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“Underground storage of Hydrogen in porous geological media”
Underground Sun Storage
European Workshop on Underground Energy Storage|
Markus Pichler | 2019 11 07
2
RAG Austria AG
Company Profile and
Vision• Among leading technical Underground
Gas Storage Operators
• State of the art facilities
• Storage volume 66 TWh (6bcm)
• Unload capacity 30 GW
• Follow the vision to serve the renewables with our existing assets by constant improvement and innovation
2030+ residual scenario for electricity in AT
+ 12.000 MW lasting for months
3
- 8.000 MW lasting for months
+ 12.000 MW lasting for months
INPUT data: 2030+ vs. 2017 @15 minute intervals:• Demand: +30% (~63 to 81 TWh/a)• RES generation : Wind x3, Solar x20, Hydro x1 (~ 41 auf 80 TWh/a)
=> Big scale seasonal storage needed
European Potential for Wind Energy Generation
4European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
European Potential for Solar Energy Generation
5European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Motivation• Gas Storage is Energy Storage
• Gas Storage is ‘invisible‘ and ‘available on demand‘-Energy
• Gas has an existing infrastructure in many regions of the world
• Gas can be greened from 0-100% without changing the system
Goals of the Project• Demonstration of Storability of renewable gases in Gas Storage facilities
• Research on effects of 10% hydrogen admixtures in existing Gas Storage Facilities
Partners
Development of the Underground Sun Storage Project
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07 6
Project
WP
5: M
ater
ials
an
dC
orr
osi
on
WP 1: Project ManagementW
P 2
Geo
chem
istr
y an
d R
eact
ive
Tran
spo
rt m
od
elli
ng
WP
3: M
icro
bia
l P
roce
sses
in
Hyd
roge
n E
xpo
sed
R
eser
voir
s
WP
4: D
emix
ing
of
Nat
ura
l Gas
an
d
Hyd
roge
n
WP
6: M
emb
ran
e
Tech
no
logy
WP
9: R
isk
Ass
essm
ent
and
Life
Cyc
le A
sses
smen
t
WP
10
: Eco
no
mic
and
Lega
l An
alys
is
WP 7: Design and Construction of Testbed
WP 8: Testbed Operation
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07 7
Physical Parameters
• HP3A is very small and isolated
• Field experiments at reasonable costs and risks
• Conditions comparable to commercial RAG storage facilities
• High Permeability (up to 600 MD) Average Porosity (25%)
• Water Saturation (~30 %) No active Aquifer
Volumetrics
• GIIP ~6,15 MMNm³ net. Production ~4,45 MMNm³
• 1,22 MMNm³ Gas Mixture 115.444 Nm³ Hydrogen
• Pressure Range Reservoir (34 – 78 Bar(a))
• Temperature 39,5°C
Test Field Key Data
8
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Subsurface Aspects
9
Open Questions from the Literature
Are the different materials in a gas storage facility resistant against hydrogen?
Is the tightness of the subsurface reservoir also given for hydrogen?
How does the hydrogen move in the subsurface?
Does the hydrogen change the chemical equilibrium of the reservoir?
Does hydrogen react with microbes in the reservoir?
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Material Behaviour
10
• Steel and cement samples tested under lab and field conditions• Cement samples show signs of
calcification in blind and hydrogen samples
• Steel samples show no signs of embrittlement or significant reduction of strain to rupture
• Elastomers where tested only in the field
• Visual observation shows no significant changes
• Changes in mass and volume comparable to gas industry standards
• Further investigation in follow up project (USC)
Reaction Seam
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Well and Reservoir Tightness
11
• Well• No observation of hydrogen in the
annulus
• No degradation of tubing or casing (USIT)
• No detection of gas migration in the well cementation (CBL)
• Rubber elements of packers where unchanged
• Reservoir• Permeability of hydrogen and methane
in the cap rock are in the same order of magnitude
Permeability [m²] Cap Rock
Formation Core Methane Hydrogen
A2 2.1 10-18 2.3 10-18
3 2.5 10-18 2.7 10-18
B1 8.5 10-19 8.2 10-19
3 3.2 10-18 1.9 10-18
< >
SSSV an hydraulic
operation line
3 1/2“ VAGT
Superior (VÖST)
Surface Tubing
2 7/8“ VAGT
Superior (VÖST)
Production Tubing
2 3/8“ VAGT
Superior (VÖST)
Production Tubing
Hydraulic Packer
Water Sampler lost
during 1st sampling
session
Perforations at 1150 MD
Formation: HP 3a
Cementation of Gas
Well
Annulus filled with KCl
Water and Corrosion
Inhibitor
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Diffusion
12
• Only relevant for gas phase• Hydrogen diffusion in water saturated
porous media 10-4 – 10-5 m²/a
• No De- Mixing of gas during Shut In (Diffusion forces stronger then gravimetric effects)
• Changes in withdrawn gas due to• Diffusion?
• Dispersion?
• Dissolution?
• Chemical Reactions?
• Conversion?
0 5 10 15 20 25 30 35 40 45 50 5512
12.25
12.5
12.75
13
ratio top
lin trend top
ratio bottom
lin trend bottom
Reactor 10 bar
week
Rat
io C
H4/H
2
0
2
4
6
8
10
12
-20,000 180,000 380,000 580,000 780,000 980,000 1,180,000
Hyd
rog
en
Co
ncecn
trati
on
%
Working Gas Volume [Nm³]
Share of hydrogen in the gas versus working gas volume
Hydrogen Concentration Withdrawal
Hydrogen Concentration Injection
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Diffusion
13
• Further equilibration of hydrogen during long time shut in (no sudden chemical reactions)
• Further experiments are conducted in the follow up project
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Dispersion
14
• Break through experiments over 7 meters of porous medium
• Hydrogen is slightly faster than methane
• Effect is independent of flow speed
• Effect is canceled out in wet environment
0%
20%
40%
60%
80%
100%
120%
7500 8000 8500 9000 9500 10000 10500 11000
Shar
e [
Vo
l%]
Time [sec]
Injection of the Gas Mixture
Methan 20 Bar 80%
Wasserstoff 20 Bar 20%
0%
20%
40%
60%
80%
100%
120%
5000 5200 5400 5600 5800 6000 6200 6400 6600 6800 7000
Shar
e [
Vo
l%]
Time [sec]
Withdrawal of the Gas Mixture
Methan 20 Bar 80%
Wasserstoff 20 Bar 20%
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Dissolution
15
• Dissolution of gas mixture was observed in the lab
• Literature gives a wide range of possible values for hydrogen dissolution in brines (0,8-10 % of injected volume)
• Time dependent process (equilibration)
• Pressure dependent => can be partly recovered
• Kinetics and volume need further research (USC)
0
2
4
6
8
10
12
-55,000 45,000 145,000 245,000 345,000 445,000
Shar
e o
f H
2/C
O2
[vo
l. %
]
Working Gas Volume
Development of Gasmixture
Hydrogen Injection
CO2 Injection
Hydrogen Production
CO2 Production
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Reservoir Changes
16
• 12 months flow through experiments conducted at DBI with 25% and 75% of H2 in CH4
• Permeability changes due to clay swelling confirmed in blind samples
• No dissolution or precipitation observed on micro scale (thin sections)
• Permeability changes in the reservoir are comparable to common storage operations
0
200
400
600
800
1000
1200
1400
0
500
1,000
1,500
2,000
2,500
3,000
3,500
4,000
4,500
5,000
10.10.2006 22.02.2008 06.07.2009 18.11.2010 01.04.2012 14.08.2013 27.12.2014 10.05.2016 22.09.2017 04.02.2019
Vo
lum
e P
rod
uce
d [
Nm
³]Ta
use
nd
e
Date
Permeability Development over Reservoir Livetime
GP Net of HP3A
Permeability
Wasserpermeabilität
kw [m²]
Gaspermeabilität
kwg [m²]
Monate vor nach vor nach
2 2.77 10-14 2.86 10-14 2.43 10-13 2.31 10-13
3 5.55 10-14 3.16 10-14 2.17 10-13 2.57 10-13
6 4.07 10-14 3.75 10-14 1.60 10-13 1.45 10-13
9 3.87 10-14 2.58 10-14 1.31 10-13 1.11 10-13
12 2.59 10-14 7.19 10-14 1.95 10-13 1.06 10-13
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Conversion
17
• No H2S was measured
• Acetate traces where found in the water samples
• No evidence of iron reduction
• Confirmed in Lab and Field-experiments• Roughly stoichiometric pressure drop
• Change of initial microbial consortia towards a higher population of methanogenic archaea
• Negative isotopic value shift
0.00
0.05
0.10
0.15
0.20
0.25
0 200000 400000 600000 800000 1000000 1200000
Car
bo
n D
ioxi
de
CO
nce
ntr
atio
n [
%]
Working Gas Volume [Nm³]
Carbon Dioxide Concentration during Storagecycle
Carbon Dioxid Injection
Carbon Dioxid Withdrawl
36.5
37
37.5
38
38.5
39
39.5
40
42,300 42,400 42,500 42,600 42,700 42,800 42,900 43,000
Tem
pe
ratu
re in
[°C
]
Date
Temperature Development
Temperature Development 2014
Temperature Development 2016
Temperature ab 01.12.16
Changes in microbiology
European Workshop on Underground
Energy Storage| Markus Pichler |
2019 11 07
18
European Workshop on Underground Energy Storage| Markus Pichler | 2019 11 07
Underground Sun Storage
19
• Renewable Energy can be stored as Hydrogen in underground gas reservoirs.
• 10 % share of H2 tested
• Project confirmed scale up potential to RAGs commercial facilities
• Open: Assignability to other geological reservoir settings
• Key Parameters Identified
• 100 % Hydrogen in natural gas reservoirs is the next development objective
• https://www.underground-sun-storage.at/
Power (Strom)
European Workshop on Underground Energy Storage | Markus Pichler | 2019 11 07
• Further research on diffusion is needed (USC)
• Dissolution of hydrogen into the reservoir brine is still not fully understood (external)
• Microbial activity throughout the reservoir needs further investigation (USC)
• Models to predict chemical and biological behavior of hydrogen bearing reservoirs are still not market ready and need further development and data (open)
• Rubber seals and elastomers still need further investigation (USC)
• Movement of hydrogen in the reservoir should be tested over longer distances. (USC)
Open Questions
20
Convert a one way industry into a sustainable cycle industry
European Workshop on Underground
Energy Storage| Markus Pichler |
2019 11 07
21
In-situ Field Experiments
European Workshop on Underground
Energy Storage| Markus Pichler | 2019
11 07
22
• Construction work finished
• Commissioning finished
• Batch experiments ongoing
• First Batch finished 03/2019
• Second Batch finished 07/2019
• Injection third Batch finished 09/2019
• Second well – May /2019
• Cycle Experiments till end of 2020
Scientific Preparation
23
• Further Research on microbial conversion in the Lab• Gas mixtures with up to 40% of
hydrogen
• Simulation of biomass development in the subsurface
• Material testing of steels, cements and elastomers in CO2/H2 atmospheres under elevated pressure and temperature conditions
European Workshop on Underground
Energy Storage| Markus Pichler |
2019 11 07
Conclusion
24
• State of the art underground gas storage facilities are
essential for Europe´s security of energy supply
• Increase of erratic renewable energy generation and
the integration of natural gas and electricity markets
in turn will generate additional demand in seasonal
and high-capacity large scale storage options
• Underground Sun Storage as well as Underground
Sun Conversion technology can solve the problem of
seasonal power storage
• Generation of renewable natural gas closes a
sustainable natural carbon cycle
• Integration of renewable gas combines the benefits
from classical natural gas infrastructure and the
sociopolitical target of renewable energy supply
European Workshop on Underground
Energy Storage| Markus Pichler |
2019 11 07
Contact
T +43 (0)50 724-5346
RAG Austria AG
Schwarzenbergplatz 16
A-1015 Vienna
www.rag-austria.at
www.underground-sun-conversion.at
Reservoir Engineer Subsurface Storage Development
Markus Pichler
Project Partners:
Thank YouForYour Attention