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齐次边界条件或周期性边界条件下的Laplace场构成Sturm-Liouville型本征值问题。求解本征值问题可得一系列的本征值和对应的本征函数。由这些本征函数构成了对应的Laplace边值问题的级数通解。揭示了用于计算电磁场问题的新型等效源方法(包括圆形等效源方法、矩形等效源方法和矩形-圆形等新源混合算法)和本征值问题之间的内在联系,也即阐明了本征值问题是新等效源方法的理论基础。应用模拟电荷法、多极子法、多极理论和新型等效源方法等方法求解计算电磁场时,有关参数(诸如模拟电荷、内外极或者等效源的数目和位置安排,尤其是模拟电荷电量的大小、内外极的次数或者等效源的阶数等)的选择问题是影响这些方法应用的瓶颈。在计算过程中综合应用解的图形显示和校核点处的计算值的误差大小来确定有关参数,既可以确保解的正确性,又可以极大地提高计算效率和计算精度。 相似文献
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不规则游动网格的蒙特卡罗方法求解船闸地基渗流,与以往各种数值计算方法相比,在计算渗流问题时要更灵活、更方便,它可根据需要独立地计算渗流区内任意一点的渗透压力、渗流流速。 相似文献
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文中通过介绍模拟电荷法计算输电线路电场问题的基本原理和计算步骤,引入了对该方法中模拟电荷点、匹配点、校核点布置方式与计算精度问题的讨论,应用MATLAB计算环境建立了输电线路电场计算实例,在实例中改变电荷点距离和角度,分析了这两种变量与计算精度的关系。结果表明,模拟电荷点间距越小,计算精度越大,电荷与坐标轴夹角对计算精度影响不大。 相似文献
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考虑阻尼力矩和恢复力矩的非线性,运用能量法对正横规则波中船舶非线性横摇运动方程进行等效线性化,导出等效线性系数表达式,并验证其工程实用性,为船舶横摇预报提供理论分析计算模型。 相似文献
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舰船壳体模块感应磁场的等效计算 总被引:1,自引:0,他引:1
典型的舰船壳体是主要由薄钢板和肋骨构成的复杂结构,采用磁矩量法计算其感应磁场时,会碰到数据准备复杂,剖分单元数目过多的问题。按照横截面积与磁化率乘积相等的原则,将舰船壳体模块等效简化为一个各向异性的简单薄钢板结构。针对一个有代表性的数值算例,采用磁矩量法分别计算简化前、后舰船壳体模块的感应磁场,并对比计算结果。研究发现,等效前后的计算误差不超过1.5%,证明所提出的磁性等效方法不仅能简化数据准备工作,而且还可以减少单元数目,对于磁矩量法计算非常有利,能够作为计算舰船壳体感应磁场的一条可行途径。 相似文献
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极低频发射天线场地等效电阻率的计算 总被引:3,自引:0,他引:3
通过对均匀半空间有限长导线源辐射场强的理论分析,表明极低频发射天线场地等效电阻率主要由天线两端接地点的位置决定。文章对MT法测量的视电阻率数据的处理和天线等效电阻率计算方法上提出了几点看法,以供参考。 相似文献
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介绍了我国港口资源的整合现状,指出港口整合可以提升港口的形象和地位,也为区域经济和城市的发展注入强大的动力。最后指出在港口资源整合中要避免的几个问题。 相似文献
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广州集装箱码头的轮胎式场桥小车制动器使用10多年后,出现了许多问题,故进行了改造.分析了轮胎式集装箱龙门起重机小车制动器的主要故障现象,提出了改造方案,并加以实施. 相似文献
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本文对现有的选定球面轴承的三种工程方法进行了分析比较.引入了“合力系数”,并给出了合力方向上投影面积的精确解. 相似文献
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分析柴油机故障中常见的机体裂纹故障原因,认为由于设计缺陷和管理及操作不当,易造成船舶柴油机缸体上的裂纹多发生在气缸套凸肩处。如不及时处理这些裂纹和故障,就会造成缸套的裂纹直至出现缸套漏水等严重后果,针对NANTAIQUEEN轮柴油机对该类型故障的检修提出具体措施。 相似文献
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The hydrophysical and hydrochemical structure of the Sea of Azov, with developed bottom anoxia, was studied during the RV “Akvanavt” cruise from July 31 to August 03, 2001. The anoxic zone with a thickness from 0.5 to 4 m above the bottom was found in all deep regions of the Sea. Concentrations of hydrochemical parameters were similar to the pronounced anoxic conditions (about 90 mmol m− 3 of hydrogen sulfide, 17 mmol m− 3 of ammonia, 6 mmol m− 3 of phosphate, 7 mmol m− 3 of total manganese). The hydrophysical structure was characterized by the uniform distribution of temperature in the upper 6–7 m mixed layer (UML). Below this a thin (0.4–0.8 m) thermocline layer was observed, just above the anoxic waters. Formation of this phenomenon was connected with that summer weather conditions. Intensive rains led to increased influx of river waters in June. That resulted in large input of allochtonous organic matter (OM) and inorganic nutrients; the latter were consumed on the additional autochthonous organic matter production. In July the weather was characterized by a significant rise in the daily averaged air temperature and large oscillations of temperature during the day. In this period a wind of constant direction was absent, but wind bursts were observed. The completed analyses showed that the formation of such a structure could be connected with the following factors: (i) positive growth trends of the daily averaged temperature and the daily oscillations of temperature, (ii) presence of wind bursts. The joint action of these factors resulted in the formation of the UML. The amplitude of wind bursts determined the depth of UML, and the value of trend determined the value of the temperature change in the thermocline. An initial presence of bottom halocline (caused by the Black Sea water influx to the bottom of the Sea of Azov) prevented the heating of the bottom layer and therefore led to an increase of vertical gradient of temperature in the thermocline. The spatial distribution of the turbulent exchange coefficient confirmed the existence of a “stagnation” area located above the anoxia zone, which is also, apparently, the reason for its occurrence. 相似文献