Networks & Deformation Analysiswebarchiv.ethz.ch/geometh-data/student/eg1/2010/05...10.11.2010 13:45...
Transcript of Networks & Deformation Analysiswebarchiv.ethz.ch/geometh-data/student/eg1/2010/05...10.11.2010 13:45...
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04.11.2010Prof. Dr. H. Ingensand Geodetic Metrology and Engineering Geodesy
Networks & Deformation Analysis
10.11.2010 13:45 – 14:30 HIL C 71.3
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Networks & Deformation Analysis
Contents
Coordinate Systems & Reference Frames
Deformation Analysis (epochal) – Epoch Approach
Deformation Analysis (continuous) – Time Series Analysis
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Networks in Engineering Geodesy
• serve as a unique, homogeneous and sufficiently precise geometric reference
• allow simultaneous work at different locations at a large construction site
• network configuration should be....– geometrical optimal (in consideration of the site, costs, time etc.)– stable over the whole construction period and beyond (reliability of
marking)– protected against destruction (natural hazards, affect of construction
traffic)– minimization of refraction impacts– observe the law of nearest neighbors
Coordinate Systems & Reference Frames
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– precision is not sufficiently high e.g. national grid 1.0 · 10-4 (1 σ), industrial requirements are ca. 1.0 · 10-5 (1 σ)
– distortions due to the Gauß-Krüger-mapping function, i.e. scaling factor varies
– point density is not sufficient (1 TP 4th order / km2)– trigonometric network is hierarchic; but homogeneous network required – location of points is driven by requirements in land surveying
establishment of a special control network– realization simpler than densification of an existing network– an unconstrained transformation to the national grid is simply achieved– coordinates obtained in 3D directly
Coordinate Systems & Reference Frames
Why is the national trigonometric network not used in Engineering Geodesy?
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The main objectives are:• confirm stability of reference points and detect single point movements• provide deformation vectors• inform about most recent deformations
2. epoch1. epoch deformation vectors
Deformation Monitoring: Two-Epoch Analysis
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deformation analysis based on geodetic methods:
1. Establishment of an observation scheme.2. Outlier detection (robust blunder tests). Important step: undetected model errors
will be interpreted as deformations!).3. Free adjustment of individual epochs.4. Combined adjustment of all epochs. Detection of movements. 5. Description of deformation pattern by a suitable deformation model.
“Classical Deformation Analyses” informs about correlations between epochs and significance of movements, based on hypothesis testing
• Congruency Test – did a point group stay stable?• Single Point Diagnosis – is there a significant displacement of one point?• Rigid Body Displacement – significant movement of point groups?
Deformation Monitoring: Two-Epoch Analysis
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Requirements for Networks in Engineering Geodesy
network planning – key task in deformation analyses
obtain information about:
• position and geometry of the network stations – high sensitivity of network, high reliability, detection of movements with significance
• limits of the deformation zone
1. direction
2. magnitude
3. temporal characteristic
horizontal movements of a dam vertical movements of a bridge
of the expected movements –sensitivity along deformation
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Specification from client: observe deformation across a valley
What is the required coordinate standard deviation?
The accuracy of the coordinate determination of one point is required better than 1 = 0.8 mm !
blunders and systematic errors not included!
• surveying tolerance standard deviationtolerance = 99%-confidence interval
= 2.5 => 1 = 4 mm / 2.5 = 1.6 mm
... between 2 epochs=> 1 ti , (Y,X,H) = 1.13 mm=> 1 ti , (Y,X,H) = 1.13 mm / 2 = 0.8 mm
• Deformation means:coordinate differences....=> 1 t = 1.6 mm=> 1 ti = 1.6 mm / 2 = 1.13 mm
Requirements for Networks in Engineering Geodesy
tolerance: ± 4mm
coordinates not directly observable
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Networks for Deformation Monitoring
Two main types of points in the network
a) object points for detection of relative displacements
note: discretisation of the object by a suitable number of object points that represent the deformations well
b) statistically stable reference points for detection of absolute displacements
relative displacements – changes in the geometry of the object
absolute displacements – movements of the whole object
problematic: stability of the so-called “stable” points
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In-Stability of Reference Points
reasons for movements of reference points:
• pressure changes of the subsoil: additional weight of buildings, less weight due to excavations
• dynamic pressure impacts due to traffic, in particular near bridges and transportation routes
• hydrological changes in the soil, oftentimes periodic (ground water table, moistness of the soil)
• impact of ground frost (some millimetre uplift while freezing, subsidence while defrost)
• above ground temperature changes to pillars and markers connected to a building
typical order of magnitude: • long term horizontal pillar translation: 1 cm up to multiple cm• short term horizontal pillar translation: 1 mm• vertical movement of cohesive soil: 2...3 mm/year• vertical movement of markers at buildings: 0.8 mm/year
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Reactions of objects to outer forces
types of deformations:
geometric changes of monitored object
rigid body motion
translationrotation
bendingtorsiondistortion
deformation
reasons for deformations:
important factor: temperature
natural: daily, yearly, sun & shademan made: artificial heat sources in industry
important factor: water level
natural: daily, yearly, participationman made: reservoirs, mining, excavation
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Reactions of objects to outer forces
single input single output model (SISO)
• different changes in the system input (sudden, gradual & periodic)
• different time delays of system reaction
• periodic events show a phase shift
defo
rmat
ion
timeinput (e.g. force)output: deformation
defo
rmat
ion
input (e.g. force)output: deformation
time
defo
rmat
ion
input (e.g. force)output: deformation
time∆t
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Reactions of objects to outer forces
displacements
absolute = the whole object↕
relative = part of the object
plastic and irreversible↕
elastic and reversible
periodical (short or long periods)↕
following a trend
geometry domain
time domain
from: Wikipedia
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Tripartite Model in Deformation Analysis
Deformation Analysis
static
equilibrium of forces
transformationL1/L2-norm
kinematic
pure geometric movements (without physical background)
frequency analysisanalysis of trends
dynamic
movements in context with the participating forces
strain, stress
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Deformation Monitoring
point positions,
geometric changes
a priory knowledge of object properties
dynamic model:
displacement functions:
dx = a0 + a1x + a2y + a3 xy + a4 x2 + ...
dy = b0 + b1x + b2y + b3 xy + b4 x2 + ...
here: polynomials
coefficients: a0, b0, a1, b2 ...
0)x ,x G(x,
quantification of
inner and outer forces, estimation of strain, refinement of deformation model
geodetic measurementsnatural & artificial load
comparison of
predicted and
determined
reactionadaptation of
model-parameters
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Deformation Monitoring
temporal discretisation
types of temporal discretisation
“continuous” foruncontrolled, sudden changes, vulnerable structures
mostly automatic
epochal, periodicforslow, predictable and innocuous reactions
mostly manual
note: so-called “continuous” measurements refer to automatic measurements with small time intervals
number of repetitions
costs
automatic
point of amortization
manual
automatic or manual observation strategy?
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“Continuous” Deformation Monitoring
temporal discretisation
time
mea
sure
d qu
antit
y true run of curve
discrete function
∆t
discretisation error
misinterpretation due to disretization
defo
rmat
ion
timetrue signal
modeled signal
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Deformation Analyses in the Time & Frequency Domain
from: Möser,
Ingenieurgeodäsie
note: some analysis algorithms require equidistant time-intervals, e.g. Fourier analysis
note: data gaps are the normal case (sensor failure, constraints don’t allow to collect continuous data)
Own PhD thesis: “On the Determination of Frequencies in Time Series”, Solving Nonlinear Adjustment Problems
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0 5 10 15 20 25-20
-15
-10
-5
0
5
10
15
20equidistant data
time [days]
ampl
itude
[cm
]
The red plot has a62 day period,
the blue plot has a frequency of 0.0847 cycles per day(= 12 day period)
Aliasing Effect
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0 5 10 15 20 25-20
-15
-10
-5
0
5
10
15
20equidistant data
time [days]
ampl
itude
[cm
]
The red plot has a62 day period,
the blue plot has a frequency of 1.93 cycles per day or a0.52 day period.
That’s the true frequency.
Aliasing Effect
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Example: Deformation Monitoring of Dams
Drilling of NEAT Tunnels: possible seduction due to falling ground water level
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Automatic Deformation Monitoring
Diploma Thesis Silvia Rossinelli 2007
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Automatic Deformation Monitoring
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Deformation Software
PANDA: Program for the Adjustment of geodetic Networks and Deformation Analysis. Hannover, for adjustments, deformation analyses of 1D, 2D und 3D nets within ordnance and engineering geodesy
CAPLAN + NETZ2X: (Cremer Auswertung und Planerstellung) also for adjustment of geodetic networks. NETZ2X in particular for deformation analysis. München, Cremer Programmentwicklung GmbH
NEPTAN und DEFAN (Technet GmbH) Berlin, also Adjustments and Deformation Analyis
LTOP – swisstopo, official Swiss governmental adjustment software