EXECUTIVE SUMMARY
Ammonia (NH₃) is the foundation of synthetic nitrogen fertiliser — urea, ammonium nitrate, ammonium sulfate, and diammonium phosphate all begin with ammonia. Nitrogen is the nutrient most limiting to plant growth, and synthetic nitrogen fertiliser is the single most important industrial chemical for food production worldwide. Approximately half of the nitrogen in the food consumed by the global population comes from the Haber-Bosch process.1 NZ imports all of its ammonia-derived fertiliser — approximately 400,000–600,000 tonnes of urea and other nitrogen products per year.2 NZ has no ammonia synthesis capability, no ammonia synthesis plant, and no near-term pathway to building one.
The Haber-Bosch process synthesises ammonia from nitrogen (from air) and hydrogen (typically from natural gas or water electrolysis) at 400–500°C and 150–300 atmospheres of pressure, over an iron-based catalyst.3 These conditions are not difficult to achieve in a laboratory. They are extraordinarily difficult to achieve at industrial scale with the reliability, containment, and throughput required to produce agriculturally meaningful quantities of ammonia. The process requires: high-pressure vessels rated for 150–300 atm at 500°C; compressors capable of reaching and maintaining those pressures; an iron catalyst prepared to specific physical and chemical specifications; a hydrogen source (either steam-methane reforming of natural gas or water electrolysis, each with its own industrial prerequisites); an air separation or purification system for nitrogen feedstock; heat exchangers, condensers, and recirculation systems; and instrumentation capable of monitoring and controlling temperatures, pressures, flow rates, and gas compositions within tight tolerances.
Each of these requirements represents either an industry NZ does not have or a capability NZ must build. The dependency chain runs through high-pressure metallurgy, compressor manufacturing, catalyst production, hydrogen generation, chemical engineering, and precision instrumentation — none of which exist in NZ at the scale or specification required for ammonia synthesis. This is why the feasibility rating is [D]: decades of staged industrial development, not years.
NZ’s interim nitrogen strategy — biological nitrogen fixation through legumes, recycling of organic nitrogen, and eventually imported ammonia or urea via maritime trade — is covered in Doc #80. This document addresses the question of whether and how NZ could eventually build domestic ammonia synthesis capability, and provides an honest assessment of the timeline and prerequisites.
The honest conclusion: NZ should pursue biological nitrogen fixation and trade-sourced ammonia as primary strategies. Domestic ammonia synthesis is a generational project — 30–60 years from the event under optimistic assumptions, possibly longer. NZ should begin laying the industrial foundations (steelmaking capability, chemical industry, compressor development) for reasons that extend well beyond ammonia, but should not plan on domestic ammonia production filling the nitrogen gap within the first several decades. If Australia or another region with a larger industrial base develops ammonia synthesis capability first, trade is almost certainly the faster path to NZ’s ammonia supply.
Contents
RECOMMENDED ACTIONS
Phase 1–2 (Years 0–3): No ammonia-specific actions
All nitrogen-related effort in Phase 1–2 should focus on biological nitrogen fixation and organic nitrogen recycling (Doc #80). Ammonia synthesis is not achievable in this timeframe and diverting scarce engineering talent toward it would be wasteful.
Phase 2–3 (Years 1–7): Foundation-laying (shared with other industrial goals)
- Maintain and expand NZ Steel operations (Doc #89). Steelmaking capability is a prerequisite for all downstream metal fabrication, including pressure vessels.
- Develop sulfuric acid production (Doc #113). Sulfuric acid is needed for superphosphate manufacturing and is a foundational chemical industry product. This development builds chemical engineering competence relevant to ammonia synthesis.
- Develop hydrogen production capability via water electrolysis (Doc #63). Low-pressure hydrogen for immediate applications (glass reduction, metal processing, laboratory use) builds toward higher-pressure hydrogen systems later.
- Preserve and train chemical engineering expertise. Universities (Doc #157) should maintain chemical engineering education. Practising chemical engineers should be identified, classified as critical personnel, and involved in long-term industrial planning.
- Document NZ’s natural gas reserves and production capability. Taranaki gas fields may provide feedstock for steam-methane reforming if that pathway is chosen. Remaining reserve estimates and wellhead equipment condition are critical planning inputs.
- Begin pressure vessel development programme. Fabrication of vessels rated to 10–50 atm for various applications (autoclaves, chemical reactors, compressed gas storage) builds the metallurgical and fabrication skills that scale toward ammonia-grade vessels later.
Phase 3–5 (Years 7–30): Industrial capability building
- Develop medium-pressure chemical processing capability. Target: vessels and systems operating reliably at 50–100 atm. Applications include methanol synthesis (Doc #102), compressed gas storage, and pilot-scale chemical processing.
- Develop compressor manufacturing or refurbishment capability. Multi-stage reciprocating compressors capable of 100+ atm are needed for ammonia synthesis and other high-pressure chemical processes. This requires precision machining (Doc #91), valve manufacturing, seal technology, and metallurgy for high-pressure cylinders and pistons.
- Develop catalyst production capability. Iron-based Haber-Bosch catalysts require preparation from magnetite (iron oxide) with promoters (aluminium oxide, calcium oxide, potassium oxide). The magnetite and promoter materials are available in NZ. Catalyst preparation — grinding, mixing, fusing in an electric furnace, crushing, and activation under hydrogen flow — requires process development.
- Build and operate a pilot-scale ammonia synthesis loop at modest pressure (100–150 atm) and small throughput (kilograms per day). This is the proof-of-concept step.
- Pursue trade agreements with Australia or other regions for ammonia or urea supply. This remains the most likely near-term source of synthetic nitrogen fertiliser for NZ.
Phase 5–7 (Years 30–100+): Production-scale development
- Scale pilot plant to production scale based on pilot experience. Target: tonnes per day rather than kilograms.
- Develop urea synthesis capability — combining ammonia with CO₂ at high pressure and temperature. Urea is the preferred fertiliser form for transport and application.
- Integrate ammonia production with NZ’s energy and chemical industry. Ammonia production consumes large quantities of energy and hydrogen; the plant must be co-located with reliable electricity and hydrogen supply.
ECONOMIC JUSTIFICATION
The value of nitrogen fertiliser
NZ’s pre-event agricultural output depended on approximately 400,000–600,000 tonnes per year of imported nitrogen fertiliser products.4 Without synthetic nitrogen, crop yields decline an estimated 30–50% for intensive cropping and 10–25% for pasture (Doc #75).5 Over a 50-year recovery period, this yield reduction translates to a cumulative food deficit measured in millions of tonnes of foregone crop and meat production. The economic and human cost of this deficit — in reduced nutrition, constrained population growth, and limited agricultural surplus for trade — is very large, though difficult to quantify precisely.
The cost of building ammonia synthesis capability
Honest assessment: The person-year cost of developing domestic ammonia synthesis cannot be meaningfully estimated at this stage because it depends on which prerequisite industries are built (and for what other reasons), how quickly they develop, and whether trade provides an alternative that makes domestic production unnecessary. A rough order-of-magnitude estimate for the ammonia-specific development (excluding shared prerequisites like steelmaking and chemical industry):
- Catalyst development: 20–50 person-years of chemical engineering and metallurgical research
- Pilot plant design, construction, and testing: 50–150 person-years of engineering and construction labour
- Compressor development (ammonia-specific): 30–80 person-years (shared with other high-pressure applications)
- Production plant construction: 200–500 person-years
- Total ammonia-specific effort: roughly 300–800 person-years over 20–40 years
This estimate has wide uncertainty — the actual cost could be higher if unexpected technical obstacles arise (and they will), or lower if trade provides catalyst or compressor technology from a more industrialised region. Moreover, these 300–800 person-years are almost entirely scarce specialist labour — chemical engineers, metallurgists, precision machinists — who face competing demands across many other recovery programmes. The headline figure understates the real difficulty because these are not person-years that can be staffed from the general unemployed population.
Comparison with alternatives
Biological nitrogen fixation (the baseline): Already underway from Phase 1 (Doc #80). Provides approximately 50–75% of NZ’s pastoral nitrogen needs through clover and other legumes, but only 20–40% of intensive cropping needs.6 Requires no industrial infrastructure. Cost: farming labour and legume seed, which NZ already has. Limitation: cannot fully replace synthetic nitrogen for intensive cropping at scale. Traditional Māori soil fertility management – composting with marine-derived organic matter (fish offal, shellfish remains, seaweed), crop rotation with fallow periods allowing fern regrowth and organic matter accumulation, and managed burn-regrowth cycles – provides tested, locally adapted low-input techniques for maintaining soil biological health during the interim decades before synthetic nitrogen becomes available (Doc #80).7
Trade-sourced ammonia or urea: If another region develops ammonia synthesis, NZ could import product by maritime trade. Australia has existing ammonia plants and natural gas reserves — if any survive and Australia maintains production capability, this is the fastest path.8 Cost: trade goods (NZ’s agricultural surplus, timber, manufactured products). Risk: depends on trade materialising and the other region maintaining production.
Domestic ammonia synthesis: The most expensive option in person-years, but the only one that makes NZ fully self-sufficient in nitrogen fertiliser. The economic case for domestic production strengthens if: (a) trade does not provide a reliable ammonia supply, (b) NZ’s population grows and food demand increases, or (c) the prerequisite industries are developed anyway for other purposes (pressure vessel fabrication for other chemical processes, compressors for hydrogen systems, chemical engineering for pharmaceutical or industrial chemistry).
Breakeven assessment
If trade provides a reliable ammonia supply, domestic synthesis may never be economically justified for a population of NZ’s size (5 million, possibly growing to 6–8 million over the recovery period). The breakeven calculation depends entirely on whether trade materialises. If NZ must be fully self-sufficient, the investment in ammonia synthesis becomes necessary regardless of its person-year cost, because the alternative is permanently constrained food production. This is a strategic necessity question that cannot be answered until the trade situation becomes clear, probably in Phase 3–4.
1. WHY AMMONIA MATTERS
1.1 The nitrogen bottleneck
Of the three macronutrients essential for plant growth — nitrogen (N), phosphorus (P), and potassium (K) — nitrogen is the most limiting and the most difficult to replace locally. Plants require nitrogen in large quantities for amino acids, proteins, chlorophyll, and nucleic acids. Nitrogen deficiency reduces growth, yield, and protein content of harvested crops.
The atmosphere is 78% nitrogen gas (N₂), but atmospheric nitrogen is chemically inert — the triple bond between the two nitrogen atoms is one of the strongest in chemistry, requiring approximately 946 kJ/mol to break.9 Plants cannot use atmospheric nitrogen directly. It must first be “fixed” — converted to a biologically available form such as ammonia (NH₃), nitrate (NO₃⁻), or ammonium (NH₄⁺).
Before the Haber-Bosch process was commercialised in the 1910s, all agricultural nitrogen came from biological fixation (legume bacteria, free-living soil bacteria, lightning), animal manure, and mined deposits (Chilean sodium nitrate, guano). These sources supported a global population of approximately 1.6 billion.10 Synthetic nitrogen fertiliser, derived from Haber-Bosch ammonia, enabled the food production that supports the current global population of approximately 8 billion.11
1.2 NZ’s nitrogen balance
NZ’s pastoral farming system has a significant advantage: NZ pastures typically contain 20–30% clover (Trifolium repens and T. pratense), which fixes atmospheric nitrogen through symbiotic Rhizobium bacteria in root nodules. Annual biological nitrogen fixation in NZ pastoral systems is estimated at 100–200 kg N/ha/year under normal conditions.12 This is a substantial nitrogen input — it is why NZ pastoral farming was productive even before synthetic fertiliser became widely used in the mid-20th century.
However, clover fixation alone is insufficient for intensive cropping. Wheat, barley, potato, and brassica crops — the crops NZ must expand under nuclear winter (Doc #76) — require 100–250 kg N/ha/year and do not fix their own nitrogen.13 In a rotation with legumes, some of this nitrogen carries over from the legume phase, but typically only 30–60 kg N/ha is available to the following crop from residual legume nitrogen.14 The deficit must come from manure, compost, or synthetic fertiliser.
Without synthetic fertiliser, NZ’s cropping yields decline substantially, and the total caloric output of NZ agriculture drops at a time when nuclear winter is already reducing yields. This is the nitrogen bottleneck that ammonia synthesis would eventually solve.
1.3 Ammonia’s other uses
While fertiliser is the primary use (approximately 80% of global ammonia production), ammonia has other recovery-relevant applications:15
- Refrigeration: Ammonia is an efficient refrigerant, used in large-scale cold storage and industrial refrigeration (Doc #40). Pre-Freon refrigeration systems used ammonia widely.
- Explosives: Ammonium nitrate (NH₄NO₃), produced from ammonia and nitric acid, is the primary industrial explosive used in mining and quarrying. NZ’s coal and aggregate mining depend on explosives. Without imported ammonium nitrate, mining becomes significantly more labour-intensive.
- Chemical feedstock: Ammonia is a precursor for nitric acid (via catalytic oxidation — the Ostwald process), which in turn is needed for explosives, pharmaceuticals, and other chemical products.
- Water treatment: Chloramine disinfection uses ammonia. Less critical if chlorination alone is maintained (Doc #48).
2. THE HABER-BOSCH PROCESS
2.1 The chemistry
The synthesis reaction is deceptively simple:
N₂ + 3H₂ → 2NH₃ (ΔH = −92 kJ/mol)
Nitrogen and hydrogen combine to form ammonia. The reaction is exothermic (releases heat) and proceeds with a decrease in volume (4 moles of gas become 2). By Le Chatelier’s principle, high pressure favours product formation (ammonia), while high temperature favours the reverse reaction (thermodynamically) but is necessary for adequate reaction rate (kinetically). The industrial process operates in a narrow window that balances these opposing effects.16
2.2 Industrial conditions
Modern Haber-Bosch plants operate at:17
- Temperature: 400–500°C
- Pressure: 150–300 atmospheres (15–30 MPa)
- Catalyst: Promoted iron — magnetite (Fe₃O₄) fused with small amounts of aluminium oxide (Al₂O₃), calcium oxide (CaO), and potassium oxide (K₂O) as promoters. The catalyst is reduced to metallic iron in situ under hydrogen flow before operation.
- Per-pass conversion: Only 10–20% of the feed gas is converted to ammonia per pass through the catalyst bed. The ammonia is condensed out (it liquefies under pressure) and the unreacted nitrogen and hydrogen are recycled back through the reactor. This recirculation loop is a critical design feature — it means the compressor must maintain continuous high-pressure circulation, not one-shot compression.
- Feed gas ratio: 1:3 nitrogen to hydrogen (stoichiometric)
2.3 What makes it hard
The chemistry is well understood and has been practised industrially since 1913.18 The difficulty is entirely in the engineering — building and operating equipment that maintains these conditions reliably at production scale:
High-pressure containment: A reactor vessel operating at 200 atm and 500°C must contain gas at pressures equivalent to 200 kg/cm² (approximately 2,940 psi) while resisting hydrogen embrittlement, thermal cycling, creep deformation, and corrosion by ammonia and hydrogen. The steel must be a specific alloy — typically a chromium-molybdenum (Cr-Mo) alloy such as ASME SA-387 Grade 22 (2.25Cr-1Mo) — that resists hydrogen attack at high temperature.19 NZ Steel at Glenbrook (Doc #89) produces basic carbon steel. It does not produce alloy steels with controlled chromium and molybdenum content. Producing alloy steel requires sourcing alloying elements — chromium and molybdenum are not mined in NZ — and developing metallurgical capability to control alloy composition precisely.
Compressors: Multi-stage reciprocating compressors capable of reaching 150–300 atm must compress a hydrogen-nitrogen mixture to extreme pressure while maintaining sealing integrity. Hydrogen is notoriously difficult to seal — it is the smallest molecule and permeates through materials that contain other gases without leakage. Compressor valves, piston rings, rod packings, and cylinder liners must be fabricated to precision tolerances from materials resistant to hydrogen embrittlement. Each compression stage requires intercooling (heat exchangers to remove the heat of compression). A four- or five-stage compressor train for ammonia synthesis represents some of the most demanding mechanical engineering in the chemical industry.20
Heat exchangers: The reactor feed must be preheated and the reactor effluent cooled. The heat exchangers operate at high pressure and must handle hydrogen-containing gas without leaking. Tube-and-shell heat exchangers with hundreds of tubes, each operating at 150–300 atm, require precision manufacturing and rigorous pressure testing.
Catalyst preparation: While the raw materials for the iron catalyst are available in NZ (magnetite from ironsand, alumina from NZ clays, lime from NZ limestone, potash from wood ash), the catalyst must be prepared to specific physical specifications: particle size, porosity, surface area, and promoter distribution all affect catalyst activity and longevity. Industrial catalyst preparation involves melting the mixture of iron oxide and promoters in an electric furnace at approximately 1,600°C, then cooling, crushing, and sizing the resulting fused mass. The catalyst is then loaded into the reactor and activated (reduced from iron oxide to metallic iron) by passing hydrogen over it at gradually increasing temperatures — a process taking several days and requiring precise temperature control.21
Gas purity: The feed gas must be free of certain poisons that deactivate the iron catalyst — particularly sulfur compounds (hydrogen sulfide), carbon monoxide, and water vapour. Sulfur concentrations as low as a few parts per million can permanently damage the catalyst. If hydrogen is produced by steam-methane reforming, the synthesis gas (syngas) contains CO and CO₂ that must be removed by shift conversion, CO₂ scrubbing, and methanation. If hydrogen is produced by water electrolysis, it is inherently purer, but trace impurities from electrode materials or water chemistry must still be controlled.22
Instrumentation: Temperature, pressure, flow rate, and gas composition must be continuously monitored and controlled. The reactor temperature must be maintained within a narrow band — too cool and reaction rate drops to nothing; too hot and the equilibrium shifts against ammonia and the catalyst sinters (loses surface area permanently). Pre-electronic instrumentation (pneumatic controllers, thermocouples, bourdon-tube pressure gauges, manual valves) was used in ammonia plants from the 1910s through the 1960s and is achievable without modern electronics, but it requires trained operators and careful calibration.23
3. THE PREREQUISITE INDUSTRIES
Each requirement of the Haber-Bosch process traces back to industrial capabilities that NZ must develop. The following sections trace the full dependency chain.
3.1 High-pressure metallurgy
What is needed: Steel alloy plate or forgings suitable for pressure vessels operating at 150–300 atm and 400–500°C, with resistance to hydrogen embrittlement.
Dependency chain:
- NZ Steel (Doc #89) produces basic carbon steel from ironsand. This is the starting point.
- Alloy steelmaking requires chromium and molybdenum additions. NZ has no known commercially significant deposits of either element.24 Sources: trade with Australia (which has chromium deposits in Queensland), or potentially chromium recovery from NZ’s small chromite occurrences in the Nelson-Marlborough ultramafic belt (quantity uncertain and probably insufficient for industrial use).25
- Even with alloy elements sourced, Glenbrook’s steelmaking process must be adapted to produce controlled-composition alloy steel — a metallurgical capability that does not currently exist at the plant.
- Heavy forgings or thick plate must be formed into pressure vessel shapes — thick-walled cylinders, hemispherical heads, flanges. This requires either a forging press (NZ does not have a heavy forge capable of producing pressure vessel components) or plate rolling and welding capability at the required thickness (50–200 mm plate, depending on vessel diameter and pressure rating). Heavy plate welding for pressure service requires specific welding procedures, post-weld heat treatment, and non-destructive testing (radiography, ultrasonic testing).
- Every pressure vessel must be pressure-tested — typically to 1.5x design pressure — before service. Testing requires high-pressure pumps and test equipment.
Assessment: This chain alone represents a decade or more of industrial development, much of which is shared with other advanced manufacturing needs (chemical reactors, compressed gas storage, boiler fabrication).
3.2 Hydrogen production
What is needed: A reliable supply of hydrogen at sufficient purity and in sufficient volume to feed the ammonia synthesis loop. For a modest production-scale plant producing 10–50 tonnes of ammonia per day, the hydrogen requirement is approximately 1.8–9 tonnes per day (three moles of H₂ per mole of NH₃).26
Pathway A — Water electrolysis:
NZ has abundant renewable electricity and abundant water. Electrolysis — splitting water into hydrogen and oxygen using an electric current — is the most natural hydrogen pathway for NZ.
Dependency chain for electrolysis: 1. Electrolyser cells — historically, alkaline electrolysers use mild steel or nickel electrodes in a potassium hydroxide (KOH) electrolyte solution. Basic alkaline electrolysis is achievable with NZ materials: steel electrodes (Doc #63), potassium hydroxide (producible from wood ash potash and lime), and diaphragms (asbestos was historically used; modern alternatives include porous ceramic or polymer membranes).27 2. Electrical power — electrolysis consumes approximately 50–55 kWh per kg of hydrogen.28 For 5 tonnes/day of hydrogen (enough for approximately 28 tonnes/day of ammonia), electrical consumption is approximately 250–275 MWh/day, or roughly 10–12 MW of continuous power. This is a meaningful but manageable load on NZ’s grid — roughly 0.3% of NZ’s total generation capacity. 3. Gas compression — electrolytic hydrogen is produced at atmospheric or low pressure and must be compressed to synthesis pressure (150–300 atm). This circles back to the compressor requirement in Section 3.3. 4. Gas purification — electrolytic hydrogen contains trace water vapour and possibly oxygen that must be removed before entering the synthesis loop.
Pathway B — Steam-methane reforming (SMR):
If NZ’s Taranaki natural gas fields remain productive, SMR is the conventional industrial route to hydrogen. Natural gas (CH₄) reacts with steam at 700–1,000°C over a nickel catalyst:
CH₄ + H₂O → CO + 3H₂ (steam reforming) CO + H₂O → CO₂ + H₂ (water-gas shift)
This is more energy-efficient than electrolysis per unit of hydrogen but requires: (a) natural gas supply, (b) reformer tube metallurgy (high-nickel alloys operating at 700–1,000°C and 20–40 atm), (c) nickel catalyst, and (d) gas purification to remove CO and CO₂ from the hydrogen stream.
Assessment: Electrolysis is the more achievable pathway for NZ because it uses NZ’s core advantage — renewable electricity — and avoids the complex reformer metallurgy and gas purification requirements of SMR. The trade-off is higher energy consumption per unit of hydrogen. Both pathways require compression to synthesis pressure.
3.3 Compression
What is needed: Multi-stage reciprocating compressors capable of compressing hydrogen-nitrogen mixture from near-atmospheric pressure to 150–300 atm.
Dependency chain:
- Precision machining capability (Doc #91) for cylinders, pistons, connecting rods, crossheads, and crankshafts.
- Valve manufacturing — compressor valves open and close thousands of times per minute and must seal against hydrogen at extreme pressure. They are precision components made from high-grade tool steel or stainless steel with lapped seating surfaces.
- Piston ring and rod packing technology — sealing against hydrogen at 150–300 atm requires materials and machining tolerances that exceed typical NZ workshop capability.
- Bearing technology for crankshaft and crosshead bearings under continuous heavy load (Doc #96).
- Intercooler fabrication — tube-and-shell heat exchangers between compression stages.
- Electric motor or other prime mover of sufficient capacity (hundreds of kW to megawatts for a production-scale compressor train).
Assessment: Compressor development is arguably the single most challenging industrial prerequisite for ammonia synthesis. High-pressure hydrogen compressors represent the frontier of NZ’s mechanical engineering capability and will likely take 15–30 years to develop from current capability. The development pathway is shared with other high-pressure applications (compressed natural gas, high-pressure chemical processing, hydraulic press systems), so compressor development serves multiple needs.
3.4 Nitrogen supply
What is needed: A supply of pure nitrogen gas (>99% purity, free of oxygen) at atmospheric or low pressure, to be compressed and mixed with hydrogen for the synthesis loop.
Pathway: NZ Steel at Glenbrook already operates an air separation unit (ASU) for oxygen production (used in the Kaldo converter). ASUs produce both oxygen and nitrogen — the nitrogen is typically vented as a byproduct. If Glenbrook’s ASU continues to operate, nitrogen supply is available.29
Alternatively, nitrogen can be produced by burning carbon (charcoal, coke) in air — the combustion consumes oxygen, leaving nitrogen with some CO₂ and water vapour that can be removed by scrubbing (CO₂ with lime water) and drying. This “producer gas scrubbing” approach was used in early ammonia plants and requires no specialised equipment.30
Assessment: Nitrogen supply is the least difficult prerequisite. NZ has multiple pathways to produce nitrogen, none of which require industries that NZ lacks.
3.5 Catalyst production
What is needed: Promoted iron catalyst — magnetite fused with aluminium oxide, calcium oxide, and potassium oxide promoters.
NZ materials availability:
- Magnetite (Fe₃O₄): NZ’s ironsand is titanomagnetite — iron oxide with titanium. Standard Haber-Bosch catalysts use magnetite without titanium. Titanium in the catalyst is undesirable — it may reduce catalyst activity.31 Pure magnetite could potentially be sourced from NZ’s ironsand by magnetic separation and chemical processing to remove titanium, or from other NZ iron oxide sources (iron-stained sands, bog iron deposits). This requires process development but uses NZ-available materials.
- Aluminium oxide (Al₂O₃): Can be produced from NZ clays (kaolin) by calcination, or from NZ bauxite if any small deposits exist. Small quantities (1–3% of catalyst mass) are needed.
- Calcium oxide (CaO): From NZ limestone. Readily available.
- Potassium oxide (K₂O): From wood ash (potash). Wood ash contains 5–15% potassium carbonate, which can be calcined to potassium oxide.32 NZ has abundant wood.
Catalyst preparation process:
- Mix magnetite with promoter oxides at the correct proportions (typically 2–4% Al₂O₃, 1–2% CaO, 0.5–1% K₂O).33
- Fuse the mixture in an electric arc furnace or other high-temperature furnace at approximately 1,500–1,600°C until homogeneous.
- Cool slowly and crush to the required particle size (typically 6–10 mm granules).
- Load into the reactor and reduce (activate) under hydrogen flow at gradually increasing temperature (200–500°C over several days). This converts the iron oxide to metallic iron with a high surface area.
Assessment: Catalyst production is achievable with NZ materials and equipment. The process development is non-trivial — catalyst performance is sensitive to preparation conditions and the titanium content of NZ ironsand introduces an additional purification challenge — but it is within the capability of a competent chemical engineering team with access to NZ Steel’s facilities. Timeline: 5–15 years of development to produce a catalyst of adequate (not optimal) performance.
4. A REALISTIC TIMELINE
The following timeline assumes NZ pursues ammonia synthesis as one goal among many in a broader industrial development programme. It assumes that prerequisite industries (steelmaking, chemical industry, machine shop network) are being developed in parallel for their own reasons, and that ammonia-specific development draws on this shared industrial base.
Phase 2–3 (Years 1–7): Foundations
- NZ Steel continues operating at reduced capacity (Doc #113)
- Sulfuric acid production developed (Doc #113)
- Low-pressure hydrogen production by electrolysis for immediate applications (Doc #113)
- Machine shop network maintained and expanded (Doc #91)
- Chemical engineering expertise preserved at universities (Doc #91)
- Pressure vessel capability developed for applications up to 10–50 atm
Ammonia-specific progress: None. No ammonia-specific work is justified at this stage.
Phase 3–4 (Years 7–15): Capability building
- Medium-pressure chemical processing (50–100 atm) developed for methanol synthesis and other applications
- Compressor capability advances through industrial experience with compressed gas systems
- Alloy steel development begins at Glenbrook (if chromium and molybdenum are available through trade or local sourcing)
- Catalyst research begins — small-scale preparation and testing of iron catalysts using NZ ironsand-derived magnetite
Ammonia-specific progress: Laboratory-scale catalyst testing. Desk-level engineering design for a pilot plant.
Phase 4–5 (Years 15–30): Pilot development
- High-pressure metallurgy capability allows fabrication of small pressure vessels rated to 150–200 atm
- Compressor technology reaches the capability for hydrogen-nitrogen compression to synthesis pressure (possibly at reduced throughput)
- Pilot-scale ammonia synthesis loop constructed — a small reactor (perhaps 50–200 litres internal volume) producing kilograms of ammonia per day
- Pilot operation reveals the practical difficulties that cannot be anticipated from textbook knowledge: hydrogen leaks, catalyst deactivation, heat management, compressor seal failures, instrumentation limitations
Ammonia-specific progress: First NZ-produced ammonia, at laboratory/pilot scale. This is a milestone, not a production capability.
Phase 5–6 (Years 30–60): Scale-up
- Scaling from pilot to production: larger reactor vessels, higher-capacity compressors, continuous operation rather than batch runs
- Target production: 5–50 tonnes of ammonia per day (a small-scale plant by global standards, but sufficient for NZ’s agricultural needs)
- Integration with urea synthesis: ammonia + CO₂ at high pressure and temperature produces urea, the most transportable and farmer-friendly nitrogen fertiliser form
- NZ-produced urea distributed to farms through the fertiliser distribution network (or what remains of it)
Ammonia-specific progress: Agriculturally meaningful quantities of nitrogen fertiliser available from domestic production.
Phase 6–7 (Years 60–100+): Mature capability
- Production plant operating reliably
- Catalyst replacement cycle established
- Compressor maintenance and rebuild capability
- Second-generation plant design incorporating lessons learned
- Possible ammonia export to Pacific trade partners
Why this takes so long
The timeline is long not because any single step is beyond human capability — every step was achieved by early 20th-century engineers with technology comparable to what NZ would have in Phase 3–5 — but because the steps are sequential and each requires the output of the previous one. NZ cannot build a compressor without precision machining capability. It cannot build a reactor vessel without alloy steel. It cannot test a catalyst without a reactor vessel. It cannot run a pilot plant without compressors, vessels, and catalysts. And it cannot scale from pilot to production without years of operating experience that reveals problems not apparent on paper.
Fritz Haber demonstrated ammonia synthesis in his laboratory in 1909. BASF’s Ludwigshafen plant began commercial production in 1913. But BASF — at that time the largest chemical company in the world — already had: a mature steel industry to draw on, precision machining capability, chemical engineering expertise, existing high-pressure equipment from other processes, and the full resources of an industrialised nation. The four years from demonstration to production represented an extreme concentration of Germany’s industrial resources under commercial and then wartime pressure.34 NZ, starting from a much smaller industrial base and developing prerequisites in parallel, cannot match that pace.
5. INTERIM ALTERNATIVES
5.1 Biological nitrogen fixation (the primary strategy)
Leguminous plants — clover, lucerne (alfalfa), peas, beans, lupins, vetch — fix atmospheric nitrogen through symbiotic bacteria in root nodules. This is already NZ’s main nitrogen input for pastoral farming and must be dramatically expanded to support cropping (Doc #74).
Capabilities: NZ pastures already fix approximately 100–200 kg N/ha/year through clover.35 Legume crops (field peas, beans, lupins) can fix 100–300 kg N/ha/year, with 30–60 kg N/ha carried over to the following crop.36 Legume green manures (crops grown and ploughed in specifically for nitrogen fixation) can provide 80–150 kg N/ha to a following crop.
Limitations: Biological fixation cannot provide the intensity of nitrogen supply that synthetic fertiliser delivers. The yield gap — 30–50% for intensive cropping — is real and persistent for as long as NZ lacks synthetic nitrogen (Doc #75). Biological fixation rates may also be affected by nuclear winter conditions (reduced temperature, altered UV, possible impacts on Rhizobium activity), though this is uncertain.37
5.2 Organic nitrogen recycling
All organic waste — crop residues, animal manure, food waste, sewage — contains nitrogen that can be recycled to soil through composting, direct application, or anaerobic digestion. This nitrogen was originally fixed either biologically or synthetically, and recycling it reduces but does not eliminate the need for new fixation.
Capabilities: NZ generates substantial organic waste from livestock farming, food processing, and urban waste streams. Composting infrastructure (Doc #80) should be developed from Phase 1 onward.
Limitations: Nitrogen is lost at every step of the recycling loop — volatilisation of ammonia from manure (10–50% loss), leaching of nitrate from compost, denitrification in waterlogged soils. The recycling loop is leaky, and total nitrogen in the system declines without new fixation inputs.38
5.3 Trade-sourced ammonia or urea
If maritime trade develops with Australia (Doc #75), ammonia or urea import is a strong candidate for NZ’s trade priorities. Australia has several ammonia plants — including Incitec Pivot’s Gibson Island (Brisbane) and Yara Pilbara (Western Australia) facilities — with combined capacity exceeding 1 million tonnes of ammonia per year.39 If any of these survive and operate post-event (using Australia’s natural gas reserves), NZ could import ammonia or urea by ship.
Volume assessment: NZ’s pre-event nitrogen fertiliser imports were approximately 400,000–600,000 tonnes of product per year (urea and other forms).40 A single cargo vessel might carry 5,000–30,000 tonnes. Even a modest sail trade could deliver tens of thousands of tonnes per year — enough to make a meaningful difference to NZ’s cropping yields.
Strategic implication: NZ should pursue trade-sourced nitrogen fertiliser as a primary strategy alongside biological fixation. Domestic ammonia synthesis is the backup — necessary if trade does not materialise but not the first-choice pathway given its cost and timeline.
5.4 Alternative nitrogen fixation methods
Lightning: Natural lightning fixes approximately 3–5 kg N/ha/year globally.41 Not controllable or augmentable.
Electric arc (Birkeland-Eyde process): An electric arc through air produces nitric oxide, which can be absorbed in water to make nitric acid. This process was used commercially in Norway from 1903 to the 1930s, powered by cheap hydroelectricity — before being displaced by the more efficient Haber-Bosch process.42 The Birkeland-Eyde process is extremely energy-intensive: approximately 60–70 MWh per tonne of fixed nitrogen, versus approximately 8–12 MWh per tonne for Haber-Bosch.43 However, it requires no high-pressure equipment, no hydrogen production, and no catalyst — only an electric arc furnace and absorption towers, both of which are achievable with NZ’s existing or near-term industrial capability.
Honest assessment of Birkeland-Eyde: At 60–70 MWh per tonne of nitrogen, producing 50,000 tonnes of fixed nitrogen per year (roughly NZ’s minimum agricultural need) would consume 3,000–3,500 GWh — approximately 7–8% of NZ’s total electricity generation. This is a very large energy commitment, but NZ’s renewable grid could potentially support it, particularly if post-event electricity demand for other uses is lower than pre-event. The Birkeland-Eyde process deserves serious evaluation as a bridge technology — achievable in Phase 3–4 (years 7–15), decades before Haber-Bosch, using equipment NZ can build. The product is dilute nitric acid, which must be neutralised with lime to produce calcium nitrate fertiliser — a usable but less convenient form than urea. This pathway warrants a separate engineering assessment that is beyond the scope of this document.
6. CRITICAL UNCERTAINTIES
| Uncertainty | Impact | Resolution pathway |
|---|---|---|
| Whether Australia or another region develops ammonia production accessible to NZ via trade | If yes, NZ may never need domestic synthesis. If no, domestic production becomes a strategic necessity. | Maritime trade development (Doc #142). Cannot be resolved until trade routes are established, probably Phase 3–4. |
| NZ’s ability to produce alloy steel with chromium and molybdenum for pressure vessel applications | If NZ cannot source Cr and Mo, pressure vessel fabrication is constrained to lower pressures, which means lower ammonia conversion efficiency and smaller plant scale. | Trade for alloying elements, or identify NZ Cr sources in the Nelson ultramafic belt. Assessment needed Phase 2–3. |
| Compressor development timeline | The single largest engineering uncertainty. If high-pressure compressors prove harder to develop than estimated, the entire timeline extends. | Progressive development through increasingly high-pressure applications. No shortcut. |
| Catalyst performance with NZ-derived magnetite (titanium content) | Titanium in the catalyst may reduce activity. If purified magnetite is required, this adds a processing step. | Laboratory-scale catalyst testing, achievable Phase 3–4 with basic equipment. |
| Taranaki natural gas reserve longevity | If gas remains available, SMR is an alternative hydrogen pathway. If gas depletes, electrolysis is the only option. | Reserve assessment. Taranaki fields have been producing for decades; remaining reserves are uncertain. |
| Nuclear winter effects on biological nitrogen fixation | If reduced temperature or UV changes impair Rhizobium activity, the nitrogen gap is larger than estimated and the urgency of synthetic nitrogen increases. | Field observations during nuclear winter period. |
| Birkeland-Eyde process feasibility for NZ | If achievable, this provides a bridge nitrogen source decades before Haber-Bosch. | Engineering assessment, possibly pilot plant in Phase 3–4. |
| Energy cost of electrolytic hydrogen at scale | If NZ’s grid cannot support the electricity demand of both electrolysis for hydrogen and other recovery needs, the ammonia plant competes with other essential loads. | Grid capacity assessment (Doc #67). |
7. CROSS-REFERENCES
- Doc #8 — National Skills and Asset Census (chemical engineering skills, pressure vessel inventory)
- Doc #63 — Hydrogen: Stationary Applications (hydrogen production, shared prerequisite)
- Doc #67 — National Grid: Transpower Operations (electricity supply for electrolysis and plant operation)
- Doc #80 — Cropping Under Nuclear Winter (nitrogen demand for crops)
- Doc #80 — Soil Fertility Without Imports (nitrogen gap quantification, biological fixation)
- Doc #89 — NZ Steel Glenbrook (steel for pressure vessels, air separation unit for nitrogen, ironsand-derived magnetite for catalyst)
- Doc #91 — Machine Shop Operations (precision machining for compressors, valves, fittings)
- Doc #93 — Foundry and Casting (potential for pressure vessel component casting)
- Doc #102 — Charcoal Production (potential carbon source for nitrogen production by combustion)
- Doc #102 — Methanol from Wood (shared high-pressure chemical engineering, compressor development)
- Doc #113 — Sulfuric Acid (foundational chemical industry, shared chemical engineering capability)
- Doc #138 — Sailing Vessel Design (maritime trade for ammonia/urea import)
- Doc #138 — Trans-Tasman Relations and Trade (Australian ammonia supply as trade priority)
- Doc #157 — Trade Training (chemical engineering workforce development)
- Doc #157 — University and Research Priorities (chemical engineering education)
- Doc #160 — Heritage Skills Preservation (institutional framework for Crown-iwi partnership, kaitiakitanga principles, traditional ecological knowledge integration, §4.5–4.7)
FOOTNOTES
Erisman, J.W., Sutton, M.A., Galloway, J., Klimont, Z., and Winiwarter, W., “How a century of ammonia synthesis changed the world,” Nature Geoscience, vol. 1, pp. 636–639, 2008. https://doi.org/10.1038/ngeo325 — The widely cited estimate that approximately 50% of the nitrogen in human diets derives from the Haber-Bosch process.↩︎
NZ fertiliser import data from Stats NZ trade statistics and the Fertiliser Association of New Zealand. https://www.fertiliser.org.nz/ — NZ imports urea, diammonium phosphate (DAP), monoammonium phosphate (MAP), ammonium sulfate, and other nitrogen products. The total volume varies by year; 400,000–600,000 tonnes is a representative range for all nitrogen-containing fertiliser products.↩︎
Appl, M., “Ammonia: Principles and Industrial Practice,” Wiley-VCH, 1999. The standard industrial reference for ammonia synthesis. Also: Smil, V., “Enriching the Earth: Fritz Haber, Carl Bosch, and the Transformation of World Food Production,” MIT Press, 2001 — an accessible history and technical overview.↩︎
NZ fertiliser import data from Stats NZ trade statistics and the Fertiliser Association of New Zealand. https://www.fertiliser.org.nz/ — NZ imports urea, diammonium phosphate (DAP), monoammonium phosphate (MAP), ammonium sulfate, and other nitrogen products. The total volume varies by year; 400,000–600,000 tonnes is a representative range for all nitrogen-containing fertiliser products.↩︎
Yield reduction estimates from Doc #80, based on agronomic research on crop response to nitrogen fertilisation. The 30–50% range for intensive cropping reflects the difference between fully fertilised and unfertilised yields in NZ field trials. See: Edmeades, D.C., “The Long-Term Effects of Manures and Fertilisers on Soil Productivity and Quality: A Review,” Nutrient Cycling in Agroecosystems, 2003.↩︎
Pastoral nitrogen fixation provides approximately 50–75% of total nitrogen input for NZ grassland systems under normal conditions. The remainder comes from synthetic fertiliser (urea and DAP). For cropping, clover in rotation provides a smaller proportion of total crop nitrogen needs. Estimates based on NZ pastoral research: Ledgard, S.F. and Steele, K.W., “Biological nitrogen fixation in mixed legume/grass pastures,” Plant and Soil, 1992.↩︎
Māori agricultural systems in NZ: Leach, H.M., “1000 Years of Gardening in New Zealand,” A.H. & A.W. Reed, Wellington, 1984 — the most thorough treatment of pre-European Māori horticulture, including soil management practices, garden siting, and crop cultivation techniques. Also: Anderson, A. et al., “Tangata Whenua: An Illustrated History,” Bridget Williams Books, Wellington, 2014, Chapter 4 (agriculture and settlement). Traditional māra kai systems in the North Island developed sophisticated mounding and drainage techniques adapted to NZ soils and climate.↩︎
Australian ammonia production facilities include Incitec Pivot’s Gibson Island (Brisbane) and Phosphate Hill (Queensland) plants, Yara Pilbara (Burrup, Western Australia), and CSBP (Kwinana, Western Australia). Combined Australian ammonia production capacity exceeds 1 million tonnes per year. Sources: Incitec Pivot Ltd annual reports; Yara International corporate publications.↩︎
The nitrogen-nitrogen triple bond dissociation energy of approximately 946 kJ/mol is one of the strongest homonuclear bonds in chemistry. This bond strength is the fundamental reason that atmospheric nitrogen is biologically inert and that industrial nitrogen fixation requires extreme conditions. Standard physical chemistry reference: Atkins, P. and de Paula, J., “Physical Chemistry,” Oxford University Press, various editions.↩︎
World population at the time of Haber-Bosch commercialisation (1910s) was approximately 1.6–1.8 billion. See: Smil, V., “Enriching the Earth: Fritz Haber, Carl Bosch, and the Transformation of World Food Production,” MIT Press, 2001, pp. 155–160. Also: United Nations, “World Population Prospects,” various editions — historical estimates for 1900 (~1.6 billion) and 1920 (~1.9 billion).↩︎
Erisman, J.W., Sutton, M.A., Galloway, J., Klimont, Z., and Winiwarter, W., “How a century of ammonia synthesis changed the world,” Nature Geoscience, vol. 1, pp. 636–639, 2008. https://doi.org/10.1038/ngeo325 — The widely cited estimate that approximately 50% of the nitrogen in human diets derives from the Haber-Bosch process.↩︎
Ledgard, S.F. and Steele, K.W., “Biological nitrogen fixation in mixed legume/grass pastures,” Plant and Soil, vol. 141, pp. 137–153, 1992. Also: Ledgard, S.F., “Nitrogen cycling in low input legume-based agriculture, with emphasis on legume/grass pastures,” Plant and Soil, vol. 228, pp. 43–59, 2001. NZ pastoral research at AgResearch (formerly DSIR Grasslands) has established the 100–200 kg N/ha/year range for well-managed clover-ryegrass pastures.↩︎
Crop nitrogen requirements from standard NZ agronomic references: FAR (Foundation for Arable Research) crop guides. https://www.far.org.nz/ — Wheat: 150–250 kg N/ha for optimum yield; potatoes: 150–200 kg N/ha; brassicas: 100–200 kg N/ha depending on species and yield target.↩︎
Residual nitrogen carry-over from legume crops to following cereal or root crops: typically 30–60 kg N/ha from field peas or beans, higher (50–100 kg N/ha) from lucerne stands that have been established for multiple years. See: Peoples, M.B. and Baldock, J.A., “Nitrogen dynamics of pastures: nitrogen fixation inputs, the impact of legumes on soil nitrogen fertility, and the contributions of fixed nitrogen to Australian farming systems,” Australian Journal of Experimental Agriculture, 2001.↩︎
Ammonia uses beyond fertiliser: IFA (International Fertiliser Association), “Fertilizer Outlook 2019–2023.” The 80% figure for agricultural use is a global average; in NZ, the proportion directed to agriculture is higher because NZ has limited chemical manufacturing.↩︎
Appl, M., “Ammonia: Principles and Industrial Practice,” Wiley-VCH, 1999. The standard industrial reference for ammonia synthesis. Also: Smil, V., “Enriching the Earth: Fritz Haber, Carl Bosch, and the Transformation of World Food Production,” MIT Press, 2001 — an accessible history and technical overview.↩︎
Appl, M., “Ammonia: Principles and Industrial Practice,” Wiley-VCH, 1999. The standard industrial reference for ammonia synthesis. Also: Smil, V., “Enriching the Earth: Fritz Haber, Carl Bosch, and the Transformation of World Food Production,” MIT Press, 2001 — an accessible history and technical overview.↩︎
Haber demonstrated ammonia synthesis at laboratory scale in 1909. Carl Bosch and the BASF engineering team scaled the process to industrial production at Oppau (Ludwigshafen), Germany, with the first commercial plant operational in 1913. See: Smil, V., “Enriching the Earth” (note 3); also Stoltzenberg, D., “Fritz Haber: Chemist, Nobel Laureate, German, Jew,” Chemical Heritage Press, 2004.↩︎
Pressure vessel steels for hydrogen service: ASME Boiler and Pressure Vessel Code, Section VIII; Nelson curves for hydrogen attack limits as a function of temperature, pressure, and steel composition. Cr-Mo steels (e.g., 2.25Cr-1Mo, ASME SA-387 Grade 22) are standard for high-temperature hydrogen service because chromium and molybdenum carbides are more resistant to hydrogen attack than the iron carbide (cementite) in carbon steel. See: API Recommended Practice 941, “Steels for Hydrogen Service at Elevated Temperatures and Pressures in Petroleum Refineries and Petrochemical Plants.”↩︎
High-pressure compressor engineering for ammonia synthesis: Bloch, H.P. and Hoefner, J.J., “Reciprocating Compressors: Operation and Maintenance,” Gulf Publishing, 1996. Also: Boyce, M.P., “Centrifugal Compressors,” PennWell, 2003 (centrifugal compressors are used in modern large ammonia plants but are more complex than reciprocating types).↩︎
Ammonia synthesis catalyst preparation and composition: Appl, M., “Ammonia: Principles and Industrial Practice” (note 3), Chapter 6 (Catalysts). Also: Nielsen, A. (ed.), “Ammonia: Catalysis and Manufacture,” Springer, 1995 — the most detailed technical reference on ammonia catalyst chemistry and preparation.↩︎
Catalyst poisons in ammonia synthesis: Sulfur compounds, carbon monoxide, and water vapour are the primary poisons for iron-based Haber-Bosch catalysts. Sulfur is the most damaging — concentrations as low as 0.1 ppm can cause measurable deactivation. See: Appl, M. (note 3), Chapter 6; also Satterfield, C.N., “Heterogeneous Catalysis in Industrial Practice,” McGraw-Hill, 1991.↩︎
Early ammonia plant instrumentation was entirely pneumatic and mechanical — pneumatic 3–15 psi controllers (e.g., Foxboro, Taylor, Honeywell brands), thermocouples with galvanometer readouts, bourdon-tube pressure gauges, manual valves with position indicators. Electronic instrumentation was introduced from the 1960s onward but is not essential to plant operation. See: Liptak, B.G. (ed.), “Instrument Engineers’ Handbook: Process Control,” CRC Press — includes historical discussion of pre-electronic process control.↩︎
NZ chromium and molybdenum resources: NZ has no known commercially significant deposits of either element. Small chromite occurrences exist in the Nelson-Marlborough ultramafic belt (Dun Mountain ophiolite complex), but these have never been mined commercially and their extent is uncertain. Molybdenum is not known to occur in NZ in any significant quantity. See: GNS Science mineral occurrence databases; Crown Minerals NZ. https://www.nzpam.govt.nz/↩︎
The Dun Mountain ophiolite complex (Nelson-Marlborough, South Island) contains ultramafic rocks including small chromite occurrences. The extent and grade of these occurrences is not well characterised — historical prospecting found small veins and disseminated chromite, but no deposits of commercial interest under normal economic conditions. Under recovery conditions, even small deposits may be worth investigating. See: GNS Science; Coombs, D.S. et al., “The Dun Mountain ophiolite belt, New Zealand, its tectonic setting, constitution, and origin,” Geological Society of America Memoir, 1976.↩︎
Appl, M., “Ammonia: Principles and Industrial Practice,” Wiley-VCH, 1999. The standard industrial reference for ammonia synthesis. Also: Smil, V., “Enriching the Earth: Fritz Haber, Carl Bosch, and the Transformation of World Food Production,” MIT Press, 2001 — an accessible history and technical overview.↩︎
Alkaline water electrolysis: well-established technology dating to the late 19th century. Industrial electrolysers have used mild steel or nickel electrodes in 25–30% KOH electrolyte with asbestos diaphragms. Modern designs use polymer membranes and improved electrode coatings, but the basic technology is achievable with NZ materials. See: Zeng, K. and Zhang, D., “Recent progress in alkaline water electrolysis for hydrogen generation and applications,” Progress in Energy and Combustion Science, 2010.↩︎
Energy consumption for alkaline water electrolysis: approximately 50–55 kWh per kg of hydrogen at atmospheric pressure. This includes electrical and thermal losses. More efficient designs (PEM electrolysis, high-temperature electrolysis) exist but require materials and technology beyond NZ’s near-term capability. See: Zeng and Zhang (note 20); also IEA, “The Future of Hydrogen,” 2019.↩︎
NZ Steel’s air separation unit (ASU) at Glenbrook produces oxygen for the Kaldo converter and nitrogen as a byproduct. ASU technology is well-established — liquefaction and distillation of air to separate oxygen and nitrogen. See Doc #51 for ASU details and maintenance concerns.↩︎
Nitrogen from combustion: burning carbon in air consumes oxygen and leaves nitrogen (approximately 79% of air by volume). The resulting gas contains CO₂ (from combustion), nitrogen, and trace noble gases. CO₂ is removed by passing through a lime water (calcium hydroxide) scrubber, which reacts with CO₂ to form calcium carbonate. Water vapour is removed by drying agents (calcium chloride, silica gel) or condensation. This was the standard nitrogen production method before cryogenic air separation became available. See: Cottrell, F.G., early 20th-century chemical engineering references.↩︎
Ammonia synthesis catalyst preparation and composition: Appl, M., “Ammonia: Principles and Industrial Practice” (note 3), Chapter 6 (Catalysts). Also: Nielsen, A. (ed.), “Ammonia: Catalysis and Manufacture,” Springer, 1995 — the most detailed technical reference on ammonia catalyst chemistry and preparation.↩︎
Wood ash as potassium source: NZ wood ash (primarily from radiata pine) contains approximately 5–15% potassium as potassium carbonate (K₂CO₃), depending on species and combustion conditions. Potassium carbonate can be calcined to potassium oxide (K₂O) for use as a catalyst promoter. The quantities needed for catalyst production are small — kilograms to tens of kilograms — well within what wood ash can supply. See: Etiegni, L. and Campbell, A.G., “Physical and chemical characteristics of wood ash,” Bioresource Technology, 1991.↩︎
Ammonia synthesis catalyst preparation and composition: Appl, M., “Ammonia: Principles and Industrial Practice” (note 3), Chapter 6 (Catalysts). Also: Nielsen, A. (ed.), “Ammonia: Catalysis and Manufacture,” Springer, 1995 — the most detailed technical reference on ammonia catalyst chemistry and preparation.↩︎
Haber demonstrated ammonia synthesis at laboratory scale in 1909. Carl Bosch and the BASF engineering team scaled the process to industrial production at Oppau (Ludwigshafen), Germany, with the first commercial plant operational in 1913. See: Smil, V., “Enriching the Earth” (note 3); also Stoltzenberg, D., “Fritz Haber: Chemist, Nobel Laureate, German, Jew,” Chemical Heritage Press, 2004.↩︎
Ledgard, S.F. and Steele, K.W., “Biological nitrogen fixation in mixed legume/grass pastures,” Plant and Soil, vol. 141, pp. 137–153, 1992. Also: Ledgard, S.F., “Nitrogen cycling in low input legume-based agriculture, with emphasis on legume/grass pastures,” Plant and Soil, vol. 228, pp. 43–59, 2001. NZ pastoral research at AgResearch (formerly DSIR Grasslands) has established the 100–200 kg N/ha/year range for well-managed clover-ryegrass pastures.↩︎
Residual nitrogen carry-over from legume crops to following cereal or root crops: typically 30–60 kg N/ha from field peas or beans, higher (50–100 kg N/ha) from lucerne stands that have been established for multiple years. See: Peoples, M.B. and Baldock, J.A., “Nitrogen dynamics of pastures: nitrogen fixation inputs, the impact of legumes on soil nitrogen fertility, and the contributions of fixed nitrogen to Australian farming systems,” Australian Journal of Experimental Agriculture, 2001.↩︎
The effect of nuclear winter conditions on biological nitrogen fixation is uncertain. Rhizobium activity is temperature-sensitive, with reduced fixation rates below approximately 10°C. Nuclear winter cooling of 5–15°C could significantly reduce clover nitrogen fixation rates, particularly in the South Island. UV changes (ozone depletion followed by recovery) may also affect soil microbiology. No specific research exists on nitrogen fixation under nuclear winter conditions. This is a critical agricultural uncertainty. See: Hungria, M. and Vargas, M.A.T., “Environmental factors affecting N₂ fixation in grain legumes in the tropics, with an emphasis on Brazil,” Field Crops Research, 2000 (temperature effects on fixation).↩︎
Nitrogen losses in the recycling loop: ammonia volatilisation from manure (10–50% of nitrogen, depending on handling), nitrate leaching from soil (variable, 5–30% in NZ pastoral soils), denitrification (conversion of nitrate to N₂ gas by soil bacteria under waterlogged conditions, 5–20% of soil nitrogen). Total losses from manure application to crop uptake are typically 40–70% of the applied nitrogen. See: Cameron, K.C. et al., “Nitrogen losses from the soil/plant system: a review,” Annals of Applied Biology, 2013.↩︎
Australian ammonia production facilities include Incitec Pivot’s Gibson Island (Brisbane) and Phosphate Hill (Queensland) plants, Yara Pilbara (Burrup, Western Australia), and CSBP (Kwinana, Western Australia). Combined Australian ammonia production capacity exceeds 1 million tonnes per year. Sources: Incitec Pivot Ltd annual reports; Yara International corporate publications.↩︎
NZ fertiliser import data from Stats NZ trade statistics and the Fertiliser Association of New Zealand. https://www.fertiliser.org.nz/ — NZ imports urea, diammonium phosphate (DAP), monoammonium phosphate (MAP), ammonium sulfate, and other nitrogen products. The total volume varies by year; 400,000–600,000 tonnes is a representative range for all nitrogen-containing fertiliser products.↩︎
Natural nitrogen fixation by lightning: approximately 3–5 kg N/ha/year globally, or approximately 5–8 Tg N/year total. This is a small fraction of biological fixation (~140 Tg N/year) or industrial fixation (~150 Tg N/year). See: Galloway, J.N. et al., “Nitrogen cycles: past, present, and future,” Biogeochemistry, 2004.↩︎
The Birkeland-Eyde process: developed by Kristian Birkeland and Sam Eyde in Norway, 1903. Used an electric arc to fix atmospheric nitrogen as nitric oxide (NO), which was then absorbed in water to produce nitric acid. Three plants operated in Norway using cheap hydroelectricity (Notodden, Rjukan, Glomfjord). Energy consumption was approximately 60–70 MWh per tonne of fixed nitrogen — approximately 6–7 times more energy-intensive than the Haber-Bosch process per unit of nitrogen. The process was economically displaced by Haber-Bosch in the 1920s–1930s but the technology itself is simple: an electric arc furnace, air intake, and acid absorption towers. See: Smil, V., “Enriching the Earth” (note 3); also Birkeland, K. and Eyde, S., original patents and Norwegian industrial history publications.↩︎
The Birkeland-Eyde process: developed by Kristian Birkeland and Sam Eyde in Norway, 1903. Used an electric arc to fix atmospheric nitrogen as nitric oxide (NO), which was then absorbed in water to produce nitric acid. Three plants operated in Norway using cheap hydroelectricity (Notodden, Rjukan, Glomfjord). Energy consumption was approximately 60–70 MWh per tonne of fixed nitrogen — approximately 6–7 times more energy-intensive than the Haber-Bosch process per unit of nitrogen. The process was economically displaced by Haber-Bosch in the 1920s–1930s but the technology itself is simple: an electric arc furnace, air intake, and acid absorption towers. See: Smil, V., “Enriching the Earth” (note 3); also Birkeland, K. and Eyde, S., original patents and Norwegian industrial history publications.↩︎