Microbial influence on
corrosion of copper in the
repository environment
Copper corrosion seminar, 15.12.2016
Aalto University, Otaniemi
Leena Carpén, Pauliina Rajala, Elina Huttunen-Saarivirta,
Maija Raunio, Malin Bomberg
VTT Technical Research Centre of Finland Ltd
Place for a photo
(no lines around photo)
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What is microbial corrosion?
Corrosion can be defined as the degradation of a material due to a
reaction with its environment
MIC = Microbially or microbiologically induced or influenced corrosion
Microbes or their metabolic by-products induce changes in chemical or
physical conditions
Microorganisms are able to accelerate several types corrosion such as:
general corrosion
localized corrosion
pitting and stress corrosion cracking
Anode:
M Mn+ + ne-
Cathode:
O2 + 2H2O +4 e- 4OH- or
2H+ + 2e- H2
Image: Mari Raulio
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Why to study MIC?
In oxygen-free water, the corrosion rate of steel and copper is low,
unless the water is very acidic or there is microbiological activity in the
environment
The groundwater contains up to 105 microbial cells mL-1 with
considerable species diversity
Microorganisms may significantly contribute to corrosion
by producing corrosive metabolic products
by consuming oxygen
by forming discontinuous accumulations
by oxidising iron(II) ions to iron(III) ions or manganese(II) to manganese(IV)
ions or ammonia to nitrites
by accelerating the electrochemical part reactions
The aim is to characterize biofilms associated with corrosion and the
ability of indigenous groundwater microbes to produce corrosive agents
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What is biofilm?
The activity of microorganisms attached to the
surfaces and the properties of formed biofilms
are essential factors when considering the
possibility of microbially induced corrosion
In aquatic environments microorganisms attach
to surfaces and form multispecies biofilms
Microbial cells in a biofilm differ from free living
cells of the same species
Formation of extracellular polymeric substances
(EPS) = slime
Under the biofilm the conditions may differ
remarkably from the surrounding solution
”Mushroom” model of biofilm
Center for Biofilm Engineering
Image: Mari Raulio
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Microorganisms associated with MIC
• Sulphate reducing bacteria, SRB (Desulfovibrio, Desulfobacter,
Desulformaculum) and Iron reducing bacteria (Pseudomonas)
• Sulphur oxidizing-bacteria (Thiobacillus)
• Organic acid producing bacteria (Clostridium)
• Manganese- and iron-oxidizing bacteria, MFOB
(Gallionella, Sphaerotilus, Leptothrix, Crenothrix)
• Manganese depositing bacteria (Bacillus, Pseudomonas, Micrococcus)
• Slime-forming bacteria (Bacillus, Flavobacterium, Sphaerotilus)
• Methane producers
• Acid producing fungi
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MIC
Not all microbes are corrosion inducing
Some might promote passivation of the surface
Majority of microbes do not have any effect on corrosion
Biofilm formation is key step for initiation of corrosion
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Corrosion in deep bedrock
Copper
Microbial activity may have an affect on the integrity of copper
capsule
Microbial metabolites may enable the stress corrosion cracking
or cause general or localized corrosion
Challenge is to identify the key microbial processes in each
phase of the repository
Aggressive agents for copper
Acetate, (nitrate), nitrite, ammonium, sulphide and organic acids
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Corrosion in deep bedrock
Copper
Native microbes form biofilm on surfaces
Distinct corrosion products when microbes are present
copper(I) sulfide deposit vs. copper(I) oxide
Carpén et al. ICC N-0-17 2014
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Results from our studies
MICCU -project 2013-2014 Final stages of disposal: temperature that of the surrounding bedrock (10 °C), all
oxygen consumed (anoxic state)
Copper in direct contact with groundwater (chemistry stabilized with bentonite)
Simulated groundwater, abiotic control
Sulfate Reducing Bacteria (SRB) present
BASUCA -project started 2015 - Same environment as in MICCU-project
SRB and methanogens (MA) present
MICOR- project started 2015 – Early stages of disposal: higher temperature (37 °C), oxygen present (oxic state)
copper in direct contact with groundwater (Onkalo PH22) with bentonite (MX80)
ammonium oxidizers (AOB) present (+ natural microbes from PH22)
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Results from our studies
All in mg l-1 Initial (MICCU)
pH 7.78
Na 3610
Cl 5340
SO4 582
Ca 279
Mg 102
K 87.5
Br 42
HCO3 13.7
Sr 7.71
Si 6.25
B 1.38
F 0.74
Mn 0.168
C3H5NaO3 1
Cu
S2-
alkalinity mmol/l 0.184
Fe2+ mg/l <0.010
sulphide mg/l 0.271
fluoride mg/l <2.00
chloride mg/l 8350
nitrate mg/l <4.00
nitrite mg/l <4.00
sulphate mg/l <6.00
phosphate mg/l <0.040
TOC mg/l 1.52
CO2, free mg/l 5.33
(HCO3-) mg/l 11.2
CO2, total mg/l 13.4
Al mg/l <0.010
Ca mg/l 1830
Cr mg/l
<0.001
0
Cu mg/l
<0.001
0
Fe mg/l 0.0081
Mg mg/l 28.4
Mn mg/l 0.106
Ni mg/l 0.0022
Ag mg/l
<0.001
0
Na mg/l 2800
Zn mg/l
<0.002
0
Si µg/l 3270
S µg/l 4740
pH 6.91
Total N mg/l 0.87
ammonium mg/l 0.135
Initial, MICOR
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Measurements
Electrochemical measurements: Open circuit potential (OCP)
Linear polarization resistance (LPR) for general corrosion rate
Tafel plots to obtain the Beta coefficient values
Electrochemical impedance spectroscopy (EIS) to sudy surface processes
Electrical resistance (ER) probe, which measures real-time the thickness reduction
due to corrosion
EFM- (electrochemical frequency modulation) measurements
Gravimetric measurements:
mass loss determinations → average corrosion rate calculated
Visual and surface analyses
stereomicroscope, EDS/SEM, XRD
Microbiological studies quantitative PCR for determination of the amount of 16S rRNA gene copies in the
water and on the surface of copper
high throughput sequencing (HTP) to study the bacterial diversity, species
composition and their relative abundance in the biofilm and in the water
SEM
Corrosion rate, µm/ a
gravimetric LPR, max ER, max
Biotic (SRB)
4 months 6.5 13.2 45.6
10 months 1.1 3.3 14.8
Abiotic (sterile)
4 months 2.1 2.3 13.2
10 months 2.2 3.9 9.6
Biotic (SRB + MA)
4 months 0.2
12 months 1.2
Abiotic (sterile)
4 months 1.1
12 months 0.95
Biotic (AOB)
3 months 16.8-17.4
Abiotic
3 months 13.8
SRB, 4 months
mostly
alphaproteobacteria in
biofilm
SRB, 10 months,
mostly deltaproteobacteria
and clostridia
SRB+MA, 4 months
EDS: Cu, C, O, S
XRD: Cu, Cu2S, Cu2O, CuO
Abiotic, 4 months
EDS: Cu, O, C XRD: Cu, Cu2O, CuO
A&B:SRB+MA, 12
months,
EDS: Cu, C, O, S
XRD: only Cu
C&D: Abiotic
EDS: Cu, O, C
and locally Cl
XRD: Cu, Cu2O
AOB+ natural groundwater+bentonite
mainly Cu2O and CaCO3
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Preliminary conclusions
Our experimental setup seems to work well
In biotic environments the microbes had attached to the copper surface and formed
biofilm
In biotic anoxic environments the average corrosion rate (measured with weight loss) is
either clearly higher (6.5 µm/a) or at the same level (1-2 µm/a) than in abiotic
environment depending on the properties of formed surface films (Cu2S and biofilms)
It seems that enrichment of SRB might be more aggressive towards copper than
enrichment of SRB and methanogens together
Microbes in Olkiluoto groundwater are able to produce several components inducing a
risk for stress corrosion cracking (SCC)
In oxic environment the corrosion rates were higher (14-18 µm/a) than in anoxic and they
were at the same level regardless of the environment (biotic/abiotic)
According to the EIS measurements also the surface properties resembled each other
At least during short exposure time (3 months) the presence of oxygen was more
decisive for corrosion than the activity of microbes
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Conlusions cont.
These results show that the prediction of microbiological activity
and its effects to corrosion is challenging.
Thus more research, especially long exposure studies are
needed to be able to evaluate the possible influence of MIC to the
long-term safety of nuclear waste disposal concept
Articles
E. Huttunen-Saarivirta, P. Rajala, M. Bomberg, L. Carpén. 2016. Corrosion of copper in oxygen-deficient
groundwater with and without deep bedrock micro-organisms: characterisation of microbial communities and
surface processes. Submitted to Applied Surface Science.
E. Huttunen-Saarivirta, P. Rajala, L. Carpén. Corrosion behaviour of copper under biotic and abiotic
conditions in anoxic ground water: electrochemical study. Electrochimica Acta, 203:350-365.
L.Carpén, P. Rajala, M. Bomberg. 2015. Microbially Induced Corrosion in Deep Bedrock. Advanced
Materials Research Vol. 1130 (2015) pp 75-78.
P.Kinnunen, M. Bomberg, P. Rajala, L. Carpén. Industrial Views to Microbe-Metal Interactions in Sub-Arctic
Conditions. 2015. Advanced Materials Research Vol. 1130 (2015) pp 114-117.
Kutvonen, P. Rajala, L. Carpén, M. Bomberg. 2015. Nitrate and ammonia as nitrogen sources for deep
subsurface microorganisms. Frontiers in Microbiology, Vol. 6, 1079.
• E. Huttunen-Saarivirta, P. Rajala, M. Bomberg, L. Carpén, EIS study on aerobic corrosion of copper in
ground water: influence of micro-organisms. Submitted to Electrochimica Acta
Conferences and workreports:
L.Carpén, P. Rajala, M. Bomberg, M. Raunio, E. Huttunen-Saarivirta. BASUCA- Vuosiraportti 2015. VTT-R-
00867-16
L.Carpén, P. Rajala, M. Bomberg. 2016. Microbially induced corrosion of copper in simulated anoxic
groundwater. Abstract and presentation at Eurocorr 2016, 11 - 15 September 2016, Montpellier, France.
L.Carpén, P. Rajala, M. Bomberg. 2015. Microbially Induced Corrosion in Deep Bedrock. Presentation in
IBS 2015 (International Biohydrometallurgy Symposium), Sanur, Bali 5-9.10.2015.
E. Huttunen-Saarivirta, P.Rajala, L. Carpén. Corrosion behaviour of copper under biotic and abiotic
conditions in anoxic ground water: electrochemical study EMCR 2015 Tróia, 24-29 May 2015.
P. Rajala, L. Carpén, E. Huttunen-Saarivirta, I. Tsitko, M. Bomberg. Vuosiraportti 2015. VTT-R-00882-16.