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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.

Dissipation of naphthenic acids mixtures by lake biofilms

Year of Publication: 2010

Abstract:
The dissipation (combined sorption and biodegradation) of naphthenic acids (C(n)H(2n+z)O(2)) by lake biofilms with no previous adaptation to oil sands acids was investigated using rotating annular bioreactors. The dissipation by the biofilm was dependent on the chemical composition of the naphthenic acids mixture. There were 2 distinct groups of Fluka naphthenic acids which dissipated with pseudo first order kinetics: (a) t(1/2)= 7 days, r(2)= 0.984 and (b) components which were less readily dissipated with t(1/2)= 134 days, r(2)= 0.618. In contrast to the results observed for Fluka naphthenic acids, no dissipation was evident for lake biofilm exposed to Athabasca oil sands naphthenic acids. The differences in dissipation observed for the systems investigated are attributed to the combination of 3 key factors: (i) molecular structure and (ii) molecular mass of the naphthenic acids; along with (iii) inhibition by some components (containing elements of S and/or N acids). The later are more prevalent in oil sands naphthenic acids compared to Fluka naphthenic acids.

Dissolution of salts encapsulated with elemental sulfur

Authors Ding, Y.
Year of Publication: 2007

Abstract:
Neutral pH conditions were found at the interface of salt-sulfur solid and CT release water. The back-calculated salt diffusion coefficients through a layer of porous elemental sulfur were in the order of that in unsaturated soils. Encapsulating solid salts with elemental sulfur and simultaneous disposal of them into tailing ponds was concluded to be a viable method of managing solid salts and elemental sulfur.

Dissolved organic carbon dynamics in constructed and natural fens in Athabasca oil sands development region near Fort McMurray, Alberta

Authors Khadka, B.
Year of Publication: 2014

Abstract:
Peatlands, mainly fens, are largely disturbed in order to recover bitumen below the surface in the Athabasca oil sands development region, Alberta. Mine closure plans require ecosystem reclamation: hence fen construction method is being investigated. In this study, dissolved organic carbon (DOC) dynamics in a constructed fen were compared with three other diverse natural fens in the region. The constructed fen had lower soil DOC concentration than all natural fens. Based on E2/E3, E4/E6 and SUVA254 of the DOC, the constructed fen had DOC with significantly greater humic content, aromatic nature and larger molecular size than the natural fens. A laboratory DOC production study revealed that these patterns are likely due to the limited DOC contribution from newly planted vegetation at the constructed fen resulting in DOC largely derived from humified peat. These preliminary results suggest that DOC dynamics in the constructed system could be useful for evaluating reclamation success through time.

Dissolved organic compounds removal from oil sands process affected water by coagulation/flocculation

Year of Publication: 2011

Abstract:
Coagulation-flocculation was used as a pretreatment for oil sands process affected waters. The main objectives were to remove the suspended and colloidal particles and organic compounds. Aluminum sulfate, ferric sulfate, and ferric chloride were applied as the coagulant. Synthetic organic polymers were also used as flocculants. The results indicated the successfully reduction of the turbidity and decrease it the concentration of the organic compounds

Dissolved oxygen requirements for fish of the Peace, Athabasca and Slave river basins

Year of Publication: 1994

Abstract:
Many factors affect the dissolved oxygen (DO) content of surface waters, including photosynthesis, respiration, temperature, ice cover, mixing and input of organic materials. In northern Alberta, the discharge of pulp mill wastes with a high biochemical oxygen demand into river systems can result in depletion of DO supplies in winter and increased concentrations of contaminants in the water. A need therefore exists to examine DO requirements of northern rivers fishes considering all life stages and interactions with other stressors, and to document the combined effects of low dissolved oxygen and contaminants on fish populations. A number of major reviews have been conducted on the general subject of dissolved oxygen and fish. The goal of this project was to establish dissolved oxygen requirements for fish species found in northern Alberta rivers, concentrating on environmental conditions found there, particularly the presence of pulp mills and winter ice cover. Material for this review was compiled from an on-line computer search of major pertinent data bases and from printed literature reference services. The report is subdivided into a number of sections that discuss: (1) physiology of fish respiration, (2) limnology of dissolved oxygen in surface waters, (3) effects of adverse DO conditions on fish and invertebrates, (4) modifying effects of other environmental factors, and (5) individual species and life stage requirements of northern rivers fishes. The primary site of gas exchange in teleost fish is the gill membrane; the diffusion of oxygen into the blood is aided by the high oxygen-binding capacity of hemoglobin. Gas exchange depends on the oxygen tension gradient, or partial pressure, between blood and water. Oxygen tension in the water, in turn, depends not only on the DO concentration, but on other physical conditions, particularly water temperature and atmospheric pressure. Large rivers generally maintain dissolved oxygen levels at or near saturation during open-water periods by reaeration. Under winter ice cover, however, DO levels often decline as a result of decomposition of organic matter; DO sags increase with downstream distance in the river. The detrimental effects of low dissolved oxygen on fish are well known. The fundamental effect at the cellular or tissue level is hypoxia, which occurs when the rate of oxygen delivery to the cells is less than that required to meet metabolic needs. Death results when insufficient oxygen delivery to the brain and other tissues results in cellular dysfunction. At the sublethal level, low environmental dissolved oxygen may cause alterations in physiological processes, blood chemistry and hematology, and result in histopathological damage. Moreover, exposure of fish to prolonged hypoxic conditions can lead to increased incidence of disease, reduced growth and decreased swimming performance, as well as altering predator avoidance, feeding, migration, reproduction and other behaviours. Just as important, adverse DO conditions may depress long-term production of fish populations by altering benthic invertebrate communities, especially food species. The detrimental effects of suboptimal dissolved oxygen levels are exacerbated by the presence of contaminants in the environment, including those typically found in pulp mill effluent. This effect of contaminants may be direct, such as by interfering with normal oxygen uptake across the gill membrane, or indirect, by elevating metabolic rate, thereby increasing oxygen demand and reducing the fish’s scope for activity. Fish exposed to reduced environmental dissolved oxygen display increased susceptibility to other toxicants and contaminants, notably those in pulp mill wastes. Increased gill ventilation in response to low DO further increases the rate of contaminant uptake. All species and life stages of fish have both acute and chronic dissolved oxygen requirements. Acute requirements are the minimal levels of dissolved oxygen necessary to avoid short-term mortality. However, chronic requirements are more important ecologically as long-term exposure to suboptimal DO levels, even those well above levels necessary for survival, create stress and decrease growth and population production. Any reduction in the natural DO content of surface waters is likely to have some detrimental effect on fish production; thus, the assumption of a "no effect" DO level below saturation is not valid. Acutely lethal DO levels are relatively straightforward to measure and, based on available evidence on tolerances of adult fish, northern rivers species are grouped into categories of DO sensitivity as follows: (1) Sensitive (acute limit >2 mg/L DO; includes all salmonids, longnose sucker and burbot); (2) Intermediate (acute limit 1-2 mg/L DO; includes all cyprinids except fathead minnow, walleye, white sucker, brook stickleback and goldeye); (3) Tolerant (acute limit < 1 mg/L DO; includes fathead minnow, northern pike and yellow perch); and (4) Unknown (insufficient information available; includes largescale sucker, ninespine stickleback, all sculpins and trout-perch). The establishment of chronic dissolved oxygen requirements, which are more important to the long-term maintenance of healthy fish communities, is more problematic. Until more complete regional data are available, general DO criteria recommended in earlier reviews of this subject (e.g., >6 mg/L for salmonids, >5 mg/L for nonsalmonids; Taylor and Barton 1992) are probably applicable to fish of the northern rivers of Alberta. Although considerable information exists on DO requirements for rainbow trout, and to a lesser extent for walleye, northern pike and fathead minnow, information on the requirements for the other northern river fish species is either very limited or lacking completely. Thus, it is recommended that future research efforts concentrate on these other species, as they are integral components of the fish community. Rainbow trout and bull trout (adults) and mountain whitefish (eggs and larvae) are recommended as sentinel species to monitor dissolved oxygen conditions. Burbot and longnose sucker might also be considered if then- suspected DO sensitivities can be confirmed and they are sufficiently common in the northern rivers.

Dissolved oxygen requirements for fish of the Peace, Athabasca and Slave River Basins: A laboratory study of Burbot (Lota lota)

Year of Publication: 1996

Abstract:
Adverse effects of low environmental oxygen on fish reproduction represents a distinct possibility in the Athabasca and Peace drainages. Species spawning in late fall and winter, such as burbot, would be the most likely to be impacted by low dissolved oxygen (DO). This report describes a study whose objective was to define the temporal changes in reproductive hormones, identify changes in blood electrolytes, haemoglobin, hematocrit, and blood oxygen content, and evaluate the viability of eggs and sperm for burbot during the period of sexual development under normal and hypoxic conditions. The results evaluate the potential of realistic winter water temperatures and hypoxic conditions to impair reproductive performance and induce stress in spawning burbot in the Northern River Basins Study area.

Dissolved oxygen requirements for fish of the Peace, Athabasca and Slave Rivers: A laboratory study of Bull Trout (Salvelinus confluentus) and Mountain Whitefish (Prosopium williamsoni)

Year of Publication: 1996

Abstract:
This report, about "Dissolved Oxygen Requirements of the Eggs of Bull Trout, Salvelinus confluentus. and Mountain Whitefish, Prosopium williamsoni. has been submitted as a partial fulfillment of contractual obligations to the Northern River Basins Study. The main objective of the study was to identify the effects upon survival, embryonic development, hatching success, and quality of larvae of bull trout and mountain whitefish eggs incubated at various levels of hypoxia at low water temperature. In early October 1993, fertilized bull trout eggs were collected from the Hill Creek Hatchery in British Columbia and whitefish eggs were collected from the upper reaches of the Athabasca River near the confluence of the Snaring River. The eggs were transported to the Freshwater Institute, in Winnipeg, Manitoba, and incubated at nominal dissolved concentrations of 3, 5, 7, 9, and 13.5 mg/1 at 2°C. These oxygen concentrations are equivalent to oxygen saturations of 22.3, 37.2, 52.0, 66.9, and 100 percent of air saturation for that locality. The period of incubation under hypoxic conditions extended from November 27, 1993 to May 5, 1994. Each dissolved oxygen treatment was replicated thrice for whitefish and, because of insufficient numbers of eggs, once for bull trout. The oxygen treatments contained 28 incubators: replicate one consisted of 14 bull trout incubators (15 eggs/incubator) and 14 whitefish incubators (50 eggs/incubator); replicates two and three consisted of 26 whitefish incubators (50 to 60 eggs/incubator) and 1 or 2 bull trout incubators (10 to 14 eggs/incubator). Dissolved oxygen and water temperature were monitored daily and egg mortality and hatching were recorded at least three times weekly. At several intervals during embryonic development the oxygen consumption, residual oxygen levels, egg and alevin weights and lengths were recorded from the bull trout. In addition to these records, cardiac rates and measurements of egg and yolk size, and of eye diameter and interorbital distance were obtained for whitefish. Following hatch the thermal tolerance of bull trout and feeding success and thermal tolerance of whitefish from each dissolved oxygen treatment were examined. Exposure to reduced oxygen did not result in any increase in egg mortality of either species. Survival rates were high in all treatments and mortality during the period of hypoxia (Nov. 27, 1993 to May 5, 1994) was less than 10% in hypoxic and normoxic treatment groups of both species. Exposure to hypoxia reduced oxygen consumption by the embryos of both species with the degree of reduction being directly related to the severity of the hypoxia. Residual oxygen levels (the amount of oxygen remaining when the embryo died from hypoxia) were very low and ranged from 0.2 to 0.7 mg/1 (1.5 to 5.5% of saturation) in bull trout eggs and alevins and from 0.4 to 1.0 mg/1 (2.8 to 7.5% of saturation) in whitefish. Cardiac rate was reduced by 8 to 22% in whitefish embryos exposed to dissolved oxygen of 3 mg/1 but was unaffected at higher oxygen levels. Mortality during hatching was insignificant in both species with hatching success generally exceeding 95 % except for one replicate at 3 mg/1 where 86% hatched. The timing of hatch in bull trout eggs was not strongly influenced by hypoxia but the level of development as illustrated by the amount of yolk remaining and smaller body size in the hatched alevins was reduced in embryos incubated at < 7 mg/1 of dissolved oxygen. In whitefish, however, hatching was delayed in embryos incubated at reduced oxygen levels such that the time from fertilization to 50% hatch was 151, 174, 185, 204, and 221 days in eggs from the 13.5, 9, 7, 5, and 3 mg/1 treatments, respectively. Whitefish larvae from all treatments were of similar size.

Distribution and abundance of macrobenthos in the Athabasca River near Fort McMurray

Authors Boerger, H.
Year of Publication: 1983

Abstract:
Benthic macroinvertebrates were collected at two-week intervals between 1982 May 13 and August 18 at 16 sites along an 85 km stretch of the Athabasca River between Fort McMurray and the Ells River. Samples were collected from gravel bars with a 0.l m2 cylinder sampler. All netting had a mesh size of 0.25 mm. Altogether, 348 samples were collected, containing a total of 27 229 specimens belonging to 68 taxonomic groups. The 32 species of Ephemeroptera comprised 21% of the total specimens. Chironomidae, Oligochaeta, Trichoptera, and Plecoptera comprised 53%, 18%, 2%, and 1% of the total specimens, respectively. Densities decreased between May 13 and May 28, then increased steadily to a maximum of 3 294 ind/m2 in early July, after which densities declined again. Individuals belonging to size categories >2 mm, 1 to 2 mm, 0.5 to I mm, 0.25 to 0.5 mm comprised 16%, 20%, 48%, and 16% of the total individuals collected. Average size was largest in early June. The density of invertebrates downstream from the Suncor Tar Sands Mining and Extraction Plant was 31% lower than at sites upstream from the plant. There were no site-specific differences with regard to number of taxa or Shannon-Weaver diversity. Abundance and composition of invertebrates upstream of the Suncor plant were influenced by the confluence of the Clearwater River and by the effluent from the Fort McMurray Sewage Treatment Plant.

Distribution and source of naturally occurring arsenic in groundwater from the southern Athabasca oil sands region

Year of Publication: 2013

Abstract:
Elevated arsenic (As) concentrations (e.g. 360 μg/L) have been measured in shallow groundwater in the Southern Athabasca Oil Sand Region. The geology of this area of Alberta includes a thick cover (up to 200 m) of unconsolidated glacial deposits, with a number of regional interglacial sand and gravel aquifers, underlain by marine shales. As concentrations measured from 201 unconsolidated sediment samples ranged between 1 to 14 ppm. A survey of over 800 water wells sampled in the area found that more than 40% of the wells contained As concentrations exceeding drinking water guidelines of 10 μg/L. Higher As concentrations were associated with reducing conditions. Speciation modeling using the WATEQ4F database showed that the majority of groundwater samples were undersaturated with respect to ferrihydrite, suggesting that reductive dissolution of Fe-oxyhydroxides is the cause of As releases. Mineralogical characterization studies revealed the presence of fresh framboidal pyrite in the deeper unweathered sediments. Electron microprobe analysis employing wavelength dispersive spectrometers indicated that the framboidal pyrite has variable As content with an average As concentration of 530 ppm. In contrast, the weathered sediments did not contain framboidal pyrite, but exhibited spheroidal Fe-oxyhydroxide grains with trace As. The habit and composition suggest that these Fe oxyhydroxide grains in the weathered sediment represent former framboidal pyrite grains. X-ray absorption near edge spectroscopy (XANES) indicated that the weathered sediments are dominated by As5+ species having spectral features similar to those of goethite or ferrihydrite with adsorbed As, suggesting that Fe-oxyhydroxides are the dominant As carriers. Unweathered sediments, on the other hand, had a shoulder on the lower energy side of the main absorption peak suggesting the presence of As1- species in addition to As5+. The derivative value of this shoulder was close to those of arsenopyrite and arsenian pyrite. Least-squares fitting of the XANES spectra with arsenopyrite and goethite model compounds indicate the proportion of As1- species make up 17 to 26 % of the total arsenic in the unoxidized sediments. These findings indicate that the reductive dissolution of Fe-oxyhydroxides is likely the source of As in the groundwater.

Distribution of clay minerals in the process streams produced by the extraction of bitumen from Athabasca oil sands

Year of Publication: 2009

Abstract:
This study investigates the affinity of clay minerals in oil sands for the water-continuous tailings and hydrocarbon-continuous froth streams produced from the extraction of bitumen from oil sands. Clay minerals in oil sands processing impact bitumen flotation in separation vessels, emulsion formation during froth treatment, and fine tailings behaviour. X-ray diffraction of oriented clay slides and random powder samples were used to quantify the clay minerals in the oil sands ore and process streams. Particle size distribution and clay activity balances were also conducted around the extraction process. The degree of partitioning during the conditioning and flotation stages in a batch extractor was determined by the surface properties of the clay minerals present. The water-continuous tailings stream was further separated into fine and coarse tailings fractions through sedimentation. The bulk of the clay minerals reported to the fine tailings stream. Illite and mixed layered illite-smectite partitioned less to the hydrocarbon-continuous froth than kaolinite. Also, the illite-smectite in the froth stream appeared to be different from the illite-smectite in the water continuous streams.

Distribution of minerals in process streams after bitumen extraction by the hot water extraction process

Year of Publication: 2008

Abstract:
Significant research has been done to examine the composition of the solids in the different streams produced by the hot water extraction process. However, very little work has been published showing how the minerals are distributed around the extraction process. This work takes a single ore and details how the minerals partition to the froth, middlings, and tailings streams after batch extraction. Size separation, X-ray fluorescence analysis, and X-ray diffraction combined with quantification by the Rietveld method, are used to provide a detailed breakdown of how elements and minerals are affected by the hot water extraction process. Results show that the primary froth is enriched in kaolinite, iron oxide-hydroxides, zircon, and titanium oxides compared with the other streams. The middlings stream, on the other hand, is enriched in all the clay minerals but especially illite-smectite. Also of interest is the observation that the majority of the titanium and iron in all streams is found in the <45 µm size fraction. These results will hopefully lead to an increased understanding of the challenges and opportunities associated with the disposal of the solid waste produced by the hot water extraction process. INTRODUCTION The mineralogy of the oil sands has been the subject of many different studies ranging from geological deposit characterization (Bayliss & Levinson, 1976) to studies on how valuable minerals deport around extraction in a pilot plant (Alberta Chamber of Resources, 1996). The short coming of these studies is that no attempt has been made to provide a mineralogical balance around extraction. This paper fills that gap in the literature.

Distribution of naphthenic acids in tissues of laboratory-exposed fish and in wild fishes from near the Athabasca oil sands in Alberta, Canada

Year of Publication: 2011

Abstract:
Naphthenic acids, which have a variety of commercial applications, occur naturally in conventional crude oil and in highly biodegraded petroleum such as that found in the Athabasca oil sands in Alberta, Canada. Oil sands extraction is done using a caustic aqueous extraction process. The alkaline pH releases the naphthenic acids from the oil sands and dissolves them into water as their soluble naphthenate forms, which are anionic surfactants. These aqueous extracts contain concentrations of naphthenates that are acutely lethal to fishes and other aquatic organisms. Previous research has shown that naphthenic acids can be taken up by fish, but the distribution of these acids in various tissues of the fish has not been determined. In this study, rainbow trout (Oncorhynchus mykiss) were exposed to commercial (Merichem) naphthenic acids in the laboratory. After a 10-d exposure to approximately 3 mg naphthenic acids/L, the fish were dissected and samples of gills, heart, liver, kidney, muscle, and eggs were extracted and analyzed for free (unconjugated) naphthenic acids by a gas chromatography–mass spectrometry method. Each of the tissues contained naphthenic acids and non-parametric statistical analyses showed that gills and livers contained higher concentrations than the muscles and that the livers had higher concentrations than the hearts. Four different species of fish (two fish of each species) were collected from the Athabasca River near two oil sands mining and extraction operations. No free naphthenic acids were detected in the muscle or liver of these fish.

Distribution of oil sands formation water in bitumen froth

Authors Jia, B.
Year of Publication: 2010

Abstract:
Bitumen froth from oil sands extraction typically contains 60 wt.% bitumen, 30 wt.% water, and 10 wt.% solids. To meet downstream process specifications, the water and solids in bitumen froth have to be removed. The objective of this study is to identify the source of the water reporting to the bitumen froth. The water comes from two sources: formation water contained in mined oil sands ore, about 3-7 wt.%; and processing water added during the extraction process to recover bitumen from oil sands. Determining the distribution of the formation water will enable us to go one step further to understand the effect of formation water on water removal from bitumen froth. After Denver Cell flotation process, the electrical conductivity of the emulsified water, free water and tailings water was determined. The results showed that the conductivity of emulsified water was higher than other water samples, indicating that high salinity formation water preferentially reported to the bitumen froth. To better differentiate distribution of formation water among various process streams, oil sands extraction was carried out using heavy water instead of normal water as processing water, the density of collected water samples was measured by high precision density meter. However, no conclusive result could be obtained by this method. To obtain more accurate quantification of formation water distribution, cobalt as chemical tracer was introduced in the processing water. Following the same procedure of oil sands extraction and water samples collection as in conductivity measurement and heavy water density measurement, the concentration of cobalt in various product streams was determined accurately by Atomic-Absorption spectroscopy. The percent of formation water in emulsified water was then calculated. To understand formation water distribution in the context of oil sands ore characteristics, different types of ores were tested. The results showed that the characteristics of an oil sands ore were decisive factor determining formation water distribution. It appeared that preferential distribution of formation water in the bitumen froth was detrimental to froth treatment.

Distribution of organic contaminants in bottom sediments Peace and Athabasca River basins 1988 to 1992

Year of Publication: 1997

Abstract:
Results of contaminant analyses are presented for bottom sediments collected from the Peace and Athabasca River basins from 1988-90 by Alberta Environmental Protection and in 1992 by the Northern River Basins Study. Contaminant groups represented are the polychlorinated dibenzo-p- dioxins and dibenzofurans, resin acids, chlorophenolic compounds and polycyclic aromatic hydrocarbons. Contaminant concentrations were correlated with percent organic carbon of the fine fraction (the fraction on which contaminant analyses were performed). There was no significant correlation. Organic carbon content of the sediments was a poor predictor of contaminant concentration. Correlations between concentrations of bleached kraft mill-related contaminants were also investigated. Correlations between 2,3,7,8-tetrachlorodibenzofuran and chlorinated dehydroabietic acid concentrations were not significant at the 20% level, but correlations between dehydroabietic acid and chlorinated resin acids were significant at the 1% level.

Distribution of saturates aromatics resins and asphaltenes fractions in the bituminous layer of Athabasca Oil Sands

Authors He, L., Li X., Wu G., Lin F., & Sui H.
Year of Publication: 2013

Abstract:
The composition and distribution of saturates, aromatics, resins, and asphaltenes (SARA) fractions in the bituminous layer on the surface of Athabasca oil sands were identified using elemental analysis (EA), X-ray photoelectron spectroscopy (XPS), field emission scanning electron microscopy (SEM) with an energy-dispersive spectrometer (EDS), and Fourier transform infrared spectrometry (FTIR). The contents of elements sulfur (S) and nitrogen (N) and the ratios of carbon/sulfur (C/S) and carbon/nitrogen (C/N) were characterized as potential indicators for evaluating the distribution of SARA fractions in the bituminous layer. Results indicated that saturates and aromatics tend to deposit at the outer bituminous layer, while asphaltenes and resins were inclined to distribute at the inner layer. Results also suggested that the distribution of SARA fractions was thermodynamically dependent and susceptible to thermal treatment. On the basis of the experimental results, a conceptual distribution model was proposed, which is supposed to serve as a basis for future studies on the liberation of bitumen from oil sands and the operation conditions for oil sands processing.

Divergent pathways of successional recovery for in situ oil sands exploration drilling pads on wooded moderate-rich fens in Alberta Canada

Year of Publication: 2014

Abstract:
Peatlands in northern Alberta, Canada, are being rapidly impacted by oil sands activities, with potentially long-term consequences for their recovery. In situ oil sands extraction requires exploration of oil resources on a dense network of drilling pads across the landscape. This study examined the recovery of wooded moderate-rich (WMR) fens 10 years after abandonment of these sites with minimal restorative measures. Bryophyte and vascular plant diversity, site microtopography, and water chemistry were assessed on drilling pads and in adjacent areas of undisturbed reference habitat. WMR fens affected by drilling activities were divided a priori into two groups based on strongly divergent trends in their successional development. One group represented the majority of WMR fens observed on the land base; at these sites hummock-forming mosses including minerotrophic Sphagnum species were infrequent and tree recruitment was almost absent. The other group was dominated by Sphagnum species, had Picea mariana and Larix laricina recruitment, and appeared to recover more quickly. Both groups had high abundance of wetland sedges, notably Carex aquatilis. Further, drilling pads belonging to the first group had a high water table, limited elevated microsites, and had surface flooding over a portion of the growing season, in contrast to Sphagnum-dominated sites. Development of the aquatic, bryophyte-poor wetland type is comparable to early stages of wetland succession and these systems will recover relatively slowly, likely from decades to more than a century. Restoring part of the vertical distribution of microhabitats before abandonment of these pads could stimulate the successional recovery of vegetation.

Do peat amendments to oil sands wet sediments affect Carex aquatilis biomass for reclamation success?

Year of Publication: 2014

Abstract:
The oil sands industries of Alberta (Canada) have reclamation objectives to return the mined landscape to equivalent pre-disturbance land capability. Industrial operators are charged with reclaiming a vast landscape of newly exposed sediments on saline-sodic marine-shales sediments. Incorporated in these sediments are by-products resulting from bitumen extraction (consolidated tailings (CT), tailings-sand (TS), and oil sands processed water (OSPW)). A sedge community dominated by Carex aquatilis was identified as a desirable and representative late-succession community for wet-meadow zones of oil sands-created marshes. However, the physical and chemical conditions, including high salinity and low nutrient content of CT and TS sediments suppress plant growth and performance. We experimentally tested the response of C. aquatilis to amendments with peat-mineral-mix (PM) on oil sand sediments (CT and TS). In a two factorial design experiment, we also tested the effects of OSPW on C. aquatilis. We assessed survival, below- and aboveground biomass, and physiology (chlorophyll a fluorescence). We demonstrated that PM amendments to oil sands sediments significantly increased C. aquatilis survival as well as below and aboveground biomass. The use of OSPW significantly reduced C. aquatilis belowground biomass and affected its physiological performance. Due to its tolerance and performance, we verified that C. aquatilis was a good candidate for use in reclaiming the wet-meadow zones of oil sands-created marshes. Ultimately, amending CT and TS with PM expedited the reclamation of the wetland to a C. aquatilis-community which was similar in gross structure to undisturbed wetlands of the region.

Does nuclear energy have a role in the development of Canada's oil sands?

Year of Publication: 2004

Abstract:
The Canadian oil sands industry consumes large quantities of natural gas to supply its energy needs and produce hydrogen The EUB expects Alberta crude bitumen production to reach 371 103m3/d by 2012, a 2.8-fold increase from 2002 Based on the configuration of currently operating projects, it is estimated that achieving this production level would require 60-75 106m3/d of natural gas in 2012 - an unsustainable level The industry is working hard to reduce energy requirements and/or find alternative energy sources

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