Simulating pumping-induced regional land subsidence with the use of InSAR and field data in the Toluca Valley, Mexico

被引:123
作者
Calderhead, A. I. [1 ,2 ]
Therrien, R. [3 ]
Rivera, A. [4 ]
Martel, R. [2 ]
Garfias, J. [5 ]
机构
[1] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[2] Ctr Eau Terre & Environm, Inst Natl Rech Sci, Quebec City, PQ G1K 9A9, Canada
[3] Univ Laval, Dept Geol & Genie Geol, Quebec City, PQ G1K 7P4, Canada
[4] Nat Resources Canada, Geol Survey Canada, Quebec City, PQ G1K 9A9, Canada
[5] Univ Autonoma Estado Mexico, Fac Ingn CIRA, Toluca 50130, Mex, Mexico
基金
加拿大自然科学与工程研究理事会;
关键词
Regional land subsidence; 1-D compaction; InSAR; Toluca; Mexico; HydroGeoSphere model; AQUIFER SYSTEM COMPACTION; SYNTHETIC-APERTURE RADAR; DEFORMATION;
D O I
10.1016/j.advwatres.2010.09.017
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
A multidisciplinary approach is presented here for quantifying land subsidence in a heavily pumped aquifer system with complex stratigraphy. The methodology consists in incorporating Terzaghi's 1D instantaneous compaction principle into a 3D groundwater flow model that is then applied and calibrated to reproduce observed hydraulic heads and compaction for the Toluca Valley, Mexico. Differential Interferometric Synthetic Aperture Radar (D-InSAR), a generated 3D-geological model, extensometers, monitoring wells, and available literature are used to constrain the model. The D-InSAR measured subsidence, extensometers, and numerical simulations of subsidence agree relatively well. Simulations show that since regional subsidence began in the mid 1960s there has been up to 2 m of subsidence in the industrial corridor, where heavy pumping and thick clay layers are found. This study shows that an approach using various sources of data is useful in estimating and constraining the vertical component of the inelastic skeletal specific storage. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:83 / 97
页数:15
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