Zobrazeno 1 - 10
of 54
pro vyhledávání: '"D. Carreón-Freyre"'
Publikováno v:
Proceedings of the International Association of Hydrological Sciences, Vol 382, Pp 433-436 (2020)
We report preliminary results of physical experiments of rupture occurrence and propagation associated with land subsidence driven by groundwater pumping and compare our analogue model results with corresponding previously reported numerical results.
Externí odkaz:
https://doaj.org/article/183f482bb1a9444db6b08e28935ad171
Autor:
T. López-Lara, J. B. Hernández-Zaragoza, D. Carreón-Freyre, M. Cerca, E. Rojas-González, A. G. Minor Franco, G. Martínez-Barrera, R. Salgado-Delgado
Publikováno v:
Advances in Civil Engineering, Vol 2018 (2018)
The volumetric change within soils containing expanding clays depends upon their spatial ordering and their mineralogy. So this work studies the spatial microstructural ordering and mineralogy of different expanding clays in order to correlate them w
Externí odkaz:
https://doaj.org/article/92f946860c43465b9bf8fa2406491071
Publikováno v:
Proceedings of the International Association of Hydrological Sciences, Vol 372, Pp 267-272 (2015)
In the eastern sector of Mexico City the sub soil consists of high contrasting sequences (lacustrine and volcanic inter bedded deposits) that favor the development of erratic fracturing in the surface causing damage to the urban infrastructure. Th
Externí odkaz:
https://doaj.org/article/9629db07beaa41d487a0b6042a26c52e
Publikováno v:
Proceedings of the International Association of Hydrological Sciences, Vol 372, Pp 285-290 (2015)
We present the results of a series of physical models aiming to reproduce rapid subsidence (at least 25 m in 30 years) observed in the sediments of a maar crater caused by extraction of groundwater in the interconnected adjacent aquifer. The model
Externí odkaz:
https://doaj.org/article/dd39d1fa4cca4b83a6eea10491c90a10
Autor:
D. Carreón-Freyre, M. González-Hernández, D. Martinez-Alfaro, S. Solís-Valdéz, M. Cerca, B. Millán-Malo, R. Gutiérrez-Calderón, F. Centeno-Salas
Publikováno v:
Proceedings of the International Association of Hydrological Sciences, Vol 372, Pp 273-279 (2015)
An analysis of the deformation conditions of lacustrine materials deposited at three sites in the volcanic valley of the Mexico City is presented. Currently geotechnical studies assume that compressibility of granular materials decreases in depth
Externí odkaz:
https://doaj.org/article/9d090bb4e8fd488cb9cee43245e52c9b
Publikováno v:
Proceedings of the International Association of Hydrological Sciences, Vol 372, Pp 63-68 (2015)
The stress variation induced by aquifer overdraft in sedimentary basins with shallow bedrock may cause rupture in the form of pre-existing fault activation or earth fissure generation. The process is causing major detrimental effects on a many are
Externí odkaz:
https://doaj.org/article/ddb59196fc94432ca2e7b9d2e684ca47
Publikováno v:
Proceedings of the International Association of Hydrological Sciences, Vol 372, Pp 261-265 (2015)
Geological and structural conditions in the Basin of Mexico coupled with natural and anthropogenic factors, such as groundwater exploitation, provokes land subsidence and differential deformation. The study area is located in to the north of Iztap
Externí odkaz:
https://doaj.org/article/6818ad3c062e4e3fb9f6946fdb5b5eb5
Autor:
T. Lopez-Lara, C. L. Gonzalez-Vega, J. B. Hernandez-Zaragoza, E. Rojas-Gonzalez, D. Carreón-Freyre, R. Salgado-Delgado, E. Garcia-Hernandez, M. Cerca
Publikováno v:
Advances in Materials Science and Engineering, Vol 2014 (2014)
In general, bricks frequently show different densities and therefore different resistances because the compaction energy is not considered in their production. Expansive soils represent a problem for light buildings over them because of volumetric in
Externí odkaz:
https://doaj.org/article/8923ffbacd3a47499aaac8e63584c1a0
Publikováno v:
Scopus-Elsevier
Summary Here we report the results of an academic exercise to locate a potential site for underground CO2 storage in east-central Mexico. The objective of this study was to interpret the main lithostratigraphic units and structures within a 3D seismi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ecd7af165e70dd636e350bc37ee5223d
https://doi.org/10.3997/2214-4609.201902502
https://doi.org/10.3997/2214-4609.201902502
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