助手标题
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
共[1582]条 当前为第1条到20条[由于搜索限制,当前仅支持显示前5页数据]
 

相关语句
equations of
    Use of Oxygen Bonds to Calculate Fractionation Equations of Oxygen Isotope for Minerals Containing Kyanite and Staurolite
    利用氧键计算兰晶石、十字石等矿物的氧同位素分馏方程
    INVERSE PROBLEMS OF THE FUZZY COMPREHENSIVE ESTIMATION OF <MAX-PRODUCT>TYPE-ON THE FUZZY RELATION EQUATIONS OF<MAX -PRODUCT> TYPE
    〈Max—product〉Fuzzy综合评判的逆问题—〈Max—product〉Fuzzy关系方程
    THE NONLINEAR INTERACTION BETWEEN ROSSBY WAVE AND INERTIAL-GRAVITY WAVE IN THE MIDDLE ATMOSPHERE (Ⅰ)THE EQUATIONS OF NONLINEAR INTERACTION
    中层大气Rossby波与惯性重力波的非线性相互作用 (Ⅰ)相互作用方程
    On the basis of laboratory and in-situ test data,the equations of regression among saturated uniaxial compressive strength and saturated unit weight and point loading strength and modulus of secant and triaxial compressive strength of politic siltstone rock in Fuzhou have been established.
    本文对抚州泥质粉砂岩的饱和单轴抗压强度与其它物理量之间相关性进行了对比试验研究,通过回归分析,建立了饱和重度与饱和单轴抗压强度、点荷载试验强度与饱和单轴抗压强度以及饱和单轴抗压强度与割线模量和三轴抗压强度的相关方程,初步实现了由易测的物理量估算难测或测试技术要求高的物理量。
    Solution for Motion Equations of Soil pile structure Systems
    土-桩-结构系统运动方程的求解方法
    Regression Equations of Content P 2O 5 and Other Chemical Compositions in Phosphorus Ore in Centrul Yunnan
    滇中磷矿P_2O_5与其它组份含量的回归方程建立
    Viscoelastic wave equations of seismic multi-wave in fractured media
    裂缝性地层黏弹性地震多波波动方程
    Comparison on several time-distance equations of reflecion wave
    几种反射波时距方程的比较
    CONSTITUTIVE EQUATIONS OF SOILS AND THERMODYNAMICS
    土的本构方程与热力学
    Molecular dynamic simulation of MgSiO_3 perovskite: the effects of sizes on elasticity properties and equations of state
    钙钛矿结构MgSiO_3的分子动力学研究——体系大小对弹性性质与状态方程的影响
    The governing equations include the conservation equations of mass, momentum and energy, as well as the state equation.
    采用热-流体连续介质的动量守恒方程、能量守恒方程和质量守恒方程,并引入了流体热力学的状态方程描述地幔对流和造山动力学过程.
    The amplitude characteristic equations of P wave and S wave in transverse isotropic media have been deduced by using the method of Aki and Richards, that is use the border conditions in elastic interface to solve the elastic wave equation and to decide the energy distribution of different types of wave.
    本文针对横向各向同性介质(TI-Transverse Isotropy),利用Aki和Richards的方法,即根据弹性分界面上的边界条件求解弹性波动方程,确定各种波之间的能量分配关系,建立了横向各向同性介质中P波和SV波入射时的振幅特征方程
    Then, by means of a iterative method of computation, equations of medium range prediction for strong earthquakes, M≥ 6 of the six regions and for earthquakes, M≥7 of both the Sichuan and Yunnan provinces.
    由此,通过一种迭代算法,又分别导出了6个 M≥6的强震活动区和川、滇两省 M≥7的强震的中期预报方程.
    The error of mathematical model is mostly resulted from near properties of the equations of trend surface.
    数学模型误差——主要由趋势面方程的逼近特性所引起.
    Therefore,the equations of trend surface are not suitable for the tool of calculation.
    所以趋势面方程不宜作为精确计算的工具.
    The differential equations of motion of a hysteresis friction base isolation system under earthquake action are established and the earthquake ground motion is modeled as a twice filtered Gaussian white noise process with zero mean.
    本文建立了滞变-摩擦基底隔震系统在地震作用下的运动微分方程,并将地震地面运动模拟成均值为零的两次过滤Gaus白噪声过程。
    The equations of motion of active tendon-adjacent building systems are established first.
    首先,建立了主动锚索相邻建筑系统的运动方程
    The recursive equations of SiO_2, quartz, quartz+feldspar, and the differentiation index (DI) versus V_p have been set up on the basis of the data obtained at normal temperature and high pressure (600 MPa), with a discussion on their application scope.
    选择常温、600MPa测定的数据建立了地震波速Vp与SiO2、石英、石英+长石、岩石分异指数DI的回归方程,并讨论了回归方程的适用范围。
    The generalized expressions of displacements,strains and stresses for general and simplified Biot's equations of consolidation are expressed in terms of the potential functions.
    获得Biot固结方程和简化Biot固结方程的位移、应变和应力的势函数通解表达式。
    According to the tectonic and sedimentary characteristics of Xuanhan-Daxian area,northeastern Sichuan basin,aimed at the existing geological traits of every set of erosion strata,the authors have restored the strata erosion thickness of the area in the key structure transform period by use of acoustic transit time,Ro-H,fluctuate analysis and thickness of nearby layer contrast,and erected the fluctuate equations of sediment and erosion section of 12 typical wells in the study area.
    在川东北宣汉—达县地区构造沉积特征分析的基础上,针对遭受剥蚀的各套地层的实际地质特点,利用泥岩声波时差、镜质体反射率(Ro-H)、波动分析和相邻层地层厚度对比等多种方法,对各关键构造变革时期地层的剥蚀厚度进行了研究,并建立了研究区12口典型井的沉积—剥蚀过程的波动方程
 

首页上一页12345下一页尾页 

 
CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社