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The investigation of dissolution subsidence incorporating microgravity geophysics at Ripon, Yorkshire

机译:约克郡Ripon溶出沉积沉积沉积微匍匐地球物理学的调查

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摘要

Dissolution subsidence affords some of the most difficult ground conditions with which engineering geologists have to deal. Within the UK, areas underlain by gypsiferous Permo-Triassic strata, most notably around Ripon in Yorkshire, are prone to dissolution structures and resultant building failures are well documented. ududConventional drilling of such unstable sites is often a ‘hit and miss’ affair and most geophysical techniques do not provide sufficient resolution to offer adequate confidence in the results. Proposals for the redevelopment of a site within the urban area at Ripon could not rely on such frequently inconclusive methods and it was necessary to implement a phased approach to site investigation. Following a desk study, high-resolution microgravity geophysics was carried out both inside and outside the existing building. This indicated a major negative anomaly of peak amplitude -74 µGal. Subsequent static core probing, rotary drilling and trial trenching confirmed the existence of a potentially unstable breccia pipe which could therefore be taken into account in the engineering design. udud
机译:解散押金提供了一些最艰难的基础条件,工程地质学家必须处理。在英国内部,由Gypsiafien obsif-Triassic Straata介绍的地区,最显着的是在约克郡的Ripon周围,易于溶出结构,并结束了建筑物失败。 ud udConventional钻探这种不稳定的网站往往是一个“击中和错过的事件”,大多数地球物理技术都没有提供足够的解决方案来提供足够的令人信心。 RIPON城市地区内设区的重建的建议不依赖于这种常规不确定的方法,有必要实施分阶段的现场调查方法。在桌面研究之后,在现有建筑物内外进行高分辨率的微匍匐地球物理学。这表明峰值幅度的主要阴性异常-74μgAl。随后的静态芯探测,旋转钻孔和试验沟槽证实存在潜在不稳定的Breccia管道,因此可以在工程设计中考虑。 ud ud

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