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On the prediction of settlement from high-resolution shear-wave reflection seismic data: The Trondheim harbour case study, mid Norway

机译:基于高分辨率剪切波反射地震数据的沉降预测:挪威中部特隆赫姆港口案例研究

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摘要

This paper presents a novel approach to predict long-term settlement in the Trondheim harbour, mid Norway, from high-resolution shear-wave seismic reflection data, complemented with cone penetration test results (CPTU) and index soil properties from nearby boreholes in this reclaimed coastal area. The data enables subsurface geo-characterisation in high-resolution, down to the basement at a depth of about 175 m. Correlations between shear-wave velocity and Janbu's classical ID consolidation parameters (m, M_0, M_1 σ'_c and OCR) are used for settlement analysis. Both the magnitude and rate of time-settlement predictions compare well with the measured settlements from GPS levelling and PSInSAR data acquired since the late 1980s and the early 1990s in the area, respectively. The shear-wave reflection data further provide important input to understand the spatial patterns of land-subsidence in the Trondheim harbour. The highest settlement rates occur in areas where depth to bedrock is greatest and where thicker deposits with low stiffness are found. In summary, the data and workflow presented here are useful tools for predicting settlements based on correlations with shear-wave velocity measurements.
机译:本文提出了一种新颖的方法,可以根据高分辨率的横波地震反射数据,再结合圆锥渗透测试结果(CPTU)和附近开挖的钻孔的土壤特性,来预测挪威中部特隆赫姆港的长期沉降沿海地带。该数据可实现高分辨率地下特征化,直至深度约175 m的地下室。横波速度与Janbu的经典ID固结参数(m,M_0,M_1σ'_c和OCR)之间的相关性用于沉降分析。时间预测的幅度和速率与分别从1980年代末和1990年代初在该地区获得的GPS水准和PSInSAR数据测得的沉降值相比,具有良好的对比。横波反射数据进一步为了解特隆赫姆海港地面沉降的空间格局提供了重要的信息。最高沉降速率发生在基岩深度最大,沉积物较厚且刚度较低的地区。总之,此处介绍的数据和工作流程是基于与剪切波速度测量值的相关性来预测沉降的有用工具。

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