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511.
Szutowicz Sławomira Królikowska Małgorzata Sitarski Grzegorz 《Earth, Moon, and Planets》2002,90(1-4):119-130
The role of non-gravitational forces in the evolution of orbitalmotion of C/1995 O1 (Hale–Bopp) has been investigated. Inorbital
calculations the observational material covering theperiod from April 1993 up to August 2001 was used. To model thenon-gravitational
acceleration, observed and theoretical profilesof the H2O production rates were employed. A set of forcedprecession models of a rotating cometary nucleus consistent withthe observed
spin axis orientation was fitted to positionalobservations. The non-gravitational models allowed us to constrainthe mass and
radius of the comet. The orbitalevolution of Comet Hale–Bopp was investigated over ±400 k yusing two sets of randomly varied
orbital elements wellrepresenting all positional observations in the pure gravitationalcase, as well as in the non-gravitational
case. The calculationsshowed that the comet's motion is predictable only over an interval ofa few orbital periods. The statistical
conclusions changesignificantly when non-gravitational effects are included in the analysis. 相似文献
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J. Bauer W. Puła 《Georisk: Assessment and Management of Risk for Engineered Systems and Geohazards》2015,9(4):242-249
ABSTRACTThe work presents calculations of shaft support reliability index during partial extraction of protection pillar deposit and the related seismic phenomena. It has been assumed that the probability of failure caused by seismic phenomena depends on the velocity random variable of the shaft support vibrations. The random vibration velocity is a function of random variables of energy, shock distance and vibration frequency. Estimations of probability distributions for energy and frequency have been based on the actual measurement data from a mine. Failure probability has been estimated by means of methods based on so-called Hasofer-Lind reliability index β. 相似文献
514.
Jóźwiak Waldemar Nowożyński Krzysztof Mazur Stanisław Jeż Maciej 《Surveys in Geophysics》2022,43(5):1563-1586
Surveys in Geophysics - This paper presents a three-dimensional (3-D) model of the resistivity distribution in the European lithosphere at the junction between the East European Craton, the... 相似文献
515.
Winkelmann Karol Żyliński Kamil Korzec Aleksandra Górski Jarosław 《Geotechnical and Geological Engineering》2022,40(9):4705-4720
Geotechnical and Geological Engineering - This work conducts a probabilistic inquiry on how the variability of the parameter defining soil deformability affects the settlement of the foundation... 相似文献
516.
Snow Accumulation on a Small High‐Arctic Glacier Svenbreen: Variability and Topographic Controls 下载免费PDF全文
Jakub Małecki 《Geografiska Annaler: Series A, Physical Geography》2015,97(4):809-817
One of the main controls on the net mass change of land‐terminating Arctic glaciers is the magnitude and distribution of snow accumulation. In Dickson Land, region of Svalbard with the greatest distance to the sea, the issue has not been receiving much scientific attention for decades. In this paper, new snow accumulation data are presented from Svenbreen in Dickson Land from end‐of‐winter surveys. The measured winter balance was 0.42 ± 0.15 m w.e. in 2010, 0.50 ± 0.10 m w.e. in 2011 and 0.62 ± 0.10 cm w.e. in 2012. Snow depth and water equivalent have been analysed in the background of altitude, slope and aspect extracted from the digital elevation model of the glacier. On steep northern slopes (>15°) accumulation was the highest, whereas it was decreased on southern slopes with moderate inclination (9–12°). Elevation, which on many glaciers proved to be highly correlated with snow depth, explained only 17–34% of snow depth variability due to complex interplay between local climate and geometry of a small valley. 相似文献
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