Tomografía geoeléctrica: dos ejemplos en la Sabana de Bogotá

With the new technologies about math algorithms and software interpretation to solve the inverse problem, two examples of electric tomography were done in two different places and over quaternary deposits that correspond to Sabana de Bogota. The first, placed, near the location of Tenjo, was done to see the behaviour of the geoelectrical model with low resistivity and electric contrast materials (alluvial deposits of Formaci6n Sabana). While the second, over deposits of fluvial-glacier origen, like Rio Tunjuelito's deposits, shows effects over high resistivity materials with great lateral vari... Mehr ...

Verfasser: Briceno Guarupe Luis Alberto
Sanín Camilo Ernesto
Dokumenttyp: Artikel
Erscheinungsdatum: 2000
Reihe/Periodikum: Earth Sciences Research Journal, Vol 0, Iss 4, Pp 73-78 (2000)
Verlag/Hrsg.: Universidad Nacional de Colombia
Schlagwörter: Tecnologías en exploración geoeléctrica / Tomografía geoeléctrica / Geology / QE1-996.5
Sprache: Englisch
Permalink: https://search.fid-benelux.de/Record/base-27640501
Datenquelle: BASE; Originalkatalog
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Link(s) : https://doaj.org/article/a5bfcdeb8f494ca0bc6ecc2aa18eb30f

With the new technologies about math algorithms and software interpretation to solve the inverse problem, two examples of electric tomography were done in two different places and over quaternary deposits that correspond to Sabana de Bogota. The first, placed, near the location of Tenjo, was done to see the behaviour of the geoelectrical model with low resistivity and electric contrast materials (alluvial deposits of Formaci6n Sabana). While the second, over deposits of fluvial-glacier origen, like Rio Tunjuelito's deposits, shows effects over high resistivity materials with great lateral variations of resistivity. The evaluation of the quality of data was made with lithologic columns in both cases, in general, the results were coherent and showed high resolution. The reached depths of investigation were 30% for the first example and 40%, for the second, situating the electrodes with Wenner amd Wenner-Sciumberguer arrays. Using the results of these two examples, clearly we can see that the depth of investigation depends on the media, the geometric array and the lenght of the section. This geophysic tool is very useful in shallow applications (100 m depth), and where high resolution and quality are needed. Con base a las nuevas tecnologías en exploración geoeléctrica en cuanto a algoritmos para resolver el problema inverso y software de interpretación, se hicieron dos secciones tomográficas o “imaging”. Los dos ejemplos se realizaron, en ubicaciones diferentes y sobre sedimentos no consolidados de edad cuaternaria. EI primero, ubicado en cercanias de Tenjo, se realizó para analizar el comportamiento del modelo geoeléctrico sobre materiales de baja resistividad y contraste eléctrico (depósitos aluviales de la Formación Sabana); mientras que el segundo, ubicado sobre los depósitos originados por procesos de tipo fluvio-glaciar, como lo son los del Rio Tunjuelito, se implementó para ver efectos sobre materiales altamente resistivos y con grandes variaciones laterales de resistividad. Utilizando columnas litológicas, ...