轉換波 的英文怎麼說
中文拼音 [zhuǎnhuànbō]
轉換波
英文
converted wave-
In designing analogic circuit, we adopt programmable filter max262 to meet the system ' s command. after the step, we can make the signal ' s frequency width is wider and noise level is lower. to make the signal ' s amplitude to meet the analogic to digital device ' s command, we adopt the max551 to finish the gain control
在模擬電路部分,採用可編程濾波器max262 ,這樣就滿足了該數據採集裝置所採集的信號的頻率范圍較寬以及具有較低的噪聲水平的要求,為了使采樣到的信號的幅度滿足後面a d轉換器的要求,採用max551對采樣到的信號進行調理(增益控制) 。Disposes the switch in the network is decided to the network performance improvement by the network analysis situs and the size, and the serviceable wave length number and uses rwa algorithm
在網路中配置轉換器對網路性能的改善取決于網路拓撲和大小,及可用波長數和所用的rwa演算法。Band switching diode
波段轉換開關二極體Prestack depth migration for p - sv converted - wave
轉換波疊前深度偏移Seismic processing method of 3d converted wave
三維轉換波地震資料處理方法High precision velocity analysis of converted wave
高精度轉換波速度分析Fast ray tracing method for converted waves in complex media
復雜地質模型轉換波快速射線追蹤方法The processing method and effect analysis of 3d wide line converted wave data
寬線三維轉換波資料處理方法及效果分析And the scheme for p - sv waves was put forward as an example of converted waves
然後,以p - sv波為例,給出了轉換波快速射線的追蹤方法。The static correction method of converted p - sv waves is always a problem in converted wave processing
摘要p - sv轉換波靜校正一直是轉換波處理中的一個難題。The numerical example has proven that the scheme for converted waves is effective
模型計算結果表明,本文所提出的轉換波快速射線追蹤方法對復雜地質模型是切實可行的。Comparison between the non - hyperbolic and hyperbolic nmo correct ion results of 3d converted waves shows that the non - hyperbolic method is better than the hyperbolic method
三維轉換波非雙曲動校正和常規雙曲動校正結果對比表明,非雙曲方法優于雙曲方法。The 3d anti 3c seismic processing flow established is used in processing of the real seismic data, achieving high quality velocity ratio spectrum and good non - hyperbolic nmo correction and stacking of 3d converted wave
應用所建立的三維三分量地震資料處理流程,對某實際地震資料進行了處理,得到了較高質量的三維轉換波速度比譜,轉換波非雙曲動校正和疊加取得了較好效果。For processing of 3d and 3c seismic data, the reflected p - waves can be processed with the conventional methods, while the reflected converted waves can not be processed with the conventional p - wave processing methods, because their travel paths are asymmetrical, their common midpoint gathers are no longer common reflection point gathers, and their time - distance equation is non hyperbolic
在三維三分量地震勘探資料處理中,對于反射縱波資料可以採用常規方法進行處理;而對于反射轉換波資料,由於其傳播路徑的非對稱性,轉換波共中心道集不再是共反射點道集,轉換波時距方程也不是雙曲方程,因此不能採用常規縱波處理方法來處理轉換波資料。In viewing of the characteristics of propagation of 3d converted wave, studies are performed on the processing methods of 3d converted waves, such as horizontal component rotation, calculation of 3d transition point, hyperbolic velocity analysis and nmo ( normal moveout ) correction of 3d converted wave, and non - hyperbolic velocity ratio analysis and nmo correction of 3d converted wave
基於三維轉換波傳播特點,對三維轉換波資料處理方法進行了研究,包括水平分量旋轉,三維轉換點計算、三維轉換波雙曲速度分析與動校正、三維轉換波非雙曲速度比分析與動校正等。Having considered the particularity in converted - wave processing we pay much attention to main links such as the generation of ccp trace gather, the azimuth angle rotation of horizontal component etc., and better converted - wave profiles have been obtained
考慮到轉換波處理的特殊性,在處理時特別注意了共轉換點( ccp )道集的生成、水平分量方位角旋轉等主要環節,從而得到了較好的轉換波剖面。Effects of a covering layer in a circular - arc canyon on incident plane sv waves
轉換波轉換點坐標的唯一解析解The reflection points for the transformed waves do not coincide with those of the non-transformed waves.
轉換波的反射點與非轉換波的反射點不一致。Key problems and solutions in processing converted - wave seismic data
轉換波地震資料處理的關鍵問題與解決方法Prestack migration method, based on wave motion equation, is also developed for receiver function, and compared with ray method. both p - to - s conversion wave and direct p phase contained in receiver function are migrated and imaged by reverse - time migration for data gather including all receiver functions recorded in all seismological stations for one event, and imaging profile is finally obtained by stacking for all events
本文還在接收函數射線反投影疊加成像的基礎上,提出了一種基於波動方程的接收函數疊前偏移成像方法,將同一事件接收函數中的轉換波和直達p波震相以各自的速度向深度方向逆時延拓成像,並通過不同慢度接收函數的疊加,得到最終的偏移成像結果。分享友人