Título: | DISCRETE MICRO-MICROMECHANICAL MODELING OF RESIDUAL SOILS | |||||||
Autor: |
JUAN PABLO IBANEZ |
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Colaborador(es): |
TACIO MAURO PEREIRA DE CAMPOS - Orientador EURIPEDES DO AMARAL VARGAS JUNIOR - Coorientador |
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Catalogação: | 10/JUL/2008 | Língua(s): | PORTUGUESE - BRAZIL |
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Tipo: | TEXT | Subtipo: |
THESIS
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Notas: |
[pt] Todos os dados constantes dos documentos são de inteira responsabilidade de seus autores. Os dados utilizados nas descrições dos documentos estão em conformidade com os sistemas da administração da PUC-Rio. [en] All data contained in the documents are the sole responsibility of the authors. The data used in the descriptions of the documents are in conformity with the systems of the administration of PUC-Rio. |
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Referência(s): |
[pt] https://www.maxwell.vrac.puc-rio.br/projetosEspeciais/ETDs/consultas/conteudo.php?strSecao=resultado&nrSeq=11888&idi=1 [en] https://www.maxwell.vrac.puc-rio.br/projetosEspeciais/ETDs/consultas/conteudo.php?strSecao=resultado&nrSeq=11888&idi=2 |
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DOI: | https://doi.org/10.17771/PUCRio.acad.11888 | |||||||
Resumo: | ||||||||
The present research studies the numerical modeling of the
mechanical behavior of residual soils, by a micro-mechanical
analysis, using as modeling tool the discrete elements
method (DEM), which allows the representation of the soil
as 2D particle assembly of circular discrete elements. There
are several micro and macro structural phenomena present in
residual soils, which determine its mechanical response:
double structure and double porosity of soil mass, the
presence of a clay-like matrix, partially saturated
condition, grain cementation, grain crushing, and the
presence of small blocks of not-weathered parental rock.
Based on the study of these phenomena, mathematical
formulations have been proposed in order to describe them,
which have been implemented in the DEMlib discrete elements
code. After calibration and validation of the implemented
analysis program, the influence of each phenomena in soil
response was studied by simulating edometrical and direct
shear tests in discrete samples with several
densities, criticizing the results and getting conclusions.
Afterwards, these phenomena were studied in a combined way
in order to reproduce the response of some young and mature
residual soils. To finish up this work the conclusions
obtained have been summarized and suggestions for deepening
and further developing of the implemented research line have
been stated.
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