. Air-drying and, to a lesser extent, freeze drying, resulted in deterioration of physical properties and in reduction of microbial activity. The stored materials at Evansburg consisted entirely of peat whereas at Mildred Lake the materials were heterogeneous peat-mineral mixtures which were grouped as follows: group I, peat predominant; group II, sand predominant; group III, sand-clay mixture; and group IV, peat-sand mixture. Optimum temperatures for microbial activity in the storage piles occurred near the surface and decreased with depth while optimum moisture conditions occurred near the 50 cm depth. Frost penetration was not greater than 1 m in any of the piles. Storage piles consisting of peat-mineral mixtures which had been fertilized had a somewhat higher level of microbial activity and organic matter decomposition than undisturbed peat or stored, relatively pure peat. Properties of the stored materials which were highly correlated with each other were carbon, nitrogen, respiration rate, enzyme activity, cation exchange capacity, ash content, bulk density, pore volume, and water capacity. Relatively simple methods for the characterization of ash, carbon, and bulk density of stored materials were used.

Characterization of sulfur oxidizing microbial communities inhabiting the sulfur blocks of Alberta's oil sands

Authors Pisz, J.
Year of Publication: 2008

Abstract:
This study was designed to determine if Alberta's sulfur blocks were inhabited by microorganisms which contribute to oxidation of elemental sulfur. The first objective was to elucidate a functional method of differentiating between viable and non-viable organisms in environmental samples. The second objective was to use this and other more established microbiological analyses to characterize the microbial population inhabiting the block and determine if they influence elemental sulfur oxidation. In order to differentiate between viable and non-viable microorganisms, I relied on a DNA binding agent called ethidium monoazide bromide (EMA). Based on previous literature, I was able to test its activity in different environmental samples. Treatment with EMA inhibits the amplification of free DNA, whereas DNA protected by the membranes of viable cells is not affected. After finding that killed pure culture cells had a substantial reduction in their DNA amplification I proceeded to inoculate the same species of killed and viable cells into either soil, biofilm, or elemental sulfur samples obtained from Syncrude's Phase I sulfur block. I have found the EMA treatment to be sufficient at inhibiting amplification of DNA from non-viable cells inoculated into both the soil and sulfur samples, but not in the biofilms. In achieving the second objective I designed experiments which tested in vitro and in situ samples of the sulfur block. Bioreactors containing microbiological inoculants from water running off the sulfur block were compared to sterile bioreactors for levels of acidity, sulfate accumulation and microbial population. Comparison between the surface block samples and the matrix samples showed a higher number of bacteria in the surface samples; however, the differences between the two bioreactor treatments were not significant. Bioreactors which received sterile water did not increase in acidity or sulfate accumulation. The two treatments which were inoculated with 10% sulfur block run off increased by 3 and 4.3 mM sulfate, and 8.6 x 10-3 and 1.8 x 10-2 hydronium ion concentration, in the surface and matrix treatments respectively. In situ samples obtained by coring the sulfur blocks showed that microbial inhabitants are present throughout the block depth profile with a discontinuous pattern, which could be attributed to the fractures associated with the solidification of the block and subsequent colonization. The level of microbiological inhabitants ranged from 2.5 to 5.5 log heterotroph colony forming units g-1 sulfur, and 3.19 x 101 to 1.62 x 102 A. thiooxidans amplified copy numbers, and 1.23 x 103 to 1.11 x 104 Eubacteria amplified DNA copy numbers μg-1 of extracted DNA from EMA treated sulfur block samples. Most probable number counts for autotrophs only detected organisms along the 0-10 cm depth of the block. The results of this study suggest that the use of ethidium monoazide bromide is a suitable method of detecting the large and varied microbial population inhabiting Alberta's sulfur blocks which can influence the level of block oxidation. The level of microorganisms present in the block is varied, which may parallel the varied pockets of air and water collected in the geomorphic fractures. Microbial communities residing in the sulfur block are partially responsible for sulfur oxidation. Methods aimed at reducing the level of sulfur oxidation must aim to reduce both the chemical and biological pathways leading to sulfur oxidation.

Characterization of trace gases measured over Alberta oil sands mining operations: 76 speciated C2-C10 volatile organic compounds (VOCs) CO2 CH4 CO NO NO2 NOy O3 and SO2

Year of Publication: 2010

Abstract:
Oil sands comprise 30% of the world’s oil reserves and the crude oil reserves in Canada’s oil sands deposits are second only to Saudi Arabia. The extraction and processing of oil sands is much more challenging than for light sweet crude oils because of the high viscosity of the bitumen con- tained within the oil sands and because the bitumen is mixed with sand and contains chemical impurities such as sulphur. Despite these challenges, the importance of oil sands is in- creasing in the energy market. To our best knowledge this is the first peer-reviewed study to characterize volatile organic compounds (VOCs) emitted from Alberta’s oil sands mining sites. We present high-precision gas chromatography mea- surements of 76 speciated C2–C10 VOCs (alkanes, alkenes, alkynes, cycloalkanes, aromatics, monoterpenes, oxygenated hydrocarbons, halocarbons and sulphur compounds) in 17 boundary layer air samples collected over surface mining operations in northeast Alberta on 10 July 2008, using the NASA DC-8 airborne laboratory as a research platform. In addition to the VOCs, we present simultaneous measure- ments of CO2, CH4, CO, NO, NO2, NOy, O3 and SO2, which were measured in situ aboard the DC-8. Carbon dioxide, CH4 , CO, NO, NO2 , NOy , SO2 and 53 VOCs (e.g., non-methane hydrocarbons, halocarbons, sul- phur species) showed clear statistical enhancements (1.1– 397×) over the oil sands compared to local background val- Correspondence to: I. J. Simpson (isimpson@uci.edu) ues and, with the exception of CO, were greater over the oil sands than at any other time during the flight. Twenty halo- carbons (e.g., CFCs, HFCs, halons, brominated species) ei- ther were not enhanced or were minimally enhanced (<10%) over the oil sands. Ozone levels remained low because of titration by NO, and three VOCs (propyne, furan, MTBE) remained below their 3 pptv detection limit throughout the flight. Based on their correlations with one another, the com- pounds emitted by the oil sands industry fell into two groups: (1) evaporative emissions from the oil sands and its prod- ucts and/or from the diluent used to lower the viscosity of the extracted bitumen (i.e., C4 –C9 alkanes, C5 –C6 cycloalka- nes, C6–C8 aromatics), together with CO; and (2) emissions associated with the mining effort, such as upgraders (i.e., CO2, CO, CH4, NO, NO2, NOy, SO2, C2–C4 alkanes, C2– C4 alkenes, C9 aromatics, short-lived solvents such as C2Cl4 and C2 HCl3 , and longer-lived species such as HCFC-22 and HCFC-142b). Prominent in the second group, SO2 and NO were remarkably enhanced over the oil sands, with maxi- mum mixing ratios of 38.7 ppbv and 5.0 ppbv, or 383× and 319× the local background, respectively. These SO2 lev- els are comparable to maximum values measured in heavily polluted megacities such as Mexico City and are attributed to coke combustion. By contrast, relatively poor correla- tions between CH4, ethane and propane suggest low levels of natural gas leakage despite its heavy use at the surface mining sites. Instead the elevated CH4 levels are attributed to methanogenic tailings pond emissions.

Characterization of unextractable organic matter associated with heavy minerals from oil sand

Year of Publication: 1986

Abstract:
Considerable quantities of organic matter are associated with heavy metal minerals recovered from Suncor aqueous sludge. This organic matter is not extractable with common organic solvents. Attempts were made to concentrate this organic matter by dissolving the mineral matter in acids. Various soluble fractions were also obtained by extraction with methanol/benzene (1:4) after each dissolution step. All these fractions were analysed by elemental analysis, infrared, proton and 13C nuclear magnetic resonance spectroscopy.

Characterizing response variability and method uncertainty in odour perception research

Year of Publication: 1999

Abstract:
Data previously collected to determine odour thresholds in fish flesh for individual contaminants identified as possible fish tainting substances from oil sands wastewaters were reanalyzed to determine both the variability in response for an 11 member panel and the range of uncertainty for the detection method. Results are presented for 8 compounds: naphthalene, 1-methylnaphthalene, 2,6-dimethylnaphthalene, 2,3,5-trimethylnaphthalene, 1.4-dimethylbenzene, benzothiophene, dibenzothiophene and 2,5-dimethylphenol. These results demonstrate that substantial variability was present in responses from a group of only 11 panelists who were selected for their sensitivity and consistency, while method uncertainty was tolerably narrow.

Characterizing the geochemical reactions in overburden waste pile: Syncrude Mine Site Fort McMurray, Alberta, Canada

Authors Wall, S. N.
Year of Publication: 2005

Abstract:
Potential environmental risks of constructing waste piles from sulphide-bearing saline- sodic overburden include acid-mine drainage and salinization of surface soils. Acid-mine drainage may result from the production o f sulphuric acid during the oxidation o f sulphide minerals. Acid production during the oxidation o f sulphide minerals may also increase the concentrations of S04 (from sulphuric acid), Ca (from dissolution of carbonates), and Na (from cation exchange with saline-sodic overburden) in surface soils. To identify and quantify these potential environmental risks, in situ S04and Caproduction rates were calculated using two different methods. Sulphide mineral oxidation rates were calculated using simple one-dimensional analytical modelling (assuming diffusive gas transport) of in situ pore-gas 02 concentrations. Ca loading from carbonate mineral dissolution (resulting in C02 production) was also calculated using the simple one-dimensional modelling of measuredpore-gasC02concentrations. Massbalancecalculationsusingsolidsample chemistry (totalS, soluble ion and TIC concentrations) were also used to quantify the rate of S04 and Ca production rates. Geochemical and geotechnical parameters controlling acid production and salt loadings were measured by installing gas probes to a depth of25 m (n = 34) for in situ pore-gas 02, C02, CH4 and N2 concentrations, and b13Cc02 values), diviner tubes to depths of 1.6 m (n = 3; for shallow moisture contents), a neutron access tube to 25 m (for deep moisture contents), and a thermistor string to 20m (for temperatures). Pore-gas 02, C02, CH4 and N2 concentrations were measured using a field-portable gas chromatograph. Depth profiles of solid sulphur (samples stored in anaerobic chambers) and carbon concentrations and forms were measured and used for acid-base accounting. Pore-gas chemistry showed that 0 2concentrations decreased from atmospheric to less than 13% at 5 m depth. C02concentrations increased from atmospheric (0.04 %) to less than 4%at the same depth The () derived primarily from an inorganic carbon source. The moisture content data indicated higher moisture contents between 0.5 and 2.5 m depth than at greater depths in the profile. The pore-gas chemistry in conjunction with solids chemistry suggested the presence o f an oxidation zone (acid producing) in the top 3m ofthe profile. However, the results suggested that the oxidation zone was limited to the top 3 m ofthe profile by the presence ofasaturatedshalezone. Acid baseaccountingresultssuggestedthattheacid-producing potential o f the shale only slightly exceeded the neutralization potential (NNP = -6.5). The rates of02 and C02flux through the reclamation cover were estimated to be 0.07 moles 02/m2/dayand0.03molesC02/m2/day. The corresponding sol-production and CaC03 dissolution rates were estimated to be 1.3 and 4.2 g/m2/day respectively. These results were in keeping with rates estimated from mass balance calculations. The results show that a current moisture content conditions, the waste pile was not at risk for acidification or salinization.

Characterizing the organic composition of snow and surface water in the Athabasca region

Year of Publication: 2013

Abstract:
This pilot study was conducted by Alberta Innovates – Technology Futures (AITF) to characterize the composition of organics present in snow and surface waters in the Athabasca Oil Sands Region (AOSR) with the goal of identifying whether atmospherically-derived organics present in snow are a significant contributor to the organics detected in rivers and lakes in the region. This study is divided into two parts, each describing a different approach to characterizing the organics present in snow and surface waters. In Part 1, we interpret existing polycyclic aromatic hydrocarbon (PAH) concentration data, collected from various monitoring programs in 2011, to compare the composition of PAHs in snow and surface waters across the AOSR. In Part 2, we interpret new ultra-high resolution mass spectrometry analyses of snow and surface water samples collected in 2012 to compare the dissolved polar organics present in snow and surface waters in the Athabasca Oil Sands region (AOSR). The first approach applied in this study uses existing data from snow, river and lake monitoring programs conducted during 2011 which measured total (dissolved + particulate) PAH concentrations in snow and surface waters in the region. The 2011 dataset includes total (dissolved + particulate) concentrations for 34 parent and alkylated PAH species for 105 snow, 272 Athabasca River and tributary, and 3 lake samples. These data were compiled so that the composition of PAHs in the Athabasca River, its tributaries and a small number of lakes could be compared with that of snowmelt. The snow data show compositional differences between the PAHs present in snow sampled from areas closest to oil sands activities (i.e., near-field sites) and from more distant (i.e., far-field) snow sampling locations. Despite large concentration variations in snow along geographic gradients, the composition of PAHs are found to be similar among near-field sites, but change significantly at far-field sites. Both the near- and far-field snow samples have PAH compositions that are different from the PAHs present in the Athabasca River, its tributaries and lakes. Compositional differences in PAH assemblages are also evident between tributaries and the Athabasca River. PAH concentrations in rivers are found to vary seasonally, with peak concentrations observed in July 2011 when Athabasca River levels were at their highest. However, the composition of PAHs present in July 2011 do not resemble the composition of PAHs identified in snow, suggesting that direct transfer of PAHs accumulated on snow from atmospheric deposition to Athabasca River and its tributaries in the area is not a major source of PAHs present in surface waters. The timing of peak PAH concentrations in rivers, which coincides with a high flow period during freshet, does suggest that snowmelt may contribute indirectly to increases in PAH concentrations due to processes such as increased catchment runoff, erosion of stream channels, and snowmelt-induced groundwater inputs during this dynamic hydrologic period. The second approach applied in this study uses Electrospray Ionization Fourier Transform Mass Spectrometry (ESI-FTICR MS) to characterize the dissolved polar organic composition of snow and surface water samples provided by various Alberta Environment and Sustainable Resource Development (AESRD) programs conducted in 2012. The 2012 samples analyzed by ESI-FTICR MS include 7 snow samples, 73 Athabasca River and tributary samples, and 6 lake samples. This profiling method identified thousands of dissolved polar compounds including the acidic organic components in negatively charged ESI(-) mode, and basic components in positively-charged ESI(+) mode. Although based on a limited number of samples, the organic profiles obtained for the snow samples in ESI(-) mode show compositional differences in the dissolved organics present in snow sampled from sites closest to oil sands activities (

Characterizing the transport of process-affected water contained in oil sands tailings ponds into the underlying Pleistocene clay till in northern Alberta's Athabasca oil sands region: A field study

Year of Publication: 2011

Abstract:
A small scale Infiltration Pond was constructed to characterize the transport of oil sands process affected (PA) water contained in Suncor’s South Tailings Pond (STP) to the Wood Creek Sand Channel (WCSC) through a 5-8 m thick glacial clay till. The extent of PA water infiltration was determined by extracting pore water samples from the clay till, analyzing their isotopic (δ18O), major ions, and metals composition over a two year time period. As conservative tracers, δ18O and chloride concentration trends indicated the water penetration line at approximately 0.9 m, while major ion and metal mobility lagged this line. Uptake of Mo, Pb, sodium and sulphate and release of Ba, Sr, calcium and magnesium suggest that adsorption and ion exchange reactions are the foremost attenuation processes controlling inorganic solutes transport. In addition, a correlation coefficient of 0.96 between diffusion analytical models and field measurements for tracers, provided evidence of a diffusion-dominated system.

Chemical and biological monitoring of muskeg drainage at the Alsands project site. Volume II: Monitoring and fish studies

Year of Publication: 1981

Abstract:
Volume I of this report reviewed the publicly available literature on stream environments in the Muskeg River basin as background to the monitoring studies. This volume (Volume II) describes the results of the studies, discusses their effectiveness, and makes suggestions about the design of similar monitoring programs that might be established in future in the AOSERP area. The 1980 monitoring studies were intended to both monitor the effects of Alsands' muskeg drainage on aquatic habitats and terrestrial vegetation, and to form the basis of a long-term program to monitor the effects of the Alsands development on aquatic habitats in the Muskeg River over the life of the project. The long-term, routine monitoring program was to be designed based on the experience with the 1980 studies, which would test methods and examine the suitability of various biological parameters for biomonitoring. To meet these objectives, a variety of biological and water quality attributes were studied within the zones of potential impact and in control areas. Measures of water quality, such as suspended solids, dissolved oxygen, major ion, metal and nutrient concentrations, were studied to obtain direct information on physical and chemical impacts at the time of sampling. Periphytic algae and benthic macroinvertebrates were sampled by several methods to detect the biological effects of physical and chemical changes in water quality. Biological monitoring had the potential of detecting impacts that occurred prior to sampling, and provided a direct measure of biological damage, usually the matter of greatest human concern. Benthic invertebrates were selected for study because they are commonly rated as the most generally useful group for biomonitoring (eg Hellawell 1977). Periphytic algae were sampled because they could be particularly useful for monitoring the effects of nutrient loading and turbidity (Hellawell 1977). A fish sampling program was conducted in conjunction with the monitoring studies to supplement available life history information on species inhabiting the Muskeg River basin. Previous studies on the fish fauna of the drainage (reviewed in Volume I) showed that Hartley Creek and the Muskeg River, at and below the Alsands development area, provide spawning and rearing habitat for Arctic grayling and two species of suckers. In addition, yearly grayling may overwinter in the lower Muskeg River, several species of small fish reside in the watershed year-round and small numbers of other large species (eg northern pike) use the watershed for at least part of the year. One de f i c i en c yin the available baseline data on fish populations in the Muskeg River drainage is the lack of information on overwintering locations, and on the distribution and numbers of spawners, eggs, fry and juveniles at specific locations and times. Without such data, only very large changes in the fish populations could be detected during routine monitoring studies. A second deficiency in the available data is that the importance of the river as Arctic grayling habitat has not been adequately quantified. Angling results indicate the summer population density is larger than spring trapping results have suggested (Bond and Machniak 1979). Despite two attempts, Bond and Machniak (1977, 1979) did not obtain a complete count of the number of Arctic grayling entering the Muskeg River in spring. Because the fish had begun their migration prior to break-up, a counting fence could not be installed in time. Their 1978 attempt to count grayling as the fish moved out of the river in the fall was thwarted by high water. The 1980 fish studies were conducted in an attempt to provide some of this missing baseline information. Specifically, the objectives of the fish studies were: 1. To locate and describe overwintering areas of yearling Arctic grayling and, if possible, to quantify (as catch per unit effort or direct counts) the importance of each site to the population; 2. To locate and quantify the importance of spawning and rearing areas of suckers and grayling; 3. To monitor and enumerate downstream migrant fish, particularly grayling, in the fall; 4. To survey small fish populations in the Muskeg River in the fall and early winter; and 5. To determine, if possible, the effects of Alsands' activities in 1980 on the relative abundance, distribution, and fall migrations of Muskeg River fish, from a comparison of the 1980 results to previously-reported results. In the winter of 1979-80, as part of the requirements for approval of drainage ditch construction, Alberta Environment requested Alsands to develop a monitoring program to assess the impact of the two drainage ditches on neighbouring lands and receiving bodies of water. Prior to removal of the peat and initiation 'of construction of the Alsands mining and processing complex, extensive muskeg areas, including ponds, would need to be drained. The two points of discharge would be the proposed tailings pond area and the Muskeg River area about 1 km south of Alsands' temporary camp. Hardy Associates (1978) Ltd. was contracted to assess the impact of the discharged water on vegetation and wildlife habitat. The purpose of their investigation was two-fold: 1. To determine the extent and type of vegetation damage; and 2. To define the short and long-term effects of flooding and siltation on vegetation. This report presents the methods that were used to carry out the study, the results of the field observations, and the conclusions made.

Chemical and biological monitoring of the muskeg drainage at the Alsands project site. Program evaluation and suggestions for continued monitoring

Authors Mayhood, D. W.
Year of Publication: 1981

Abstract:
Volume I of this report reviewed the available data on the aquatic resources of the Muskeg River drainage as a background to further studies on the river system. Volume II presented the results of monitoring and fish studies conducted in 1980. The present volume evaluates the 1980 monitoring program, and makes suggestions for the conduct of future monitoring studies on the Muskeg River and elsewhere in the AOSERP area. More specifically, this volume is intended to meet the following requirements of Alberta Environment that have not been addressed in preceding volumes. 1. Assess the effectiveness of the ditch and outfall designs in limiting the suspended solids load contributed to the Muskeg River. 2. Discuss possible mitigative measures, based on the findings of the present monitoring program. 3. Evaluate the usefulness and suitability of the parameters chosen for monitoring in the current program. In addition, Alberta Environment requested the following: Discuss general alternatives for future monitoring programs in the Alberta Tar Sands area. Consider: a) timing, with respect to season and specific events (floods, washouts, droughts, etc); b) integration of chemical, physical and biological approaches; c) sampling station selection; d) choice of chemical, physical and biological parameters for monitoring; e) methodology; and f) biological indicators. These and many other related topics have recently been treated at some length for Alberta Oil Sands Environmental Research Program by Aquatic Environments Limited (McCart and Mayhood 1980).

Chemical characterization of various oil sands substrates

Authors Powter, C. B.
Year of Publication: 1994

Abstract:
This report is a condensed version of two reports on the chemistry of a variety of oil sands substrates from Syncrude, Suncor, OSLO and SolvEx. The study was conducted by EnviroTest Laboratories for RRTAC, Syncrude, Suncor and OSLO. Page 2 of the report identifies the source of the various samples. Data are provided for: • The raw sample; • Leachate from the raw sample (using the TCLP - Toxicity Characteristic Leaching Procedure of the US Environmental Protection Agency); and • The leached solid. Inorganic analytical data are given for the raw sample and the leachate. Organic analytical data (gravimetric and GCIFID) are provided for all three substrates for various fractions (acid, base/neutral) as well as for targeted priority pollutant polyaromatic hydrocarbons (PAH's) and target substituted PAH's. The GC/FID chromatograms were provided in the original data but are not presented here. The chromatograms indicated a wide of compounds were present in the samples following example). Some of the samples were also analyzed for non-target organic chemicals. Only those samples where identifiable compounds were quantified are presented.

Chemical disequilibrium in oil sands fine tailings

Year of Publication: 1991

Abstract:
Fine tailings from the Oil Sand Mining and Extraction Plant of Syncrude Canada,Ltd. were repeatedly extracted with distilled water and allowed to react for 24hours at each stage. The concentrations of major extractable ions were measuredand used in the geochemical computer program SOLMINEQ_88PC/Shell. Calcite wascalculated to be stable up the second extraction stage. Gypsum is not stable inthe initial liquid at either 25 or 60 ° C. Dissolved SiO2 is inequilibrium with quartz in the starting suspension, when the calculation isdone for 60 ° C. Sio2 remains high in subsequent extracts. Illitedissolution is insufficient to explain the K and Sio2 concentrationsin the extracts. A hypothetical phase such as analcime is also insufficient toexplain Na and Sio2 concentrations. The results suggest furtherinvestigation of amorphous and microcrystalline phases should be carried out.High HC03 - and SO42- concentrations cannot beexplained by mineral reactions, and may be associated with the oxidation oforganics associated with the solids during the extraction procedure. Volumereduction of fine tailings by recrystallization of colloids should be tested asa part of a study to characterize the kinetic response of the tailings tochanges in the chemical environment.

Chemical fingerprinting of naphthenic acids and oil sands process waters - A review of analytical methods for environmental samples

Year of Publication: 2013

Abstract:
This article provides a review of the routine methods currently utilized for total naphthenic acid analyses. There is a growing need to develop chemical methods that can selectively distinguish compounds found within industrially derived oil sands process affected waters (OSPW) from those derived from the natural weathering of oil sands deposits. Attention is thus given to the characterization of other OSPW components such as oil sands polar organic compounds, PAHs, and heavy metals along with characterization of chemical additives such as polyacrylamide polymers and trace levels of boron species. Environmental samples discussed cover the following matrices: OSPW containments, on-lease interceptor well systems, on- and off-lease groundwater, and river and lake surface waters. There are diverse ranges of methods available for analyses of total naphthenic acids. However, there is a need for inter-laboratory studies to compare their accuracy and precision for routine analyses. Recent advances in high- and medium-resolution mass spectrometry, concomitant with comprehensive mass spectrometry techniques following multi-dimensional chromatography or ion-mobility separations, have allowed for the speciation of monocarboxylic naphthenic acids along with a wide range of other species including humics. The distributions of oil sands polar organic compounds, particularly the sulphur containing species (i.e., OxS and OxS2) may allow for distinguishing sources of OSPW. The ratios of oxygen- (i.e., Ox) and nitrogen-containing species (i.e., NOx, and N2Ox) are useful for differentiating organic components derived from OSPW from natural components found within receiving waters. Synchronous fluorescence spectroscopy also provides a powerful screening technique capable of quickly detecting the presence of aromatic organic acids contained within oil sands naphthenic acid mixtures. Synchronous fluorescence spectroscopy provides diagnostic profiles for OSPW and potentially impacted groundwater that can be compared against reference groundwater and surface water samples. Novel applications of X-ray absorption near edge spectroscopy (XANES) are emerging for speciation of sulphur-containing species (both organic and inorganic components) as well as industrially derived boron-containing species. There is strong potential for an environmental forensics application of XANES for chemical fingerprinting of weathered sulphur-containing species and industrial additives in OSPW.

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