The Thomson Line (TSL) is a 30 km underground train line that is expected to be fully completed in 2021, and will be the sixth Mass Rapid Transit system in Singapore. The line will run through the north-south corridor, starting in the northern Woodlands area, passing through the industrial estate of Sin Ming, down to the residential Thomson area and the shopping districts of Orchard and Marina Bay, before ending at Gardens by the Bay. One of the key challenges is bored tunnelling through the soils and rocks of Bukit Timah Granite near to existing buildings, especially within the densely built-up regions near Orchard. Specifically, there are pockets of areas where it is not possible to conduct conventional borehole investigation method due to accessibility issues for the drilling rigs. To overcome the challenges in investigating the soil-rock interface at these locations, seismic survey methods were proposed to enhance the clarity on geological profile.The paper first explains the nuances and limitations between various seismic acquisition methods, such as 2-dimensional (2-D) methods, and 3-dimensional (3-D) methods. These have used in combination for oil and gas exploratory functions, but is uncommon to see their application in ground investigations for land infrastructure projects in Singapore. Eventually, a decision was made to make use of 3-D seismic refraction in the ground investigations for Thomson Line in Singapore.In practical sense, the paper presents an instance whereby 3-D acquisition method is scaled down to solve a civil engineering problem which in LTA’s case was determining bedrock depth that the bored tunnels will encounter during construction phase. The target depth for the soil-rock interface was between 30 m to 60 m, and is small-scale as compared to hundreds of metres of potential information that could be mapped using the acquisition method. Other than discussing the technicalities in implementing the 3-D survey, the effectiveness of the seismic acquisition in mapping the soil-rock interface of the Bukit Timah Granite Formation will be discussed. Future application of the seismic acquisition for LTA projects is also briefly included.
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