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  • PANGAEA  (164)
  • International Union of Crystallography (IUCr)  (4)
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  • 1
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 31 (1998), S. 820-822 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: Superscrew dislocations are visible in back-reflection synchrotron white-beam X-ray topographs of basal-cut SiC wafers in striking contrast as black rings surrounding white circles, even though such topographs suffer from extensive harmonic contamination. The contributions to the synchrotron white-beam topograph of each member of its series of harmonic reflections, {\bf g}=(0006n), where n=3 to 16, were calculated. Through intensity considerations and comparison with a {\bf g}=00018 topograph taken with Cu Kα1 radiation, the {\bf g}=00024 harmonic was determined to be the most important contributor. The contrast of features lying deep beneath the crystal's surface was attributed to higher harmonics with larger penetration depths.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 34 (2001), S. 20-26 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: Contrast is associated with micropipes in X-ray topographs of SiC crystals obtained with prismatic reflections, representing an apparent violation of the g·b = 0 invisibility criterion. This is explained as a population of basal-plane dislocations with Burgers vectors of the set b = {\textstyle{1 \over 3}}〈11{\bar{2}}0〉 that occur in a high density within a few micrometers of the micropipes, below the resolution of X-ray topography. These basal-plane dislocations could be observed under an electron microscope. The presence of the surfaces of the micropipes influences the dislocation images in the topographs taken with prismatic reflections, often resulting in a band of light contrast along the axes of the micropipes.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Acta crystallographica 55 (1999), S. 272-275 
    ISSN: 1399-0047
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: RCC1, the regulator of chromosome condensation, is the guanine nucleotide-exchange factor (GEF) of the GTP-binding protein Ran. Its GEF activity on Ran makes it a key element in nucleo-cytoplasmic transport and cell-cycle regulation. Crystals of human RCC1 suitable for X-ray analysis have been obtained using the seeding technique in hanging drops with sodium citrate as a precipitant. The crystals diffract to 1.7 Å at 100 K and belong to the space group P1, with unit-cell parameters a = 49.5, b = 84.3, c = 84.9 Å, α = 113.0, β = 103.9,γ = 103.3°. The Matthews parameter (Vm) and the self-rotation function are consistent with three molecules in the unit cell, which is confirmed by the averaged single isomorphous replacement (SIR) electron-density map.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Copenhagen : International Union of Crystallography (IUCr)
    Applied crystallography online 32 (1999), S. 516-524 
    ISSN: 1600-5767
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Geosciences , Physics
    Notes: A kinematic (geometrical) diffraction simulation model has been developed to provide understanding of direct dislocation images on synchrotron white-beam X-ray topographs, and has been successfully applied to illustrate the contrast formation mechanisms involved in images of micropipe-related superscrew dislocations in silicon carbide crystals. The coincidence of the simulations with the contrast features of the superscrew dislocation images, recorded using a series of synchrotron topography techniques, shows that this model is capable of revealing the detailed diffraction behavior of the highly distorted region around the dislocation core and determining the quantitative characteristics of the dislocations. The simulation technique is thus demonstrated to be a simple but efficient method for interpretation of synchrotron topographs, and may be applied to explain the topographic contrast characters of general crystal defects.
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2023-05-12
    Description: The Vernagtferner region has a long tradition of glaciological research performed by groups from Munich. It started in 1889, when Prof. Sebastian Finsterwalder from the Technical University in Munich produced the first map of a complete glacier based on terrestrial photogrammetry. Since then, numerous maps of the glacier have been made, describing the change in surface elevation for more than a century. These maps form the basis of the geodetic method of glacier mass balance determination, which provides volume changes as average data for the period between two surveys, i.e. typically for 10 years. Since the start of the glaciological method on Vernagtferner in 1964, annual as well as winter and summer mass balance data are available continuously. But only since 1973, the construction of the Vernagtbach station, approximately 1 km below the glacier margin at that time, provided the means to record a larger number of hydrological and meteorological parameters with a temporal resolution of typically 1 hour.
    Keywords: Glaciers Austria; Pegelstation_Vernagtbach; Pegelstation_Vernagtbach_meteorology; UGS; Unmanned gauge station; Unmanned weather station/meteorological observation; UWST; Vernagtferner, Ötztaler Alpen, Austria
    Type: Dataset
    Format: application/zip, 87 datasets
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  • 6
    Publication Date: 2023-01-13
    Description: In November 2001, two separate Campbell loggers ("Meteologger" and "Hydrologger", both type CR23X) were installed at the Vernagtbach site in the Oetztal Alps, Austria (Latitude: 46.85; Longitude: 10.82; Elevation: 2640 m). On these loggers, 10-minutes centred averages for the meteorological data and 5-minutes centred averages for the hydrological data are recorded. The meteorological parameters comprise air temperature, humidity of the air, air pressure, four radiation components, wind direction and speed, precipitation and snow height. For air temperature, two records are published, recorded with a ventilated and an unventilated Pt-100 in a Stevenson screen; for precipitation, three time series are available: (I) the cumulative record of a weighing gauge for the whole year, (II) single events derived from (I), and (III) single events from a tipping bucket; (II) and (III) are only provided for the period 1, May to 31, October of each year. Wind records are also given with a time step of one hour, as only these records include several statistics of speed and direction. Hydrological parameters are recorded on the "Hydrologger", they comprise water stage, discharge, water temperature and electrolytic conductivity of the water. An identifying number gives the kind of instrument used in the water stage time series. Daily photographs of the glacier are provided and analysed with respect to precipitation type.
    Type: Dataset
    Format: application/zip, 46 datasets
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  • 7
    Publication Date: 2023-01-13
    Description: The first meteorological station in the Vernagtferner basin, called 'Gletschermitte' was run from 1968 to 1987. It was positioned on a small rock in the western part of the glacier at an elevation of 3078 m a.s.l. The coordinates were 46.868939° N (Latitude) and 10.802986° E (Longitude). The following parameters were recorded mainly during the summer months: Wind speed and wind direction, air temperature and humidity of the air and precipitation. The records of the first four parameters comprise hourly values from 1968 to 1986 /1987, daily sums of precipitation run from 1977 to 1987. All quantities were recorded on paper chart, i.e. 'Woelfle-Windschreiber' for the wind components, mechanically driven thermo-hygrographs (1968 to 1975) and 'BTW-Langzeit-Thermo-Hygrograph' (1977 to 1987) for temperature and humidity, Belfort analogue weighing gauge for precipitation. In 1976, air temperature was recorded on a Schenk paper chart recorder. In addition, photographs of the eastern part of Vernagtferner were taken once a day in summer between 1981 and 1986.
    Type: Dataset
    Format: application/zip, 20 datasets
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  • 8
    Publication Date: 2023-01-13
    Keywords: Anemometer, Wölfle; DATE/TIME; HEIGHT above ground; Temperature, air; Thermograph, Wilhelm Lambrecht; Unmanned weather station/meteorological observation; UWST; Vernagtferner_Gletschermitte; Vernagtferner, Ötztaler Alpen, Austria; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 3997 data points
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  • 9
    Publication Date: 2023-01-13
    Keywords: Anemometer, Wölfle; DATE/TIME; HEIGHT above ground; Temperature, air; Thermograph, Wilhelm Lambrecht; Unmanned weather station/meteorological observation; UWST; Vernagtferner_Gletschermitte; Vernagtferner, Ötztaler Alpen, Austria; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 6281 data points
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  • 10
    Publication Date: 2023-01-13
    Keywords: Anemometer, Wölfle; DATE/TIME; HEIGHT above ground; Temperature, air; Thermograph, Wilhelm Lambrecht; Unmanned weather station/meteorological observation; UWST; Vernagtferner_Gletschermitte; Vernagtferner, Ötztaler Alpen, Austria; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 10501 data points
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