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Regional subsidence modelling in Murcia city (SE Spain) using 1-D vertical finite element analysis and 2-D interpolation of ground surface displacements

机译:穆尔西亚市(西班牙东南部)的区域沉降模拟,使用一维垂直有限元分析和地表位移的二维插值

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摘要

Subsidence is a hazard that may have natural or anthropogenic origin causing important economic losses. The area of Murcia city (SE Spain) has been affected by subsidence due to groundwater overexploitation since the year 1992. The main observed historical piezometric level declines occurred in the periods 1982–1984, 1992–1995 and 2004–2008 and showed a close correlation with the temporal evolution of ground displacements. Since 2008, the pressure recovery in the aquifer has led to an uplift of the ground surface that has been detected by the extensometers. In the present work an elastic hydro-mechanical finite element code has been used to compute the subsidence time series for 24 geotechnical boreholes, prescribing the measured groundwater table evolution. The achieved results have been compared with the displacements estimated through an advanced DInSAR technique and measured by the extensometers. These spatio-temporal comparisons have showed that, in spite of the limited geomechanical data available, the model has turned out to satisfactorily reproduce the subsidence phenomenon affecting Murcia City. The model will allow the prediction of future induced deformations\udand the consequences of any piezometric level variation in the study area.
机译:沉陷是一种可能来自自然或人为来源的危险,会造成重大的经济损失。自1992年以来,穆尔西亚市(西班牙东南部)由于地下水的过度开采而受到地面沉降的影响。主要的历史测压水平下降发生在1982–1984、1992–1995和2004–2008年期间,并显示出密切的相关性。随着地面位移的时间演变。自2008年以来,含水层中的压力恢复导致引伸计检测到的地面升高。在目前的工作中,已经使用弹性的水力机械有限元代码来计算24个岩土钻孔的沉降时间序列,并规定了被测地下水位的变化。将获得的结果与通过先进的DInSAR技术估算并由引伸计测量的位移进行了比较。这些时空比较表明,尽管可用的地质力学数据有限,但该模型已证明可以令人满意地重现影响穆尔西亚市的沉降现象。该模型将允许预测将来引起的变形\ ud,以及研究区域中任何压力水平变化的后果。

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