source: water |
electrolysis |
2H2O → O2 + 4H+ + 4e–; ΔH = 285 kJ/mol, ΔG = 237 kJ/mol |
• carbon-free
H2 generation |
• low efficiency of
electrolyzer over a range of operational
conditions |
• possibility
of using renewable/nuclear
feedstock |
• high capital and production costs |
• low operational life of electrodes |
• in early stages of development |
photochemical |
2H2O → O2 + 4H+ + 4e– ; ΔH = 285 kJ/mol, ΔG = 237 kJ/mol |
• ability to generate negligible or no greenhouse
gas
emissions |
• only developed at lab-scale |
• no intake of fossil fuels |
• low efficiency and stability of photoelectrodes/photocatalysts
due to high reaction impedance |
• low operating temperatures |
• high risk
of photocorrosion of active materials |
•
spontaneous and rapid back reactions |
•
overwhelming production costs |
thermochemical |
2H2O → O2 + 4H+ + 4e– ; ΔH = 285 kJ/mol, ΔG = 237 kJ/mol |
• potentially
negligible or no greenhouse gas emissions |
• highly
energy intensive with requirement of temperature
up to 2000 °C |
• follows a closed loop cycle consuming only water and
producing only H2 and O2
|
•
low efficiency of thermochemical reactors and materials |
• chemicals can be reused within a
cycle |
• high cost of solar concentrating mirrors |
• developed at lab scale only |
source:
organic matter |
biomass gasification |
C6H12O6 + O2 + H2O → CO + CO2 + H2 + other byproducts (taking glucose molecules only) |
• high efficiency and rapid process |
•
emission of COx and other
components such as H2S, NH3 and tar |
• availability of abundant and cheap raw materials |
• requirement of gas separation and COx removal processes |
•
low cost syngas production |
• high reactor and
feedstock costs |
• quality of H2 produced is poor |
• demonstrated
at lab scale only |
photobiological |
2H2O → O2 + 2H2 ; ΔH = 285 kJ/mol, ΔG = 237 kJ/mol |
• can be used in a wide range of water conditions |
• in early stages of development |
• the process is self-sustaining |
• low efficiency and sustainability of microorganisms |
• designing robust reactor configurations
that can use
sunlight effectively and produce H2
|
source: fossil
fuels (natural
gas/methane) |
steam methane reforming
(SMR) |
CH4+ H2O ↔
CO + 3H2; ΔH298K = 206
kJ/mol |
• low-cost H2 production technology |
• emission of greenhouse gases in to atmosphere |
• high H/C ratio |
• requirement
of downstream separation and purification
processes |
• high efficiency |
• a complex system of reactions including water-gas
shift reaction and pressure-swing adsorption reactions |
dry reforming of methane (DRM) |
CH4 + CO2 ↔ 2CO +
2H2; ΔH = 247 kJ/mol |
• utilizes
CO2 to produce H2
|
• more
energy intensive than SMR |
•
can be used for the Fischer–Tropsch
process |
• high equipment cost |
• complex downstream processes for H2 purification |
• emission of greenhouse gases |
partial oxidation of methane (POM) |
CH4 + 1/2O2 ⇆ CO + 2H2; ΔH =
−36 kJ/mol |
• high efficiency and selectivity |
• high emissions of COx and
possibility of emissions of NOx
|
• very short residence time |
• formation of soot byproduct |
• requirement of pure O2
|
catalytic decomposition of methane (CDM) |
CH4 → C(s) + 2H2;
ΔH298K = 75.4 kJmol |
• simple and one-step process |
• in early
stages of development |
• no COx or NOx emissions |
• low stability of catalysts, requiring effective regeneration
techniques |
• produces high quality
H2
|
• unreacted methane
in out stream |
• produces solid carbon
as a byproduct, which is easier
to separate |
• solid carbon in the
form of value-added nanocarbons
is generated |