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DMS

DMS
Lars Harald Blikra & Lene Kristensen, Åknes/Tafjord Monitoring Centre
Mario Lovisolo, Centro Servizi di Geoingegneria (CSG), Italy
Åknes/Tafjord Beredskap IKS
Risk related to large rockslides in Norway

Åknes
Tafjord 1934

Loen 1905 og 1936

Åknes/Tafjord Beredskap IKS
Monitored rockslides
in Norway
Handled by two monitoring
centres funded by
government/NVE,
municipalities and counties:
• Åknes/Tafjord Beredskap
(technical and geological)
• Nordnorsk fjellovervåking
(technical)

Åknes/Tafjord Beredskap IKS

CONTENT
 Requirements
 Subsurface investigations &
instrumentation
 Åknes and Jettan case
 Conclusions
Regulations in Norwegain building code
• The population safety needs to be taken care of by realtime monitoring, warning and evacuation

• The warning time shall not be shorter than 72 hours and
the evacuation time shall be maximum 12 hours
• A system for daily continuous monitoring of the
conditions, e.g. by measurements of displacements
• Independent monitoring instruments and backup
communication and power systems
• Sufficient technical and geo personnel/competence for
safe and reliable monitoring and warning

Åknes/Tafjord Beredskap IKS
(1) Investigations
• Surface
• Subsurface

(2) Monitoring systems
• Surface
• Subsurface
• Driving mechanisms

Åknes/Tafjord Beredskap IKS





Geophysics were possible
Core drillings
Borehole logging – televiewer and other sensors
Borehole displacements

Åknes/Tafjord Beredskap IKS
INSTRUMENTATION
Inclinometer probe – manual readings
?
Long columns with continuous records
Considerations
•
•
•
•
•

Åknes/Tafjord Beredskap IKS

High cost of boreholes
Robustness
Characterization vs real-time warning
Resolution
Flexibility
• Robust technology
• Leading technology
• Large economic savings in a
long-term perspective
The DMS borehole instrumentation:
• Documented to have survived
more than 70 cm movements
Conventional methods: c. 3 cm

Åknes/Tafjord Beredskap IKS

DMS
Casing

Åknes/Tafjord Beredskap IKS
Method: Differential monitoring system (DMS)

1 m modules

Åknes/Tafjord Beredskap IKS
Differential monitoring system, DMS – “Snake”
Real-time , continuous measurements
Steel
modules
with sensors

Flexible centralizers
fixed to the borehole
casing
Flexible
junctions

Åknes/Tafjord Beredskap IKS

Subsurface LAB:
• 2D Inclinometer (0,4
mm resolution)
• Pietzometer
• Temperature sensor
• Digital compass
• One systems of 150
m length, total of 304
sensors
Example: Åknes

Deep drillings

Åknes/Tafjord Beredskap IKS
SEE ALSO POSTER: GB INSAR
MEASUREMENT AT THE ÅKNES
ROCKSLIDE, NORWAY

Åknes/Tafjord Beredskap IKS
Åknes/Tafjord Beredskap IKS
Deep core drillings – 200 m deep

Åknes/Tafjord Beredskap IKS
N

E

Televiewer image
of the sliding plane

Sliding zone

Åknes/Tafjord Beredskap IKS

S

W

N
2 years of
displacements
2011and 2012:
Direction towards
SW

Sliding plane
2009 - 2013:
• Total of 9 cm
movements on
2 sensors

Åknes/Tafjord Beredskap IKS

Accumulated
total

Differential
Movement
for each
individual
sensor
DMS time series: 49-51 m depth

Åknes/Tafjord Beredskap IKS
Åknes/Tafjord Beredskap IKS
Time line for sensor
at 49-50 m depth.
• Displacement
• Water level
• Temperature

Internal changes/
dynamics of the
rockslide controls
the hydrological
system and the
deformations

Åknes/Tafjord Beredskap IKS
Lyngseidet

Åknes/Tafjord Beredskap IKS
Aktive back fracture:
20-25 m deep, 2,5 cm/year

Åknes/Tafjord Beredskap IKS
Active movements

Åknes/Tafjord Beredskap IKS
Depth/Size/Volume?

Åknes/Tafjord Beredskap IKS
Rock cores

Åknes/Tafjord Beredskap IKS
Clay in sliding zone: 45 m depth

Åknes/Tafjord Beredskap IKS
Borehole instrumentation to measure movements, temperature and water

Åknes/Tafjord Beredskap IKS
DMS movements at 45/46
m depth:
1th of May – 3rd of October

E

Åknes/Tafjord Beredskap IKS
Time series February – August 2013
May 2013

Åknes/Tafjord Beredskap IKS
Active movements

Åknes/Tafjord Beredskap IKS
Volume: Probably 5-6 mill. m3

Åknes/Tafjord Beredskap IKS
DMS and Real-time warning
• Each sensor have threshold values for displacements
• Can follow directly the critical sliding zones
• Sms thresholds: 1 mm/day

• Threshold values for different hazard levels
• Trustable and robust system
• Little noise compared to surface measurements

Åknes/Tafjord Beredskap IKS
 Norwegian building codes has strong requirements
for monitoring and permanent handling of the EWS
 Subsurface data gives a knowledge platform for
early-warning and key data for geological
models/volumes needed for evaluation of runout/tsunamis (RISK)
 Borehole instrumentation is a vital part of real-time
monitoring
 DMS instrumentation is a robust in-situ
laboratorium:
• Direct displacement at sliding planes with directions
• Water pressure vs movements
• Temperature/permafrost vs movements

Åknes/Tafjord Beredskap IKS
Important that the geoscientific
community clearly tells the
government what knowledge is
needed for reliable monitoring and EW

Åknes/Tafjord Beredskap IKS

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Blikra - vajont 2013

  • 1. DMS DMS Lars Harald Blikra & Lene Kristensen, Åknes/Tafjord Monitoring Centre Mario Lovisolo, Centro Servizi di Geoingegneria (CSG), Italy Åknes/Tafjord Beredskap IKS
  • 2. Risk related to large rockslides in Norway Åknes Tafjord 1934 Loen 1905 og 1936 Åknes/Tafjord Beredskap IKS
  • 3. Monitored rockslides in Norway Handled by two monitoring centres funded by government/NVE, municipalities and counties: • Åknes/Tafjord Beredskap (technical and geological) • Nordnorsk fjellovervåking (technical) Åknes/Tafjord Beredskap IKS CONTENT  Requirements  Subsurface investigations & instrumentation  Åknes and Jettan case  Conclusions
  • 4. Regulations in Norwegain building code • The population safety needs to be taken care of by realtime monitoring, warning and evacuation • The warning time shall not be shorter than 72 hours and the evacuation time shall be maximum 12 hours • A system for daily continuous monitoring of the conditions, e.g. by measurements of displacements • Independent monitoring instruments and backup communication and power systems • Sufficient technical and geo personnel/competence for safe and reliable monitoring and warning Åknes/Tafjord Beredskap IKS
  • 5. (1) Investigations • Surface • Subsurface (2) Monitoring systems • Surface • Subsurface • Driving mechanisms Åknes/Tafjord Beredskap IKS
  • 6.     Geophysics were possible Core drillings Borehole logging – televiewer and other sensors Borehole displacements Åknes/Tafjord Beredskap IKS
  • 7. INSTRUMENTATION Inclinometer probe – manual readings ? Long columns with continuous records Considerations • • • • • Åknes/Tafjord Beredskap IKS High cost of boreholes Robustness Characterization vs real-time warning Resolution Flexibility
  • 8. • Robust technology • Leading technology • Large economic savings in a long-term perspective The DMS borehole instrumentation: • Documented to have survived more than 70 cm movements Conventional methods: c. 3 cm Åknes/Tafjord Beredskap IKS DMS
  • 10. Method: Differential monitoring system (DMS) 1 m modules Åknes/Tafjord Beredskap IKS
  • 11. Differential monitoring system, DMS – “Snake” Real-time , continuous measurements Steel modules with sensors Flexible centralizers fixed to the borehole casing Flexible junctions Åknes/Tafjord Beredskap IKS Subsurface LAB: • 2D Inclinometer (0,4 mm resolution) • Pietzometer • Temperature sensor • Digital compass • One systems of 150 m length, total of 304 sensors
  • 13. SEE ALSO POSTER: GB INSAR MEASUREMENT AT THE ÅKNES ROCKSLIDE, NORWAY Åknes/Tafjord Beredskap IKS
  • 15. Deep core drillings – 200 m deep Åknes/Tafjord Beredskap IKS
  • 16. N E Televiewer image of the sliding plane Sliding zone Åknes/Tafjord Beredskap IKS S W N
  • 17. 2 years of displacements 2011and 2012: Direction towards SW Sliding plane 2009 - 2013: • Total of 9 cm movements on 2 sensors Åknes/Tafjord Beredskap IKS Accumulated total Differential Movement for each individual sensor
  • 18. DMS time series: 49-51 m depth Åknes/Tafjord Beredskap IKS
  • 20. Time line for sensor at 49-50 m depth. • Displacement • Water level • Temperature Internal changes/ dynamics of the rockslide controls the hydrological system and the deformations Åknes/Tafjord Beredskap IKS
  • 22. Aktive back fracture: 20-25 m deep, 2,5 cm/year Åknes/Tafjord Beredskap IKS
  • 26. Clay in sliding zone: 45 m depth Åknes/Tafjord Beredskap IKS
  • 27. Borehole instrumentation to measure movements, temperature and water Åknes/Tafjord Beredskap IKS
  • 28. DMS movements at 45/46 m depth: 1th of May – 3rd of October E Åknes/Tafjord Beredskap IKS
  • 29. Time series February – August 2013 May 2013 Åknes/Tafjord Beredskap IKS
  • 31. Volume: Probably 5-6 mill. m3 Åknes/Tafjord Beredskap IKS
  • 32. DMS and Real-time warning • Each sensor have threshold values for displacements • Can follow directly the critical sliding zones • Sms thresholds: 1 mm/day • Threshold values for different hazard levels • Trustable and robust system • Little noise compared to surface measurements Åknes/Tafjord Beredskap IKS
  • 33.  Norwegian building codes has strong requirements for monitoring and permanent handling of the EWS  Subsurface data gives a knowledge platform for early-warning and key data for geological models/volumes needed for evaluation of runout/tsunamis (RISK)  Borehole instrumentation is a vital part of real-time monitoring  DMS instrumentation is a robust in-situ laboratorium: • Direct displacement at sliding planes with directions • Water pressure vs movements • Temperature/permafrost vs movements Åknes/Tafjord Beredskap IKS
  • 34. Important that the geoscientific community clearly tells the government what knowledge is needed for reliable monitoring and EW Åknes/Tafjord Beredskap IKS