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GEOPHONE AND METHOD FOR THE STUDY OF ELASTIC WAVE PHENOMENA

机译:地球电话和弹性波现象的研究方法

摘要

A method for the study of elastic wave phenomena in the ground, where the detection of said phenomena is carried out with the use of at least a geophone comprising at least a couple of transducers (20, 21; 37, 38), each transducer (20, 21; 37, 38) being apt to detect horizontally polarized shear waves, represented by SH signals, and compression waves, represented by P signals. The method comprises: i) a first detection, by means of one of said transducers (20, 21; 37, 38) of the sum of said P and PH signals (P+SH); ii) a second detection, by means of the other one of said transducer (20, 21; 37, 38) of the difference between said P and SH signals ([P-SH] or [-P+SH]); iii) the compensation ([P+SH]-[P-SH]) or [P+SH]+[P-SH]) between said first and said second detection, in order to acquire signals being representative of horizontally polarized shear waves with an increased sensitivity and being less affected by the presence of compression waves.
机译:一种研究地下弹性波现象的方法,其中至少使用地震检波器对地震现象进行检测,该地震检波器包括至少两个换能器(20,21; 37,38),每个换能器( 20、21; 37、38)易于检测由SH信号表示的水平极化剪切波和由P信号表示的压缩波。该方法包括:i)通过所述换能器(20、21; 37、38)之一对所述P和PH信号(P + SH)之和进行第一次检测; ii)借助于所述换能器(20、21; 37、38)中的另一个对所述P和SH信号([P-SH]或[-P + SH])之间的差进行第二次检测; iii)在所述第一检测和所述第二检测之间的补偿([P + SH]-[P-SH])或[P + SH] + [P-SH]),以便获取代表水平极化剪切波的信号具有更高的灵敏度并且受压缩波的影响较小。

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