Continuous Monitoring – the Lines of Evidence Approach to ...€¦ · Presentation Content 1...
Transcript of Continuous Monitoring – the Lines of Evidence Approach to ...€¦ · Presentation Content 1...
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Brownfieldbriefing Ground Gas 2018
Continuous Monitoring – the Lines of Evidence Approach to Ground-
Gas Risk Assessment
Simon Talbot - 1st Mar 2018
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Presentation Content 1 History of continuous ground-gas monitoring
2 Challenges of ground-gases
3 Over ten years of continuous monitoring
4 Additional lines of evidence a) Environmental correlations
b) Purge & recovery tests
c) Differential pressure assessment
d) Concentration duration
5 New techniques
6 Case study
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History to continuous monitoring - Traditional Spot Monitoring
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IRP-IGM
GMGU
2006 - dti Research Project:
“Development and assessment of an in-borehole gas monitoring device as a decision making tool” Collaboration between: • Stephen Boult Salamander
• Simon Talbot GMGU • Peter Morris University of Manchester
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dti Research - Expert Advisory Group • Hugh Mallett Buro Happold • Geoff Card GB Card & Partners • Peter Witherington RSK ENSR • Steve Wilson EPG Ltd
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dti 2009 research outcomes: • First commercial deployment of
GasClam®
• Development of additional lines of evidence:
• Environmental correlations
• Concentration duration curves
• Purge & recovery gas-flux
• Differential pressure assessment
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Also in 2009 • GGS established
• Ground Gas Handbook published making reference to the research
Christmas Borehole – case study
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CL:AIRE RB 13 Boult, Morris & Talbot, 2011
• Sets out many of the different lines of evidence provided by continuous monitoring
• Moved the approach from an esoteric university research spin off into a main stream technique
• Now widely adopted and has been used on 1,000s of sites in the UK and elsewhere.
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Continuous Ground-Gas Monitoring
1st Generation In-borehole device
GasClam®
Ambisense 2nd Generation In-borehole device
Gas Sentinel®
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Gas Sentinel® • First British made device • Secure installation • Telemetry enabled • Continuous flow
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31 Jan 02 Feb 04 Feb 06 Feb 08 Feb 10 Feb 12 Feb
When the frequency of monitoring exceeds the frequency of change of the measured parameter, the monitoring can be termed ‘continuous’
Continuous Monitoring Co
ncen
trat
ion
(v/v
%)
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Solid Liquid Gas
Environmental monitoring challenges
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Permeability Anisotropy
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Permeability anisotropy and borehole monitoring
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Importance of the Conceptual Site Model
Source - Pathway - Receptor Pollutant Linkage
Driving mechanism
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Lines of Evidence - Environmental Correlations
Multi-parameter continuous data…
Identify or eliminate correlations with the environment
Identify or rule out ground-gas drivers
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Atmospheric Pressure as a Ground-Gas Driver
985
990
995
1000
1005
1010
1015
0.0
10.0
20.0
30.0
40.0
50.0
60.0
70.0
80.0
27-Dec 28-Dec 29-Dec
Pres
sure
(mill
ibar
s)
Met
hane
(% v
/v)
Methane
Atmospheric Pressure
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930
940
950
960
970
980
990
1000Pr
essu
re (m
bar)
Atmospheric Pressure
05
101520253035
20 Dec 22 Dec 24 Dec 26 Dec 28 Dec 30 Dec
Con
cent
ratio
n (%
v/v
) Methane
Atmospheric Pressure as a Ground-Gas Driver
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25
30
35
40
45
50
55
16 Aug 23 Aug 30 Aug 06 Sep
Con
cent
ratio
n (p
pmv)
TVOC
05
10152025303540
Tem
pera
ture
(ºC
)
Temperature
Temperature as a Ground-Gas Driver
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2.502.602.702.802.903.003.103.203.30
Wat
er le
vel (
mbg
l)
Water Level
0
5
10
15
20
25
26 Aug 31 Aug 05 Sep 10 Sep 15 Sep 20 Sep 25 Sep
Con
cent
ratio
n (%
v/
v)
O₂ CH4
Water Level as a Ground-Gas Driver
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99510001005101010151020
Pres
sure
(mba
r) Atmospheric pressure
0
20
40
60
80
12-Feb 13-Feb 14-Feb 15-Feb 16-Feb 17-Feb 18-Feb 19-Feb
Con
cent
ratio
n (%
v/
v)
MethaneCarbon dioxide
What’s happening here?
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Purge & Recovery Test (PRT)
Measures Gas Flux
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GGS Purge & Recovery Test
Δy
Δx
PRT recovery curves
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Calculating Gas Flux
• Back calculate the borehole volume then:
Where:
Q = Gas Flux
V = Volume of the internal vadose zone of the borehole
c = Change in gas concentration expressed as a percentage
t = change in time over which the change in concentration was measured
Repeatability demonstrates that the gas flux is a valid characteristic of that location
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940
960
980
1000
1020
Pres
sure
(mba
r)
-20-10
0102030
Pres
sure
(m
bar)
Negative flow Positive flow
No flow
Atmospheric pressure
Borehole pressure
Differential pressure
Differential Pressure Assessment
‘Barometric Pumping’
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0
5
10
15
20
25
27 Nov 29 Nov 01 Dec 03 Dec 05 Dec 07 Dec 09 Dec 11 Dec
Con
cent
ratio
n (%
)
CH4 Continuous Data
0
5
10
15
20
25
0 20 40 60 80 100
Con
cent
ratio
n (%
v/v
)
% Time
CH4 Concentration Duration Curve
Concentration Duration Curves
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Characterising Gas Regimes Data Sets Conc. Dur. Curves Data Sets Conc. Dur. Curves
Families of curves describing different behaviour
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New Tools - Ternary Plots
• Consider ratios with large data sets • Useful for looking at trends and source
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Gas Sentinel® telemetry
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Continuous Flow
Gas Sentinel®
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GSV with Continuous Data
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GSV with Continuous Data
CS2
CS4
CS3
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Prevailing Wind
Air Vents
Receptor Monitoring (Sub-floor Void Monitoring)
Continuous monitoring on the down-wind side
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Gorebridge CO2 Incident April 2014
- Incident Management Team set up in April 2014
- NHS
- Midlothian Council
- Coal Authority
- By Sept 2014, 22 people had attended A&E or local GP
- Extensive Source – Pathway – Receptor investigations carried out
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2013/14 Coal Authority Investigations 87 Newbyres Crescent found to have:
• 8% C02 in downstairs toilet
• 12% C02 in Lounge (where son had been sleeping)
• 19% CO2 beneath kitchen flooring
• 21% CO2 measured in hole drilled through raft
• 23% CO2 in wall cavity
Borehole drilled to the shallowest coal seam at 13m bgl: • 25.1 % CO2 & 4.6% O2
• No grout was found in the coal seam
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Coal Authority continuous gas monitoring
Highest CO2 associated with falling atmospheric pressure
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2017 IMT Report Conclusions
(IMT Report – from Fairhurst)
3-4m
c13m
“Was this was an entirely preventable incident?”
• Source confirmed as worked coal seam
• Workings not fully grouted
• Grout holes beneath houses possibly not sealed
• SI boreholes beneath houses possible not sealed
• Vibro stone column foundations
• Service entries through raft not sealed
• No gas protection measures installed
• Highest CO2 associated with falling atmospheric pressure
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In Summary • Ten years of experience of continuous ground-
gas monitoring
• The technique provides a range of additional lines of evidence
• It can provide higher quality information in a shorter period of time than spot monitoring
• It’s a technique that is now widely used
• Helps focus gas protection measures on those sites that needs it