Memory-Efficient Categorical Multi-point Statistics Algorithms Based on Compact Search Trees   总被引：1，自引：1，他引：0  

Tuanfeng Zhang  Stein Inge Pedersen  Christen Knudby  David McCormick 《Mathematical Geosciences》2012,44(7):863-879

Multi-point statistics (MPS) has emerged as an advanced geomodeling approach. A practical MPS algorithm named snesim (simple normal equations simulation), which uses categorical-variable training images, was proposed in 2001. The snesim algorithm generates a search tree to store the occurrence statistics of all patterns in the training image within a given set of search templates before the simulation proceeds. The snesim search tree concept makes MPS simulation central processing unit efficient but consumes large amounts of memory, particularly when three-dimensional training images contain complex patterns and when a large search template is required to ensure optimal reproduction of the image patterns. To crack the memory-restriction bottleneck, we have developed a compact search tree that contains the same information but reduces memory cost by one order of magnitude. Furthermore, the compact structure also accelerates MPS simulation significantly. Such remarkable improvement makes MPS a more practical tool to use in building the large and complex three-dimensional facies models required in the oil and gas industry.  相似文献   

Surface passivation model explains pyrite oxidation kinetics in column experiments with up to 11 bars <Emphasis Type="Italic">p</Emphasis>(O<Subscript>2</Subscript>)     

Marton Berta  Frank Dethlefsen  Markus Ebert  Karsten Gundske  Andreas Dahmke 《Environmental Earth Sciences》2016,75(16):1175

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The pseudometeorite Angara     

Holger Pedersen 《Meteoritics & planetary science》2013,48(6):1091-1095

Several pallasites are known to have formed strewn fields with multiple fragments. Therefore, it seems possible that the famous Krasnojarsk pallasite—the Pallas Iron of 687 kg—could have been accompanied by one or more additional fragments that had not been recovered due to incomplete observations from the overgrown and remote place of fall. During a survey for literature accounts of distant fragments in such a hypothetical strewn field, a report of native iron was found, dating to 1847. The fragments of nickel‐free iron—amounting to at least a few kg—had been recovered 1836–1843 during placer gold mining north of the Angara River. The position of these finds is coincident with Burovaya, Murozhna, and Uderei, the three known fragments of the pseudometeorite Angara, all collected in 1885.  相似文献   

Concerning the generation of geomagnetic giant pulsations by drift-bounce resonance ring current instabilities     

K.-H. Glassmeier  S. Buchert  U. Motschmann  A. Korth  A. Pedersen 《Annales Geophysicae》1999,17(3):338-350

Giant pulsations are nearly monochromatic ULF-pulsations of the Earth’s magnetic field with periods of about 100 s and amplitudes of up to 40 nT. For one such event ground-magnetic observations as well as simultaneous GEOS-2 magnetic and electric field data and proton flux measurements made in the geostationary orbit have been analysed. The observations of the electromagnetic field indicate the excitation of an odd-mode type fundamental field line oscillation. A clear correlation between variations of the proton flux in the energy range 30–90 keV with the giant pulsation event observed at the ground is found. Furthermore, the proton phase space density exhibits a bump-on-the-tail signature at about 60 keV. Assuming a drift-bounce resonance instability as a possible generation mechanism, the azimuthal wave number of the pulsation wave field may be determined using a generalized resonance condition. The value determined in this way, m = −21±4, is in accord with the value m = −27±6 determined from ground-magnetic measurements. A more detailed examination of the observed ring current plasma distribution function f shows that odd-mode type eigenoscillations are expected for the case ∂f/∂W ≥ 0, much as observed. This result is different from previous theoretical studies as we not only consider local gradients of the distribution function in real space, but also in velocity space. It is therefore concluded that the observed giant pulsation is the result of a drift-bounce resonance instability of the ring current plasma coupling to an odd-mode fundamental standing wave. The generation of the bump-on-the-tail distribution causing ≥f/≥W ≥ 0 can be explained due to velocity dispersion of protons injected into the ring current. Both this velocity dispersion and the necessary substorm activity causing the injection of protons into the nightside magnetosphere are observed.  相似文献   

Determination of the crustal structure in southern Tibet by dispersion and amplitude analysis of Rayleigh waves   总被引：2，自引：0，他引：2  

N. Cotte  H. Pedersen  M. Campillo  J. Mars  J. F. Ni  R. Kind  E. Sandvol  & W. Zhao 《Geophysical Journal International》1999,138(3):809-819

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