Effect of cage design on characteristics of high-speed-jet-lubricated 35-millimeter-bore ball bearing

Parametric tests were conducted with a 35 mm bore angular contact ball bearing with a double outer land guided cage. Provisions were made for jet lubrication and outer-ring cooling of the bearing. Test conditions included a combined thrust and radial load at nominal shaft speeds of 48,000 rpm, and an oil-in temperature of 394 K (250 F). Successful operation of the test bearing was accomplished up to 2.5 million DN. Test results were compared with those obtained with similar bearing having a single outer land guided cage. Higher temperatures were generated with the double outer land guided cage bearing, and bearing power loss and cage slip were greater. Cooling the outer ring resulted in a decrease in overall bearing operating temperature

Effect of two inner-ring oil-flow distribution schemes on the operating characteristics of a 35 millimeter bore ball bearing to 2.5 million DN

Parametric tests were conducted with a 35-mm-bore, split-inner-ring ball bearing with a double-inner-land-guided cage. Provisions were made for through-the-inner-ring lubrication. Test condictions were either a thrust load of 667 N (150 lb) or a combined load of 667 N (150 lb) thrust and 222 N (50 lb) radial, shaft speeds from 32000 to 72000 rpm, and an oil-inlet temperature of 394 K (250 deg F). Outer ring cooling was used in some tests. Tests were run with either 50 or 75 percent of the total oil flow distributed to the inner-ring raceway. Successful operation was experienced with both 50% and 75% flow patterns to 2.5 million DN. Cooling the outer ring had little effect on inner-ring temperature; however, the outer-ring temperature decreased as much as 7% at 2.5 million DN. Maximum recorded power loss was 3.1 kW (4.2 hp), and maximum cage slip was 8.7 percent. Both occurred at a shaft speed of 72000 rpm, a lubricant flow rate of 1900 cu/min (0.50 gal/min), a combined load, and no outer-ring cooling

Variations spatiotemporelles des compartiments autotrophes et hétérotrophes de la boucle microbienne dans les lacs du sud du Québec

Les variations de la biomasse des compartiments autotrophes et hétérotrophes de la boucle microbienne ont été examinées dans neuf lacs de deux régions du sud du Québec. Six lacs étaient situés dans les Laurentides et trois lacs dans les Cantons de l'Est. Ils se différenciaient en fonction de leur statut trophique, de la géologie du bassin versant, et de la physicochimie des eaux. Dans chaque lac, l'échantillonnage a été réalisé à trois profondeurs correspondant aux strates épi-, méta- et hypolimnétiques et à cinq dates au cours de l'été (1990-1992). Les biomasses moyennes de picoplancton autotrophe (PPA : 16-80 µg·C·L-1), de picoplancton hétérotrophe (PPH : 97-647 µg·C·L-1), de nanoplancton autotrophe (NPA : 7-37 µg·C·L-1) et de nanoplancton hétérotrophe (NPH : 9-29 µg·C·L-1) notées dans les lacs du sud du Québec le long d'un gradient trophique de PT variant de 7 à 73 µg·L-1 étaient du même ordre de grandeur que celles rapportées pour d'autres écosystèmes d'eau douce au Canada.La majeure partie de la variation dans les biomasses des compartiments microbiens étaient reliée aux variations inter-lacs mais il existaient aussi des sources de variation significatives au sein des lacs, soit au niveau spatial entre les strates limnétiques ou au niveau temporel entre les dates d'échantillonnage durant l'été. Toutefois, les patrons de variation spatiotemporelle intra-lac variaient d'un lac à l'autre. Les variations inter-lacs de la biomasse des quatre compartiments microbiens ont été mises en relation avec les changements dans les concentrations de phosphore total (PT) et dans les densités de macrozooplancton. Le niveau trophique des lacs, exprimés en PT, et l'abondance du macrozooplancton avaient un effet sur les biomasses des compartiments picoplanctoniques. La biomasse de PPA et PPH décroissait dans les lacs eutrophes des Cantons de l'Est ayant des concentrations de PT supérieures à 20 µg·L-1 et dans les lacs ayant de fortes densités de macrozooplancton ou un faible rapport micro-macrozooplancton. Notre étude n'a pas mis clairement en évidence les effets du niveau trophique ou du macrozoopancton sur les compartiments nanoplanctoniques (NPA, NPH).The biomass of autotrophic and heterotrophic microbial compartments were measured in nine lakes in two regions of southern Quebec. Six lakes were located in the Laurentides while three lakes were situated in the Eastern Townships. They varied in trophic status, watershed geology, and water chemistry. Each lake was sampled at three depths, corresponding to the epi-, meta-, and hypolimnion strata, and at five dates over the summer season (1991-1992). The mean biomass of autotrophic picoplankton (PPA: 16-80 µg·C·L-1), heterotrophic picoplankton (PPH: 97-647 µg·C·L-1), autotrophic nanoplankton (NPA: 7-37 µg·C·L-1), and heterotrophic nanoplankton (NPH: 9-29 µg·C·L-1) found in Quebec lakes over a PT range of trophy varying from 7 to 73 µg·L-1 were of the same order as those reported in other freshwater environments in Canada.Most of the variation in the biomass of the four microbial compartments was related to among-lake variation. Some variation was also due to within-lake spatial variation among limnetic strata or temporal variation over the summer season. However, within-lake patterns of variation patterns were different among lakes. Among-lake variations in the biomass of the four microbial compartments were examined in relation to changes in total phosphorus concentrations (PT) and macrozooplankton densities between lakes. Both lake trophy, expressed by PT, and macrozooplankton abundance influence the biomass of picoplankton compartments. The biomass of PPA and PPH decline in the most eutrophic lakes of the Eastern Townships where PT > 20 µg·L-1. PPA and PPH biomass were also reduced in lakes with the highest density of macrozooplankton or with low micro-/macrozooplankton ratio. Our study did not clearly detected the effects of lake trophy or macrozooplankton on nanoplanktonic compartments

Effet de la prédation et des nutriments sur les réseaux microbiens planctoniques

Les effets de l'ajout de nutriments et de poissons planctonophages sur le réseau trophique microbien (protozoaires, phytoplancton, zooplancton) ont été évalués lors d'une étude expérimentale utilisant des enclos de grande taille (8 m diam., 12 m prof.), placés dans un lac humique du Bouclier Canadien. Un plan factoriel avec 4 traitements, C (contrôle), N (ajout de nutriments), P (ajout de poissons planctonophages) et NP (ajout de nutriments et poissons) a été appliqué. L'abondance et la biomasse du zooplancton (Rotifères, Cladocères, Copépodes), des Protozoaires Ciliés et du phytoplancton (Chl. a) ont été déterminées pendant 6 semaines dans chaque strate (épi-, méta- et hypolimnion). La présence de poissons planctonophages a entraîné une baisse de la biomasse du zooplancton de grande taille (Cladocères), mais a favorisé le développement du zooplancton de petite taille (Rotifères). La diminution de biomasse des Cladocères dans les enclos avec poissons s'associait avec une hausse de l'abondance des Protozoaires Ciliés et du phytoplancton pour les enclos NP. L'ajout de nutriments a augmenté la biomasse des Cladocères, des Ciliés et du phytoplancton qui présentait une tendance monospécifique. L'étude a montré que dans un lac humique riche en carbone organique dissous, les nutriments ne sont pas le seul facteur déterminant la structure des communautés microbiennes. Celles-ci subissent également les effets en cascade de la prédation des poissons planctonophages situés au sommet de la chaîne alimentaire.An experimental study was conducted using large enclosures (8 m diam., 12 m depth.) set up in a humic lake on the Canadian Shield to determine the effects of nutrients and planktivorous fish on the microbial food web (protozoans, phytoplankton and zooplankton). A four treatments factorial design was applied as following: C (control), N (nutrients), P (planktivorous fish) and NP (nutrients and fish). Zooplankton, ciliate and phytoplankton abundance and biomass were measured for six weeks in the epi-, meta- and hypolimnion. In the fish enclosure, the decrease of cladoceran biomass produced an increase in ciliate abundance and phytoplankton biomass when both fish and nutrients were present. Nutrient loading increased the biomass of cladocerans, phytoplankton and ciliates. This study showed that, in humic lakes, the microbial community is regulated not only by nutrients, but top-down effects, via fish predation, must also be considered

Multiple effects of ice load changes and associated stress change on magmatic systems

Ice retreat on volcanoes reduces pressure at the surface of the Earth and induces stress changes in magmatic systems. The consequences can include increased generation of magma at depth, increased magma capture in the crust, and modification of failure conditions of magma chambers. We review the methodology to evaluate each of these effects, and consider the influence of ongoing ice retreat on volcanoes at the Mid-Atlantic divergent plate boundary in Iceland. Evaluation of each of these effects requires a series of assumptions regarding the rheology of the crust and mantle, and the nature of magmatic systems, contributing to relatively large uncertainty in response of a magmatic system to climate warming and associated ice retreat. Pressure release melting due to ice cap retreat in Iceland may at present times generate a similar amount of magma as plate tectonic processes; larger than realized previously. However, new modelling shows that part of this magma may be captured in the crust, rather than being erupted. Gradual retreat of ice caps do steadily modify failure conditions at magma chambers, which is highly dependent on their geometry and depth, as well as the details of ice load variations. A model is presented where long-term ice retreat at Katla volcano decreases the likelihood of eruption, as more magma is needed in the magma chamber to cause failure than in the absence of the ice retreat

Three decades of coastal subsidence in the slow-moving Nice Côte d'Azur Airport area (France) revealed by InSAR (interferometric synthetic-aperture radar): insights into the deformation mechanism

Coastal areas can be tremendously biodiverse and host a substantial part of the world's population and critical infrastructure. However, there are often fragile environments that face various hazards such as flooding, coastal erosion, land salinization or pollution, earthquake-induced land motion, or anthropogenic processes. In this article, we investigate the stability of the Nice Côte d'Azur Airport, which has been built on reclaimed land in the Var River delta (French Riviera, France). This infrastructure, as well as the ongoing subsidence of the airport runways, has been a permanent concern since the partial collapse of the platform in 1979. Here, we used the full archive of ESA SAR (synthetic-aperture radar) images from 1992 to 2020 to comprehensively monitor the dynamics of the airport subsidence. We found that the maximum downward motion rate has been slowing down from 16 mm yr−1 in the 1990s to 8 mm yr−1 today. However, sediment compaction is still active, and an acceleration phase of the continuous creep leading to a potential failure of a part of the platform cannot be excluded. Our study demonstrates the importance of remotely monitoring of the platform to better understand the motion of coastal land, which will ultimately help evaluate and reduce associated hazards.</p

Prospective evaluation of a new Aspergillus IgG EIA kit for the diagnosis of chronic and allergic pulmonary aspergillosis

International audienc

Evaluating Thermal Infrared Drone Flight Parameters on Spider Monkey Detection in Tropical Forests

Geoffroy’s spider monkeys, an endangered, fast-moving arboreal primate species with a large home range and a high degree of fission–fusion dynamics, are challenging to survey in their natural habitats. Our objective was to evaluate how different flight parameters affect the detectability of spider monkeys in videos recorded by a drone equipped with a thermal infrared camera and examine the level of agreement between coders. We used generalized linear mixed models to evaluate the impact of flight speed (2, 4, 6 m/s), flight height (40, 50 m above ground level), and camera angle (−45°, −90°) on spider monkey counts in a closed-canopy forest in the Yucatan Peninsula, Mexico. Our results indicate that none of the three flight parameters affected the number of detected spider monkeys. Agreement between coders was “substantial” (Fleiss’ kappa coefficient = 0.61–0.80) in most cases for high thermal-contrast zones. Our study contributes to the development of standardized flight protocols, which are essential to obtain accurate data on the presence and abundance of wild populations. Based on our results, we recommend performing drone surveys for spider monkeys and other medium-sized arboreal mammals with a small commercial drone at a 4 m/s speed, 15 m above canopy height, and with a −90° camera angle. However, these recommendations may vary depending on the size and noise level produced by the drone model

Rapid onset of mafic magmatism facilitated by volcanic edifice collapse

Volcanic edifice collapses generate some of Earth's largest landslides. How such unloading affects the magma storage systems is important for both hazard assessment and for determining long-term controls on volcano growth and decay. Here we present a detailed stratigraphic and petrological analyses of volcanic landslide and eruption deposits offshore Montserrat, in a subduction zone setting, sampled during Integrated Ocean Drilling Program Expedition 340. A large (6–10 km3) collapse of the Soufrière Hills Volcano at ~130 ka was followed by explosive basaltic volcanism and the formation of a new basaltic volcanic center, the South Soufrière Hills, estimated to have initiated <100 years after collapse. This basaltic volcanism was a sharp departure from the andesitic volcanism that characterized Soufrière Hills' activity before the collapse. Mineral-melt thermobarometry demonstrates that the basaltic magma's transit through the crust was rapid and from midcrustal depths. We suggest that this rapid ascent was promoted by unloading following collapse

How caldera collapse shapes the shallow emplacement and transfer of magma in active volcanoes

Calderas are topographic depressions formed by the collapse of a partly drained magma reservoir. At volcanic edifices with calderas, eruptive fissures can circumscribe the outer caldera rim, be oriented radially and/or align with the regional tectonic stress field. Constraining the mechanisms that govern this spatial arrangement is fundamental to understand the dynamics of shallow magma storage and transport and evaluate volcanic hazard. Here we show with numerical models that the previously unappreciated unloading effect of caldera formation may contribute significantly to the stress budget of a volcano. We first test this hypothesis against the ideal case of Fernandina, Galápagos, where previous models only partly explained the peculiar pattern of circumferential and radial eruptive fissures and the geometry of the intrusions determined by inverting the deformation data. We show that by taking into account the decompression due to the caldera formation, the modeled edifice stress field is consistent with all the observations. We then develop a general model for the stress state at volcanic edifices with calderas based on the competition of caldera decompression, magma buoyancy forces and tectonic stresses. These factors control: 1) the shallow accumulation of magma in stacked sills, consistently with observations; 2) the conditions for the development of circumferential and/or radial eruptive fissures, as observed on active volcanoes. This top-down control exerted by changes in the distribution of mass at the surface allows better understanding of how shallow magma is transferred at active calderas, contributing to forecasting the location and type of opening fissures