Biofuels & bioenergy
Marine biofuels: biomethanol and bio-LNG
Why ocean shipping converged on methanol and liquefied biomethane, the synthesis routes from syngas and biogas that produce them, and the volumetric, cryogenic and slip limits each carries.
Ocean shipping cannot electrify. A battery pack stores roughly half a megajoule per kilogram; heavy fuel oil stores about forty — a gap near two orders of magnitude that no projected chemistry closes for a vessel crossing an ocean between bunkers. So the fuel must be a molecule, and the molecule is chosen by port logistics and tank volume before anyone asks how it was made. Two candidates currently satisfy both shipbuilders and fuel producers: methanol and liquefied biomethane.
Methanol: the minimal synthesis target
Methanol is the terminal point of one-carbon chemistry: CO + 2H2 over a copper-zinc-alumina catalyst at roughly 220–280 °C and 50–100 bar, with CO2 + 3H2 as a parallel route. Both reactions are exothermic and equilibrium-limited, so plants run recycle loops and convert per pass only partially. What makes methanol the natural first target of the syngas platform is selectivity: there is no chain-growth distribution to fight, no Anderson-Schulz-Flory ceiling, because the product is the single molecule itself. Gas cleanup matters exactly as much as on the Fischer-Tropsch page — sulfur poisons the copper catalyst — but everything after cleanup is comparatively easy. As a marine fuel, methanol is liquid at ambient temperature and pressure, boiling at 65 °C, so it needs no cryogenics and fits tank and bunker practice with modest adaptation. The price is volumetric: at roughly 16 MJ per litre it carries less than half the energy of heavy fuel oil, so tanks must be two and a half times larger for the same range, and its low lubricity and toxicity force engines to ignite it with a diesel pilot rather than by compression alone.
Bio-LNG: riding an installed combustion base
Liquefied biomethane is simply the product of the digester chain pushed one step further: upgrade biogas to pipeline-grade methane, then liquefy at −162 °C, shrinking the volume about six-hundred-fold. The liquefaction step has its own hard edge — CO2 must be stripped to trace levels first, because it freezes at −78.5 °C and would plug the cold box — but the combustion side is the appeal: an existing and growing fleet of dual-fuel engines already burns methane, so the biofuel drops into hardware bought for the fossil version. The unresolved liability is methane slip: gas engines let a fraction of unburned fuel escape, and methane is roughly thirty times stronger than CO2 as a greenhouse gas over a century, so a few percent of slip visibly erodes the climate case.
Why these two and not something better
Neither molecule is energetically remarkable. They win on constraint satisfaction: both are storable in ship-scale tanks, both run in certified engines, and both have production routes — gasification to methanol, digestion to LNG — that draw on the two feedstock families of the cluster framework. The limiting quantities are unglamorous: litres per nautical mile, cryogenic capital, and slip percentage. A better chemistry would have to beat methanol not as a molecule but as cargo.