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1)  2D RE
二维反求
1.
On the basis of computer vision and finite element method (FEM) simulation technology, we build a set of measurement system of 2D RE, which provides a rapid, wide-range, maneuverable measurement method compared to the traditional coord.
二维测量技术在反求工程、工业检测及质量控制等领域占有一席之地,反求工程中轮廓曲线的重建对于曲面重建是至关重要的,基于视觉和有限元双线性插值方法建立的二维反求建模测量系统,与传统的三坐标测量机相比,具有速度快、量程大、操作方便的优点。
2)  Two-dimensional inversion
二维反演
1.
However,two-dimensional inversion of EH-4 data has a problem.
然而,进行资料的二维反演时,遇到了在大地电磁测深中同样的问题:TE极化模式和TM极化模式不容易辨别。
2.
Considering the influence of the topography, the authors analyzed in detail the geoelectric section model and made CSAMT two-dimensional inversion for the direct calculation data of the model.
复杂地形严重地影响可控源音频大地电磁测深(CSAMT)的解释结果,为此,笔者考虑了地形的影响,将地电断面模型经过精细剖分,对模型正演计算的数据进行CSAMT二维反演,得出的结果与正演模型的形态基本一致,获得的电性断面能很好地反映地下地质结构,与实际地质资料相吻合,证实了该方法的正确性和有效性。
3.
: In order to enhance the capacity of data inversion in the electrical method and to find out a better inversion method, we have introduced and developed the Box-Kanemasu method successfully in this paper in addition to studying the application of the modified damping least-square method in a two-dimensional inversion.
为了提高电法勘探数据解释的能力,寻找较好的二维反演方法,本文在研究改进的阻尼最小二乘法在二维反演中应用的同时,成功地引进和发展了Box-Kanemasu反演法。
3)  2 D inversion
二维反演
1.
The 2 D inversion is the best method in the interpretation of DC resistivity sounding profiles data owing to its high speed, but the 3 D inversion, by contrast, needs more measured data and more computer time.
直流电阻率测深剖面数据解释最好的方法是二维反演 ,这是由于它反演速度快 ,而三维反演则需要很多的实测数据、很长的计算时间 。
4)  2D inversion
二维反演
1.
After 3D forward modeling and 2D inversion,we realized the relationship between the inversion data and the real object,then we inversed the field data and given a reasonable conclusion.
在完成三维正演与二维反演数值模拟的基础上进行了野外数据的反演解释工作,利用三维局部异常体的正演响应特征及二维反演结构与真实模型的对应关系,对实际的数据进行了认识解释,得到了目的层的异常体可能是地道而不是木箱的初步结论。
2.
At present,the researches on 2D inversion of IP data mainly aim at the HD(high density) IP data,which is mainly due to the equivalent distances between neighboring poles during data collection.
目前,激电数据的二维反演主要针对高密度激电数据,而对于常规的激电测深则很少涉及。
3.
The 2D inversion cross-sections show that the eastern and western boundaries of the Songliao basin are steeper while the southern boundary is gentler and that low-resistivity objects are commonly present at 15-30 km depth in volcanic areas, which offers a basis for int.
采用具有国际先进水平的二维连续自动反演技术对收集的MT资料进行了二维反演和综合解释。
5)  two dimensional inversion
二维反演
1.
From the approximate reduction to the inverse objective function of two dimensional layer model, the two dimensional inversion along the total profile was reduced to the one dimensional inversion of each site along the profile, and a simple easy scheme of the parametric inversion for tw.
本文在大地电磁测深松弛(rapid)反演理论方法的基础上,探讨了电偶源频率电磁测深(赤道装置)阻抗视电阻率的二维反演问题。
6)  2-D inversion
二维反演
1.
Joint 2-D inversion of magnetotelluric sounding data having landform effect;
带地形的大地电磁测深联合二维反演
2.
This paper studied the 2-D inversion interpreting technique of electrical sounding with the finite element method and the damped least square method.
本文对应用有限元及阻尼最小二乘法进行电测深二维反演解释技术做了进一步的研究。
3.
A new fast magnatotelluric 2-D inversion method has been developed, which utilizing the same method as that of rapid relax inversion (RRI) to calculate the partial derivatives of apparent resistivity with respect to model parameter and presented the model structure of Catherine de Groot-Hed-lin and Steven Constable.
利用大地电磁快速松弛反演法(RRI)中求偏导数的方法,结合二维块状地质模型建模法,提出了一种块状地质单元边界的快速二维反演方法。
补充资料:反,反-4,4'-二丙基-[1,1'-联二环己基]-4-腈
CAS: 88510-85-4
中文名称: 反,反-4,4'-二丙基-[1,1'-联二环己基]-4-腈
英文名称: trans,trans-4,4'-Dipropyl-[1,1'-bicyclohexyl]-4-carbonitrile
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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