154 research outputs found

    A Paleomagnetic Analysis of the Deformation and Hydrothermal Alteration in the Killarney Igneous Complex, Ontario

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    Title: A Paleomagnetic Analysis of the Deformation and Hydrothermal Alteration in the Killarney Igneous Complex, Ontario, Author: Andrew Wiacek, Location: ThodeThe Killarney Igneous Complex lies along the Grenville Front, forming a wedge between the Grenville and Southern Provinces of the Canadian Shield. The complex consists of a granitic pluton and associated felsic volcanic rocks that have been subjected to both mid-Proterozoic and Grenvillian tectonism. This study sought paleomagnetic confirmation of pre-Grenville deformation by carrying out AF and thermal demagnetization experiments on 226 samples representing both the massive and foliated parts of the complex. This was accompanied by an analysis of polished thin-sections to attempt to determine a paragenesis for the remanence carrying minerals. Sixty-four specimens of foliated and veined, hematiteenriched porphyry carry a stable southwesterly magnetization (Declination= 242.4°, Inclination= -26.4°, K = 17.5, A95 = 11.2°) or its antipole. The paleomagnetic pole implied by this magnetization (Longitude= 19.3°E, Latitude= 29.1°, dp = 9.6°, dm = 10.9°) is consistent with an age of somewhat less than 1100 Ma. This magnetization is a CRM that was acquired during the hydrothermal alteration of the porphyry. As a consistent magnetization is carried by highly sheared rocks as well as the hematite-enriched porphyry, it is concluded that the shearing must have occurred prior to the hydrothermal event. Thus, the onset of Grenville tectonism in the Killarney region began before 1100 Ma. Sufficient paleomagnetic evidence was not obtained to determine the timing of pre-Grenville tectonism.ThesisMaster of Science (MS

    À lire / À voir / À suivre

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    Histoire de l’armée polonaise en France. L’alliance blessée 1939‑1940 Jacques Wiacek, Histoire de l’armée polonaise en France. L’alliance blessée 1939-1940, Louviers, YSEC, 2022, 448 p. Jacques Wiacek, “Histoire de l’armée polonaise en France” Après l’écrasement de la Pologne en 1939 par les troupes allemandes et russes, la France focalise tous les espoirs des Polonais. Un gouvernement en exil émerge à Paris, renouvelant une longue alliance entre les deux pays. Entre les mois d’octobre 1939 ..

    Omega-3 fatty acids supplementation affects tryptophan metabolism during a 12-week endurance training in amateur runners – a randomized controlled trial

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    The effects of long-term omega-3 fatty acid (n-3 PUFAs) supplementation during endurance training on tryptophan (Trp) metabolism and mental state of healthy individuals have not been evaluated so far. Concentrations of plasma Trp, its metabolites and IL-6 were assessed in 26 male runners before and after a 12-week training combined with supplementation of n-3 PUFAs (O-3 + TRAIN group) or medium chain triglycerides (MCTs; TRAIN group). Mood and stress tests were also performed. The effects of the same supplementation protocol were evaluated also in 14 inactive subjects (O-3 + SEDEN group). Concentrations of 3-hydroxykynurenine (3-HK) and picolinic acid (PA) significantly increased only in the O-3 + TRAIN group (p = 0.01; η_p^2 = 0.22 and p = 0.01; η_(p )^2= 0.26). Favorable, but not statistically significant changes in the kynurenic acid (KYNA) (p = 0.06; η_(p )^2= 0.14), xanthurenic acid (XA) (p = 0.07; η_(p )^2= 0.13) and 3-hydroxyanthranilic acid (3-HAA) (p = 0.06; η_(p )^2= 0.15) and ratio of neurotoxic to neuroprotective metabolites was seen also only in the O-3 + TRAIN group. No changes in results of mental state tests and IL-6 concentrations were observed in either group. Supplementation with n-3 PUFAs during endurance training has beneficial effects on Trp's neuroprotective metabolites.<br/

    Land- and water-only Level 3 products from MOPITT TIR-NIR Version 8 CO retrievals

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    This dataset contains alternative products to the official Level 3 (L3) product from Measurements of Pollution in the Troposphere (MOPITT) joint thermal infrared (TIR) – near infrared (NIR) Version 8 Carbon Monoxide (CO) retrievals (available here: https://doi.org/10.5067/TERRA/MOPITT/MOP03J_L3.008). The products are described and analysed in a paper in the journal Atmospheric Measurement Techniques by Ian Ashpole and Aldona Wiacek (2022, https://doi.org/10.5194/amt-2022-90). In short, whereas the official MOPITT L3 product is based on retrievals performed over both land AND water surface types, the products here are created separately from retrievals performed ONLY over land (“L3L”) OR water (“L3W”). The code for creating L3L and L3W is available here: https://github.com/ianashpole/MOPITT_L3L_L3W The version naming is consistent with the official MOPITT product version, although note that version 8 is the first version that these alternatives are produced for (i.e. although MOPITT product versions 1-7 exist, L3L and L3W do not). However, it is intended that L3L and L3W are created for MOPITT product versions after version 8. The dataset stored here consists of two main .zip archives: “MOPITT_v8.L3L.20010901_20190228.zip” “MOPITT_v8.L3W.20010901_20190228.zip” When unzipped, each archive contains 6057 individual NetCDF (".nc") files that correspond to the daily L3L and L3W data products for the period 2001-09-01 to 2019-02-28, inclusive. Daily files represent the satellite instrument measurements for a single day. Users are referred to the "README.txt" file for a full description of the individual file contents. Note that when unzipped, the products require ~22.5 GB of data storage each (45 GB total for both L3L and L3W). Because of this, a single file from each product has been uploaded separately (file date = “20020801”; see below for naming convention) to facilitate user experimentation before unpacking the full L3L/L3W products. Individual L3L/L3W NetCDF files are ~3.4 MB in size. The individual NetCDF files are named as follows: MOPITT_v8.L3L.from_MOPO2J.selected_variables.YYYYMMDD.nc (replace “L3L” with “L3W” in the filename for the corresponding L3W product.) The date corresponds to the YYYYMMDD that the retrievals were made. E.g. the file “MOPITT_v8.L3L.from_MOPO2J.selected_variables.20020801.nc” corresponds to the L3L product for MOPITT retrievals made on August 1st 2002. Variables contained within the file are described in detail in the "README.txt" file. NetCDF is a common format for gridded geoscientific data, easily readable by all widely used scientific programming languages (e.g. Python, R, Matlab, IDL…), as well as dedicated command line tools (e.g. cdo, gdal). Panoply (https://www.giss.nasa.gov/tools/panoply/) is an alternative application for quickly plotting these data without the requirement of coding experience. Most GIS packages can also handle NetCDF data. An example python code for reading and plotting data from a single L3L file is available here: https://github.com/ianashpole/MOPITT_L3L_L3W/blob/main/example_read_and_plot_MOPITT_L3L.ipynb</p

    Development and optimisation of supercritical fluid deposition of semiconductor films

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    This thesis is concerned with the deposition, and characterisation, of semiconductor thin films and microstructures deposited from a supercritical fluid. Thin films of CdS, GaP, InP, InAs, and Ge were deposited using supercritical CO2 and CO2-solvent mixtures. Ge was deposited into macropores etched into crystalline silicon substrates. A variety of reactors were designed in order to achieve the successful deposition of the materials. The surface morphology and crystallinity of the films were characterised by scanning electron microscopy and X-ray diffraction. The chemical composition of the films was analysed by energy or wavelength dispersive X-ray spectroscopy, secondary ion mass spectroscopy, Auger electron spectroscopy, and X-ray photoelectron spectroscopy. The optoelectronic quality of the CdS and InP films was analysed by photoluminescence spectroscopy and mapping. The CdS films deposited were confirmed to be of hexagonal phase by X-ray diffraction and exhibited band edge luminescence. The InP and InAs films were determined to be of cubic structure and the InP films were found to exhibit weak band edge luminescence. The fabrication of macroporous silicon templates by photoelectrochemical etching is also discussed. Pores with diameters of between 60 nm and 2 µm were fabricated, having aspect ratios of up to 100:1. Ge was successfully deposited into macropores etched into these crystalline silicon templates with near conformal coverage

    Energy resolution of a silicon detector with the RX64 ASIC designed for X-ray imaging

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    Results from a silicon microstrip detector coupled to the RX64 ASIC are presented. The system is capable of single photon counting in digital X-ray imaging, with foreseen applications to dual energy mammography and angiography. The main features of the detecting system are low noise (operation with threshold as low as E4 keV is possible), good spatial resolution (a pixel of 100 mm 300 mm when oriented edge-on) and good counting rate capability (up to one million counts per channel with a maximum rate of about 200 kHz per channel). The energy resolution of the system, as obtained with several fluorescence X-ray lines, is described

    Controls on the production of ground level ozone in Halifax, Nova Scotia

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    1 online resource (96 p.) : colour illustrations, colour mapsIncludes abstract and appendices.Includes bibliographical references (p. 80-88).Atmospheric ozone (O3) is a secondary pollutant produced via complex chemical reactions involving precursors like nitrogen oxides (NOx), Volatile Organic Compounds (VOC) and carbon monoxide (CO). The key to reducing ozone concentrations is to regulate the precursors. Using data from the National Air Pollutant Surveillance (NAPS) program, possible controls on ozone production are examined for Halifax and other regions across Nova Scotia, including meteorological and chemical variables.Long-term trends of ozone and its precursors in Nova Scotia were analyzed to see the effect of emissions regulations across North America. Diurnal and monthly averages were also examined to show short-term patterns in Halifax. It was found that 1-hour average ozone levels are relatively steady in Halifax under decreasing NOx emissions, due to a reduction of the strong NOx titration effect on O3; however, Total Ozone (TO), comprised of O3 and NO2, is decreasing, along with maximum 1-hr ozone. Additionally, it was found that there are no strong signatures of biogenic VOC influence on ozone levels in Halifax (as opposed to anthropogenic VOC), although more frequent measurements of VOC are needed to better study VOC-sensitivity. There is indication from the high NOx levels that ozone production is on the whole VOC-sensitive in Halifax.Lastly, long-range transport was examined during an event of maximum elevated O3 at the background air Aylesford NAPS station in 2016. The high O3 levels were correlated with high values in Halifax and transport to both locations was consistent with pollutant import from the the northeast U.S. Flow to Halifax vs. Aylesford is in general more complicated because there is no obvious correlation between ozone in Halifax and at the Aylesford NAPS station, which requires further study.All of the above findings are policy-relevant in the regulation of ozone precursors

    Comparison of first Saint Mary’s University Open-Path Fourier Transform Infrared (OP-FTIR) spectrometer measurement results with National Air Pollution Surveillance (NAPS) air quality measurements in Halifax

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    1 online resource (171 p.) : ill. (chiefly col.), col. mapsIncludes bibliographical references (p. 167-171).Includes abstract and appendices.The atmosphere is very complex and it involves many chemical and physical processes that affect the air people breathe. This is why it is important to characterize the air in the atmosphere in order to determine what people are exposed to every day. Carbon monoxide (CO), a toxic air pollutant emitted primarily as a result of incomplete combustion and oxidation of hydrocarbons, was measured in Halifax, Nova Scotia using an Open-Path Fourier Transform Infrared (OP-FTIR) spectrometer and compared to National Air Pollution Surveillance (NAPS) CO measurements as a verification step in the characterization of this new instrument. Measured NAPS data was compared to OP-FTIR spectrometer results for three different measurement campaigns: Robie Street (at Inglis for 2 hours), Rice Building (at SMU for ~1 week), and Lake Major (in Dartmouth for ~1 week). For each campaign, spectra were recorded and a concentration of CO was retrieved for each spectrum (one per minute) by the program MALT. The retrieved CO concentrations were plotted in a time series for each campaign and compared to NAPS CO concentration measurements obtained on Barrington Street at the same time. Data quality of the OP-FTIR spectrometer was assessed in detail, with the majority of spectral fit residuals and their RMS values below 0.01 (1%), indicating a reasonable fit between the measured spectra and the fitted spectra simulated by MALT. The technique’s accuracy was previously conservatively estimated to be no worse than 10%; however, for all three campaigns, there was a clear systematic bias of up to 0.35 ppm (a factor of ~3) between the OP-FTIR spectrometer and NAPS measurements, along with unexplained enhancements in CO concentration at times and locations with minimal vehicle activity. Further studies are suggested in order to fully explain the reason for the systematic bias and unusual enhancements in CO concentration observed
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