2003
DOI: 10.1016/s0013-7952(02)00263-6
|View full text |Cite
|
Sign up to set email alerts
|

Parameterization of soil properties for a model of topographic controls on shallow landsliding: application to Rio de Janeiro

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

1
63
0
23

Year Published

2004
2004
2017
2017

Publication Types

Select...
7
1

Relationship

1
7

Authors

Journals

citations
Cited by 89 publications
(87 citation statements)
references
References 14 publications
1
63
0
23
Order By: Relevance
“…Representation of soil properties is a key problem in the use of physically based slope stability models for landslide hazard assessments, particularly for shallow failures such as debris avalanches and debris slides, as well as deepseated slumps in soil (Guimaraes et al 2003). Regolith depth, often referred to by geomorphologists and engineers as soil depth, is defined as the depth from the surface to more-or-less consolidated material.…”
Section: Predisposing Factorsmentioning
confidence: 99%
“…Representation of soil properties is a key problem in the use of physically based slope stability models for landslide hazard assessments, particularly for shallow failures such as debris avalanches and debris slides, as well as deepseated slumps in soil (Guimaraes et al 2003). Regolith depth, often referred to by geomorphologists and engineers as soil depth, is defined as the depth from the surface to more-or-less consolidated material.…”
Section: Predisposing Factorsmentioning
confidence: 99%
“…Due to the fact that the "hollows" are sometimes made by deposits of materials from their surroundings (nose and ridge), when accumulated it can generate discontinuities between the original material developed in situ and the deposited material, thus favoring heterogeneity in permeability. These differences of permeability may favor the generation of zones of saturation and induce shallow landslides (Small, 1970;Pierson, 1980: Wilson andDietrich, 1987;Guimarães et al, 2003;Bogaart and Troch, 2006). Soils or "alteration mantles" are responses to the conditions imposed by weathering agents (physical-chemical) in the rock.…”
Section: Methodsmentioning
confidence: 99%
“…This pattern does not necessarily occur in the municipalities studied, because if some area is urbanized, it is not possible to identify scars at the present time, since it is assumed that such phenomena may occur in the future. Several studies use mathematical models to predict the unstable areas (e.g., SHALSTAB, TRIGRS, SinMAP, and others) from a high-resolution digital elevation model (DEM), and considering, for validation, landslide-scar maps (Dietrich and Montgomery, 1998;Guimarães et al, 2003;Vieira, 2007;Listo and Vieira, 2012). Although the methods used involve high-resolution information, geotechnical parameters and models based on the physical phenomena of landslides, the accuracy rate found in these studies is similar to the ones found in the present study, as shown below.…”
Section: Rating From Related Studiesmentioning
confidence: 99%
See 1 more Smart Citation
“…Moreover, the statistical models generally ignore the temporal aspects of landslides, and are not able to predict the impact of changes in landslide controlling conditions [64]. The physically based approach, on the other hand, analyzes the mechanical condition of slopes and evaluates their stability using mathematical calculations [5,[65][66][67][68][69][70][71][72][73][74][75][76]. This approach couples distributed hydrological and stability models that can evaluate dynamically the risk of rainfall-induced landslide.…”
Section: Introductionmentioning
confidence: 99%