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首页> 外文期刊>International Journal of Technology >Development of a New Blasting Vibroseis Technique and its Application to the Exploration of Geological Structures
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Development of a New Blasting Vibroseis Technique and its Application to the Exploration of Geological Structures

机译：爆破振动技术的发展及其在地质构造勘探中的应用

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Seismic waves used for exploration of geological structures are mostly generated from blast sources. A new blasting vibroseis apparatus, which utilizes the homogeneity, isotropy, and incompressibility of water to reduce damage to adjacent rock from blast waves, was developed. This method overcomes the low repeatability and low control issues of traditional blast methods (downhole charge) while maintaining the advantages of high explosive power, sharp pulse signal, and a wide range of frequency domains. Blasting vibroseis and traditional blasting tests were implemented in the Three Gorges Reservoir Region, China. The finite element method (FEM) method was used to numerically calculate blasting vibroseis-induced dynamic ground pressures. Through a series of comparison tests, the characteristics of the seismic waves generated by blasting vibroseis were summarized and the repeatability and controllability of the blasting vibroseis test was validated. The blasting vibroseis apparatus was then used to detect geological structures below the surface of the Maoping landslide, China, and the results were very consistent with previous drilling exploration (89%), which reflects the practical value of the new blasting vibroseis for the exploration of geological structures. Blasting vibroseis can be used as a practical and cost-effective method to detect geological structures.
机译：用于勘探地质结构的地震波主要来自爆炸源。开发了一种利用水的均匀性，各向同性和水的不可压缩性来减少爆炸波对相邻岩石的破坏的新型爆破振动仪。该方法克服了传统爆炸方法（井下装药）的低重复性和低控制问题，同时保持了高爆炸功率，尖锐脉冲信号和宽范围频域的优势。在中国三峡水库地区进行了爆破振动和传统爆破试验。有限元方法（FEM）方法用于数值计算爆破振动引起的动态地面压力。通过一系列比较试验，总结了爆破振动产生的地震波的特征，并验证了爆破振动试验的可重复性和可控性。然后用爆破振动仪检测中国茅坪滑坡表面以下的地质构造，其结果与以前的钻探勘​​探非常吻合（89％），这反映了新型爆破振动仪在勘探中的实用价值。地质结构。爆破振动可以用作一种实用且经济有效的方法来检测地质结构。

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