Biological hydrogen formation by thermophilic bacteria
Abraham A.M. Bielen
Thesis committee
Promotors Prof. Dr J. van der Oost Personal chair at the Laboratory of Microbiology Wageningen University
Prof. Dr W.M. de Vos Professor of Microbiology Wageningen University
Co‐promotor Dr S.W.M. Kengen Assistant professor, Laboratory of Microbiology Wageningen University
Other members Prof. Dr G. Eggink, Wageningen University Prof. Dr W.R. Hagen, Delft University of Technology Dr T.J.G. Ettema, Uppsala University, Sweden Dr R. van Kranenburg, Corbion, Gorinchem
This research was conducted under the auspices of the Graduate School SENSE (Netherlands Research School for the Socio‐Economic and Natural Sciences of the Environment)
Biological hydrogen formation by thermophilic bacteria
Abraham A.M. Bielen
Thesis submitted in fulfilment of the requirements for the degree of doctor at Wageningen University by the authority of the Rector Magnificus Prof. Dr M.J. Kropff, in the presence of the Thesis Committee appointed by the Academic Board to be defended in public on Tuesday 10 June 2014 at 4 p.m. in the Aula.
Abraham A.M. Bielen Biological hydrogen formation by thermophilic bacteria 234 pages.
PhD thesis, Wageningen University, Wageningen, NL (2014) With references, with summaries in Dutch and English
ISBN 978‐94‐6173‐936‐0
Table of Contents
Chapter 1 General introduction and thesis outline 009
Chapter 2 Glycerol fermentation to hydrogen by Thermotoga maritima: proposed pathway and bioenergetic considerations 031
Chapter 3 A thermophile under pressure: Transcriptional analysis of the
response of Caldicellulosiruptor saccharolyticus to different H2 partial pressures 054
Chapter 4 Biohydrogen production by the thermophilic bacterium Caldicellulosiruptor saccharolyticus: Current status and perspectives 081
Chapter 5 Pyrophosphate as a central energy carrier in the hydrogen producing extremely thermophilic Caldicellulosiruptor saccharolyticus 115
Chapter 6 The involvement of pyrophosphate in glycolysis and gluconeogenesis: Remarkable singularities or wide spread phenomena? 129
Chapter 7 Thesis summary and general discussion 179
Appendices References 208 Dutch summary ‐ Nederlandse samenvatting 222 Acknowledgements ‐ Dankwoord 226 About the author 229 List of publications 230 Overview of completed training activities 232
Chapter 1
General introduction and thesis outline
Chapter 1
Abstract
A growing awareness of the negative aspects associated with traditional production processes for fuels and chemicals has resulted in an increase in research on the development of alternative more sustainable processes. This includes the production processes for hydrogen gas (H2) a very important industrial commodity with indispensable roles in many processes. Moreover, H2 could be used as an energy storage/transportation medium and is directly applicable as a fuel. In a biological H2
(bioH2) production process, known as dark fermentation, fermentative microorganisms are able to generate H2 from renewable resources like carbohydrate‐ rich plant material or industrial waste streams. Especially thermophilic microorganisms possess several desirable traits making them attractive candidates to implement in a bioH2 production process. The thermophilic bacteria Caldicellulosiruptor saccharolyticus and Thermotoga maritima have the hydrolytic capacity to decompose complex biomass in readily fermentable di‐ or mono saccharides, moreover, their catabolic pathways lead only to a limited number of possible fermentation end‐products. Under ideal conditions these thermophiles are able to ferment sugar substrates to H2 with yields close to the theoretical maximum of
4 H2/hexose. The investigation of the underlying mechanisms of the H2 generating processes including i) the routes of carbohydrate metabolism, ii) reductant recycling and iii) the effect of cultivation conditions on performance, allows us to achieve a better understanding of the limiting factors of current bioH2 production processes, and thereby bringing the large‐scale industrial application of dark fermentation a step closer.
10 General introduction
1. Hydrogen gas : Why do we need it and how can it be made?
th Since its discovery in the 18 century [1], molecular hydrogen (H2) has become an important chemical commodity. With an estimated annual worldwide production exceeding 50 million tons, H2 finds its application in numerous industrial processes.
Particularly, H2 is used as a bulk chemical in the glass, food, electronics and metal‐ processing industries, in petroleum refining processes and during the synthesis of basic chemicals like methanol and ammonia [2, 3]. H2 can also be used as a fuel e.g. for commercial transport or space‐flight. The energy associated with the oxidative conversion of H2 to water (H2O) (Eq. 1.1) generates heat in a combustion engine or electrical current in H2‐fuelled fuel cells, where the latter process is considered to be more efficient. Moreover, H2 can be implemented as an energy storage and transportation medium, and for this reason it has been proposed as the central chemical energy carrier in a future hydrogen energy economy [3].
(Eq. 1.1) 2 H g O g ⟶2 H O l ° ‐474 kJ/reaction (∆ )[4]
In nature, molecular hydrogen is scarce, atmospheric H2 concentrations are low
(0.000055%) and, contrary to natural gas (methane, CH4), there are no natural accumulation sites of H2 gas. Hydrogen is commonly bound in other compounds like water, hydrocarbons (CnHm) or carbohydrates (Cn(H2O)m). To free hydrogen from these compounds several methods are available [5], including i) electrolytic [6], ii) photoelectrochemical [7], iii) thermal [8], and (iv) biological processes [9‐11] (Figure
1.1). H2 formation via electrolytic processes (electrolysis) requires an energy conversion from a primary energy carrier to electricity, which provides the current that drives the decomposition of water into O2 and H2, i.e. the reverse reaction of the reaction displayed in Eq. 1.1 [6]. During photoelectrochemical processes solar energy (photons) directly assists in generating a current that drives the electrolysis of water [7]. Thermochemical methods which employ nuclear or solar energy use generated heat to drive the thermolysis of water [8], whereas thermal processes like steam reforming (Eq. 1.2), hydrocarbon partial oxidation (Eq. 1.3), hydrocarbon decomposition (Eq. 1.4) and coal gasification (Eq. 1.5) require fossil fuels and water as starting material alongside an input of heat to drive these reactions [8]. Hydrogen formation via reaction 2, 3, and 5 generates a gas mixture containing CO and H2, also known as syngas. By coupling syngas production with a water‐gas shift reaction (Eq.
1.6), the overall H2 yield of these processes is further enhanced. The use of fossil
(hydro)carbons as a source for H2 production is inevitably coupled with the emission the greenhouse gas carbon dioxide (CO2). Gasification of renewable biomass‐derived carbohydrates (Eq. 1.7) is also coupled to CO2 emission, however, the carbon
11 Chapter 1
retention time in renewable biomass is much smaller than in fossil carbon compounds. Because the CO2 fixed from the atmosphere during biomass formation is released on a relative short timescale (generally less than several years) compared to geological time scales for fossil fuels, the use of renewable biomass will not lead to a net increase in atmospheric CO2 concentrations. Biological processes implement biological systems, i.e. microorganisms like algae or bacteria, for H2 production. These microorganisms generate H2 from water or biomass‐derived carbon compounds, using either solar energy, electricity and/or biomass as an energy source [9‐12].
(Eq. 1.2) C H n H O⇆n CO m 2n / H
n m (Eq. 1.3) C H 2 O ⟶n CO 2 H
1 (Eq. 1.4) C H ⟶n C 2 m H
(Eq. 1.5) C H O⇆CO H
(Eq. 1.6) CO H O⇆CO H
(Eq. 1.7) C H O p O q H O⇢x CO y CO z H
In all described H2 production processes an input of energy is required to release hydrogen from the basic starting materials. This energy is either provided directly by a primary energy carrier or indirectly via electricity. In this perspective H2 can also be considered a secondary energy carrier (Figure 1.1). Based on the negative effects associated with the use of nuclear and fossil resources, like their impact on the environment (e.g. radioactive waste, greenhouse gas emissions), related geopolitical issues and the non‐renewable nature of these resources, the production of H2 via their related processes are presumed to be non‐sustainable. An entire H2 production process is only considered sustainable when both the energy sources and the basic starting materials for H2 formation are renewable. Hence H2 is only considered a sustainable commodity when it is generated using renewable resources like solar‐, wind‐, water‐ and geothermal‐energy or biomass. Currently 94% of the global H2 production is based on fossil fuel [8]. To be able to increase the share of H2 production processes based on renewable resources, many challenges have to be overcome and technological advances have to be made.
12 General introduction
Figure 1.1 Overview of the conversion processes involved in the formation of molecular hydrogen (H2) form renewable (dark green boxes) and non‐renewable (light green boxes) primary energy carriers. The interconversion between the secondary energy carriers electricity and H2 is achievable via electrolytic processes (electrolysis) and H2 fuelled fuel cells.
2. Biological hydrogen production: What are the alternatives?
Biological H2 formation processes can be classified into four major categories: (i) bio‐ photolytic, (ii) photo‐fermentative, (iii) bio‐electrochemical, and (iv) fermentative processes [9‐12]. The formation of H2 by such biological systems revolves around a seemingly simple reaction: two protons (H+) and two electrons (e‐) brought together form H2 (Eq. 1.8). Except for bio‐electrochemical H2 formation processes this reaction is catalysed by specific enzymes. The electrons involved in the catalysed reactions are generally associated to electron carriers, like NAD+ or ferredoxin, which are able to accept electrons from a donor and transfer them to the hydrogen generating enzymes (e.g. hydrogenases or nitrogenases). Bio‐photolytic microorganisms like algae or cyanobacteria capture incoming solar + ‐ energy, leading to the decomposition of water into O2, protons (H ) and electrons (e ) (Eq. 1.9). These electrons, which are shuttled via the electron transport chain producing energy required for growth, are finally used by hydrogenases (Eq. 1.8) or by nitrogenases (Eq. 1.10). In nitrogenase catalysed reactions H2 is actually formed as a side‐product of the energy consuming N2 fixation reaction. In photo‐fermentative
13 Chapter 1
organisms, like purple non‐sulfur bacteria, the electrons required for H2 formation during N2 fixation (Eq. 1.10) are provided via the metabolism of biomass‐derived organic acids (e.g. acetate), while the additional energy for growth is obtained via their light‐driven proton pumps. In electrochemically assisted microbial H2 production, the free electrons generated during the metabolism of organic matter are transferred to the anode electrode. Under non‐augmented conditions the generated potential is too low to drive the H2 formation reaction (Eq. 1.8); however, by supplementing the generated potential with an external power source, H2 formation becomes possible. Fermentative hydrogen production, often referred to as dark fermentation, to distinguish it from the light driven photo‐fermentation, involves the metabolism of biomass‐derived carbohydrates (e.g. sugars like glucose) to organic acids. Electrons generated throughout metabolism are transferred to hydrogenases, subsequently leading to H2 formation.