均方根速度

  • 网络rms;Root mean square velocity;Even Square Velocity;Even Square Root Velocity;root-meall-square velocity
均方根速度均方根速度
  1. 根据地震勘探中的CDP资料,可以提取每个反射层的平均速度、层速度以及均方根速度,利用这些速度参数可以预测地层压力和计算钻井用的泥浆比重。

    The average velocity , interval velocity and RMS velocity of each layer can be obtained from seismic CDP data . They may be used to predict formation pressure and to calculate the specific gravity of drilling mud .

  2. 本文完成的工作主要有以下几个方面:1.论述了几种常用地震波速度的定义,如平均速度、层速度、均方根速度及叠加速度,并总结了它们之间的联系。

    The work mainly in the following aspects : 1 . This paper discusses some common seismic wave velocity definition , such as the mean velocity 、 layer velocity 、 root mean square velocity and superimpose velocity , and summarizes the relationship between them . 2 .

  3. 用修正后的模型计算出的平均速度分布、均方根速度的分布以及雷诺应力的分布,均与直接数值模拟(DNS)的结果吻合较好。

    The mean velocity profiles , the RMS ( root-mean-square ) velocity profiles and Reynolds stress profiles calculated by the modified model are consistent with the results of DNS .

  4. 导出深度域中均方根速度与层速度之间的关系;

    The relationship between stack velocity and interval velocity was deduced in depth .

  5. 如果使用均方根速度代替单一地层速度,这个双曲线公式可以被推广到多层反射。

    If equivalent velocity is considered , this equation can be extended to fit multi-interfaces reflections .

  6. 因此,获得的速度分析结果低于介质的均方根速度。

    As a result , the velocity calculated is lower than the root mean square velocity of media .

  7. 由于多次波包含了一次反射波的速度信息,因此,凡提取到相同均方根速度时,其时间滞后的反射波必是多次反射波。

    The information about the velocity of the primary reflection is included in that of the multiple reflection . The time-lag reflections which have the same root-mean-square velocity must be multiple reflections .

  8. 基于随机振动理论关于多自由度系统的频率响应函数、功率谱密度函数和均方根速度获得了夹层板的均方根速度响应表达式,从而发展该粘弹性夹层板的随机微振动响应分析方法。

    The random micro-vibration response analysis method for viscoelastic sandwich plate is developed based on the frequency-response function , response power spectral density and root-mean-square velocity spectrum of the theory of random vibration .

  9. 本文依据反射波理论双曲线方程,提出了一种通过判别检测到的均方根速度的方法来鉴别全程多次波,并自动检测一次反射波。

    Based on the theoretical reflection hyperbolic equation , a new method is proposed in this paper for auto-determination of the primary reflection and auto-differentiation of the multiple reflection by distinguishing the detected root-mean-square velocity .

  10. 为了得到较好的动校正效果,必须进行三参量速度分析,确定地下反射界面的三参量速度信息,即倾向、倾角和均方根速度。

    In order to achieve good dynamic correction , we must do three-parameter velocity analysis , namely determination of three-parameter velocity informations of subsurface reflector : dip direction , dip angle and mean square-root velocity .

  11. 提出了适用于二维工区和大倾角地区的三维逐层层速度反演方法,并据此层速度计算法射线方向和铅垂方向的平均速度及均方根速度。

    The author advances a 3-D inversion method of layer-by-layer interval velocity suitable the 2-D area and the large dip area . At the same time , the average velocities and RMS velocities in normal ray direction and plumb direction can be computed ~ th the interval velocity .

  12. 线位移或均方根振动速度做基础振动判据的探讨

    Inquisition into Foundation Vibration Criteria of Linear Displacement or RMS Velocity

  13. 哈特曼装置上均方根湍流速度的测量及研究

    Measurement and Research of Root mean square Turbulence Velocity on Hartmann Bomb