Canada has distinct contemporary faith communities that differ from western and European counterparts. Unfortunately statistics tracking denominational allegiances give little insight into the daily intricacies of collective religious practice. The purpose of this study is to contribute towards filling a gap within scholarly research on the lived culture and experiences of contemporary religious communities within Canada. This study examines the pattern of culture-sharing within a non-denominational faith community as lived and practiced in Ottawa. Through autoethnography, this study asks why members attend and how members view the use of popular culture video clips within church. Individual and collective religious identities are constructed through observations, interviews and material artifacts gleaned through participant observation from January 2011 to December 2011. The results show that within the church, a community of practice is built around shared parenthood and spiritual journey. Members place importance on children, on providing support of all kinds for one another, and on keeping religion relevant. Reasons for attending are echoes of the patterns of culture-sharing: members enjoy the feeling of community, the support, the friendships, the play dates. Participants view popular culture video clips played within church as one aspect of an overall importance placed upon relevance. Mutuality of engagement results in members experiencing their lives as meaningful, it validates their worth through belonging, and it creates personal histories of becoming within the context of a community of practice. Future research recommendations include further study of other contemporary faith communities within Canada, with investigation into the possibility that communities of practice may be what the churched and unchurched are seeking.

The fundamental forces of adhesion are responsible for the spreading of fluids such as crude oil/brine on the reservoir rock surface. These physico-chemical interactions determine the surface energetics of a reservoir and thus their wetting phenomena. Inverse Gas Chromatography is introduced to characterize the surface energy of carbonates (calcite and dolomite) and sandstones (Ottawa sand and Berea sandstone). The behavior of the polar and non-polar interaction forces was investigated at varying water coverage and at different temperatures. The results indicated that in general as the water coverage increased, the Lifshitz-van der Waals component of surface energy decreased to nearly that of the bulk water, while the acid-base component also showed a decreasing trend. The Lifshitz-van der Waals component of surface energy always decreased with increase in temperature, while the acid-base properties mostly increased with temperature with the exception of calcite. / text

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“Word up” is a catch phrase that denotes agreement or enthusiasm about what another has said. A question central to this thesis was whether study participants thought that Algonquin College should endeavour to be a sustainability leader. Online and clipboard surveys, involving on- and off-campus participants, compiled new ideas of how Algonquin could educate for sustainability. These ideas formed a needs analysis that, combined with a review of trends in North American colleges’ education for sustainability, fed into program design recommendations. The program design phase of the research involved participants in an assessment of the survey results and the development of program recommendations for academic development at Algonquin College. Off-campus participants suggested new types of experiential learning involving community partners and encouraged the college to educate for careers related to sustainable food and renewable energy. On-campus participants were concerned foremost with the infusion of sustainable principles across all college curricula.

The i-Tree Eco model, developed by the U.S. Forest Service, is commonly used to estimate the value of the urban forest and the ecosystem services trees provide. The model relies on field-based measurements to estimate ecosystem service values. However, the methods for collecting the field data required for the model can be extensive and costly for large areas, and data collection can thus be a barrier to implementing the model for many cities. This study investigated the use of geospatial technologies as a means to collect urban forest structure measurements within the City of Ottawa, Ontario. Results show that geospatial data collection methods can serve as a proxy for urban forest structure parameters required by i-Tree Eco. Valuations using the geospatial approach are shown to be less accurate than those developed from field-based data, but significantly less expensive. Planners must weigh the limitations of either approach when planning assessment projects.

No description available.

No description available.

The geochemistry of surface media above two known U deposits were examined to observe any possible dispersion products could be detected from them, and based on these findings, improved geochemical exploration techniques are proposed to reduce cost of finding undiscovered U resources. This study examined the materials overlying the Phoenix deposits, which have indicated resources of approximately 58.2 million lbs U3O8 grading 15 wt% that lie at 400 m depth below surface at the unconformity between the overlying Athabasca sandstones and Paleoproterozoic basement rocks. Aqua regia digestion, ammonium acetate at pH 5 and hydroxylamine leaches revealed U, Pb, Co, Ni, Mo, and W anomalies in humus and U, W and As anomalies in B-horizon soils above the ore zones and the basement location of a deposit-hosting, northeast-trending “WS Hanging Wall” shear zone over a three year period. These metal signatures suggest likely upward transport of metals from the deposits to overlying sandstones, and subsequently into the overlying till and soils. This study also looked at materials above the Millennium U deposit, which has indicated resources of 68.2 million lbs U3O8 grading 4 wt% at ~750 m depth that occurs along a major fault in granites & metamorphosed pelites of Paleoproterozoic age below the Athabasca sandstones. Soil samples taken over the surface projections of an ore-hosting fault and the ore zone yielded anomalous values in U, Ni, Cu and Pb in aqua regia digestion of humus and U, Cu and Pb values in ammonium acetate leach of pH 5 of B-horizon soils. Hydroxylamine leach did not yield as many anomalies as ammonium acetate leach. Measured 4He/36Ar ratios of gas dissolved in water-filled drill holes were observed to be up to about 700 times the atmosphere value for air-saturated water, revealing the presence of radiogenic 4He that was likely produced from decaying U and released in the groundwater above the deposit. Our results suggest upward migration of metals to surface through porous sandstone and fault systems at Phoenix, and upward migration of metals along faults and He gas at Millennium. Both studies indicate the importance of the traverse method of sampling over targets perpendicular to the last major ice-flow event to discern U deposits that are defined by other means.

Thesis (D.W.S.)--Institute for Worship Studies, 2004. / Abstract. Includes bibliographical references (leaves 197-202).

Thesis (D. Min.)--Trinity Evangelical Divinity School, 2006. / Abstract. Includes bibliographical references (leaves 253-259).