GeoNitra

Natural hydrogen.
Made into ammonia.

The Hajar mountains behind Fujairah make hydrogen on their own. GeoNitra turns it into low-GHG ammonia on the Gulf of Oman coast, beside the ships that carry it to the world.

Clean ammonia costs whatever its hydrogen costs.

Almost all of the world’s ammonia is made from fossil gas, and clean hydrogen is expensive wherever it has to be manufactured. GeoNitra starts from hydrogen the rock has already made, so the most costly and carbon-heavy part of an ammonia plant is never built.

The opportunity.

180
million tonnes a year
Global ammonia demand: fertiliser, industry and now shipping fuel.
<1%
low-carbon today
The buyers are asking. The supply at a workable cost does not exist yet.
1
million tonnes a year
The potential scale at Fujairah, built in trains as the hydrogen is proven.
1.6–2.4
tonnes of CO₂ avoided
For every tonne of ammonia, against the way it is made today.
The market

A molecule the world already ships.

Ammonia feeds about half the planet and is being built into the shipping fuel mix. It already moves by sea in gas carriers, through terminals and bunkering ports that exist today.

The opening is the feedstock. Clean ammonia made with electrolytic hydrogen runs at $700 to $1,000 or more a tonne, and almost all of that premium is the hydrogen. A plant that starts with hydrogen from the ground changes that equation.

A gas carrier at sea, seen from above
Ammonia already moves by sea. The infrastructure is not something we have to invent.
The process

Three steps, not six.

A conventional ammonia plant spends most of its capital, most of its fuel and all of its carbon on one job: tearing hydrogen out of methane. Two reformers, shift reactors, CO₂ removal and methanation all run before any ammonia is made.

We start where they finish. The hydrogen arrives already made, so the plant treats the gas, takes nitrogen from the air and runs the synthesis loop.

N₂ + 3H₂ → 2NH₃
One tonne of ammonia takes about 178 kg of hydrogen. That is fixed by the chemistry.
An ammonia synthesis unit at night
The synthesis loop: proven technology, licensed at scale since the 1960s.
Two routes to one molecule
Process unit CO₂ released Not built
TODAY
Steam-methane reforming
  1. INNatural gas + steamCH₄, H₂O
  2. 01Primary reformer~850 °C, firedCO₂
  3. 02Secondary reformer~1,000 °C, air in
  4. 03Shift reactorsCO → CO₂
  5. 04CO₂ removalAmine washCO₂
  6. 05Methan­ationTrace CO clean-up
  7. 06Synthesis loopN₂ + 3H₂ → 2NH₃
  8. OUTAmmoniaNH₃
1.6–2.4 t
CO₂ PER TONNE NH₃
GEONITRA
Natural hydrogen
  1. INHydrogen from the groundMade by the rock
  2. 01Gas treatmentDry, purify, compress
  3. No reformers, no shift, no CO₂ removalThe front end of the plant is not built
  4. 02Air separationN₂ from air
  5. 03Synthesis loopN₂ + 3H₂ → 2NH₃
  6. OUTAmmoniaNH₃
0 t
PROCESS CO₂

The synthesis loop is the same proven technology on both routes; what changes is everything before it. The synthesis itself makes no CO₂. The compressors and the air-separation unit run on power, so the plant’s footprint follows its electricity supply.

Fujairah

Where the rock meets the deep water.

The ophiolite that makes the hydrogen runs under the Hajar mountains. The jetties are on the Gulf of Oman, outside the Strait of Hormuz, at one of the world’s largest bunkering ports.

Feedstock and export share the same stretch of coast, with no long hydrogen pipeline in between.

An ammonia terminal between desert mountains and the sea
Tank farms, berths and bulk-liquid handling already operate at scale on this coast.
1 Mt/yr
Ammonia, scale case
About 2,900 tonnes a day, built in trains rather than in one step.
178 kt/yr
Hydrogen in
About 510 tonnes a day from the ground at full scale.
822 kt/yr
Nitrogen in
Taken from the air on site by an air-separation unit.
1.6–2.4 Mt/yr
CO₂ not emitted
Against the same tonnage made the way it is made today.
The resource

The hydrogen is already there.

The Hajar mountains are mantle rock brought to the surface, one of the great ophiolite exposures on earth. Where water meets that rock it serpentinises, and serpentinisation makes hydrogen: continuously, for as long as the rock and the water keep meeting. Hydrogen-bearing springs and seeps are documented along this belt.

Everything difficult about clean ammonia is the hydrogen, and here nature has already done that part. Our work is above ground: gather it, clean it, and turn it into a molecule the world already ships by the million tonnes.

A milky-turquoise hyperalkaline stream in an ophiolite gorge in Fujairah
Field photoA hyperalkaline stream in an ophiolite gorge, Fujairah.
A pH meter reading about 11 over a carbonate-crusted spring
Field photopH about 11 at a spring: the chemical signature of serpentinisation.
A milky-blue alkaline pool among dark ophiolite rocks
Field photoAlkaline spring water pooling in the ophiolite.
Contact

Let’s talk.

If you buy ammonia, license synthesis technology, build plants or invest in energy infrastructure, and want to be early to a feedstock nobody else is using yet, we would like to hear from you.

Write to us
[email protected]

GeoNitra · Fujairah, United Arab Emirates