1) quadratic inversion
二次反演
2) sequential inversion
依次反演
1.
Then, we introduce two basic cooperative inversion algorithms: sequential inversion and joint inversion.
其次,根据目前国内外的相关研究,介绍了当前联合反演的两种算法:依次反演和同时反演。
3) twice evolution
二次演化
1.
Compared with the original, it has three characteristics as follows: (1) avoiding prematurity by simulating Annealing; (2) using gene pool to conserve dominant genes, and thus it not only speeds up the convergence, but also improves the solution’s quality; (3) using twice evolution to improve the precision.
新算法有三大改进:(1)采用模拟退火选择策略避免早熟;(2)用基因库技术保存优势基因,既加速了算法的收敛性,又提高了解的质量;(3)使用二次演化进一步提高解的精度。
4) 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。
5) 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 。
6) 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。
补充资料：和中甫端午韵不依次
【诗文】：
黄茅古道外，羸马发南州。
有客嗤齐鲁，何人念楚囚。
岁年付流水，风雨满沧洲。
手把菖莆看，黑头非所求。
【注释】：
【出处】：
黄茅古道外，羸马发南州。
有客嗤齐鲁，何人念楚囚。
岁年付流水，风雨满沧洲。
手把菖莆看，黑头非所求。
【注释】：
【出处】：
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条