Methodological procedures to landslide risk mapping in brazilian slums
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Transcript of Methodological procedures to landslide risk mapping in brazilian slums
Methodological procedures to landslide
risk mapping in Brazilian slums
AuthorsEduardo Soares de Macedo(1), Kátia Canil(1), Fabrício Araujo Mirandola(1), Fabiana Checchinato Silva(1), Marcelo
Fischer Gramani(1), Agostinho Tadashi Ogura(1), Alessandra Cristina Corsi(1), Luciana Pascarelli Santos(2)
Presenter
Luciana Pascarelli Santos
(2) São Paulo City Council, São Paulo (SP), Brazil
(1) Institute for Technological Research – IPT , São Paulo (SP), Brazil
In this methodology, the factors that make assessment and risk analysis are
simplified, grouped and analyzed qualitatively, from direct observation in the
Description of mapping methodology
simplified, grouped and analyzed qualitatively, from direct observation in the
field. In this sense we have evaluated the following factors, considered essential
to risk analysis:
• typology of the expected process and its probability or possibility of occurrence;
• vulnerability of urban settlements; and
• potential damage.
Stages of the mapping methodology
In accordance with the requirements, the specific objectives of the performed activities
were the following:
• to obtain low-altitude oblique photos of the areas at risk from helicopter overflights;
• identify the sectors with different degrees of probability of occurrence of destructive
processes (landslides on slopes and/or washouts of stream banks) and enclose them in the
oblique photos;
• indicate the number of threatened houses or buildings that could be affected due to the
occurrence of the destructive processes mentioned above;
• present alternative measures to control the identified risks;
• design a database containing the results of the mapping.
In the areas selected by the council were performed:
• a survey of the area occupation characteristics and its infrastructure
Description of mapping methodology
CATEGORY OF CATEGORY OF
OCCUPATION CHARACTERISTICS
Consolidated area Densely occupied areas, with basic
infrastructure.
Partially consolidated
area
Areas in process of settlement,
adjacent to areas of established
occupation. Density of occupation
ranging from 30% a 90%. Reasonable
basic infrastructure.
Split area
Expansion areas, remote and distant
from urban nucleus. Low density of
occupation (up to 30%). Devoid of basic
infrastructure.
Mixed area
In such cases, characterize the area
with regard to occupation density and
implementation of basic infrastructure
• risk mapping procedures using geological and geotechnical surface investigations in order
to identify the types of gravitational mass movements
Description of mapping methodology
PROCESSES CHARACTERISTICS OF THE
MOVEMENT/MATERIAL/GEOMETRY
CREEP
- several (internal) displacement planes / -
very low to low (cm/year) velocities that
decrease with depth / - constant, seasonal
or intermittent movements /- soil, deposits,
altered/fractured rock /- undefined
geometry geometry
SLIDES
- few (external) displacement planes / -
medium (m/h) to high (m/s) velocities / -
small to large volumes of material
- variable geometry and material / PLANAR:
thin soils, soils and rocks with one weakness
plane / CIRCULAR: homogeneous thick soils
and very fractures rocks / WEDGE: soils and
rocks with two weakness planes
FALLS
- no displacement planes / - free fall- or
inclined plane-type movement / - very high
(several m/s) velocities
- rocky material / - small to medium
volumes / - variable geometry: flakes,
plates, blocks, etc. / BOULDER ROLLING /
TOPPLING
FLOWS
- many displacement surfaces (internal and
external to the moving mass) / - movement
similar to that of a viscous liquid / -
development along drainage / - medium to
high velocities / - soil, rock, debris and
water mobilization / - large volumes of
material / - extensive range, even in flat
areas
• as well as the constraints of the destabilizing processes, evidence of instability and
indication of the development of destructive processes. Thus the prevailing destabilizing
processes will be identified, delimiting and characterizing the risk sectors.
Description of mapping methodology
SITE CHARACTERIZATION MOVEMENT
EVIDENCE SITE CHARACTERIZATION
EVIDENCE
- Natural slope
- Cut slope
- Slope height
- Compacted fill
- hauled fill
- Distance from
home
- Declivity
- Unfavorable
structures in
soil/rock
- Presence of blocks
of rock/boulders/rock
walls
- Presence of
trash/debris
- Amphitheater
Landfill
- Occupation of
headwaters
- House
cracks/landfill
- Trees/poles/walls
inclination
- Etch-plains
- Landslide scars
- Swollen walls
- Erosion features
- Stream margins
undermining
PRESENCE OF WATER PRESENCE OF
VEGETATION
- Surface concentration of stormwater
- Release of wastewater into surface
- Presence of septic tanks/sewage/water
mains
- Upwelling water
- Leakings
- Trees
- Undergrowth
- Deforested area
- Farming area
Field activities
The materials to be used to obtain the support information and product to the risk
mapping are:
• vertical aerial photos, with appropriate scale, up to 1:5.000;• vertical aerial photos, with appropriate scale, up to 1:5.000;
• copies of the plano-altimetric maps, basis for the indicated mapping areas;
• information on risk areas, such as development records and/or occurrences of instability
processes, copies of technical reports and expert opinions previously prepared, any
intervention guidelines proposed (implemented or not) etc.;
• technical publications, geological, geotechnical, geomorphological and slope angle maps,
with information on areas indicated for risk mapping;
• copy of the street guide page on which is located the chosen mapping area.
LogA log is a tool to determine the potential of
accidents through field surveys carried out in order
to identify risk situations. The cards used in field
surveys should contain the aspects to be analyzed
(check list), allowing the professional come to a
conclusion as to the risk of the analyzed area.
FICHA PARA AVALIAÇÃO DE ÁREA DE RISCO
LOCALIZAÇÃO DA ÁREA
Endereço: Área nº:
SITUAÇÃO DA ÁREA (VIDE MODELOS ANEXOS)
( ) Encosta ( ) Margem de córrego ( ) Encosta + Margem de córrego
CIRCUNSTÂNCIAS EM QUE SE DESENVOLVEM OS PROCESSOS
ENCOSTA MARGEM DE CÓRREGO
( ) Concentração ou lançamento de águas em superfície ( ) Pontos de infiltração ou minas
( ) Presença de vegetação. Qual? ________ ( ) Área desmatada ( ) Presença de lixo e entulho
( ) Trechos aterrados ou escavados ( ) Outros. Citar:_______________
EVIDÊNCIAS DE PROCESSO DE INSTABILIZAÇÃO
( ) trincas/rachaduras ( ) degraus de abatimento ( ) muros embarrigados
( ) cicatrizes de escorregamento ( ) árvores/postes inclinados ( ) outros. descrever:___________
Nº DE MORADIAS (A SEREM) EFETIVAMENTE ATINGIDAS
HÁ POSSIBILIDADES DE CONVIVÊNCIA COM O RISCO? POR QUÊ?
GRAU DE PROBABILIDADE DE OCORRÊNCIA DE PROCESSO DE INSTABILIZAÇÃO
( ) R1 – Baixo ( ) R2 – Médio ( ) R3 – Alto ( ) R4 – Muito Alto
RESPONSÁVEL PELAS INFORMAÇÕES:
Distância observada:______ m Distância observada:______ m
OverflightOverflights by helicopter should be preceded by flights planning supported by technical field visits in
order to obtain coordinates from the GPS readings.
Besides the programming of helicopter overflights, all the technical material will allow the
optimization of the field activities, as well as a preliminary analysis of the areas to be mapped,
allowing for a fast and efficient mapping.
The risk sectors will be delimited with the indication of the probable destabilizing processes, that is,
landslides on natural slopes or cutting slopes and embankments. The criteria for judging the
probability of the destabilizing processes of occupied slopes landslides kind, as well as the
parameters analyzed for further procedures.
Description of mapping methodology
PROBABILITY DEGREE
R1 - Low Risk R3 - High Risk
Concerning to evaluated
indicators, the area shows
low risk to develop landslides
processes
Concerning to evaluated
indicators, the area shows high
risk to develop landslides
processes. Relevant indicators
of instability processes can be
observed
R2 - Medium Risk R4 - Very High Risk
Concerning to evaluated
indicators, the area shows
medium risk to develop
landslides processes. Just
some indicators of instability
processes can be observed.
Concerning to evaluated
indicators, the area shows very
high risk to develop landslides
processes. Almost all the
indicators of instability
processes can be observed. It is
the most critical condition.
Representation of sectors in the oblique photosFor the representation of the sectors at low-altitude oblique photos the following procedures,
criteria, symbols and conventions were adopted
• on the oblique photos, with the delimited risk factors the identification of the houses to be removed is
done with the letter “r”;
• in cases where the same sector is represented in more than one oblique photo, preference should be
given to the photo where the sectors can be better seen and their boundaries more precise.
Final Comments
For The risk mapping allows an assessment of the areas aiming to provide immediate, medium and
long term solutions for the slums in the most critical situation.
The obtained results will enable the city administration develop a strategic plan of interventions to
reduce and control the mapped risks, enabling the cost estimate for the suggested interventions for
each sector and the establishment of sequence of priorities for the implementation in accordance
with the technical criteria.
An example of applying this methodology can be seen in the paper entitled “Mapping of geological
at-risk areas in the city of São Paulo: issues and results from the largest survey of risk in Brazil”,
present in session "Landslide risk assessment and management" of the Second World Landslide
Forum.