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Pipeline Planning
Shallow
overburden
Ridge
Deep overburden
Bedrock outcrop
2 km
Depth (m)
5
1
2
12
3
7
9
Pipeline Planning
FUGRO AIRBORNE SURVEYS
Ottawa
2060 Walkley Road
Ontario, Canada K1G 3P5
Phone
Fax
Email
:1-613-731-9575
:1-613-731-0453
:postmaster@geoterrex.ca
:1-905-812-0212
:1-905-812-1504
:dighem@dighem.com
Toronto
2270 Argentia Road, Unit 2
Mississauga, Ontario, Canada L5N 6A6
Phone
Fax
Email
Fugro Airborne Surveys is a member of the Fugro Group, with offices throughout the world.
0
10m
Pipe
Depth
1 km
Overburden
Bedrock
N
Helicopter EM surveys have been borderline between soils, which
used to map apparentconductivity could be trenched, and rock which
as an aid to characterizing ground would have to be blasted. The
conditions in advance of pipeline data can be mathematically
construction. The cost of pipeline inverted to produce maps of the
construction is strongly dependent depth to bedrock, as shown on the
on the ground conditions front.
en co un te re d, an d ac cu ra te The calculated depth to bedrock
prediction of these conditions can can also be presented as a
reduce the planning risk geological cross-section, shown
considerably. on this page. This section is
V
A DIGHEM conductivity survey derived from the depth information
was used to map ground along the central flight line(s) of the
conditions along approximately map shown on the front.
130km of prospective pipeline The airborne EM survey reduced
corridor, 400m in width. The the time and cost associated with
survey took about two days to gaining land access and
complete, providing a map of permission for drilling. The survey
apparent conductivity with a also served as a check for buried,
resolution of approximately 10m. unknown power lines and
The results are interpreted to pipelines. Airborne EM surveys
determine the extent of shallow have also been used to map
bedrock (which would require ground conductivity after the
blasting) and deeper overburden pipelines have been constructed
which could be trenched to the to detect areas of high ground
depth necessary for the pipeline. conductivity due to clays or saline
Over much of the survey area it is soils. These soils can create
possible to define a single conditions in which pipeline
apparent conductivity value as the corrosion isaccelerated.

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Geotechnical Mapping with Airborne EM

  • 2. Pipeline Planning FUGRO AIRBORNE SURVEYS Ottawa 2060 Walkley Road Ontario, Canada K1G 3P5 Phone Fax Email :1-613-731-9575 :1-613-731-0453 :postmaster@geoterrex.ca :1-905-812-0212 :1-905-812-1504 :dighem@dighem.com Toronto 2270 Argentia Road, Unit 2 Mississauga, Ontario, Canada L5N 6A6 Phone Fax Email Fugro Airborne Surveys is a member of the Fugro Group, with offices throughout the world. 0 10m Pipe Depth 1 km Overburden Bedrock N Helicopter EM surveys have been borderline between soils, which used to map apparentconductivity could be trenched, and rock which as an aid to characterizing ground would have to be blasted. The conditions in advance of pipeline data can be mathematically construction. The cost of pipeline inverted to produce maps of the construction is strongly dependent depth to bedrock, as shown on the on the ground conditions front. en co un te re d, an d ac cu ra te The calculated depth to bedrock prediction of these conditions can can also be presented as a reduce the planning risk geological cross-section, shown considerably. on this page. This section is V A DIGHEM conductivity survey derived from the depth information was used to map ground along the central flight line(s) of the conditions along approximately map shown on the front. 130km of prospective pipeline The airborne EM survey reduced corridor, 400m in width. The the time and cost associated with survey took about two days to gaining land access and complete, providing a map of permission for drilling. The survey apparent conductivity with a also served as a check for buried, resolution of approximately 10m. unknown power lines and The results are interpreted to pipelines. Airborne EM surveys determine the extent of shallow have also been used to map bedrock (which would require ground conductivity after the blasting) and deeper overburden pipelines have been constructed which could be trenched to the to detect areas of high ground depth necessary for the pipeline. conductivity due to clays or saline Over much of the survey area it is soils. These soils can create possible to define a single conditions in which pipeline apparent conductivity value as the corrosion isaccelerated.