Industrial routes Nearly all of the world's current supply of hydrogen gas() is produced from fossil fuels, with less than 1% of hydrogen being produced by low-emissions technologies in 2025. Many methods exist for producing H2, but three dominate commercially: steam reforming often coupled to water-gas shift, partial oxidation of hydrocarbons, and water electrolysis. The production of natural gas feedstock also produces emissions such as
vented and
fugitive methane, which further contributes to the overall carbon footprint of hydrogen. This reaction is favored at low pressures but is nonetheless conducted at high pressures() because high-pressure is the most marketable product, and
pressure swing adsorption(PSA) purification systems work better at higher pressures. The product mixture is known as "
synthesis gas" because it is often used directly for the production of
methanol and many other compounds.
Hydrocarbons other than methane can be used to produce synthesis gas with varying product ratios. One of the many complications to this highly-optimized technology is the formation of
coke or carbon: Therefore, steam reforming typically employs an excess of. Additional hydrogen can be recovered from the steam by using carbon monoxide through the
water gas shift reaction(WGS). This process requires an
iron oxide catalyst:
Partial oxidation of hydrocarbons Other methods for CO and production include partial oxidation of hydrocarbons:
Water electrolysis Electrolysis of water is a conceptually simple method of producing hydrogen. Commercial
electrolyzers use
nickel-based catalysts in strongly alkaline solution.
Platinum is a better catalyst but is expensive. The hydrogen created through electrolysis using renewable energy is commonly referred to as "
green hydrogen".
Electrolysis of
brine to yield
chlorine also produces high-purity hydrogen as a co-product, which is used for a variety of transformations such as
hydrogenations. The electrolysis process is more expensive than producing hydrogen from methane without
carbon capture and storage. Innovation in
hydrogen electrolyzers could make large-scale production of hydrogen from electricity more cost-competitive.
Thermochemical Water splitting is the process by which water is decomposed into its components. Relevant to the biological scenario is this equation: The reaction occurs in the
light-dependent reactions in all
photosynthetic organisms. A few organisms, including the alga and
cyanobacteria, have evolved a second step in the
dark reactions in which protons and electrons are reduced to form gas by specialized
hydrogenases in the
chloroplast. Efforts have been undertaken to
genetically modify cyanobacterial hydrogenases to more efficiently generate gas even in the presence of oxygen. Efforts have also been undertaken with genetically‐modified alga in a
bioreactor. Relevant to the thermal water-splitting scenario is this simple equation: Over 200 thermochemical cycles can be used for
water splitting. Many of these cycles such as the
iron oxide cycle,
cerium(IV) oxide–cerium(III) oxide cycle,
zinc–zinc oxide cycle,
sulfur–iodine cycle,
copper–chlorine cycle and
hybrid sulfur cycle have been evaluated for their commercial potential to produce hydrogen and oxygen from water and heat without using electricity. A number of labs (including in
France,
Germany,
Greece,
Japan, and the
United States) are developing thermochemical methods to produce hydrogen from solar energy and water.
Natural routes Biohydrogen is produced in organisms by enzymes called
hydrogenases. This process allows the host organism to use
fermentation as a source of energy. These same enzymes also can
oxidizeH2, such that the host organisms can subsist by reducing oxidized substrates using electrons extracted fromH2. Hydrogenase enzymes feature
iron or
iron–nickel centers at their
active sites. The natural cycle of hydrogen production and consumption by organisms is called the
hydrogen cycle. Some bacteria such as can use the small amount of hydrogen in the atmosphere as a source of energy when other sources are lacking. Their hydrogenases feature small channels that exclude oxygen from the active site, permitting the reaction to occur even though the hydrogen concentration is very low and the oxygen concentration is as in normal air. Confirming the existence of hydrogenase‐employing microbes
in the human gut, occurs in human breath. The concentration in the breath of fasting people at rest is typically under (ppm), but can reach when people with intestinal disorders consume molecules they cannot absorb during diagnostic
hydrogen breath tests.
Serpentinization Serpentinization is a geological mechanism which produces highly-
reducing conditions. Under these conditions, water is capable of oxidizing
ferrous() ions in
fayalite, generating hydrogen gas: Closely related to this geological process is the
reaction: This process also is relevant to the corrosion of
iron and
steel in
oxygen-free groundwater and in
reducing soils below the
water table.
Laboratory syntheses is produced in laboratory settings, such as in the small-scale
electrolysis of water using metal
electrodes and water containing an
electrolyte, which liberates hydrogen gas at the
cathode: Many metals, such as aluminium, are slow to react with water because they form
passivated oxide coatings. An alloy of aluminium and
gallium, however, does react with water. In high-pH solutions, aluminium can react with : H2 can be stored in compressed form, although compressing costs energy. Liquefaction is impractical given hydrogen's low
critical temperature. In contrast, ammonia and many hydrocarbons can be liquified at room temperature under pressure. For these reasons, hydrogen
carriers—materials that reversibly bindH2—have attracted much attention. The key question is then the weight percent of H2-equivalents within the carrier material. For example, hydrogen can be reversibly absorbed into many
rare earths and
transition metals and is soluble in both nanocrystalline and
amorphous metals. Hydrogen
solubility in metals is influenced by local distortions or impurities in the
crystal lattice. These properties may be useful when hydrogen is purified by passage through hot
palladium disks, but the gas's high solubility is also a metallurgical problem, contributing to the
embrittlement of many metals, complicating the design of pipelines and storage tanks. The most problematic aspect of metal hydrides for storage is their modest H2content, often on the order of1%. For this reason, there is interest in storage of H2 in compounds of low
molecular weight. For example,
ammonia borane () contains 19.8
weight percent ofH2. The problem with this material is that after release of H2, the resulting boron nitride does not re-add H2: i.e., ammonia borane is an irreversible hydrogen carrier. More attractive are
hydrocarbons such as
tetrahydroquinoline, which reversibly release someH2 when heated in the presence of a catalyst: == Applications ==