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首页> 外文期刊>Near surface geophysics >Underwater ERT surveying in water with resistivity layering with example of application to site investigation for a rock tunnel in central Stockholm
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Underwater ERT surveying in water with resistivity layering with example of application to site investigation for a rock tunnel in central Stockholm

机译:水下的ert测量在水中的电阻分层,其中斯德哥尔摩中央岩石隧道现场调查

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摘要

We present an approach to underwater electrical resistivity tomography surveying under conditions with several water layers with different resistivity in the water above the electrode layout. The approach is verified against a synthetic model example and tested in full scale on data from a field survey. The field survey was carried out in central Stockholm as part of pre-investigations for a new metro train (T-bana) tunnel planned to pass under seawater. The water passage is associated with major tectonic zones that can potentially be very difficult from a tunnel construction point of view. The aim was to identify variations in depth of the bottom sediments and variations in rock quality including the possible presence of weak zones in the rock. Survey conditions are complicated by boat traffic and electrical disturbances from the power grid and train traffic. The water depth was mapped using sonar combined with recording pressure transducers, and water resistivity as a function of water depth was recorded using geophysical borehole logging equipment. Water resistivity as a function of depth was integrated in the inversion model. The results show that the rather difficult survey conditions could be handled in a satisfactory way thanks to adequate equipment, careful planning, and attention to details. The measured data contain information that is relevant for creating coherent models of the variation in depth to rock,which corresponds well with data from drilling. The results also indicate that information in variation in rock quality that can be of critical importance for planning of underground construction can be derived from the data.
机译:在电极布局之上的水中具有不同电阻率的几个水层的条件下,我们提出了一种在水下电阻率断层摄影测量的方法。该方法是针对合成模型示例验证的,并以现场调查的数据全规模测试。该田间调查是在斯德哥尔摩中央进行的,作为计划在海水下通过的新地铁列车(T-Bana)隧道进行预调查的一部分。水通道与主要构造区域相关联,这些区域可能来自隧道施工的观点非常困难。目的是识别底部沉积物深度的变化以及岩石质量的变化,包括岩石中可能存在的弱区。船舶交通和电网流量的电气干扰复杂,调查条件复杂化。使用声纳结合记录压力传感器映射水深,并使用地球物理钻孔测井设备记录作为水深函数的水电阻率。作为深度函数的防水率集成在反转模型中。结果表明,由于设备,仔细规划和对细节的关注,可以以令人满意的方式处理相当困难的调查条件。测量数据包含与创建对Rock的深度变化的相干模型相关的信息,这与来自钻井的数据很好。结果还表明,岩石质量变化的信息可以从数据中获取可能是规划地下施工的重要性。

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