Textual characteristics of coarse sediments in selected streams of the Niagara Peninsula, Ontario

The streams flowing through the Niagara Escarpment are paved by coarse carbonate and sandstone sediments which have originated from the escarpment units and can be traced downstream from their source. Fifty-nine sediment samples were taken from five streams, over distances of 3,000 to 10,000 feet (915 to 3050 m), to determine downstream changes in sediment composition, textural characteristics and sorting. In addition, fluorometric velocity measurements were used in conjunction with measured -discharge and flow records to estimate the frequency of sediment movement. The frequency of sediments of a given lithology changes downstream in direct response to the outcrop position of the formations in the channels. Clasts derived from a single stratigraphic unit usually reach a maximum frequency within the first 1,000 feet (305 m) of transport. Sediments derived from formations at the top of waterfalls reach a modal frequency farther downstream than material originating at the base of waterfalls. Downstream variations in sediment size over the lengths of the study reaches reflect the changes in channel morphology and lithologic composition of the sediment samples. Linear regression analyses indicate that there is a decrease in the axial lengths between the intial and final samples and that the long axis decreases in length more rapidly than the intermediate, while the short axis remains almost constant. Carbonate sediments from coarse-grained, fossiliferous units - iii - are more variable in size than fine-grained dolostones and sandstones. The average sphericity for carbonates and sandstones increases from 0.65 to 0.67, while maximum projection sphericity remains nearly constant with an average value of 0.52. Pebble roundness increases more rapidly than either of the sphericity parameters and the sediments change from subrounded to rounded. The Hjulstrom diagram indicates that the velocities required to initiate transport of sediments with an average intermediate diameter of 10 cm range from 200 cm/s to 300 cm/s (6.6 ft./sec. to 9.8 ft./sec.). From the modal velocitydischarge relations, the flows corresponding to these velocities are greater than 3,500 cfs (99 m3s). These discharges occur less than 0.01 p~r cent (0.4 days) of the time and correspond to a discharge occurring during the spring flood.

Climbers' perceptions toward sustainable bouldering at the Niagara Glen Nature Reserve

Currently, there are a variety of concerns about the future of bouldering, a form of rock climbing, a t the Niagara Glen Nature Reserve near Niagara Falls, Ontario due to environmental impacts at the site. The purpose of this study was to describe the perceptions ofbouldering participants toward sustainable bouldering practices at the Niagara Glen. The methodological framework for this study was based on action research, which attempts to solve specific problems through having people in a community study, discuss, and act on those problems. Five separate focus group interviews elicited data from nineteen men and seven women, while there were twenty one men and ten women observed through participant observations at the Niagara Glen. Analysis was conducted through coding processes where data were compared repeatedly and then organized into themes. From the open coding process, two main themes were identified and interpreted as 1) Barriers to Sustainable Bouldering at the Niagara Glen Nature Reserve, and 2) Environmental and Social Role and Responsibility ofBoulde r ing Participants at the Niagara Glen. The implications of the findings include a variety of recommendations for the bouldering community and the Niagara Parks Commission to consider for future collaborative planning. Some of these recommendations include more open communication between all stakeholders at the Glen, additional leadership from local climbing access coalitions and the Niagara Parks Commission, and greater implementation of minimum impact practices from the bouldering community. Additionally, these implications are discussed through a three-part framework based on a conceptual intersection of sense of place, community empowerment, and sustainable recreational use as a way to potentially unify the bouldering community's voice and vision toward sustainable practice.

Interlake Tissue Mills Fire Slides

The Interlake Tissue Mills storage location was at the intersection of Glendale and Merritt Street in Merritton. In the 1850s, the Beaver Cotton Mills (later Merritton Cotton Mills) was built. It was a frame building that burned down in 1881. A sandstone structure replaced the previous building. In 1906, the cotton mill closed and in 1912, the Independent Rubber Company took over the building. The mill was doubled in size. The rubber company remained there for ten years and then the building remained vacant until 1935. Interlake Tissue Mills acquired the building for storage purposes. A fire razed the larger of the plant’s buildings on Memorial Day weekend in 1961. After the fire, Domtar used the smaller building for storage for a short time. This is currently the site of the Keg Restaurant.

Analyse cinématique de la marche de travailleurs exposés à une surcharge mécanique sur l’articulation fémoro-tibiale (AF-T)

De nombreuses études concluent que la charge mécanique supportée par le genou, qu’elle soit reliée à l’obésité, aux sports intenses, à une altération biomécanique des structures de l’articulation ou à une exposition à des charges lourdes durant les activités occupationnelles, est considérée comme un facteur de risque important au développement de la gonarthrose. La gonarthrose reliée au travail a été le sujet de nombreuses études et plusieurs d’entre elles ont rapporté une prévalence accrue de la gonarthrose chez les travailleurs de certains domaines en particulier, comme la construction, la pose de plancher, la peinture, l’exploitation minière, l’agriculture et le travail en atelier et en milieu de la santé. Les personnes qui travaillent dans ces métiers sont exposées à des positions ou des activités nuisibles, comme travailler à genoux ou accroupi, monter des escaliers ou des échelles, transporter des changes lourdes et marcher de façon prolongée. Ces gestes surchargent l’articulation du genou, ce qui cause des modifications aux structures de l’articulation du genou ou aux adaptations neuromusculaires de patron de mouvement du genou. Ces modifications structurelles et adaptations neuromusculaires peuvent apporter des changements cinématiques à la marche qui peuvent initier la gonarthrose ou contribuer à sa progression. L’objectif principal de la présente étude était d’analyser l’effet d’une surcharge mécanique sur l’articulation fémoro-tibiale (AF-T) subie au travail lors d’une tâche de marche et comparer le patron cinématique de l’articulation fémoro-tibiale des travailleurs exposés à une surcharge mécanique à celui des travailleurs non exposés. Vingt-quatre travailleurs exposés à une surcharge mécanique et neuf travailleurs non exposés ont participé à l’étude. Les données cinématiques de la marche ont été enregistrées au niveau du genou dans des conditions cliniques en utilisant un système de suivi du mouvement électromagnétique. Les paramètres suivant ont été extraits et utilisés pour la comparaison des groupes : l’angle maximum lors du contact initial, l’angle ii maximum de flexion durant la réponse à la charge, l’angle minimum au moment de l’appui unipodal et l’étendue max-min du cycle. La comparaison des groupes pour les variables cliniques et cinématiques a été effectué par l’utilisation de tests-t bilatéraux (« Student-t tests ») et de tests ANCOVA utilisant le poids et la vitesse comme covariables. Les travailleurs exposés à une surcharge mécanique présentaient un plus grand angle de flexion de l’articulation fémoro-tibiale au contact initial, durant la réponse au chargement et à la phase unipodale et ils ont démontré une étendue d’angle moindre que les travailleurs non exposés. Nous croyons que les données cinématiques de la marche peuvent donner des idées sur les facteurs biomécaniques qui pourraient prédisposer les travailleurs au développement ou à la progression de la gonarthrose. Une meilleure compréhension de ces facteurs pourrait être un premier pas vers le développement d’une intervention plus efficace pour cette population.

Effets de l’utilisation d’un chien d’assistance sur les efforts aux membres supérieurs lors de la montée d’une pente en fauteuil roulant chez les individus ayant une lésion médullaire

Problématique. L'utilisation d'un chien d'assistance à la mobilité (CAM) représente une option novatrice pour préserver l’intégrité des membres supérieurs (MSs) chez les utilisateurs de fauteuil roulant manuel (FRM). Aucune étude biomécanique n’a quantifié les effets du CAM sur les efforts aux MSs lors de la montée d’un plan incliné. Objectif. Cette étude quasi-expérimentale vise à comparer les efforts aux MSs lors de la montée d’un plan incliné avec et sans l’assistance d’un CAM. Méthodologie. Dix participants avec une lésion de la moelle épinière (LME) qui utilisent un FRM et possèdent un CAM ont monté un plan incliné à trois reprises avec et sans l’assistance du CAM. Les forces appliquées sur les cerceaux, mesurées avec des roues instrumentées, et les mouvements du FRM et des MSs, enregistrés avec un système d'analyse du mouvement, ont permis de mesurer les efforts mécaniques aux MSs. Simultanément, l'activité électromyographique (EMG) des muscles grand pectoral, deltoïde antérieur, biceps et triceps a été enregistrée et normalisée avec sa valeur maximale pour mesurer les efforts musculaires aux MSs. Résultats. En général, le CAM réduit significativement les valeurs moyennes et maximales de la force totale appliquée aux cerceaux et de sa composante tangentielle, des moments nets de flexion, de rotation interne et d’adduction aux épaules et des taux d’utilisation musculaire du deltoïde antérieur, du biceps et du triceps. Conclusion. L’assistance d’un CAM réduit les efforts aux MSs lors de la montée d’un plan incliné chez les utilisateurs d’un FRM ayant une LME.

Median computation in graphs using consensus strategies

Following the Majority Strategy in graphs, other consensus strategies, namely Plurality Strategy, Hill Climbing and Steepest Ascent Hill Climbing strategies on graphs are discussed as methods for the computation of median sets of pro¯les. A review of algorithms for median computation on median graphs is discussed and their time complexities are compared. Implementation of the consensus strategies on median computation in arbitrary graphs is discussed

Topogenèse et sécurité en escalade. Illustration d’un cas particulier

Le cas que nous exposons ici est extrait d’un travail de recherche plus vaste ayant pour objet une analyse comparative de plusieurs institutions1 où vivent et se transmettent des savoirs sécuritaires propres à l’escalade. Notre étude met en face à face des institutions clairement identifiées comme didactiques - c’est le cas de l’école au sens large de l’acception - c’est-à-dire des institutions où l’intention de transmettre y est toujours mise en avant, mais aussi d’autres institutions «à la limite» du didactique telles les organismes de loisirs sportifs, ainsi que des institutions a priori non didactiques comme une famille ou un groupe d’amis, où le mode de transmission des savoirs relève majoritairement d’un système d’apprentissage par frayage (Delbos & Jorion, 1990), (Hutchins, 1995). Le sujet est abordé sous l’angle didactique de la gestion des risques (Mangeant, 2008). La recherche repose en partie sur la théorie des situations didactiques (Brousseau, 1998) et notamment la notion de contrat entendu comme une convention implicite, mais aussi pour nous dans notre sujet, comme accord explicite sur les règles de fonctionnement. Elle s’appuie également sur le modèle de l’action enseignante et le triplet des genèses (Sensevy, Mercier & Schubauer- Leoni, 2000) et plus précisément sur le principe de l’action conjointe du professeur et des élèves (Sensevy & Mercier, 2007). Le travail s’attache à démontrer que des phénomènes de contrat, peuvent être à l’origine de failles dans la sécurité, et potentiellement pourvoyeurs de futurs accidents. Ainsi, au-delà du manque de vigilance communément invoqué, il y aurait donc des causes didactiques à l’occurrence des accidents, dont les explications sont parfois à rechercher à l’origine dans la formation des intervenants ou dans le mode de transmission des savoirs

Interpretación sedimentológica y paleogeográfica del nivel de areniscas eocénicas de Sarrià de Ter (Prov. de Gerona)

There is in this work a description of sedimentological characters of the medium Eocene sandstone level from Sarriá de Ter (Gerona province Spain) and an interpretation of their genesis and situation in the regional paleogeography. The conclusion is that these sandstones form a deltaic channel(delta front). To wards the E and NE the become fluvial deposits, to wards the W, Plana de Vic, they become clay and silstones considered as a prodelta

Spatangoid-produced ichnofabrics (Bateig Limestone, Miocene, Spain) and the preservation of spatangoid trace fossils

A spatangoid-produced ichnofabric is described from the Miocene Bateig Limestone, SE Spain. This ichnofabric is characterized by the dominant presence of large meniscate burrows (Bichordites) produced by irregular echinoids. This constitutes an unusual mode of occurrence for spatangoid bioturbation, as their traces are most typically preserved in bases and tops of sandstone event beds. In fact, despite their important role as burrowers in modern settings (that can be extended back to the Early Cretaceous based on their body fossil record), spatangoid trace fossils (Scolicia and Bichordites) are comparatively rare. Several factors play an important role in their preservation: mechanism of burrowing, sediment characteristics, early diagenesis and presence/absence of deep-tier burrowers. Spatangoid-produced ichnofabrics, such as those from the Bateig Limestone, characterize depositional settings with intermittent deposition of event beds where there is an absence of deeper-tier bioturbation. (C) 2008 Elsevier B.V. All rights reserved

The effect of the functional attributes of objects within the caged environment on interaction time in laboratory rats

Determining rat preferences for, and behaviour towards, environmental enrichment objects allows us to provide evidence-based information about how the caged environment may be enriched. In recent years there have been many studies investigating the preferences of laboratory rodents for a wide variety of environmental enrichment objects and materials. While these have provided important information regarding the animals' perception of the items, very few studies have attempted to systematically investigate the precise attributes that constitute a preferred object and the behaviour that these objects afford. We have designed a research program to systematically study rats' motivation to interact with enrichment objects. Here we present the results from two experiments which examined the time rats spent with objects that only differed in size. This showed that rats spent longer with large objects rather than small ones, even though objects were presented individually. We also investigated the rats' behaviour with the objects in an open field and found that rats spent longer climbing on top of the large object. This behaviour continued when the large objects were laid on their sides instead of placed upright in the arena, suggesting that the rats were not simply climbing on the objects to investigate the top of the arena and thus an escape route, but instead were genuinely motivated to climb. This suggests that rat welfare could be enhanced by the addition to their cages of objects that permit climbing. (C) 2009 Elsevier B.V. All rights reserved.

Suboptimal system recovery from communication loss in a multi-robot localization scenario using EKF algorithms

This paper describes a multi-robot localization scenario where, for a period of time, the robot team loses communication with one of the robots due to system error. In this novel approach, extended Kalman filter (EKF) algorithms utilize relative measurements to localize the robots in space. These measurements are used to reliably compensate "dead-com" periods were no information can be exchanged between the members of the robot group.

Results of applying sensor fusion to a control system using optic flow

The results from applying a sensor fusion process to an adaptive controller used to balance all inverted pendulum axe presented. The goal of the sensor fusion process was to replace some of the four mechanical measurements, which are known to be sufficient inputs for a linear state feedback controller to balance the system, with optic flow variables. Results from research into the psychology of the sense of balance in humans were the motivation for the investigation of this new type of controller input. The simulated model of the inverted pendulum and the virtual reality environments used to provide the optical input are described. The successful introduction of optical information is found to require the preservation of at least two of the traditional input types and entail increased training till-le for the adaptive controller and reduced performance (measured as the time the pendulum remains upright)

Investigation into the performance of an algorithm for deriving concise descriptions of optic flow fields for real-time control

This paper describes a region-based algorithm for deriving a concise description of a first order optical flow field. The algorithm described achieves performance improvements over existing algorithms without compromising the accuracy of the flow field values calculated. These improvements are brought about by not computing the entire flow field between two consecutive images, but by considering only the flow vectors of a selected subset of the images. The algorithm is presented in the context of a project to balance a bipedal robot using visual information.

Seismic activity triggered by water wells in the Parana Basin, Brazil

Triggered seismicity is commonly associated with deep water reservoirs or injection wells where water is injected at high pressure into the reservoir rock. However, earth tremors related solely to the opening of groundwater wells are extremely rare. Here we present a clear case of seismicity induced by pore-pressure changes following the drilling of water wells that exploit a confined aquifer in the intracratonic Parana Basin of southeastern Brazil. Since 2004, shallow seismic activity, with magnitudes up to 2.9 and intensities V MM, has been observed near deep wells (120-200 m) that were drilled in early 2003 near the town of Bebedouro. The wells were drilled for irrigation purposes, cross a sandstone layer about 60-80 m thick and extract water from a confined aquifer in fractured zones between basalt flow layers. Seismic activity, mainly event swarms, has occurred yearly since 2004, mostly during the rainy season when the wells are not pumped. During the dry season when the wells are pumped almost continuously, the activity is very low. A seismographic network, installed in March 2005, has located more than 2000 microearthquakes. The events are less than 1 km deep (mostly within the 0.5 km thick basalt layer) and cover an area roughly 1.5 km x 5 km across. The seismicity generally starts in a small area and expands to larger distances with an equivalent hydraulic diffusivity ranging from 0.06 to 0.6 m(2)/s. Geophysical and geothermal logging of several wells in the area showed that water from the shallow sandstone aquifer enters the well at the top and usually forms waterfalls. The waterfalls flow down the sides of the wells and feed the confined, fractured aquifer in the basalt layer at the bottom. Two seismic areas are observed: the main area surrounds several wells that are pumped continuously during the dry season, and a second area near another well (about 10 km from the first area) that is not used for irrigation and not pumped regularly. The main area displays cyclic annual activity, but the second area does not. We explain the earthquake swarms as being triggered by pore pressure diffusion in the fractured basalt layer due to additional pressure from the newly connected surface aquifer. This reaches critically prestressed areas up to a few kilometers away from the wells. During periods of continuous pumping, the reduction of pore pressure in the confined aquifer stops the seismic activity. Our study suggests that this kind of activity may be more common than previously thought and implies that many other cases of small tremors associated with the drilling of water wells may have gone unnoticed.