Abstract

Multichannel analysis of surface wave (MASW) is one of the novel seismic methods in geophysic field in Vietnam. MASW is able to survey the stiffness of the soil environment under the ground via the shear-wave velocity VS by analyzing the spectral image of surface wave. We did the 1D MASW survey upon the borehole belonged to the residential development project at district 2, Ho Chi Minh city with fixed receiver system, different source orientations and different source offsets. The spectral images of surface wave were combined to maximize the surface wave’s energy on the spectral image of surface wave to minimize the effect of lateral inhomogenousness and near - far source offsets. The data points were chosen on the phase curve on spectral image of surface wave for the inversion process to define shear wave velocity VS. The VS from MASW was compared to the petrographic components and another seismic method (downhole). The relative difference of the obtained VS values between two methods was less than 10%. The change of VS in MASW was absolutely compatible to petrographic components in geological borehole, near surface filled soil layer (93 m/s), dark-gray silty layer (68–157 m/s), sandy clay layer (250–265 m/s) and lower clay layer (254–400 m/s).

Highlights

  • able to survey the stiffness of the soil environment under the ground

  • We did the 1D Multichannel analysis of surface wave (MASW) survey upon the borehole belonged to the residential development project at district 2

  • maximize the surface wave's energy on the spectral image of surface wave to minimize the effect of lateral inhomogenousness

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Summary

Sóng Rayleigh

Sóng Rayleigh hình thành từ sự giao thoa giữa sóng dọc P và sóng ngang SV khi đến bề mặt ranh giới tự do (ranh giới giữa môi trường đất đá bên dưới và môi trường không khí bên trên bề mặt). Phương trình truyền sóng Rayleigh thể hiện mối quan hệ giữa vận tốc pha sóng Rayleigh (c) và vận tốc truyền sóng ngang VS, vận tốc truyền sóng dọc VP [7, 8]:. Đối với môi trường đất đá là vỏ trái đất, = 0,25 và q = 1/3, phương trình (2) trở thành [7, 8]:. (5) Trong môi trường bán không gian đồng nhất, sóng Rayleigh truyền với vận tốc pha [7, 8]:

Đường cong vận tốc pha sóng Rayleigh
Bài toán ngược
Vị trí lỗ khoan
Findings
Biên độ
Full Text
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