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Locations of Uraniferous Boulder Fields and Swamps along the North Shore of Lake Athabasca, NTS 74M (GIS data, polygon features)


Year: 2014

Abstract:
Locations of uraniferous boulders fields and uraniferous swamps extracted from industry assessment reports are useful metallogenetic indicators for uranium exploration within and around the Athabasca Basin. They are used as pathfinders to uranium occurrences and prospects. These locations along the northern rim of the Athabasca Basin in Alberta have been compiled in GIS format and delivered as a polygon shapefile. In Alberta, the northern rim of the Athabasca Basin and the regolith underlying the Athabasca unconformity are locally exposed along the northern shore of Lake Athabasca. Extensive uranium exploration work in the 1970s, including scintillometer prospecting traverses, geological mapping, airborne and ground geophysics, and drilling, have documented several uraniferous outcrops with scintillometer readings of up to 10 000 counts per second, and uraniferous boulders and boulder trains with radioactivity up to two orders of magnitude higher than the background. Near the Alberta-Saskatchewan border, uraniferous boulders show geochemical characteristics consistent with a Saskatchewan source, whereas to the west boulders have a distinct geochemical signal suggesting a local source in Alberta.

Locations of Uraniferous Boulders, Outcrops and Pits along the North Shore of Lake Athabasca, NTS 74L,M (GIS data, point features)


Year: 1989

Abstract:
Locations of uraniferous boulder-fields and uraniferous swamps extracted from industry assessment reports are useful metallogenetic indicators for uranium exploration within and around the Athabasca Basin. They are used as pathfinders to uranium occurrences and prospects. These locations along the northern rim of the Athabasca Basin in Alberta have been compiled in GIS format and delivered as a point shapefile. In Alberta, the northern rim of the Athabasca Basin and the regolith underlying the Athabasca unconformity are locally exposed along the northern shore of Lake Athabasca. Extensive uranium exploration work in the 1970s, including scintillometer prospecting traverses, geological mapping, airborne and ground geophysics, and drilling, have documented several uraniferous outcrops with scintillometer readings of up to 10 000 counts per second, and uraniferous boulders and boulder trains with radioactivity up to two orders of magnitude higher than the background. Near the Alberta-Saskatchewan border, uraniferous boulders show geochemical characteristics consistent with a Saskatchewan source, whereas to the west boulders have a distinct geochemical signal suggesting a local source in Alberta.

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.

Lower Athabasca Region groundwater management framework: Supporting document for the Cold Lake - Beaver River (CLBR) area


Year: 2013

Abstract:
The Groundwater Management Framework outlines a strategy for monitoring, evaluation and reporting, sets early warning triggers to indicate changes in groundwater conditions, and identifies management actions that may be taken when such changes are observed.

Lower Athabasca Region groundwater management framework: Supporting document for the South Athabasca Oil Sands (SAOS) area


Year: 2013

Abstract:
This Supporting Document provides summary information about the geology and hydrogeology of the SAOS area, providing a basis for understanding groundwater conditions.

Mammal and bird names in the Indian languages of the Lake Athabasca region


Author(s): Hohn, E. O.

Year: 1973

Abstract:
This article talks about the traditional land area of the Athapaskan speaking Natives (Beaver Indians, Slave Indians, Chipewyans, and Eskimos) and the Algonkian speakers (Cree, and Blackfoot) north, south, east and west of the Lake Athabasca area. Hohn briefly discusses the cultural variation between the Chipewyans and the Crees who currently occupy this area. Although not complete, this article provides a list of the mammal and bird species names and meanings, located in the Lake Athabasca area. This list is provided in the English, Cree, and Chipewyan languages. The author also provides a helpful guide to the pronunciation of these words. Hohn interestingly points out some apparent linguistic connections between some species names. The Cree names were provided by Henry Powder, a long-time resident of Camsell Portage, Saskatchewan (originally from Lac la Biche, Alberta); Solomon Cardinal of Fort Chipewyan, Alberta; and Mrs. A. Anderson of Edmonton (originally from the nearby Calahoo Indian Reserve.) The Chipewyan names were obtained in part from Fr. F. Marcel, former chief of the Chipewyan band at Fort Chipewyan; and George Norm, an elderly Chipewyan or Métis who resides in Little Buffalo River on Great Slave Lake, Northwest Territories. This lends further authenticity to the study.

Mammalian toxicity of naphthenic acids derived from the Athabasca oil sands


Author(s): Rogers, V. V.

Year: 2003

Abstract:
Naphthenic acids are a diverse group of saturated mono- and polycyclic carboxylic acids that are natural constituents of petroleum. These compounds are a major contributor to petroleum's acidic nature and can account for as much as 4% of crude petroleum by weight. At the Athabasca oil sands (AOS) located in northeastern Alberta, Canada, naphthenic acids have received considerable attention. The AOS represent the world's largest, single petroleum deposit, where the petroleum is in the form of bitumen. Extracting bitumen from AOS is a complex process, requiring the mixing of oil sands with hot,alkaline (pH = 8.0) water to separate the bitumen from sand and other waste products. This process produces an immense volume of aqueous tailings, about 7.5 m 3 for each m3 of synthetic crude petroleum produced. Nearly one billion cubic meters of aqueous tailings will have amassed in large holding ponds near the mine sites by 2025, and will be incorporated into the ecosystem under wet and dry landscape reclamation strategies. Another consequence of the extraction process is that naphthenic acids (pKa ≅ 5) become solubilized and concentrated (90--110 mg/L) in aqueous tailings. Numerous studies have investigated the aquatic toxicity of naphthenic acids, demonstrating them to be highly toxic to invertebrates and fish at concentrations well below those found in AOS tailings. In contrast, information about the mammalian toxicity of naphthenic acids is limited, particularly the effects of repeated, oral exposure. In the current research, naphthenic acids were isolated from tailings obtained from Mildred Lake settling basin, the main tailings pond of Syncrude Canada Ltd, and used in mammalian toxicity testing. An acidification/solvent extraction procedure was used, followed by ultrafiltration to isolate the naphthenic acids. These were chemically analysed, revealing a highly heterogenous mixture of acyclic and 1-, 2-, 3-, and 4-ringed compounds. Acute testing using Wistar rats demonstrated significant (P < 0.05) behavioural and histopathological effects in both sexes at a single dosage of 300 mg/kg body weight of napthenic acids. This dosage is 50 times higher than the estimated worst-case, single day environmental exposure through drinking water for small mammals in the wild. Effects included temporary suppression of appetite, and pericholangitis, a biliary inflammatory response. Subchronic dosing, involving administration of naphthenic acids to females over a 90 d period, indicated that 60 mg/kg/d was sufficient to elicit significant (P < 0.05), toxic effects.

Mapping how we use our land: Using participatory action research


Year: 1994

Abstract:
The study area of the traditional land use and occupancy study profiled in this booklet is broadly speaking northeast Alberta, south of the Clearwater River, west of the Alberta/Saskatchewan border, north of the Cold Lake air weapons range and east of the Athabasca River. In this region Athapaskan, Cree, and Métis people have mixed with Euro-Canadians engaged in the fur trade since the arrival of Peter Pond in 1780. The area generally opened up to settlement with steamboats on the Athabasca, the Alberta and Great Waterways Railway and the impetus created by World War II to construct roads into the region. By the 1950s the industrial economy was becoming more and more established and Aboriginal participation in wage work began to increase. Through the 1960s and 1970s with the establishment of new tar sands plants with state of the art technology, Fort McMurray became a Canadian boom town, and there was less and less incentive for Aboriginal people to maintain a full-time presence in the bush economy. Trapping, hunting, fishing and gathering became part-time activities for most, and thousands of outsiders also began to hunt and fish in the Aboriginal homelands with the assistance of seismic access roads, four-wheel-drive vehicles and float planes. Life for regional residents continues to change at a fast pace as the Alberta-Pacific pulp mill comes on stream and tar sands projects are expanded. These factors provided the incentive for the Athabasca Native Development Corporation to undertake the traditional land use and occupancy study described in this booklet.

Marital Status, Alberta Economic Regions


Year: 2009

Abstract:
This Alberta Official Statistic describes the marital status of Alberta’s census families by economic regions for the 2011 census year. Alberta is divided into eight economic regions as follows: Lethbridge – Medicine -Hat; Camrose-Drumheller; Calgary; Banff – Jasper – Rocky Mountain House; Red Deer; Edmonton; Athabasca – Grande Prairie – Peace River; and Wood Buffalo – Cold Lake. This Alberta Official Statistic describes the marital status of Albertans by these economic regions based on the 2011 population census. The graph describes six marital statuses categorized as ’married (and not separated)’, ‘living common-law’, ‘single (never legally married)’, ‘separated’, ‘divorced’ and ‘widowed’.

Mature fine tailings from oil sands processing harbour diverse methanogenic communities


Author(s): Penner, T. J., & Foght J. M.

Year: 2010

Abstract:
Processing oil sands to extract bitumen produces large volumes of a tailings slurry comprising water, silt, clays, unrecovered bitumen, and residual solvent used in the extraction process. Tailings are deposited into large settling basins, where the solids settle by gravity to become denser mature fine tailings (MFT). A substantial flux of methane, currently estimated at ~40 million L/day, is being emitted from the Mildred Lake Settling Basin. To better understand the biogenesis of this greenhouse gas, the methanogenic consortia in MFT samples from depth profiles in 2 tailings deposits (Mildred Lake Settling Basin and West In-Pit) were analyzed by constructing clone libraries of amplified archaeal and bacterial 16S rRNA genes. The archaeal sequences, whose closest matches were almost exclusively cultivated methanogens, were com- parable within and between basins and were predominantly (87% of clones) affiliated with acetoclastic Methanosaeta spp. In contrast, bacterial clone libraries were unexpectedly diverse, with the majority (~55%) of sequences related to Proteo- bacteria, including some presumptive nitrate-, iron-, or sulfate-reducing, hydrocarbon-degrading genera (e.g., Thauera, Rhodoferax, and Desulfatibacillum). Thus, MFT harbour a diverse community of prokaryotes presumptively responsible for producing methane from substrates indigenous to the MFT. These findings contribute to our understanding of biogenic methane production and densification of MFT in oil sands tailings deposits.

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.

Mercury trends in colonial waterbird eggs downstream of the oil sands region of Alberta Canada


Year: 2013

Abstract:
Mercury levels were measured in colonial waterbird eggs collected from two sites in northern Alberta and one site in southern Alberta, Canada. Northern sites in the Peace-Athabasca Delta and Lake Athabasca were located in receiving waters of the Athabasca River which drains the oil sands industrial region north of Fort McMurray, Alberta. Temporal trends in egg mercury (Hg) levels were assessed as were egg stable nitrogen isotope values as an indicator of dietary change. In northern Alberta, California and Ring-billed Gulls exhibited statistically significant increases in egg Hg concentrations in 2012 compared to data from the earliest year of sampling. Hg levels in Caspian and Common Tern eggs showed a nonstatistically significant increase. In southern Alberta, Hg concentrations in California Gull eggs declined significantly through time. Bird dietary change was not responsible for any of these trends. Neither were egg Hg trends related to recent forest fires. Differences in egg Hg temporal trends between northern and southern Alberta combined with greater Hg levels in eggs from northern Alberta identified the likely importance of local Hg sources in regulating regional Hg trends. Hg concentrations in gull and Common Tern eggs were generally below generic thresholds associated with toxic effects in birds. However, in 2012, Hg levels in the majority of Caspian Tern eggs exceeded the lower toxicity threshold. Increasing Hg levels in eggs of multiple species nesting downstream of the oil sands region of northern Alberta warrant continued monitoring and research to further evaluate Hg trends and to conclusively identify sources.

Metals and polycyclic aromatic hydrocarbons in colonial waterbird eggs from Lake Athabasca and the Peace-Athabasca Delta Canada


Year: 2011

Abstract:
In 2009, aquatic bird eggs from a variety of species were collected from three sites in northern Alberta, Canada. Two sites were located in receiving waters of the Athabasca River, which drains the oil sands industrial region north of Fort McMurray, Alberta. The third site, located on the Peace River, was remote from the influence of the Athabasca River. Levels of mercury, arsenic, and polycyclic aromatic hydrocarbons (PAHs) were measured in the eggs along with nitrogen stable isotopes (δ¹⁵N) as an indicator of bird trophic position. Levels of As and PAHs in eggs were low, whereas Hg was measureable in all samples. Egg Hg levels increased with δ¹⁵N values (a proxy of food web trophic position); however, some eggs exhibited Hg levels greater than expected based on trophic position. These eggs were from sites in receiving waters of the Athabasca River, namely, Mamawi Lake and Egg Island. Levels of Hg in egg pools were correlated with naphthalene levels, perhaps indicating a common source of contamination. Temporal comparison of Hg levels in California gull (Larus californicus) eggs from the Lake Athabasca colony indicated that egg Hg burdens increased 40% from 1977 to 2009. More research is required to evaluate temporal trends in levels of environmental contaminants and to identify sources.

Mineralogy and geochemistry of a Precambrian regolith in the Athabasca Basin


Author(s): Macdonald, C. C.

Year: 1980

Abstract:
The regolith beneath the Helikian Athabasca Group sandstones in northern Saskatchewan displays up to four laterally correlatable colour zones. Their sequence, vertical extent, and chemical and mineralogical characteristics correspond closely to those of recent lateritic profiles formed in subtropical to tropical climates. Under these conditions, abundant rainfall on an unvegetated Precambrian surface would likely have resulted in rapid erosional losses from the upper hematite zone (equivalent to a modern laterite horizon), preventing the high residual concentrations of Fe and A1 characteristic of modern laterites. Post-weathering alteration from Athabasca diagenetic solutions was restricted to a relatively thin bleached zone adjacent to the unconformity. However, the pressure-temperature conditions accompanying burial caused recrystallization of illites, transformation of Mg-smectite to Mg-dioctahedral chlorite, and the possible dehydration of goethite to hematite within the pre-existing weathering profile. The presence of an oxidized upper horizon in the pre-1500 m.y. regolith is consistent with previous estimates of 1700-2000 m.y. for the beginning of an oxidizing atmosphere. Comparison with other published descriptions of Precambrian weathering shows a much closer similarity to the late Precambrian profiles than to those formed in a reducing early Precambrian environment. Within the study area, large-scale depletions of the trace elements associated with uranium mineralization have not occurred from the regolith, supporting the hypothesis that diagenetic leaching of detrital heavy minerals in the Athabasca sediments provided the main source of these elements for ore deposition. Since the bleaching alteration at the unconformity appears to be the regional equivalent of alteration observed in the ore deposits, both the extent and the trace element geochemistry of the bleached zone have potential use as exploration tools. Based on the weathering environment deduced from the study profiles, an alternative explanation for the composition of the Athabasca Group sediments can be proposed. If the tropical conditions present during weathering continued through the time of deposition, erosion of the lateritic source material would have generated a detrital assemblage of quartz, kaolinite, illite, and iron oxides - the present constituents of most of the Athabasca sediments. Thus the clay and iron oxide in the sandstone can be more simply explained by deposition of this lateritic detritus than by diagenetic alteration of detrital primary silicates produced by physical weathering in an arid climate. The role of diagenesis in the tropical model would be a much lesser one, consisting of textural and crystallinity modifications to the detrital secondary minerals. **There was no page 91 in the original thesis**

Modelling catchment response to acid deposition: A regional dual application of the MAGIC model to soils and lakes in the Athabasca oil sands region, Alberta


Year: 2010

Abstract:
The effects-based acid emissions management framework (EMF) for determining the need for emission control policies in the Athabasca Oil Sands Region, Canada is dependent on model simulations of future soil and surface water chemistry. An approach for regional application of the Model of Acidification of Groundwater in Catchments (MAGIC) was developed that addresses the differential sensitivity of forest soils and lakes. The approach used was a dual application wherein a plot-scale calibration to forest soils and a catchment-based calibration to lake chemistry were used to account for poorly understood hydrologic connections between uplands and lakes, key processes including sulphur (S) and nitrogen (N) retention as well as groundwater sources of base cations to the lakes. The regional application was carried out at 50 lake catchments currently monitored for response to acid deposition. Simulated forest soil chemistry (modelled at 28 catchments) exhibited small changes in base saturation under future conditions of elevated acid deposition, while in general molar BC:Al exhibited considerable change but remained well above critical chemical limits used to protect acid-sensitive forest soils. Similarly, simulations of charge balance acid neutralizing capacity (ANCCB) for the lakes suggested very small decreases since industrialization, and forecast projections under acid deposition double the current level suggested that only one lake will reach the critical threshold for ANCCB (75 μeq L–1) specified by the EMF. There is limited potential for acidification impacts at the study sites.

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.

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.

Net percolation as a function of topographic variation in a reclamation cover over a saline-sodic overburden dump


Author(s): Hilderman, J. N.

Year: 2011

Abstract:
Surface mining of oil sands in northern Alberta requires stripping of saline-sodic shale overburden, which is typically placed in large upland overburden dumps. Due to the chemical nature of this shale, engineered soil covers must be constructed over the shale to support the growth of forest vegetation. A research site on South Bison Hill (SBH), a shale overburden dump at the Syncrude Canada Ltd. Mildred Lake Mine, has been used by researchers over the past decade to study the performance of a reclamation cover. This study was undertaken to improve the understanding of salt and moisture dynamics in the cover-shale system. In particular, the objective of this study was to develop an estimate of the net percolation rate through the cover soil and into the shale overburden. Stable isotope (δ2H and δ18O) measurements obtained from the pore water of soil samples were used to develop stable isotope profiles at various sampling locations along the slope and plateau of the SBH. Simulated profiles were then generated using 2D, finite element numerical modelling software and compared to the measured profiles. Model parameters were obtained from testing and the work of previous researchers. The model results revealed that the net percolation is greatest (32-50 mm/yr) for the plateau and mid-slope bench sample locations. Net percolation rates for sample locations on the slope were lower at 0-12 mm/yr. The results from the stable isotope modelling were utilized in a SO42- transport model to ascertain if calculated net percolation rates could explain measured salinity profiles. This modelling exercise revealed that calculated SO42- profiles are highly dependent on the assumed SO42- production rates in the shale, which is primarily attributed to pyrite oxidation. The model results showed the isotope-based net percolation rates could explain the measured SO42-profiles for a reasonable range SO42- production rates. The SO42- production rates calculated in the model were greatest for the plateau and mid- slope bench locations and lesser for the sloped locations. The model also showed that the mass of SO42- removed by interflow was minimal compared to the mass generated by pyrite oxidation and that net percolation is the dominant flushing mechanism at net percolation rates of 8 mm/yr or more.

North of Athabasca: Slave Lake and Mackenzie River documents of the North West Company, 1800-1821


Year: 2001

Citation:
[Anonymous] (2001).  North of Athabasca: Slave Lake and Mackenzie River documents of the North West Company, 1800-1821. Slave Lake and Mackenzie River documents of the North West Company, 1800-1821., Canadian publishers collection. 1-504.

Nutrient enrichment in the Peace Athabasca and Slave River: Assessment of present conditions and future trends


Author(s): Chambers, P. A.

Year: 1996

Abstract:
The aim of this report was to address the Northern River Basins Study (NRBS) question: “Are the substances added to the rivers by natural and manmade discharges likely to cause deterioration of the water quality?” In this report, the word “substances” was taken to mean nutrients or, more specifically, nitrogen and phosphorus. Other NRBS reports have addressed the impact of effluent loading from the perspective of contaminants. This report synthesizes results from research and monitoring studies undertaken as part of the NRBS to characterize nutrient loading from all point and diffuse sources in the Northern River basins, evaluate the impacts of nutrient loading on river chemistry, assess the response of riverine biota to nutrient loading from pulp mill and municipal effluents in situ, quantify nutrient responses of benthic biota, and investigate interactions between nutrients and contaminants in pulp mill effluent on food webs. These findings are used to assess the state of aquatic ecosystem health, and develop scientific and management recommendations for the Northern River basins. During fall, winter and spring, elevated nitrogen and phosphorus concentrations were observed on the Athabasca River downstream of Jasper, Hinton, Whitecourt and Fort McMurray and on the Wapiti River downstream of Grande Prairie. In the Athabasca River, 20% of all TP samples and 2% of all TN samples exceeded the Alberta Surface Water Quality Objective of 0.05 mg/L TP as P and 1.0 mg/L TN as N. Most of these exceedances occurred during summer and were likely due to high particulate concentrations. In the Wapiti River, 74% of TP samples and 19% of TN samples collected near the mouth exceeded the Alberta Surface Water Quality Objectives compared with exceedances of only 12% for TP and 0% for TN upstream of Grande Prairie. This suggests that nutrients from the City of Grande Prairie and Weyerhaeuser of Canada Ltd. effluents contribute to non-compliance. Annually, continuously-discharging industrial and municipal sources contribute 4 to 10% of the TN load and 6 to 16% of the TP load in the Athabasca River, with the contribution being higher during winter. Likewise, continuously- discharging industrial and municipal sources contribute 20% of the TN and 22% of the TP load in the Wapiti River annually. For the Peace River mainstem there is no evidence of nutrient impacts and the same is likely, true for the Slave River, although there are only limited nutrient data for this river. Elevated nutrient concentrations in the Athabasca and Wapiti rivers have increased periphyton biomass and benthic invertebrate densities and, for the Athabasca River downstream of Hinton, increased the length and body weight of spoonhead sculpin (Cottus ricei), a small insectivorous fish species. Enrichment studies conducted with nutrient diffusing substrata in fall 1994 showed that periphyton growth was nutrient saturated for at least 2.5-4 km downstream of Jasper, from downstream of Hinton to upstream of Whitecourt, for at least 3 km and possibly up to 48 km downstream of Fort McMurray, and for at least 2 km downstream of the Grande Prairie bleached kraft pulp mill. Phosphorus concentrations at sites immediately upstream of the outfalls to these nutrient-saturated reaches were usually < 2 g/L SRP in the Athabasca River and 4-6 g/L SRP in the Wapiti River. These concentrations are similar to the 2-5 g/L SRP that was determined to be the concentration above which the growth of individual cells and thin periphyton films in artificial streams are phosphorus saturated. Periphyton growth was nitrogen limited from downstream of the Alberta Newsprint Co. to the confluence of Lesser Slave River and in the Smoky River. The increase in periphyton biomass and benthic invertebrate densities downstream of effluent outfalls and, in the case of the benthic invertebrates, no loss of species suggests that the response to effluents is one of nutrient enrichment not toxicity. Studies conducted in artificial streams further showed that periphyton biomass and growth of several mayflies, stoneflies and caddisflies increased in response to nutrient or 1% effluent addition, with no significant difference between the two treatments. These results further verify that the response to the current level of effluent loading is one of nutrient enrichment. There is no evidence of adverse effects to the ecosystem (e.g., no benthic invertebrate species loss, no problems with dissolved oxygen levels that are directly caused by nutrient addition). While detailed investigations of spawning grounds and early rearing habitat for fish in the Northern Rivers were not undertaken, it does appear not that dissolved oxygen problems caused by nutrient addition are adversely affecting fish populations at present. The concern with nutrient addition to the Athabasca and Wapiti rivers appears, at present, to be largely one of aesthetics as perceived by increased periphyton growth. Aesthetic criteria for the protection of water bodies are often site specific and developed in consensus with the users of the lake or river. In the absence of any detectable deleterious effects of nutrient loading on the Athabasca and Wapiti rivers, the users must determine whether the increase in periphyton growth downstream of outfalls is acceptable or unacceptable. Given our current state of knowledge, setting effluent permit limits for phosphorus to control periphyton biomass at a specific level is not possible since there is as yet no quantitative relationship between river phosphorus concentrations and periphyton biomass for a given site. For example, periphyton biomass 1 km downstream of Hinton was found to range from 25 to 242 mg chlo/m2 for October 1990, 1992, 1993 and 1994 despite relatively constant TP loads from Weldwood of Canada Ltd. and relatively constant river flows (111, 134, 97 and 118 m3/s for October 1990, 1992, 1993 and 1994, respectively). Yet despite the lack of site-specific quantitative relationships between periphyton biomass and phosphorus concentration, experiments and in situ observations undertaken by the NRBS and other agencies have clearly shown that phosphorus (and, in some locations, nitrogen) are controlling factors for periphyton abundance in the Athabasca, Wapiti and Smoky rivers. Based on findings from studies reviewed in this synthesis report, the following key recommendations are proposed: • regular monitoring and reporting of nutrients from sewage treatment plants. This should be a license requirement. In addition, provision is needed for ensuring compliance with sampling and analytical procedures for all licensed dischargers (industrial and municipal) and to ensure training of certified operators to measure (and record) flow rates and discharge volumes and for enforcement of reporting requirements. Standard reporting requirements for water quality parameters should be established and reporting proper data should be a license requirement.

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