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Relationships between lake water chemistry and benthic macroinvertebrates in the Athabasca oil sands region, Alberta


Year: 2010

Abstract:
Sulphur and nitrogen emissions in the Athabasca Oil Sands Region (AOSR) are a threat to regional lentic ecosystems. Benthic macroinvertebrates have been used successfully elsewhere to monitor the impacts of acid emissions on water bodies and the opportunity exists to implement a regional lentic biomonitoring program in the AOSR. Metrics are often used to assess the impacts of anthropogenic stressors because they describe biological conditions through a variety of measures. The selection of appropriate metrics is an integral component of any biomonitoring program and it depends on the in situ relationships between water chemistry and benthic macroinvertebrates. In order to establish these relationships we compared lake water chemistry parameters with benthic macroinvertebrate communities and metric scores from 32 lakes in the AOSR through Redundancy Analyses. Lake acidity correlates positively with Hyallelidae and negatively with Chironomidae and Oligochaeta while dissolved organic carbon is also an important determinant of benthic macroinvertebrate community composition. A number of metrics were strongly correlated with lake acidity and the following compositional metrics proved to be the most suitable for monitoring acidification in the AOSR: % Diptera, % Oligochaeta, % EPT, Total Ephemeroptera and Total Trichoptera.

Reply to D. L. Peters' Comment on "Streamflow input to Lake Athabasca, Canada" by Rasouli et al. (2013)


Year: 2015

Abstract:
This paper provides a reply to a comment from Peters (2014) on our recent effort focused on evaluating changes in streamflow input to Lake Athabasca, Canada. Lake Athabasca experienced a 21.2% decline in streamflow input between 1960 and 2010 that has led to a marked decline in its water levels in recent decades. A reassessment of trends in naturalized Lake Athabasca water levels shows insignificant changes from our previous findings reported in Rasouli et al. (2013), and hence our previous conclusions remain unchanged. The reply closes with recommendations for future research to minimize uncertainties in historical assessments of trends in Lake Athabasca water levels and to better project its future water levels driven by climate change and anthropogenic activities in the Athabasca Lake basin.

Report on Lake Athabasca walleye samples for use in the validation of the walleye evaluation criteria


Author(s): Franzin, W. G.

Year: 2011

Abstract:
This document is a summary report on the length, weight data and otoliths for aging of 200 Walleye taken in the June 2011 Fort Chipewyan commercial fishery.

Report on movement and habitat use of fishes in the lower Athabasca River from 2008 -2009


Year: 2009

Abstract:
The objectives of this study were to monitor movements and determine fall and winter habitat use for key target fish species including flathead chub, burbot, lake whitefish and longnose sucker, and collect supplemental information of the location of burbot and lake whitefish spawning and egg incubation areas in the Lower Athabasca River.

Resource management in Wood Buffalo National Park: striving for cooperation


Author(s): Pye, C. D.

Year: 1998

Abstract:
"As efforts to conserve natural resources grow in scope and prominence, it becomes increasingly important to examine resource use and resource users, particularly within the confines of protected areas. The least-known group of resource users are aboriginal hunters. This study provides information on the traditional ecological knowledge, land use and hunting strategies, as well as the harvest of moose by a community of Cree hunters located in Wood Buffalo National Park. This information is used to determine whether cooperative management is an appropriate strategy for both Wood Buffalo National Park and the resource users, the Little Red River Cree; allowing for sustainable use of the resource while respecting constitutional law. The research revealed that cooperative management is an achievable goal within Wood Buffalo National Park, but that much work must be done to ensure that a legally binding agreement will benefit both parties as well as the environment.

Response of confined aquatic biota to mine depressurization water in Beaver Creek Reservoir


Year: 1980

Abstract:
Beaver Creek Reservoir was formed as a result of diverting the natural flow of Beaver Creek away from mine and plant areas and southward to the Athabasca River via Poplar Creek. The diversion was initiated in the fall of 1975 with the closure of the Beaver Creek Dam; filling of the reservoir was completed in the spring of 1976. When it became necessary to remove mine depressurization water from the mining area, Syncrude was granted permission by the Government of Alberta to discharge this effluent into Beaver Creek Reservoir, on the condition that chloride levels in water entering Poplar Creek did not exceed 400 mg/L above ambient levels. The present study was designed to investigate the survival of selected organisms in Beaver Creek Reservoir during 1979. The primary objective was to determine the response of selected species of aquatic biota to saline mine depressurization water after average dilution in the Beaver Creek Reservoir. More specific requirements of the study were: a) the study was to be carried out entirely within the Beaver Creek Reservoir using test organisms held in situ; b) the study must include three sampling locations and three replicates of each test organism at each station; c) test organisms must include: periphyton (on artificial substrates), native species of fish (white sucker and fathead minnow), and native species of invertebrates (either Gammarus or Hyalella); and d) field studies were to be conducted between June and October, 1979 and were to examine both short and long term effects.

Response of Sphagnum fuscum to nitrogen deposition: A case study of ombrogenous peatlands in Alberta, Canada


Year: 2003

Abstract:
Peatlands cover about 30% of northeastern Alberta and are ecosystems that are sensitive to nitrogen deposition. In polluted areas of the UK, high atmospheric N deposition (as a component of acid deposition) has been considered among the causes of Sphagnum decline in bogs (ombrogenous peatlands). In relatively unpolluted areas of western Canada and northern Sweden, short-term experimental studies have shown that Sphagnum responds quickly to nutrient loading, with uptake and retention of nitrogen and increased production. Here we examine the response of Sphagnum fuscum to enhanced nitrogen deposition generated during 34 years of oil sands mining through the determination of net primary production (NPP) and nitrogen concentrations in the upper peat column. We chose six continental bogs receiving differing atmospheric nitrogen loads (modeled using a CALPUFF 2D dispersion model). Sphagnum fuscum net primary production (NPP) at the high deposition site (Steepbank-mean of 600 g/m2; median of 486 g/m2) was over three times as high than at five other sites with lower N deposition. Additionally, production of S. fuscum may be influenced to some extent by distance of the moss surface from the water table. Across all sites, peat nitrogen concentrations are highest at the surface, decreasing in the top 3 cm with no significant change with increasing depth. We conclude that elevated N deposition at the Steepbank site has enhanced Sphagnum production. Increased N concentrations are evident only in the top 1-cm of the peat profile. Thus, 34 years after mine startup, increased N-deposition has increased net primary production of Sphagnum fuscum without causing elevated levels of nitrogen in the organic matter profile. A response to N-stress for Sphagnum fuscum is proposed at 14-34 kg ha-1 yr-1. A review of N-deposition values reveals a critical N-deposition value of between 14.8 and 15.7 kg ha-1 yr-1 for NPP of Sphagnum species.

Review and compilation of surface water research and reports for selected waterbodies in the Municipal District of Wood Buffalo


Year: 2002

Abstract:
Dillon Consulting was retained by the Water Working Group (WWG), under the auspices of the Cumulative Environmental Management Association (CEMA) to complete a literature review, assessment, and synopsis of existing surface water research and reports for selected water bodies in the Municipal District of Wood Buffalo. The report was not intended to provide a detailed statistical analysis of existing data.

Review of reclamation options for oil sands tailings substrates


Year: 2010

Abstract:
BGC Engineering Inc. (BGC) conducted a scoping study of the state of knowledge related to technologies for reclaiming oil sands tailings substrates to upland boreal forests and wetlands for the Oil Sands Research and Information Network (OSRIN). The objective of the scoping study is to help establish an understanding of the status of fine tailings reclamation technology in the Athabasca Oil Sands Region (AOSR). Relevant research was compiled from peer reviewed and non-peer reviewed sources including journals, conference proceedings, magazine articles, internal and consultant reports. Industry researchers and academics were contacted for their information. Until recently, a wet landscape scenario, in which mature fine tailings (MFT) would be stored in pits and capped with a layer of freshwater to form an artificial lake, was the most likely reclamation option for MFT. In this scenario, pit lakes (PL), or end-pit lakes (EPL) are designed to remediate process-affected waters from tailings landforms through bioremediation and dilution. As an alternative to water-capping, much of the current research has focused on reclamation technologies that would result in a dry landscape. Reclamation of fine tailings using a dry landscape scenario first requires stabilization of the deposit to allow access for heavy machinery (trafficability). Soil cover designs and revegetation prescriptions are used to reclaim the tailings substrate to an equivalent land capability or ecosystem function. Wetland design and upland forest reclamation are active areas of research in fine tailings reclamation, including the potential impacts of increased salinity on plant species selection, germination and growth.

Risking rupture: Integral accidents and in/security in Canada's bitumen sands


Author(s): Greaves, W.

Year: 2013

Abstract:
The expansion of unconventional hydrocarbon development in Western Canada is one of the most contentious issues in contemporary Canadian politics. Although widely studied, little attention has been paid to the framing of Alberta's bitumen sands within distinct and incompatible discourses of energy and environmental security. This essay examines these discourses using the tools of securitization analysis, asking the basic questions of what each presents as needing to be secured, from what, and by what means. Presented with two sets of socially constructed in/ security claims related to the bitumen sands and proposed pipeline expansion, the author suggests the social theory of Paul Virilio provides a useful intervention into securitization analysis that allows the material implications of these discourses to be clarified and assessed. Drawing upon Virilio's critical account of technological progress and his theory of accidents, this essay proposes that conventional accounts of "energy security" in the bitumen sands cannot result in meaningful conditions of security because they remain premised upon continued and expanded hydrocarbon consumption in an era of anthropogenic climate change.

Rock Lake - Solomon Creek Wildland Park


Year: 2001

Abstract:
Rock Lake-Solomon Creek Wildland Park is located northwest of Hinton and extends from the Athabasca River in the south to Rock Lake Provincial Recreation Area (PRA) and Willmore Wilderness to the northwest. You can reach the south end of the park along Solomon Creek by taking the road to the hamlet of Brule. The access to Rock Lake PRA is 70 kilometres north of Hinton. A 32 km graveled road leaves Highway 40 and winds along a route used by the petroleum and forest industries. Use caution when traveling this road and be aware that the road is not regularly maintained.

Root distribution activity and development for boreal species on reclaimed oil sand mine soils in Alberta Canada


Author(s): Lazorko, H. M.

Year: 2008

Abstract:
Alberta’s oil sands are located in the boreal forest where surface mining disturbs huge tracts of land. One such area, Syncrude Canada Ltd.’s Mildred Lake mine, contains waste overburden (OB) piles which can be saline and sodic (SSOB). The objectives of this research were to 1) determine SSOB material impacts on planted tree root distributions, 2) quantify root activity to identify plant species growing at depth, and 3) document coarse woody root structure for planted trees. Root distributions for three mixedwood stands on reclaimed OB in relation to electrical conductivity (EC) and sodium absorption ratio (SAR) were examined using soil cores. Root distributions followed a similar pattern with soil depth as those from undisturbed boreal forest stands and appeared unaffected by the SSOB at this stage; however, future monitoring will be required as the stands mature. Root activity was assessed for jack pine (jP) and white spruce (wS) stands on tailings sand (TS) and OB using a strontium (Sr) chloride tracer. Understory and tree foliage was collected prior to and after application to measure Sr concentration in the control, broadcast, and depth treatments. A small proportion of roots grew in the OB material regardless of its chemical properties. Results from the Sr tracer study suggested that these roots were probably from the clover, sow thistle, and grasses. Planted trees showed little to no change in Sr tissue content suggesting that there were little to no roots in the treatment zones, the understory species out-competed the trees for Sr accessibility, or the tracer was diluted in the tree biomass to undetectable levels. Root systems of planted jP trees older than 10 years and older than 20 years on TS and OB were excavated and the number and diameter of lateral roots, the degree of kinking and coiling, and the presence of a taproot were recorded. Excavated trees showed poor taproot development on 70% of the trees and numerous root deformities, suggesting that more emphasis is needed in correct planting techniques and good planting stock to ensure proper root development. Roots are critical components of boreal forest ecosystems; without healthy root systems productivity may decline, stands may be susceptible to windthrow, and general forest health may suffer.

Sand land


Author(s): Mark, A.

Year: 2009

Citation:
Mark, A. (2009).  Sand land. Spring, 48-61.

Segmentation analysis and bathymetric surveys of the Athabasca River - Segment 1


Year: 2008

Abstract:
This report provides a review available literature and data sources to determine segment boundaries within the Peace-Athabasca Delta (PAD) for the Athabasca River Delta channels. To support the segmentation analysis, and to determine the overwintering habitat potential within the major Delta channels, mapping grade bathymetric data were collected for several critical sites identified by the Instream Flow Needs Technical Task Group including: the Embarras River; Embarras River breakthrough channel to Mamawi Creek ( may also be known as Cree Creek); Mamawi Creek; Jackfish Creek (conveys Athabasca River water into Richardson Lake during flow reversals); Richardson River (conveys Athabasca River water during flow reversals); Fletcher Channel; Goose Island Channel; Big Point Channel; and, the area known as Big Eddy. The report contains a description of the field survey as well as its results.

Sensitivity to acidification of forest soils in two watersheds with contrasting hydrological regimes in the oil sands region of Alberta


Year: 2007

Abstract:
Input of large amounts of N and S compounds into forest ecosystems through atmospheric deposition is a significant risk for soil acidification in the oil sands region of Alberta. We evaluated the sensitivity of forest soils to acidification in two watersheds (Lake 287 and Lake 185) with contrasting hydrological regimes as a part of a larger project assessing the role of N and S cycling in soil acidification in forest ecosystems. Fifty six forest soil samples were collected from the two watersheds by horizon from 10 monitoring plots dominated by either jack pine (Pinus banksiana) or aspen (Populus tremuloides). Soils in the two watersheds were extremely to moderately acidic with pH (CaCl2) ranging from 2.83 to 4.91. Soil acid-base chemistry variables such as pH, base saturation, Al saturation, and acid-buffering capacity measured using the acetic acid equilibrium procedure indicated that soils in Lake 287 were more acidified than those in Lake 185. Acid-buffering capacity decreased in the order of forest floor > subsurface mineral soil > surface mineral soil. The most dramatic differences in percent Ca and Al saturations between the two watersheds were found in the surface mineral soil horizon. Percent Ca and Al saturation in the surface mineral soil in Lake 287 were 15% and 70%, respectively; the percent Ca saturation value fell within a critical range proposed in the literature that indicates soil acidification. Our results suggest that the soils in the two watersheds have low acid buffering capacity and would be sensitive to increased acidic deposition in the region.

Shortjaw Cisco species at risk assessment 2001


Author(s): Steinhilber, M.

Year: 2004

Abstract:
the shortjaw cisco is considered "threatened" in Canada and has been approved for listing in "threatened" in Alberta. The Alberta designation is based on the restricted redistribution in this species in the province and its isolation from other populations. To date, it has been verified at only one locality - Barry Lake in the Canadian Shield region north of Lake Athabasca - although unconfirmed reports have also come from Lake Athabasca, Gregoire Lake, and Cold lake. The main objective of the work undertaken in 2001 was to search for other populations of shortjaw cisco in the province. Additional distribution data would assist in assessing the status of this species by providing 1) updated distirbution data, 2) a search effort context in which to evaluate the number of reported element occurrences, and 3) a baseline for evaluation of future distribution trends. Previous work on the shortjaw cisco in Barrow Lake determined that this population appears stable and is under little immediate threat.

Citation:

Soil ingestion rate determination in a rural population of Alberta, Canada practicing a wilderness lifestyle


Year: 2014

Abstract:
The inadvertent ingestion of contaminated soil can be a major pathway for chemical exposure to humans. Few studies to date have quantified soil ingestion rates to develop exposure estimates for human health risk assessments (HHRA), and almost all of those were for children in suburban/urban environments. Here we employed a quantitative mass balance tracer approach on a rural population practicing outdoor activities to estimate inadvertent soil ingestion. This study followed 9 subjects over a 13 day period in Cold Lake, Alberta, near the largest in situ thermal heavy oil (bitumen) extraction operation in the world. The mean soil ingestion rate in this study using Al Ce, La, and Si tracers was 32 mg d− 1, with a 90th percentile of 152 mg d− 1 and median soil ingestion rate of 18 mg d− 1. These soil ingestion values are greater than the standard recommended soil ingestion rates for HHRA from Health Canada, and are similar to soil ingestion estimates found in the only other study on a rural population.

Soils of permanent sample plots in the Athabasca oil sands area


Author(s): Turchenek, L. W.

Year: 1982

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

Source apportionment of background PAHs in the Peace-Athabasca Delta (Alberta, Canada) using molecular level radiocarbon analysis


Year: 2015

Abstract:
The downstream accumulation of polycyclic aromatic hydrocarbons (PAHs) in the Peace-Athabasca Delta (PAD), an ecologically important landscape, is a key issue of concern given the rapid development of the oil sands industry in Northern Alberta, Canada. In addition to PAHs derived from industrial activity (i.e., oil sands mining) within the Athabasca watershed, however, forest fires and erosion of fossil fuel deposits within both the Athabasca and Peace watersheds are two potentially important natural sources of PAHs delivered to the PAD. Consequently, evaluating the environmental impact of mining activities requires a quantitative understanding of natural, background PAHs. Here, we utilize molecular-level natural-abundance radiocarbon measurements on an amalgamated sediment record from a Peace River flood-susceptible oxbow lake in the northern Peace sector of the PAD to quantitatively discriminate sources of naturally occurring alkylated PAHs (fossil and modern biomass). A radiocarbon mass balance quantified a predominantly natural petrogenic source (93% petrogenic, 7% forest fire) for alkylated PAHs during the past ∼50 years. Additionally, a significant petrogenic component determined for retene, a compound usually considered a biomarker for softwood combustion, suggests that its use as a unique forest fire indicator may not be suitable in PAD sediments receiving Peace watershed-derived fluvial inputs.

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