The International dry-farming congress, containing: the official call of the seventh international session, and exposition, at Lethbridge, Alberta, October 19-26, 1912. The dry-farming congress--its history, its sims, its successes. The province of Alberta ... its resources, its development, its possibilities, and the agricultural and industrial districts of southern Alberta. Pub. by the Department of agriculture of the province of Alberta, and the Board of control, of the seventh International dry-farming congress.

Edited by Charles S. Hotchkiss.

Wrestling Card - John Katan

The wrestler's name is John Katan and the number stamped on the reverse is 341. He was born in the Ukraine and moved to Lethbridge, Alberta and became a coal miner. He wrestled after work until he was discovered and went pro. He bought two wrestling franchises based in Hamilton and became a promoter when he retired from active wrestling. His honours include the Canadian Wrestling Hall of Fame.

MAGGnet: an international network to foster mitigation of agricultural greenhouse gases.

Research networks provide a framework for review, synthesis and systematic testing of theories by multiple scientists across international borders critical for addressing global-scale issues. In 2012, a GHG research network referred to as MAGGnet (Managing Agricultural Greenhouse Gases Network) was established within the Croplands Research Group of the Global Research Alliance on Agricultural Greenhouse Gases (GRA). With involvement from 46 alliance member countries, MAGGnet seeks to provide a platform for the inventory and analysis of agricultural GHG mitigation research throughout the world. To date, metadata from 315 experimental studies in 20 countries have been compiled using a standardized spreadsheet. Most studies were completed (74%) and conducted within a 1-3-year duration (68%). Soil carbon and nitrous oxide emissions were measured in over 80% of the studies. Among plant variables, grain yield was assessed across studies most frequently (56%), followed by stover (35%) and root (9%) biomass. MAGGnet has contributed to modeling efforts and has spurred other research groups in the GRA to collect experimental site metadata using an adapted spreadsheet. With continued growth and investment, MAGGnet will leverage limited-resource investments by any one country to produce an inclusive, globally shared meta-database focused on the science of GHG mitigation.

Wherefore art thou, inclusion? Analysing the development of inclusive education in New South Wales, Finland and Alberta

Over the last two decades, moves toward “inclusion” have prompted change in the formation of education policies, schooling structures and pedagogical practice. Yet, exclusion through the categorisation and segregation of students with diverse abilities has grown; particularly for students with challenging behaviour. This paper considers what has happened to inclusive education by focusing on three educational jurisdictions known to be experiencing different rates of growth in the identification of special educational needs: New South Wales (Australia), Alberta (Canada) and Finland (Europe). In our analysis, we consider the effects of competing policy forces that appear to thwart the development of inclusive schools in two of our case-study regions.

Influence and increased funding in Canadian public libraries : the case of Alberta in fiscal year 2009–10

This exploratory case study examined the role of social influence in the decision-making process to increase public library funding in the Canadian province of Alberta in the 2009–10 fiscal year. Using Robert Cialdini’s theory of factors of influence (i.e., commitment and consistency, authority, liking, social proof, scarcity, and reciprocity) as a framework for analysis, findings show that consistency and commitment and authority were relevant and that liking was also important. These findings are consistent with Cialdini’s theory, which suggests that the quality of relationships is one factor that can most strongly influence a decision maker. This study gives insight into the factors motivating those involved in public library funding allocation decisions. No prior studies have examined the construct of influence in decision making about funding for public libraries at any level of government.

'It's Africa. It's Arizona. It's Antarctica. It's Afghanistan. Actually, it's Alberta' : Marketing locations to film producers

This chapter begins by outlining the dynamics of contemporary international film production and the inherent tension between ‘design interest’ and ‘location interest’. A history of the promotion of particular places as filmmaking locations (including Hollywood) is presented, prior to the establishment of the first film commissions. The creation of international associations and their role in professionalization, norm setting and the standardization of offerings and activities, is then described. The chapter concludes with a discussion of commissions’ work, the emergent discourse of ‘film friendliness,’ and the differences between location marketing and other kinds of destination marketing.

Isotope Hydrology of the Oldman River basin, southern Alberta, Canada

The partially semi-arid Oldman River basin (OMRB), located in southern Alberta (Canada), has an area of 28 200 km2, is forested in its western headwater part, and is used for agriculture in its eastern part. Hydrometric measurements indicate that flow in the Oldman River has decreased by ~34% between 1913 and 2003, and it is predicted that water withdrawals will increase in the next 20 years. The objective of this study was to determine whether isotope ratio measurements can provide further insight into the water dynamics of the Oldman River and its tributaries. Surface water samples were collected monthly between December 2000 and March 2003. Groundwater samples were taken from 58 wells during one-time sampling trips. Runoff within the OMRB is currently about 70 mm year-1, with a corresponding runoff ratio of 0Ð18. Seasonal flow characteristics are markedly different upstream and downstream of the Oldman River reservoir. Upstream, sharp increases in flow in late spring and early summer are followed by a rapid decrease to base flow levels. Downstream, a prolonged high flow peak is observed due to the storage effect of the Oldman River reservoir. The seasonal variation in the isotopic composition of surface water from upstream sites is small. This suggests that peak runoff is not predominantly generated by melting snow accumulated during the preceding winter, but mainly by relatively well-mixed young groundwater. A significant increase in the d18O and d2H values in the downstream part of the basin was observed. The increase in the isotopic values is partly due to surface water and groundwater influx with progressively higher d18O and d2H values in the eastern part, and partly due to evaporation. Hence, the combination of hydrometric data with isotope measurements yields valuable insights into the water dynamics in the OMRB that may be further refined with more intensive measurement programmes in the future.

Nitrogen budget for the Oldman River Basin, southern Alberta, Canada

The Oldman River Basin (OMRB), located in southern Alberta (Canada), with an area of 28,200 km2, is mainly forested in its western part and is used for intensive agriculture in its eastern part. The objective of this paper is to estimate the nitrogen (N) budget for the Oldman River Basin as a whole and its sub-basins, and to discuss differences in the N budget between various sub-basins. Better knowledge of the N budget in this watershed may be also utilized for understanding N dynamics in similar watersheds within semi-arid climatic regions. The model used is a mass balance spreadsheet model that takes into account N inputs and N export through surface water. During the last 120 years, anthropogenic N inputs to the OMRB have increased circa 40 fold. By the end of the 20th century, the OMRB received an annualN input of about 5174 kg N km-2 yr-1, whereas only about 25 kg N km-2 yr-1 were exported via riverine flow. For the sub-basins, annual N inputs ranged from 2516 to 19011 kg N km-2 yr-1, and annual N export via riverine flows varied between 6 and 277 kg N km-2 yr-1. Over 85% of total N inputs to the OMRB are due to anthropogenic activities, including manure (55%), synthetic fertilizer (27%), and N fixation on agricultural lands (4%). Sewage accounted for less than 1%, and N inputs from atmospheric deposition and fixation in forests represented 6 and 8% respectively. Despite increasing anthropogenic N inputs, N export with riverine flow currently accounts for only 1% of the inputs, indicating thatmost of theNinputs are currently retained in the OMRB or are re-emitted into the atmosphere.

Isotopic Assessment of Sources of Surface Water Nitrate within the Oldman River Basin, Southern Alberta, Canada

Concentrations and isotopic compositions of NO-3 from the Oldman River (OMR) and some of its tributaries (Alberta, Canada) have been determined on a monthly basis since December 2000 to assess temporal and spatial variations of riverine NO-3 sources within the OMR basin. For the OMR sites, NO-3 -N concentrations reached up to 0.34 mg L-1, d15N-NO-3 values varied between –0.3 and +13.8‰, and d18O-NO-3 values ranged from –10.0 to +5.7‰. For the tributary sites, NO-3 -N concentrations were as high as 8.81 mg L-1, d15N-NO-3 values varied between –2.5 and +23.4‰, and d18O-NO-3 values ranged from –15.2 to +3.4‰. Tributaries in the western, relatively pristine forested part of the watershed add predominantly NO-3 to the OMR with d15N-NO-3 indicative of soil nitrification. In contrast, tributaries in the eastern agriculturally-urban-industrially-used part of the basin contribute NO-3 with d15N-NO-3 values of about +16‰ indicative of manure and/or sewage derived NO-3. This difference in d15N-NO-3 values of tributaries was found to be independent of the season, but rather indicates a spatial change in the NO-3 source, which correlates with land use changes within the OMR basin. As a consequence of tributary influx, d15N-NO-3 values in the Oldman River increased from +6‰ in the downstream direction (W to E), although [NO-3 -N] increased only moderately (generally

Paléoécologie du Quaternaire dans la région de Wainwright en Alberta

En 2012, la Commission géologique du Canada a procédé à une série de forages dans les dépôts quaternaires de la région de Wainwright dans le centre-est de l’Alberta dans le cadre d’un projet en hydrogéologie. Les forages, qui atteignent plus de 60 m de profondeur, montrent la présence de niveaux organiques intercalés dans les unités stratigraphiques minérales, dont certains contiennent des morceaux de bois qui suggèrent la présence passée in situ d’une végétation ligneuse. La position stratigraphique des sables contenant des niveaux organiques sous le till régional (Wisconsinien supérieur) laisse penser qu’ils correspondraient à des épisodes interstadiaires, voire même de l’interglaciaire Sangamonien, des datations 14C ayant livré des âges non-finis (>43 500 ans A.A.). L’objectif principal de la présente étude était de documenter la composition du couvert végétal associé aux niveaux organiques à l’aide de l’analyse pollinique et macrofossile. Plusieurs des niveaux se sont avérés pauvres ou même stériles en grains de pollen et en macrorestes végétaux. Les assemblages polliniques sont le plus souvent dominés par des espèces herbacées (p. ex.: Cyperaceae, Artemisia sp.) et des fougères. Chez les arbres, l’épinette est l’espèce la mieux représentée mais elle montre des pourcentages polliniques relativement faibles. Les assemblages macrofossiles sont notamment caractérisés par la présence de matière ligneuse, de l’épinette et de plantes aquatiques. Plusieurs échantillons contiennent aussi des charbons de bois qui témoignent de l’incidence de feux. Les résultats des analyses paléoécologiques suggèrent que le couvert végétal contemporain du dépôt des niveaux organiques était à caractère boréal ouvert. Ces niveaux auraient donc été mis en place au cours d’un intervalle climatique plus froid que l’actuel, présumément un interstade wisconsinien plutôt qu’au cours du dernier interglaciaire (Sangamonien).

Entre Nós : entrevista a Maria Alberta Menéres

Emissões - Entre Nós

A exploração não convencional de recursos energéticos: exemplo de Alberta (Canadá)

Nas últimas décadas, temos assistido a uma mudança no sector energético. A utilização de métodos não convencionais para a extracção de recursos energéticos, nomeadamente petróleo e gás natural, tem vindo a aumentar em diversas regiões do globo − nomeadamente no Canadá com as areias betuminosas e nos EUA com o gás de xisto − atingindo uma expressão já bastante significativa, pela escala, pela especificidade tecnológica e pela influência que este tipo de explorações tem no sector energético. Com uma procura crescente de energia e com o declínio de recursos energéticos convencionais, os recursos não convencionais apresentam-se como alternativa para responder às necessidades do mercado. O aumento dos custos (de exploração e da energia final) e a necessidade de tecnologia apropriada pressupõe uma associação muito directa à investigação e à inovação limitando o acesso a estes recursos a um escasso número de empresas e países. O principal objectivo desta dissertação é avaliar o potencial de exploração não convencional de recursos energéticos na actualidade, tendo como referência o Canadá, que constitui uma das principais áreas a nível mundial deste tipo de exploração e um importante difusor de tecnologia. A metodologia utilizada baseia-se na análise de informação disponibilizada nas últimas décadas e em estudos de instituições e consultores internacionais relevantes na área da energia. Sendo um tipo de exploração muito específico em termos tecnológicos e económicos, a opção não convencional poderá levar a uma mudança dos métodos de exploração de hidrocarbonetos bem como à sua disponibilidade, a qual teria um fim anunciado. Com o aumento das reservas e de recursos disponíveis bem como com o aumento do preço poderemos estar perante uma nova “era energética” baseada, uma vez mais, em recursos de origem fóssil (petróleo e gás) como aconteceu no séc. XX