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Inverse modeling using PS-InSAR for improved calibration of hydraulic parameters and prediction of future subsidence for Las Vegas Valley, USA

机译:使用PS-Insar的逆建模改进了Las Vegas山谷未来沉降的校准和预测

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Las Vegas Valley has had a long history of surface deformation due to groundwater pumping that began in the early 20th century. After nearly 80 years of pumping, PS-InSAR interferograms have revealed detailed and complex spatial patterns of subsidence in the Las Vegas Valley area that do not coincide with major pumping regions. High spatial and temporal resolution subsidence observations from InSAR and hydraulic head data were used to inversely calibrate transmissivities (T), elastic and inelastic skeletal storage coefficients (Ske and Skv) of the developed-zone aquifer and conductance (CR) of the basin-fill faults for the entire Las Vegas basin. The results indicate that the subsidence observations from PS-InSAR are extremely beneficial for accurately quantifying hydraulic parameters, and the model calibration results are far more accurate than when using only water-levels as observations, and just a few random subsidence observations. Future predictions of land subsidence to year 2030 were made on the basis of existing pumping patterns and rates. Simulation results suggests that subsidence will continue in northwest subsidence bowl area, which is expected to undergo an additional 11.3 cm of subsidence. Even mitigation measures that include artificial recharge and reduced pumping do not significantly reduce the compaction in the northwest subsidence bowl. This is due to the slow draining of thick confining units in the region. However, a small amount of uplift of 0.4 cm is expected in the North and Central bowl areas over the next 20 years.
机译:拉斯维加斯山谷已地表变形的悠久历史,由于地下水开采始于20世纪初。经过近80年的抽水,PS-InSAR的干涉已经透露,在拉斯维加斯山谷面积不重合与主要泵送地区沉降的详细和复杂的空间格局。从干涉SAR和液压头数据的高空间和时间分辨率沉降观测来逆校准透射率(T),弹性和非弹性骨架存储系数的盆地填充的(SKE和Skv变)显影区的含水层和电导(CR)故障对整个拉斯维加斯盆地。结果表明,从PS-InSAR的沉降观测对精确量化水力参数非常有益,模型校准结果远远使用时,作为观察只有水的水平,只是一些随机的沉降观测比更准确。地面沉降到2030年的未来预测是现有的抽水模式和价格的基础上作出的。仿真结果表明,地面沉降将继续在西北部塌陷区碗,预计将经历额外的11.3厘米下沉。即使缓解措施,其中包括人工补给,降低抽不显著减少在西北部沉降区压实。这是由于在该地区厚厚的围台的缓慢排水。然而,0.4厘米隆起少量在北部和中部地区的碗在未来20年的预期。

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