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911.
The spinel solid solution was found to exist in the whole range between Fe3O4 and γ-Fe2SiO4 at over 10 GPa. The resistivity of Fe3−
x
Si
x
O4 (0.0<x<0.288) was measured in the temperature range of 80∼300 K by the AC impedance method. Electron hopping between Fe3+ and Fe2+ in the octahedral site of iron-rich phases gives a large electric conductivity at room temperature. The activation energy
of the electron hopping becomes larger with increasing γ-Fe2SiO4 component. A nonlinear change in electric conductivity is not simply caused by the statistical probability of Fe3+–Fe2+ electron hopping with increasing the total Si content. This is probably because a large number of Si4+ ions occupies the octahedral site and the adjacent Fe2+ keeping the local electric neutrality around Si4+ makes a cluster, which generates a local deformation by Si substitution.
The temperature dependence of the conductivity of solid solutions indicates the Verwey transition temperature, which decreases
from 124(±2) K at x=0 (Fe3O4) to 102(±5) K at x=0.288, and the electric conductivity gap at the transition temperature decreases with Si4+ substitution.
Received: 15 March 2000 / Accepted: 4 September 2000 相似文献
912.
The electronic structure of the three polymorphs of Al2SiO5, andalusite, sillimanite, and kyanite, is studied by linearized-augmented-plane-wave (LAPW) calculations using the WIEN code.
Total energy calculations verify, in agreement with recent pseudopotential calculations, that andalusite is the most stable
phase, followed by sillimanite and kyanite.We determine the electronic charge density distribution and find strong polarizations
on all oxygen ions. We identify different polarizations due to Al or Si neighbors which depend on their respective distances
to the oxygen atom. The chemical bonding is not purely ionic in nature but has important covalent contributions. Electric
field gradients (EFGs) at all sites are calculated and agree well (within 10%) with available experimental data on Al. We
identify the origin of the EFGs and demonstrate its relation to the nearest-neighbor coordination and the resulting anisotropy
of the electronic charge distribution.
Received: 22 March 2000 / Accepted: 3 August 2000 相似文献
913.
福建龙卷风的活动特点 总被引:11,自引:1,他引:11
分析福建千余年25次的龙卷风记载,得出如下几点认识:(1)福建的龙卷均在春夏两季,且几率相近;1949年以来的12次龙卷有11次出现于13-18时(占92%),另一次是上午9时(占8%)。空间分布为:沿海地区有20次,占80%,内陆5次,占20%,且有多发挥地段,(2)龙卷风多出现于低压,高温,高湿点附近,天空以积雨云占多数,地面多有强风相伴,(3)福建12次龙卷风的诱发系统为:台风(6次,均在7 相似文献
914.
915.
916.
S. M. El shazly 《大气科学进展》1996,13(3):349-358
The performance of two models,Jam and Baig,based on the modified version of Gaussian distribution function in estimating the daily total of global solar radiation and its distribution through the hours of the day from sunrise to sunset al any clear day is evaluated with our own measured data in the period from June 1992 to May 1993 in Qena Egypt The results show a high relative deviation of calculated values from measured ones,especially for Jain model,in the most hours of the day,except for those near to local noon.This misfit behavior is quite obvious in the early morning and late afternoon A new approach has been proposed in this paper to estimate the daily and hourly global solar radiation This model performs with very high accuracy on the recorded data in our region.The validity of this approach was verified with new measurements in some clear days in June and August 1994.The resultant very low relative deviation of the calculated values of global solar radiation from the measured ones confirms the 相似文献
917.
采用动力学方程,求解了定态情况下磁层中上行离子沿磁力线的分布函数,针对不同的Kp指数,分别对北半球极光带区起源的上行离子O+、H+和He+在子午面内沿磁力线的密度分布及其特性进行了研究.结果表明:1.沿磁力线向外,上行离子密度在近地空间呈急剧下降趋势,在远地空间呈缓慢下降趋势;2.重离子或初始能量较小的离子,其密度沿磁力线向外下降较快;3.Kp指数越大,离子进入磁层的空间范围越大;4.离子的投掷角分布对密度分布的影响甚小;5.离子密度沿磁力线的下降程度随到X轴距离的增大而呈增大趋势;6.在典型参数条件下,求得上行离子O+在等离子体片边界附近的密度为10-3-10-2个cm-3,这与观测结果相一致. 相似文献
918.
潜在震源区内部空间非均匀分布地震区划方法在攀西地区和晋中南地区的应用 总被引:2,自引:1,他引:2
本文依据潜在震源区内部地震非均匀分布模型研究了攀西地区和晋中南地区地震区划问题。研究结果表明,一般使用的均匀分布模型会低估地震危险性结果,导致高烈度分区的面积缩小。本文讨论了不同的确定非均匀分布概率的方法对地震区划结果的影响。 相似文献
919.
In this paper we study the rooted tree model applying the concepts of probability to obtain results of importance in understanding power-law distributions in pure populations and also in an ensemble of pure populations. The well-known Gutenberg-Richter relation, which is an empirical relation providing the number of earthquakes whose magnitude exceeds a given value, is shown to be an asymptotic form of survivor function of earthquake magnitudes. The implications of this model are briefly discussed in relation to other branches of sciences where power-law distributions are encountered. 相似文献
920.
J. -H. Heo J. D. Salas 《Stochastic Environmental Research and Risk Assessment (SERRA)》1996,10(3):187-207
The log-Gumbel distribution is one of the extreme value distributions which has been widely used in flood frequency analysis. This distribution has been examined in this paper regarding quantile estimation and confidence intervals of quantiles. Specific estimation algorithms based on the methods of moments (MOM), probability weighted moments (PWM) and maximum likelihood (ML) are presented. The applicability of the estimation procedures and comparison among the methods have been illustrated based on an application example considering the flood data of the St. Mary's River. 相似文献