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Integrated ground penetrating radar, electrical resistivity tomography and multichannel analysis of surface waves for detecting near-surface caverns at Duqm area, Sultanate of Oman

机译:用于检测DUQM地区近地区洞穴,阿曼苏丹国近视洞穴的地面透过雷达,电阻率断层扫描和多通道分析

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摘要

Caverns in hard limestone form natural karstic features. Surveying, detecting, and managing caverns are valuable as they provide an accurate and reliable understanding of the geohazards that caverns represent. With the construction of the highway network in Duqm (Duqm Port, Sultanate of Oman), near-surface stability problem (caverns) appeared. Three geophysical tools - ground penetrating radar, electrical resistivity tomography, and multichannel analysis of surface waves - were utilized to delineate the subsurface cavities beneath an area of 10,000 m(2) (200 m x 50 m). Based on interpretation of the results of two-dimensional and three-dimensional ground penetrating radar, electrical resistivity tomography and multichannel analysis of surface waves, the caverns are found to extend in the N-S direction. The results show two cavern systems of varying thicknesses. The caverns are separated at the top, but at some locations they become an one-unit cavern system, especially in the northerly direction. The cavern system is not completely hollow; at some locations, they are filled with materials of different physical properties than the host rock. The depth of the cavern system varies between 0 and 5.2 m. The caverns are found only within the limestone rock unit. There is no evidence of caverns within the shale rock unit. The results from the three methods show good agreement in terms of depth and dimensions of the detected caverns.
机译:硬石灰岩中的洞穴形式自然的岩溶特征。测量,检测和管理洞穴是有价值的,因为它们提供了对洞穴所代表的地质曲线的准确和可靠的理解。随着DUQM(DUQM港口,阿曼苏丹国)的公路网络的建设,近似表面稳定性问题(洞穴)出现。三个地球物理工具 - 地面穿透雷达,电阻率断层扫描和表面波的多通道分析 - 用于描绘面积10,000m(2)(200m×50μm)下方的地下腔。基于解释二维和三维地面穿透雷达的结果,电阻率断层扫描和表面波的多通道分析,发现洞穴在N-S方向上延伸。结果显示了两个不同厚度的洞穴系统。洞穴在顶部分开,但在一些位置,它们成为一个单位洞穴系统,特别是在北方方向上。洞穴系统不是完全空心;在某些位置,它们充满了不同物理性质的材料而不是主体岩石。洞穴系统的深度在0到5.2米之间变化。洞穴仅在石灰石岩石单元内被发现。页岩岩石单元内没有证据。三种方法的结果在检测到的洞穴的深度和尺寸方面展示了良好的一致性。

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