WE Report

Lessons Learned

Lesson Learned





By: Karina Helle

Report No.

1150

Discipline/Origin

HSEQ
PSA Q&A

Well

Kallåsen
35/12-6 S

Date created

2018/03/21
2817 days ago

Project Phase

Project Phase

LL Type/Classification

PSA Q&A
N/A

Transocean Arctic


PSA Q&A

Question

Risiko for shallow water flow og mitigerende tiltak.

Answer

Ref AfC chapter 3.6.2, shallow water flow is considered a regional risk in the Kallåsen area. From
offset experience, the Utsira sands may result in shallow water flow if drilled with seawater as the
drilling fluid.
With this risk in mind Wellesley requested Gardline to address the shallow water flow risk when
assessing the site survey data over all well locations. From an assessment of the seismic data
Gardline concluded the risk of shallow water flow is higher when remobilized sands are drilled into.
For this reason, Gardline recommended to move the top-hole location of the Kallåsen well away
from the disturbed zone (with remobilized sands) which Wellesley have done (hence the S shaped
well) ref. attached document ‘Gardline SWF Kallåsen Location Study’.
None the less Wellesley are of the view the risk of shallow water flow cannot be negated by moving
the top-hole location alone and therefore consider it prudent to drill this section with a weighted
mud. After evaluating the options Wellesley have concluded the best option is to drill the section
using a riserless mud recovery system from IKM (MMR system) that allows both a weighted mud to
be employed and enables proper isolation of any potential shallow water flow sands behind
cemented casing.
Utilizing a foamed cement slurry is critical when cementing the casing to prevent the cement from
losing its fluid weight properties as it sets. Traditional cements, as they gels up and pressure/volume
losses occur, lose their ability to act as a fluid and therefore can result in loss hydrostatic pressure
which could provoke any shallow water interval to flow. See Figure 1-1 below.
The recommended practice from Halliburton is to cement with a foamed Deep Water Flow Stop
(DWFS) cement that is specifically designed to address this problem. Figure 1-2 is a demo version to
show importance of cement compressibility on the overbalance short term after placement. Key is
to maintain overbalance until gel is into safe zone.
Foamed DWFS has an aggressive strength development and high compressibility (foam essential for
high compressibility) that maintains its hydrostatic pressure longer into gel development period
ensuring the hydrostatic pressure against any shallow water flow interval is maintained until the
cement has begun to bond. This ensures the cement does not get contaminated and avoids
channeling. The foaming of the cement is essential to this process in combination with the gelling
properties of the DWFS mix.
References is also made to ‘KallÃ¥sen Risk Register – Shallow Water Flow’ which summarises the risk
assessments done.

Additional Documentation


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