9: Biohydrogen - An Introduction
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Evaluate Hydrogen as an Energy Carrier:
- Compare the energy content and combustion properties of hydrogen with other fuels, emphasizing its high heat of combustion and clean byproducts (water).
-
Understand the "Color" Coding of Hydrogen:
- Describe the various production methods for hydrogen (e.g., green, blue, grey, black, pink, turquoise, yellow, white) and their implications for environmental impact and sustainability.
-
Differentiate Hydrogen Production Methods:
- Explain the three main categories of hydrogen production—biological, thermochemical, and electrochemical—and how each method utilizes different feedstocks and reaction conditions.
-
Explore Biological Production of Biohydrogen:
- Analyze the photobiological pathways (direct and indirect photolysis) in microalgae that lead to hydrogen production, including the roles of hydrogenases, photosystem II, and fermentation processes.
- Discuss the role of dark fermentation and how organic substrates are converted into hydrogen by microbes.
-
Examine Electrochemical Approaches to Hydrogen Production:
- Describe the principles behind photoelectrochemical and electrolytic hydrogen production, including the function of microbial electrolytic cells and the role of semiconductor electrodes.
-
Investigate Thermochemical Production from Biomass:
- Understand the process of biomass gasification to produce syngas (H₂ and CO) and how thermochemical methods, including aqueous phase reforming, can yield hydrogen.
-
Analyze the Redox Chemistry and Catalytic Reactions Involving H₂:
- Explain the oxidation of hydrogen in fuel cells and its role as a source of electrons for reduction reactions.
- Discuss how hydrogen’s reaction with hydroxyl radicals affects atmospheric methane levels and the overall greenhouse gas balance.
-
Critically Assess Environmental Implications:
- Evaluate the potential benefits of biohydrogen production for reducing greenhouse gas emissions compared to fossil fuel-based hydrogen production.
- Identify the challenges related to hydrogen leakage and its indirect impact on atmospheric chemistry and climate.
-
Integrate Biochemical and Electrochemical Perspectives:
- Relate enzymatic and microbial processes (e.g., those catalyzed by hydrogenases) to the large-scale electrochemical production of hydrogen, bridging fundamental biochemistry with applied energy technologies.
-
Discuss Future Directions and Technological Challenges:
- Explore the current limitations in hydrogen storage and transport, and discuss emerging strategies to produce, capture, and utilize biohydrogen in a sustainable and economically viable manner.
These learning goals aim to provide junior and senior biochemistry majors with a comprehensive understanding of hydrogen's potential as a clean fuel, the diverse methods of its production—especially through biological and electrochemical pathways—and the broader environmental and technological context of its use.
Hydrogen as a fuel
Hydrogen gas would be ideal if it could be produced at scale, easily transported and stored, or produced at local sites on demand. The reaction for the "burning" of hydrogen shows that the only greenhouse gas emitted is H2O.
\begin{equation}
2 \mathrm{H}_2(\mathrm{~g})+\mathrm{O}_2(\mathrm{~g}) \rightarrow 2 \mathrm{H}_2 \mathrm{O}(\mathrm{g})
\end{equation}
H2O comes and goes in our atmosphere in short timescales and does not continually build up, as does CO2 from burning fossil fuels. The standard heat of combustion (in kJ/g or kcal/kg) for H2 is far higher than any other fuel, as shown in Table \(\PageIndex{1}\) below, making it an ideal fuel.
Name |
Formula |
State |
-ΔHc° |
-ΔHc° |
-ΔHc° |
Ammonia |
NH3 |
gas |
383 |
22.48 |
5369 |
Butane |
C4H10 |
gas |
2878 |
49.50 |
11823 |
Carbon (graphite) |
C |
cry |
394 |
32.81 |
7836 |
Ethanol |
C2H6O |
liq |
1367 |
29.67 |
7086 |
Hydrogen |
H2 |
gas |
286 |
141.58 |
33817 |
Methane | CH4 | gas | 891 | 55.51 | 13259 |
methyl stearate (biodiesel) |
(CH3(CH2)16(CO)CH3 | liq | 1764 | 40 | 9560 |
Naphthalene |
C10H8 |
cry |
5157 |
40.23 |
9609 |
Octane |
C8H18 |
liq |
5470 |
47.87 |
11434 |
Propane |
C3H8 |
gas |
2220 |
50.33 |
12021 |
wood (red oak) | - | solid | - | 14.8 | 3540 |
coal (lignite) | - | solid | - | 15 | 3590 |
coal (anthracite) | - | solid | 27 | 4060 |
Table \(\PageIndex{1}\): Energy values for various fuels. Data source: https://www.engineeringtoolbox.com/s...nt-d_1987.html
We won't discuss large-scale H2 storage or transport, which are two fundamental engineering problems. Instead, we will focus on the production of "biohydrogen." Of course, the prefix "bio" can mean many things, including the production of H2 in syngas using cellulose as a feedstock, the electrolysis of water powered by solar/wind energy, and its production by hydrogenases, enzymes found in some microbes.
The fuel industry uses different colors as descriptors of hydrogen based on how it is produced. They are shown in Table \(\PageIndex{2}\).
Color | Method of production |
Green | electrolysis of H2O using solar/wind to generate electricity (expensive at present) |
Blue | steam reforming of natural gas (CH4) with the other product, CO2 captured and stored (CCS) |
Grey | steam reforming of natural gas (CH4) without CO2 capture and storage |
Black (coal/oil) |
gasification to form syngas |
Pink (purple/red) | electrolysis powered by nuclear energy, which does not emit CO2; heat emitted produces steam for blue/gray H2 production |
Turquoise | methane pyrolysis (heat in the absence of O2) to form H2 and C |
Yellow | electrolysis using solar power without conversion to electricity as the power source. |
White | underground H2 released through fracking |
Table \(\PageIndex{2}\): Different "colors" of hydrogen based on production methods
Of course, H2 in syngas can be produced from biomass, as described in Chapter 32.8, but it is unclear if a hydrogen color has been assigned to it.
At present, the important feedstocks for H2 production worldwide are natural gas (48%), oil (30%), coal (18%), and electrolysis (4%)—mostly fossil fuels.
Methods of Production
H2 production is also classified based on the chemical processes used to produce it. These processes include
- Biological (use of live bacteria and algae cells)
- Thermochemical: (gas and liquid fuel reforming, coal and biomass gasification),
- Electrochemical (electrolytic): (photothermal, photoelectrolytic, and photobiological)
We will organize this chapter section using these three processes. We will start with Biological (1), followed by Electrochemical/Electrolytic (3), and end with Thermochemical (2). They are summarized in Figure \(\PageIndex{1}\).
Figure \(\PageIndex{1}\): The main pathways for H2 production based on biomass. M.G. Eloffy et al., Chemical Engineering Journal Advances, 12 (2022). https://doi.org/10.1016/j.ceja.2022.100410. Creative Commons license
Biomass can be used as the feedstock for all these methods, and the resulting product can be called biohydrogen. Of course, as discussed in the previous chapter, nonbiological sources of feedstock are also the predominant ones used in thermochemical and electrochemical methods.
2H+ ↔ H2: An Overview
We will discuss the production of H2 as an energy source for society. For industry use, it can be used in fuel cells to power spacecraft and cars, as shown in the reaction below.
\begin{equation}
\begin{aligned}
& \mathrm{O}_2+4 \mathrm{H}^{+}+4 \mathrm{e}^{-} \longrightarrow 2 \mathrm{H}_2 \mathrm{O} \\
& \mathrm{H}_2 \longrightarrow 4 \mathrm{H}^{+}+4 \mathrm{e}^{-}
\end{aligned}
\end{equation}
In the next section, we will discuss the hydrogenases that produce and use H2 in microbes, so this chapter will treat them very generally. However, we need to review the topic.
Use of H2 as a source of electrons for reduction reactions.
Each hydrogen in H2 has an oxidation number of 0. Each can be oxidized to H+ (oxidation number +1) with the 2 electrons passed on to a substrate/cofactor or a sequential series of substrates with higher and higher standard reduction potentials (better oxidizing agents), forming reduced products.
H2 + (substrate)OX → 2H+ + (product)RED
This general reaction is analogous to the mitochondrial electron transport chain, in which electrons are passed from a source (NADH) to oxidized forms of acceptors. The general reaction below shows each redox pair in the electron transport chain.
NADH/NAD+ → FAD/FADH2 → UQ/UQH2 → Cyto COX/Cyto CRED → O2/H2O
Some organisms have evolved to produce energy by oxidizing H2. This reaction is analogous to how photosynthetic organisms obtain energy through water oxidation. In photosystem II, the oxygen-evolving complex oxidizes oxygen in H2O (oxidation number -2) to O2 (oxidation number—0). Some redox pairs, starting with H2O/O2, are shown below for photosystem II.
H2O/O2 → P680/P680* → (Plastoquione)OX/(Plastoquione)RED
The first reaction is endergonic and requires photons as an energy source photons.
Use of H+ as a sink for electrons for oxidation reactions that produce H2.
H+ has an oxidation number of +1. Hence, it can be reduced to H2 (oxidation number of 0) as it gains electrons from substrates/cofactors, which get oxidized. This general reaction is shown below.
2H+ + (substrate/cofactor)RED → H2 + (substrate/cofactor)OX
Many microorganisms can produce H2 through variants of photosynthesis or fermentation, both of which provide the two electrons needed. E. Coi has four hydrogenases (Hyd 1, 2, 3, and 4). It forms H2 through two reactions catalyzed by:
- formate (HCO2-) dehydrogenase (FDH): 2HCO2- ⇌ 2CO2 + 2H+ + 2e-
- hydrogenase (H2ase): 2H+ + 2e- → H2
The C in formate has an oxidation number of +2 and is oxidized to CO2, in which the C has an oxidation number of +4.
H2 is not a greenhouse gas as it doesn't have any bond vibrations that produce transient dipoles and, hence, does not absorb in the infrared region of the spectrum. Yet it can affect atmospheric methane levels, a potent greenhouse gas, and ozone, leading to warming. It's not emission from the combustion of H2 but rather the leakage into the atmosphere of transported and stored H2 gas that is problematic.
Most of the H2 that enters the atmosphere diffuses into the soil and is taken up by bacteria. The rest reacts with hydroxy radicals (.OH) in the atmosphere, as shown in the reaction below.
H2 + .OH → H2O + H. (atomic hydrogen)
The reaction of .OH with H2 decreases the hydroxy radical's availability to react with the very potent greenhouse gas methane, CH4. That reaction is shown below.
CH4 + .OH → .CH3 + H2O
The methyl radical .CH3 reacts rapidly with oxygen to form the methylperoxy radical (CH3O2.). This eventually forms formaldehyde, a water-soluble molecule that is removed from the atmosphere on precipitation. Hence, the reaction of H2 with .OH increases the half-live of CH4 in the atmosphere.
.OH is a key molecule in the troposphere and is considered a methane "sink" that leads to the drawdown of methane. We discussed the extreme reactivity of .OH in Chapter sections 12.3 and 12.4. It's so reactive that its half-life is in the order of seconds. It is also at very low concentrations of less than 1 part per trillion.
.OH is produced from ozone, O3, by the following reactions:
O3 + hν (UV) → O2 + .O
.O + H2O → 2 .OH
The first reaction is photolysis and experiments during a solar eclipse have shown that the production of atmospheric .OH stops!
Dr. Paul Crutzen, Nobel Prize winner in Chemistry, described .OH as the "detergent of the atmosphere" since it can react with and oxidize many deleterious trace gases in the troposphere, making them more water-soluble and removing them from the atmosphere. A main reaction of .OH is carbon monoxide (CO). It also reacts with volatile organic compounds (VOCs) and NOx (NO + NO2), which are precursors of tropospheric ozone, a health hazard. Even though dioxygen, which comprises 20% of the atmosphere, is also an excellent oxidizing agent, it is kinetically slow to react.
Very few gases are not oxidized by .OH. The refrigerant gases chlorofluorocarbons are and would enter the stratosphere if they didn't react with .OH. In the stratosphere, they react with stratospheric ozone and reduce its protective effect against dangerous UV light. It does react with hydrochlorofluorocarbons (HCFCs).
Figure \(\PageIndex{2}\) below summarizes the adverse climatic effects of the oxidation of H2 in the atmosphere.
Figure \(\PageIndex{2}\): Effects of hydrogen oxidation on atmospheric greenhouse gas concentrations and warming. I. Ocko and Steven P. HamburgAtmos. Chem. Phys., 22, 9349–9368, 2022. https://doi.org/10.5194/acp-22-9349-2022. Creative Commons Attribution 4.0 License.
The central panel notes that H. (atomic hydrogen) can start a free radical change reaction to produce tropospheric ozone, O3. This pollutant is a greenhouse gas and causes serious health consequences.
The message is this: Care must be taken to minimize methane and H2 leakage during production and use as fuels.
Biohydrogen from Microalgae
We will focus most of our attention on the Biological (1) and Electrolytic (3) processes for producing biohydrogen from microalgae. The Biological processes (1) require hydrogenases for H2 production within cells. The Electrolytic (3) processes use microalgae as a feedstock to provide substrates that other microbes can ferment. These can be combined to increase production. Figure \(\PageIndex{3}\) below summarizes the Biological (1) and Electrolytic (3) metabolic processes that can be used for microalgae H2 production.
Figure \(\PageIndex{3}\): Metabolic pathways of biohydrogen production by micro-algal biomass. modified from Ahmed SF et al. Front. Energy Res. 9:753878. doi: 10.3389/fenrg.2021.753878. Creative Commons Attribution License (CC BY).
These are mainly classified into three categories: i) the photobiological process through which biohydrogen is produced via direct and indirect photolysis in the microalgae, ii) fermentation, and iii) the electrochemical process that comprises photoelectrochemical and electrolytic.
BIOLOGICAL (1) - Biophotolysis (photosynthesis)
This consists of two processes: Direct and Indirect Photolysis (photosynthesis). Both use light to drive the ultimate reduction of 2H+ to H2 using hydrogenase or nitrogenase. We will explore the details in the next chapter section. The biophotolysis process is divided into indirect (using electrons from substrates) and direct (using electrons from water). These processes are simplified in Figure \(\PageIndex{4}\).
Figure \(\PageIndex{4}\): Schematic diagram for biological (biophotolysis) process. M.G. Eloffy et al.
Direct Biophotolysis (photosynthesis)
In direct biophotolysis (photosynthesis), water molecules are oxidized in Photosystem II, which contains the Oxygen Evolving Complex (OEC). This endergonic process is driven by light. The electrons lost from water are passed through Cytochrome b6f and Photosystem I to ferredoxin, then NADP+, which gets reduced to NADPH (as discussed in Chapter 20). These reactions are illustrated in Figure \(\PageIndex{5}\).
Figure \(\PageIndex{5}\): Light reaction of photosynthesis and associated standard reduction potentials
In direct photolysis, electrons are passed directly from reduced ferredoxin to 2H+ in a reaction catalyzed by a hydrogenase, as shown in Figure \(\PageIndex{6}\) below.
Figure \(\PageIndex{6}\): Metabolic hydrogen production pathways used by Chlamydomonas reinhartii.FDX: ferredoxin; H2ase: hydrogenase; NPQR: NADPH−plastoquinone oxidoreductase; PFR: pyruvate:ferredoxin oxidoreductase; PSI: photosystem I; PSII: photosystem II. Touloupakis, E.; Faraloni, C.; Silva Benavides, A.M.; Torzillo, G. Recent Achievements in Microalgal Photobiological Hydrogen Production. Energies 2021, 14, 7170. https://doi.org/10.3390/en14217170. Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
The overall reaction is simplified in the equation below.
\begin{equation}
2 \mathrm{H}_2 \mathrm{O}+\text { Light } \rightarrow 2 \mathrm{H}_2+\mathrm{O}_2
\end{equation}
One problem with direct photolysis is that O2 can damage hydrogenases. Again, we will discuss the biochemistry of hydrogenases in great detail in the next chapter section.
Indirect Biophotolysis
This process bypasses the damaging effects of O2 on hydrogenase by being carried out in the absence of O2 using fermentation to provide electrons for the hydrogenase reduction of 2H+ to H2. Photosynthesis is required to make the carbohydrates necessary for fermentation. Glucose can then be oxidized anaerobically (in the dark to avoid O2 formation from photosynthesis) to form pyruvate through the glycolytic pathway. Pyruvate can then be oxidatively decarboxylated through the pyruvate:ferredoxin oxioreductase (PFR) as ferredoxin gets reduced. It then passes its electrons on through hydrogenase to produce H2. The pathway is illustrated in the top/right parts of the above figure and the reaction diagram in Figure \(\PageIndex{7}\) below.
Figure \(\PageIndex{7}\): Model of fermentative pathways involved in dark anaerobic H2 production in C. reinhardtii. Proteins are shown as ovals. Photosynthetic ferredoxin (PETF). Jens Noth et al., Journal of Biological Chemistry, 288 (2013). https://doi.org/10.1074/jbc.M112.429985. Creative Commons license.
Glucose and some amino acids can be converted into pyruvate, a substrate for PFR1 in the single-cell algae C. reinhardtii. PFR1 converts pyruvate to acetyl-CoA and CO2 with the electrons that reduce ferredoxin. The reduced FDX2 passes electrons through hydrogenase (HYDA1) to form H2.
Another enzyme used to continue fermentation, pyruvate:formate lyase (PFL1), converts pyruvate to formate and acetyl-CoA, which can be metabolized further to acetate and ethanol. A shift to pyruvate oxidation to PFR1 occurs if PFL1 is mutated or in long-term anoxic conditions.
The key enzyme, pyruvate:ferredoxin oxioreductase(PFR), uses thiamine pyrophosphate (TPP) as a cofactor for the oxidative decarboxylation of the α-keto acid pyruvate, as expected. Figure \(\PageIndex{8}\) shows an interactive iCn3D modelof the pyruvate ferredoxin oxidoreductase (PFOR) from Desulfocurvibacter africanus in anaerobic conditions (7PLM).
Figure \(\PageIndex{8}\): Pyruvate ferredoxin oxidoreductase (PFOR) from Desulfocurvibacter africanus in anaerobic conditions (7PLM). (Copyright; author via source). Click the image for a popup or use this external link: https://structure.ncbi.nlm.nih.gov/i...XRFMoVhaoRbW86
PFOR, abbreviated here, is a 267 kDa homodimer containing three [Fe4S4] clusters (spacefill) per monomer. Only one monomer is shown, and TPP is shown in sticks.
Again, indirect photolysis occurs in the absence of O2. Light illumination leads to only transient H2 synthesis. If sulfur is limited in the growth media of the algae, more sustained H2 production occurs, as the lack of sulfur reduces PSII activity. Hence, H2 production can be maximized by depleting sulfur and minimizing O2, even in the presence of light. In the absence of O2, hydrogenase gene expression increases. Nutrient depletion also produces formate and acetyl-CoA through the enzyme pyruvate:formate lyase (PFL1). This is predominant in Chlamydomonas cells in the dark.
The green microalgae C. reinhardtii makes most of its H2 (approximately 90%) using direct photolysis. Commercially, the production of H2 in indirect photolysis is carried out in a separate sealed bioreactor to avoid O2. Indirect photolysis is shown in the above figures.
The reactions to this process are as follows :
\begin{equation}
\begin{gathered}
12 \mathrm{H}_2 \mathrm{O}+6 \mathrm{CO}_2+\text { hν } \rightarrow \mathrm{C}_6 \mathrm{H}_{12} \mathrm{O}_6+6 \mathrm{O}_2 \\
\mathrm{C}_6 \mathrm{H}_{12} \mathrm{O}_6+12 \mathrm{H}_2 \mathrm{O}+\text { hν } \rightarrow 12 \mathrm{H}_2+6 \mathrm{CO}_2
\end{gathered}
\end{equation}
BIOLOGICAL (1) - Fermentation
We have just discussed fermentation processes within living microalgae cells. Now, let's consider fermentation processes using nonliving biomass feedstocks supplied to microbes to produce H2. This offers a significant way to make biohydrogen. A schematic diagram for Biological (1) fermentation is shown below in Figure \(\PageIndex{9}\):
Figure \(\PageIndex{9}\): Schematic diagram for biological (fermentation) process. M.G. Eloffy et al.
Fermentation involves the decomposition of organic biomass to produce CO2 and H2. The fermentation process can be separated into photofermentation (light fermentation) and dark fermentation.
Photofermentation
Some photosynthetic bacteria and microalgae use Photofermentation to produce H2 from organic acids like acetic, butyric, lactic, and succinic acids. Oxidation of the acids produces CO2, along with H+s and e- for H2 production. Electrons are transferred through photosystem I and eventually, believe it or not, nitrogenase. It is a fermentation process as the process is anoxic.
Some photosynthetic bacteria, like the purple nonsulfur bacteria, a facultative anoxygenic phototroph, and some microalgae, can produce H2 using a simplified system that has only one photosystem and uses the enzyme nitrogenase to produce H2. The photosystem can not generate an oxidizing agent strong enough to oxidize H2O, but under anaerobic conditions, they can oxidize organic acids and even H2S to provide electrons from H2 production. These reactions are shown below in Figure \(\PageIndex{10}\).
Figure \(\PageIndex{10}\): Photofermentative hydrogen production in PNSB.
Deo, D., Ozgur, E., Eroglu, I., Gunduz, U., & Yucel, M. (2012). Photofermentative Hydrogen Production in Outdoor Conditions. Hydrogen Energy - Challenges and Perspectives. doi: 10.5772/50390. Creative Commons Attribution 3.0 License,
We studied nitrogenase in Chapter x.xx. The net reaction for the fixation of nitrogen is shown below.
\begin{equation}
\mathrm{N}_2+8 \mathrm{H}^{+}+8 \mathrm{e}^{-}+16 \mathrm{ATP} \rightarrow 2 \mathrm{NH}_3+\mathrm{H}_2+16 \mathrm{ADP}+16 \mathrm{Pi}
\end{equation}
In this reaction, N2 is reduced as the N atoms go from a 0 oxidation state to +3 in NH3. The needed electrons are made from organic acids and fed into the system and eventually go to ferredoxin, which transfers them to protons. The ratio of N2 to H2 produced is 1:1, at the expense of 16ATPs per H2 produced.
The ATP produced by the collapse of the produced proton gradient through FoF1ATPase powers the reaction.
In the absence of N2, the net reaction becomes
\begin{equation}
2 \mathrm{H}^{+}+2 \mathrm{e}^{-}+4 \mathrm{ATP} \rightarrow \mathrm{H}_2+4 \mathrm{ADP}+4 \mathrm{Pi}
\end{equation}
The electrons are still fed into nitrogenase, but in the absence of the substrate N2, they are used to reduce 2H+ to H2. Note that only 4 ATPs are required per each H2 produced, a significant energy gain.
ATP produced during photosynthesis would be used for anabolic biosynthesis contributing to biomass, so extra ATP is needed to support H2 synthesis past that needed for growth. As anabolism is a reductive process (compared to oxidative catabolism), adequate sources of electrons for reduction are required. Multiple pathways need electrons, including CO2 fixation, N2 fixation (with associated H2 production, and organic acids like polyhydroxbutyrate. The bacteria use photosynthesis and the Calvin cycle under photoautotrophic conditions to fix CO2. When external energy supplies from organic acids are present, the bacteria can become photoheterotropic. Under these conditions, the Calvin cycle is used to maintain redox balance.
Dark Fermentation
We studied dark fermentation indirectly above in our discussion of hydrogenases in microalgae. Hydrogenases are induced in dark conditions, and this pathway involves heterotrophic fermentation (anaerobic) in some bacteria and microalgae. Many microbial species are used. Industrial wastewater enriched in organic material can be used as a feedstock.
Feedstock materials are hydrolyzed and subjected to fermentation, during which H2 can be produced. For example, pyruvate produced by glycolytic fermentation can be oxidatively decarboxylated to acetyl-CoA and CO2 by pyruvate:ferredoxin oxidoreductase with electrons passed on to ferredoxin and even through hydrogenase to form H2 (as we described above). H2 is involved in steps after fermentation, including acetogenesis and methanogenesis. These processes are illustrated in Figure \(\PageIndex{11}\) below.
Figure \(\PageIndex{11}\): The steps involved in anaerobic digestion [9]. Rosa, P. R. F., & Silva, E. L. (2017). Review of Continuous Fermentative Hydrogen-Producing Bioreactors from Complex Wastewater. Frontiers in Bioenergy and Biofuels. doi: 10.5772/65548. Creative Commons Attribution 3.0 License
Examples of acidogenic (formation of short carboxylic/fatty acid), acetogenic (formation of acetic acid), and methanogenic (formation of methane) reactions that produce (and a few that consume) H2 are shown in Table \(\PageIndex{3}\) below.
Acidogenic reactions |
C6H12O6 + 2H2O → 2CH3COOH + 2CO2 + 4H2 |
C6H12O6 + 2H2O→ CH3CH2CH2COOH + 2CO2 + 2H2 |
Acetogenic reactions |
CO2+ 4H2→ CH3COOH+ 2 H2O |
CH3CHOHCOOH + H2O → CH3COOH + CO2 + 2H2 |
CH3CH2OH + H2O →CH3COOH + 2H2 |
CH3CH2COOH + 2 H2O → CH3COOH + CO2 + 3 H2 |
CH3(CH2)2COOH + 2 H2O → 2 CH3COOH + 2H2 |
Methanogenic reactions |
4 H2 + CO2→ CH4 + 2 H2O |
CH3COOH → CH4 + CO2 |
2CH3(CH2)2COOH + 2H2O + CO2→ 4CH3COOH + CH4 |
Table \(\PageIndex{3}\): Example of acidogenic, acetogenic, and methanogenic reactions in dark fermentation. Adapted from Rosa, P. R. F., & Silva, E. L., ibid.
We have described a few of the enzymes involved in acidogenic reactions above. Figure \(\PageIndex{12}\) summarizes the steps in acidogenesis.
Figure \(\PageIndex{12}\): An overview of the metabolic pathways of acidogenesis. Dzulkarnain, E.L.N., Audu, J.O., Wan Dagang, W.R.Z. et al. Microbiomes of biohydrogen production from dark fermentation of industrial wastes: current trends, advanced tools, and future outlook. Bioresour. Bioprocess. 9, 16 (2022). https://doi.org/10.1186/s40643-022-00504-8. http://creativecommons.org/licenses/by/4.0/.
Figure \(\PageIndex{13}\) below shows a more complex list and summary of dark fermentation reactions.
Figure \(\PageIndex{13}\): Key enzymes and dominant microbial taxa involved during anaerobic digestion of organic matter. Dzulkarnain, E.L.N.et al. Ibid.
ELECTROCHEMICAL/ELECTROLYTIC (3)
Two primary electrochemical/electrolytic methods for H2 production are photoelectrochemical and electrolytic, as shown below in Figure \(\PageIndex{14}\).
Figure \(\PageIndex{14}\): Schematic diagram for the electrochemical process. M.G. Eloffy et al.
Electrolysis
In a microbial electrolytic cell (MEC), microalgae/cyanobacteria use industrially- and metabolically-processed feedstocks to oxidize organic substrates (for example, acetic acid) to CO2. The released electrons move from the anode (where the oxidation occurs) to the cathode for H+ reduction to H2. An external voltage increases electron flow to the cathode to facilitate the process. This increases the production of H2 over and above that of just fermentation by microbes in the electrolytic cell. Cyanobacteria and a mix of green microalgae are used, as well as bacteria that can use dark fermentation (i.e., combining the processes described above).
Photoelectrochemical
Microbial photoelectrochemical cells (PEC) use light-sensitive semiconductor electrodes for water electrolysis. A membrane separates the two electrodes so the protons can be reduced to form H2.
2. THERMOCHEMICAL from Biomass
We have already explored thermochemical methods to produce syngas (H2 and CO) and further use in the Fishcer-Tropsch reaction to make small and large molecules for chemical feedstocks and fuels. We also discussed electrochemical methods to produce syngas and other small organic molecules like formate and ethanol from CO2. Figure \(\PageIndex{15}\) shows a schematic diagram for thermochemical (gasification) processes to produce H2.
Figure \(\PageIndex{15}\): Schematic diagram for thermochemical (aqueous phase reforming) process. M.G. Eloffy et al.
Summary
This chapter explores hydrogen as a clean fuel alternative, emphasizing its exceptional energy density and environmentally benign combustion—producing only water as a byproduct. The chapter begins by comparing hydrogen’s high heat of combustion with other fuels, underscoring its potential as an ideal energy carrier if challenges related to storage, transport, and scalable production can be overcome.
Key production methods are categorized into three primary groups:
-
Biological Production:
The chapter details how microbes and microalgae use enzymes like hydrogenases to generate hydrogen through photobiolysis and fermentation. It explains both direct photolysis—where water is oxidized in photosystem II and electrons from reduced ferredoxin are used by hydrogenases—and indirect photolysis, where organic substrates produced by photosynthesis are fermented anaerobically to yield hydrogen. The discussion also covers dark fermentation pathways in which glycolytic intermediates are converted to hydrogen, linking these biochemical processes to potential biohydrogen production. -
Electrochemical/Electrolytic Production:
This section describes methods such as photoelectrochemical cells and microbial electrolytic cells (MECs), which use light-sensitive semiconductors or external voltage to drive water electrolysis. The integration of renewable electricity into these systems is highlighted as a way to produce “green hydrogen” with minimal carbon emissions. -
Thermochemical Production:
The chapter explains how biomass can be converted into syngas—a mixture primarily of CO and H₂—via processes like gasification and aqueous-phase reforming. It covers subsequent reactions, including the water-gas shift, which adjust the H₂/CO ratio, and discusses how syngas serves as a precursor for hydrogen production in industrial settings.
Additionally, the chapter examines the atmospheric chemistry of hydrogen. Although H₂ itself is not a greenhouse gas, its reaction with hydroxyl radicals (.OH) can indirectly affect the lifetime of potent greenhouse gases like methane, illustrating the complex interplay between hydrogen and atmospheric processes.
Overall, this chapter integrates biochemical, electrochemical, and thermochemical principles to provide a comprehensive overview of hydrogen production strategies. It emphasizes the potential of biohydrogen—produced via biological and electrochemical routes—as a sustainable, low-carbon fuel, while also addressing the challenges and environmental considerations associated with hydrogen production and use. This multidisciplinary approach equips junior and senior biochemistry majors with the knowledge to critically assess hydrogen’s role in future energy systems.