基于微动H/V谱比法的土质基质厚度探测——以阿荣旗那吉镇为例
Soil matrix thickness detection based on microtremor horizon-to-vertical spectral ratio: A case study of Naji Town in Arong Banner
-
摘要: 土质基质厚度是地表基质调查中的重要指标, 阿荣旗地区的地形地貌主要为低山丘陵, 利用传统钻探手段调查土石界面成本较高、施工难度较大, 而微动H/V谱比法抗干扰能力强、施工灵活, 有利于完成面积性调查工作。以1 km×1 km的网度开展调查, 结合H/V谱比曲线与钻孔资料, 总结出研究区的深度-频率经验关系, 计算得到区内的土质基质厚度分布。结果显示: 该地区的土质基质厚度为9~60 m, 受古河道的影响, 总体呈现自西北向东南逐渐增加的趋势, 根据基岩界面高程可以圈定古河道的边界和延伸方向。研究可为在低山丘陵区调查土质基质厚度分布提供参考。Abstract: Soil matrix thickness is an important index in the investigation of ground substrate. The topography and geomorphology of Arong Banner are mainly low mountains and hills. The cost of using traditional drilling methods to investigate the soil matrix thickness is high, and the construction is difficult. While the microtremor horizon-to-vertical (H/V) spectral ratio method has strong anti-interference ability and flexible construction, which is convenient to complete areal investigation work. In this paper, the spectral ratio method was used to investigate the 1 km×1 km network. Combined with the spectral ratio curve and borehole data, the authors summarized the depth-frequency empirical relationship of the study area, and calculated the soil matrix thickness distribution in the area. The results show that thickness of the soil matrix in the area is estimated to be between 9~60 m. And it generally shows a trend of gradually deepening from northwest to southeast, influenced by ancient river channels. The boundaries and extension directions of the ancient river channels can be delineated based on the undulating interfaces of bedrock. The study could provide references for determining the thickness distribution of soil matrix in low hilly areas.
下载: