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1)  S-shadow
S波影区
2)  S wave
S波
1.
Based on S wave records of deep teleseisms on Shanxi Province Digital Network, and by modeling S wave waveform, shear wave velocity structures under 6 stations were obtained.
收集山西省数字台网记录的深源远震S波 ,采用S波理论波形拟合的方法 ,获得了山西省境内共 6个台站下方的剪切波速度结构 。
2.
The device has solved the s wave measurement problem in pressure/shear gas gun experiments.
该装置基于Faraday电磁感应定律 ,可实时测量多点斜碰撞产生的纵向和横向质点速度波形 ,从而解决了压剪炮试验中的s波测量问题 。
3)  S-wave
S波
1.
S-wave attenuation tomography of upper crust in Japan;
日本上地壳S波衰减成像
2.
Exploration of S-wave in Shadow Zone by Digital Data Recorded in Kunming Seismic Station;
用昆明地震台数字资料探讨影区地震S波
3.
Based on the inversion method of 2-D velocity structure and interface, the crustal velocity structures of P-wave and S-wave along the profile L_1 are determined simultaneously with deep seismic sounding data in Changbaishan Tianchi volcanic region, and then its Poisson′s ratio is obtained.
尝试应用一种同时获得地壳二维速度结构和界面形态的地震走时反演算法,通过分别反演P波和S波速度结构,计算深地震测深剖面的泊松比分布的方法,并对长白山天池火山区测深剖面(L1)进行处理解释。
4)  S-wave
橫波、S波
5)  sector-projection-wavelet-descriptor
扇区投影-小波描述子
1.
Aiming to the defects that some traditional contour descriptors can’t classify similar contours and that others o not have a good internal rotation-invariant property,the sector-projection-wavelet-descriptor was proposed.
针对传统轮廓描述子不能识别相似样本或者确定图像方向复杂等一系列缺陷,本文提出了基于主轴归一化方法的轮廓扇区投影-小波描述子。
6)  T-S wave
T-S波
1.
At a chosen location,a T-S wave and a couple of T-S waves were fed into the flow field.
以某一剖面为入口,加入一个及一对三维T-S波,发现随展向波数的增加,扰动幅值的增长率逐渐减小,证实了M=4。
2.
For the given base flow,T-S wave at the entrance to research the evolution of perturbance spatially is imposed.
对于给定的基本流,在计算域入口加入T-S波扰动,研究扰动的空间发展演化。
3.
Whether or not the sound field would be generated by the interactions among the T-S wave introduced at the entrance of one side of the plate,the trailing edge and wake flows is studied by direct numerical simulation,while the same .
用直接数值模拟的方法,研究了二维亚音速情况下,上下来流相同的流体流过无限薄平板时,平板单边的T-S波和尾缘及尾迹流相互作用产生声场的可能性。
补充资料:四祖优波鞠多尊者《八十八祖道影传赞》
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