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Land subsidence monitoring using distributed fiber optic sensing with Brillouin scattering in coastal and deltaic regions

机译:沿海地区沿海地区布里渊散射的分布式光纤传感土地沉降监控

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Excessive withdrawal of groundwater in coastal and deltaic regions is one of the main reasons which induce land subsidence in these areas. Land surface displacement monitoring with conventional methods is not able to pinpoint subsurface compacting, which is very challenging. Instead of groups of extensometers, we apply distributed fiber optic sensing (DFOS) with Brillouin scattering in vertical boreholes to identify the deformation distribution along the entire borehole with meter-scale spatial resolution. We here present 10 boreholes with depths range from 100 to 600 m with DFOS monitoring along the east coastal line of Jiangsu and Shanghai since 2015, and 1 borehole of 300 m in depth in Yangtze River delta since 2012. The results provide clear images on the deformation distribution along entire boreholes, by identifying the main contributors to the subsidence and the deformation evolutionary processes, with stable long-term monitoring performance. Hence, we demonstrate that DFOS can open window into subsurface deformation and could be important complementary to conventional methods to understand the land subsidence processes in coastal and deltaic regions.
机译:过度撤离沿海和红细胞区的地下水是诱导这些地区土地沉降的主要原因之一。用常规方法的陆地表面位移监测无法确定地下压实,这是非常具有挑战性的。我们在垂直钻孔中使用布里渊散射的分布式光纤感测(DFO)应用分布式光纤感测(DFO),以沿着具有仪表尺度空间分辨率的整个钻孔的变形分布。我们在这里展示了10个深度,深度范围为100至600米,沿2015年以来江苏东沿海线和上海的DFOS监控,自2012年以来,长江三角洲的1个钻孔300米。结果提供了清晰的图像通过识别沉降和变形进化过程的主要贡献,沿整个钻孔的变形分布,具有稳定的长期监测性能。因此,我们证明了DFO可以将窗户打开进入地下变形,并且可能与常规方法互补,以了解沿海和红细胞区中的土地沉降过程。

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