Articles | Volume 382
https://doi.org/10.5194/piahs-382-99-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/piahs-382-99-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Ongoing research on the pumping-induced land deformation in the Aguascalientes Valley: an analysis of the recent data of vertical deformation, groundwater level variations and local seismicity
Martin Hernandez-Marin
CORRESPONDING AUTHOR
Departamento de Geotecnia e hidráulica, Universidad Autónoma de Aguascalientes, Aguascalientes, Ags. 20131, Mexico
Ruben Esquivel-Ramirez
Instituto Nacional de Estadistica y Geografía, Héroe de Nacozari Sur 2301, Aguascalientes, Ags., 20266, Mexico
Mario Eduardo Zermeño-De-Leon
Departamento de Geotecnia e hidráulica, Universidad Autónoma de Aguascalientes, Aguascalientes, Ags. 20131, Mexico
Lilia Guerrero-Martinez
Departamento de Geotecnia e hidráulica, Universidad Autónoma de Aguascalientes, Aguascalientes, Ags. 20131, Mexico
Jesus Pacheco-Martinez
Departamento de Geotecnia e hidráulica, Universidad Autónoma de Aguascalientes, Aguascalientes, Ags. 20131, Mexico
Thomas J. Burbey
Department of Geosciences, Virginia Tech, Blacksburg, VA, USA
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The impact of faults and fissures (discontinuities) on the groundwater flow has become important in several parts of the world because the heterogeneous and anisotropic distribution of permeability in fault zones is difficult to characterize. Based on this, we propose an analysis of patterns of parameters measured in groundwater, under the premise that the observed anomalies can be indicators of the hydraulic behavior of the flow in the direction perpendicular to the fault plane.
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Land subsidence is an anthropogenic hazard triggered by different causes, one of them is groundwater overexploitation over aquifer systems, becoming risk points for aquifer pollution The obtained results showed that the Schlumberger configuration appears to be more helpful to detect changes in the stratigraphy toward depth, while dipole-dipole and Wenner are more suitable to detect lateral variations such as the vertical wastewater leakage in the first 6 to 8 m depth.
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Aguascalientes valley, located in the central part of México, is affected for a land subsidence process triggered by groundwater withdrawal. The resulted P-wave velocity models show a low-velocity anomaly within the fracture trace with widths from 50 to 100 meters. This anomaly is interpreted as a mechanically disturbed zone due to the activity of the surface fault, this is, due to the presence of fracturing caused to the adjacent material by the differential subsidence.
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The organization and working way of an interdisciplinary and intragovernmental committee to face the effects of the land subsidence related ground failures in Aguascalientes State, México is showed. The committee is composed by federal, state, and municipal governmental agencies, as well as privet and civil associations, and the state university, working split in four groups to manage the risk related to ground cracks and surface faults.
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This research contributes to the understanding of surface deformation in the study area with new knowledge of the upper soil sequence. An established sequence distribution of the shallow layers was set and some of their geotechnical properties were determined. The analized samples are composed by compressible clayey silt and several lenses of volcanic sandy ash. Heterogeneities may be contributing to differential subsidence which is controlling the occurrence of surface faulting.
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Water level and subsidence measurements from extensometers can be used to extract important hydraulic parameters of each aquifer in a multi-level aquifer system if cyclical pumping has occurred and water level data for each aquifer is available. Fourteen years of water-level and subsidence data are analyzed for Las Vegas Valley and data analysis of daily and seasonal pumping patterns allow for the calculation of hydraulic conductivity and elastic and inelastic storage properties of the aquifer.
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The impact of faults and fissures (discontinuities) on the groundwater flow has become important in several parts of the world because the heterogeneous and anisotropic distribution of permeability in fault zones is difficult to characterize. Based on this, we propose an analysis of patterns of parameters measured in groundwater, under the premise that the observed anomalies can be indicators of the hydraulic behavior of the flow in the direction perpendicular to the fault plane.
Fernando Acuña-Lara, Jesús Pacheco-Martinez, Hugo Luna-Villavicencio, Martín Hernández-Marín, and Norma González-Cervantes
Proc. IAHS, 382, 5–9, https://doi.org/10.5194/piahs-382-5-2020, https://doi.org/10.5194/piahs-382-5-2020, 2020
Short summary
Short summary
Land subsidence is an anthropogenic hazard triggered by different causes, one of them is groundwater overexploitation over aquifer systems, becoming risk points for aquifer pollution The obtained results showed that the Schlumberger configuration appears to be more helpful to detect changes in the stratigraphy toward depth, while dipole-dipole and Wenner are more suitable to detect lateral variations such as the vertical wastewater leakage in the first 6 to 8 m depth.
Hugo Luna-Villavicencio, Jesús Pacheco-Martínez, Fernando Acuña-Lara, Martín Hernández-Marín, and Norma González-Cervantes
Proc. IAHS, 382, 781–785, https://doi.org/10.5194/piahs-382-781-2020, https://doi.org/10.5194/piahs-382-781-2020, 2020
Short summary
Short summary
Aguascalientes valley, located in the central part of México, is affected for a land subsidence process triggered by groundwater withdrawal. The resulted P-wave velocity models show a low-velocity anomaly within the fracture trace with widths from 50 to 100 meters. This anomaly is interpreted as a mechanically disturbed zone due to the activity of the surface fault, this is, due to the presence of fracturing caused to the adjacent material by the differential subsidence.
Jesús Pacheco-Martínez, Martín Hernández-Marín, Mario E. Zermeño-de-León, Norma González-Cervantes, José A. Ortiz-Lozano, Omar Vázquez-Gloria, and Armando Roque-Cruz
Proc. IAHS, 382, 791–795, https://doi.org/10.5194/piahs-382-791-2020, https://doi.org/10.5194/piahs-382-791-2020, 2020
Short summary
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The organization and working way of an interdisciplinary and intragovernmental committee to face the effects of the land subsidence related ground failures in Aguascalientes State, México is showed. The committee is composed by federal, state, and municipal governmental agencies, as well as privet and civil associations, and the state university, working split in four groups to manage the risk related to ground cracks and surface faults.
J. A. Ortiz, L. A. Hernández, M. Hernández, J. Pacheco, M. E. Zermeño, and R. Salinas
Proc. IAHS, 372, 141–144, https://doi.org/10.5194/piahs-372-141-2015, https://doi.org/10.5194/piahs-372-141-2015, 2015
Short summary
Short summary
This work presents the experimental and numerical results about a study regarding the performance of a full-scale thin-walled cold-formed steel building affected by ground differential settlements.
M. Hernandez-Marin, J. Pacheco-Martinez, J. A. Ortiz-Lozano, G. Araiza-Garaygordobil, and A. Ramirez-Cortes
Proc. IAHS, 372, 89–93, https://doi.org/10.5194/piahs-372-89-2015, https://doi.org/10.5194/piahs-372-89-2015, 2015
Short summary
Short summary
This research contributes to the understanding of surface deformation in the study area with new knowledge of the upper soil sequence. An established sequence distribution of the shallow layers was set and some of their geotechnical properties were determined. The analized samples are composed by compressible clayey silt and several lenses of volcanic sandy ash. Heterogeneities may be contributing to differential subsidence which is controlling the occurrence of surface faulting.
E. Cabral-Cano, D. Solano-Rojas, T. Oliver-Cabrera, S. Wdowinski, E. Chaussard, L. Salazar-Tlaczani, F. Cigna, C. DeMets, and J. Pacheco-Martínez
Proc. IAHS, 372, 255–260, https://doi.org/10.5194/piahs-372-255-2015, https://doi.org/10.5194/piahs-372-255-2015, 2015
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Ground subsidence has affected Mexico City for over a century, as a result of its large urban expansion and aggressive groundwater extraction rates. The continuous subsidence results in severe damage to urban infrastructure and civil structures. This work is aimed towards a better recognition of subsidence as a major hazard in Mexico, assess the number of inhabitants affected and the spatial extent of the subsiding areas affected by this process.
J. Pacheco-Martínez, S. Wdowinski, E. Cabral-Cano, M. Hernández-Marín, J. A. Ortiz-Lozano, T. Oliver-Cabrera, D. Solano-Rojas, and E. Havazli
Proc. IAHS, 372, 121–127, https://doi.org/10.5194/piahs-372-121-2015, https://doi.org/10.5194/piahs-372-121-2015, 2015
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In this work we present the application of InSAR analysis and gravimetric surveying to generate valuable information for risk management related to land subsidence and surface faulting. Subsidence of the city of Aguascalientes, México is presented as study case.
Our work based on gravimetric and InSAR surveys is aimed for improving the subsidence hazard zoning proposed in the State Urban Code in a more comprehensive way.
M. Hernández-Marín, N. González-Cervantes, J. Pacheco-Martínez, and D. H. Frías-Guzmán
Proc. IAHS, 372, 235–238, https://doi.org/10.5194/piahs-372-235-2015, https://doi.org/10.5194/piahs-372-235-2015, 2015
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This paper provides a discussion related to the origin of surface failures in the graben of Aguascalientes. Observations indicate that some of these failures are older than the beginning of pumping, suggesting a natural tectonic origin. Some questions regarding surface failures are formulated, for instance, are the surface failures caused by the combined stresses of pumping and tectonism? Is the current tectonism sufficient to cause some surface or deep failures?
T. J. Burbey and M. Zhang
Proc. IAHS, 372, 411–416, https://doi.org/10.5194/piahs-372-411-2015, https://doi.org/10.5194/piahs-372-411-2015, 2015
Short summary
Short summary
Land subsidence due to long-term pumping in Las Vegas Valley has been a problem for more than 40 years. A new groundwater flow and deformation model was built to accompany new radar and water-level data. Results show that although rising water levels have resulted in uplift in some areas, the Northwest region will continue to subside for the foreseeable future in spite of these mitigation measures.
Cited articles
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Hernández-Marín, M., González-Cervantes, N., Pacheco-Martínez, J., and Frías-Guzmán, D. H.: Discussion on the origin of surface failures in the Valley of Aguascalientes, México, Proc. IAHS, 372, 235–238, https://doi.org/10.5194/piahs-372-235-2015, 2015.
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Short summary
This paper studies the appearance of low-magnitude earthquakes linked to rapid movements of subsidence-related faults in the Aguascalientes valley. A particular seismic event is studied and occurred in the normal ancient Oriente Fault whose rapid movement was captured with PSInSAR.
This paper studies the appearance of low-magnitude earthquakes linked to rapid movements of...