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 the reciprocity principle 互惠原则(0)互易定理(2)
 互易定理
 We treat magnetic dipoles as circulation equivalently,apply the reciprocity principle,and give a method of the spatial distribution of a magnetic field. 对磁偶极子作环流等效处理 ,应用互易定理 ,给出了确定磁场空间分布的一种方法 . 短句来源 In this paper, based on the integral equation of ground wave attenuation factor and the reciprocity principle, a new solution of lateral wave propagation along irregular and inhomogeneous ground has been obtained. 以沿不均匀地面传播的地波衰减因子所满足的积分方程算法以及互易定理出发,导出了适用于不规则不均匀地面传播的侧面波一般公式,并进行了数值计算。 短句来源
 “the reciprocity principle”译为未确定词的双语例句
 The BSMC method (Bi-directionally Statistical Monte Carlo Method) is an improvement of the conventional MC method (CMC), which is based on the reciprocity principle of radiative transfer. BSMC法(Bi-directionally Statistical Monte Carlo Method)是一种基于热辐射传递可逆性原理的改进蒙特卡罗法。 短句来源 In the two-dimensional interpretation, we adopt the point source finite-element method and the reciprocity principle which can lighten the calculation burden. 二维解释是采用点源有限单元法,为减少计算量,利用了互换原理。 短句来源 Based on the reciprocity principle of radiation transfer, a bidirectionally statistical Monte Carlo method (BSMC method) was presented. 基于热辐射传输的光路可逆性原理,提出了求解介质内热辐射传递的双向统计蒙特卡罗法(BSMC法)。 短句来源 Magnetic Field Created by Magnetic Dipole beyond the Mid-vertical plane Using the Reciprocity Principle 用互易~[1]法求磁偶极子中垂面远处的磁场 短句来源 The method starts with the eikonal equation and calculates all kinds of travel times and raypaths using the reciprocity principle and fermat principle,so it solves the problems in the ray tracing calculation. 该方法从程函方程出发，利用互换原理和Fermat原理计算出各种波的到时和射线。 解决了射线追踪方法存在的问题。 短句来源 更多
 相似匹配句对
 On the Principle of Reciprocity 论对等原则 短句来源 Be Internationalized in Reciprocity Era 对等时代的国际化思路 短句来源 Diversity Communication&Reciprocity 相异 沟通 互惠——采访日本丸红(北京)商业贸易有限公司粮油食品部部长伊藤武司 短句来源 On the Conception of Reciprocity of Justice 关于正义的互惠性概念 短句来源 On the Reciprocity and Integration of Leisure and PUS 论PUS与休闲的互动与融合 短句来源

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 the reciprocity principle
 The use of the reciprocity principle in problems of the radiation of moving charges Properties of the transformation matrix resulted from the reciprocity principle and the energy conservatin law are studied. On the Reciprocity Principle in the Scattering of Plane Electromagnetic Waves by a Conic Scatterer Energy flux density and the reciprocity principle for electromagnetic waves in absorbing uniaxial crystals An algorithm and code for stochastic modeling of the radiant heat transfer inside cavities has been developed on the basis of the reciprocity principle and backward ray tracing. 更多
 The different distributive behaviors of the current density at variousdepths under ground are compared for a point contact source, a currentelectrode pair of source and a focused current system. A calculationexample is given, which is about the penetration capability of the focusedsystem's underground current through the horizontal two-layer with a lowresistivity overburden. Shown tbe quantitative laws of the shielding effect from a low resisti-vity overburden. Using the reciprocity principle for potential,... The different distributive behaviors of the current density at variousdepths under ground are compared for a point contact source, a currentelectrode pair of source and a focused current system. A calculationexample is given, which is about the penetration capability of the focusedsystem's underground current through the horizontal two-layer with a lowresistivity overburden. Shown tbe quantitative laws of the shielding effect from a low resisti-vity overburden. Using the reciprocity principle for potential, the relationformulas between both the resistivity of the pole-pole array and thefocusing potential arrangement are given. According to these results,pointed out that tbe pole-pole array can be used to replace the focusingpotential arrangement in actual work, which will get a lot of advdntages.The relation formulas of the apparent chargeability between the pole-polearray and the focused arrangement are also given on the reciprocityprinciple. It is pointed out that the pole-pole array can replace the focusedarrangement in IP method. Finally, the relation of apparent resistivitybetween thep ole-pole array and the focused gradient arrangement isdiscussed, and the results of the scale-model experiment for proying aregiven. 对聚焦供电系统与单个点源和两个异性点源地中电流随深度变化的分布特征作了比较。以二层水平地层为例,对聚焦法供电系统地中电流穿透低阻复盖层的能力给出了计算结果并作了分析,指出了聚焦法受低阻复盖层屏蔽作用的数量规律。利用互换原理给出聚焦电位法与二极法其视电阻率之间的关系式,并依此指出在野外实际工作中用二极法代替聚焦电位法的有益之处。根据互换原理给出了聚焦电位法与二极法其视极化率之间的关系式,并依此指出在激发极化法中用二极法代替聚焦电位法的优点。最后,讨论了聚焦梯度法与三极联合剖面法其视电阻率的关系,并给出验证性的模型实验结果。 A method to measure several forces exciting a structure simultaneously is proposed. It is based on the theorem of exchange energies which can be considered as a multiple application of the reciprocity principle. First experiments using the method showed measure errors to be only a few dB. The calculated phases agreed reasonably well with the measured data. It is recommended to use more than the minimum number of measuring points to increase the reliability of the method. 本文介绍了在一个结构中如何同时测量几个激励力的一种方法。该方法称为能量交换原理,它是在互易原理的基础上建立起来的。该试验给出的误差只有几个分贝,而相位误差与实际值吻合得很好。 Geoelectricity variations are complicated in igneous rock area, where the conditions of horizontal bedded media cannot be met and the quantitative interpretation of electrical sounding data is difficult. For the first time, we have tried two-dimensional interpretation of electrical sounding in northwestern sector of the Yangxin rock mass and achieved good re-sults. In the two-dimensional interpretation, we adopt the point source finite-element method and the reciprocity principle which can lighten the... Geoelectricity variations are complicated in igneous rock area, where the conditions of horizontal bedded media cannot be met and the quantitative interpretation of electrical sounding data is difficult. For the first time, we have tried two-dimensional interpretation of electrical sounding in northwestern sector of the Yangxin rock mass and achieved good re-sults. In the two-dimensional interpretation, we adopt the point source finite-element method and the reciprocity principle which can lighten the calculation burden. The two-dimensional interpretation can be divided into four steps: 1. Forming initial geoelectric section model, after the one-dimensional interpretation generally; 3. Carrying out forward calculation with computer and repeating interactive modification until sat-isfactory results have been obtained; 4. Geological interpretation for calculation results. Compared with one-dimensional interpretation, the two-dimensional interpretation of electrical sounding can help us to study geological structures and boundaries more distinctly and accurately. 火成岩分布区,地电变化复杂,不能满足水平层状介质条件,造成电测深资料定量解释困难。我们首次在阳新岩体西北段进行了电测深二维解释的尝试,并取得了较好效果。二维解释是采用点源有限单元法,为减少计算量,利用了互换原理。二维解释工作可分为四个阶段:(1)构组初始地电断面模型,通常在一维解释成果基础上进行,(2)部分:将地电断面划分为计算小单元;(3)用计算机进行正演计算,不断迭代修改,直至得到满意的给果;(4)计算结果的地质解释。与一维解释结果对比,用电测深二维解释方法研究剖面的构造特征、划定地质界线比较清晰准确。 << 更多相关文摘
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