Sulfuric Acid In Titanium Dioxide Production Sulfate Route Demand
Sulfuric Acid in Titanium Dioxide Production: Sulfate Route Demand is concentrated in the digestion section, where technical-grade H2SO4 functions as a decomposition reagent for ilmenite and sulfated titania slag. The sulfate route consumes fresh sulfuric acid mainly through iron oxide reactions, weak-acid bleed, washing losses, and neutralization of purge streams. Industrial consumption ranges from 2.5 t to 4.0 t H2SO4 per tonne of finished TiO2 for rock ilmenite, and from 1.6 t to 2.2 t per tonne when sulfate slag is the titanium source.
In digestion, technical-grade sulfuric acid at 85–92 wt% is preheated to 60–80 °C and charged into brick-lined reactors. Direct steam injection raises the reaction mass to 150–200 °C. Ilmenite decomposes according to FeTiO3 + 2H2SO4 → TiOSO4 + FeSO4 + 2H2O. The acid-to-ore mass ratio is maintained between 1.5:1 and 1.8:1 in ilmenite operations; lower ratios depress titanium extraction, while higher ratios increase free acid load in hydrolysis.
Global sulfate-route demand for sulfuric acid is tied to ilmenite and slag supply decisions. Published capacity estimates place the sulfate route at approximately 40% of global TiO2 capacity, with the remainder using the chloride route. Because each sulfate-route tonne of pigment consumes 1.6–4.0 t H2SO4, regional shifts from chloride to sulfate-route capacity directly alter merchant acid balances and storage logistics.
Sulfate-route demand for acid is also linked to anatase production. The chloride route predominantly yields rutile, whereas the sulfate route can produce both anatase and rutile. Anatase is required in certain pigment, catalyst, and low-hardness applications, and its production via sulfate route keeps sulfuric acid demand structurally stable even when chloride-route rutile capacity expands.
What Controls Specific Acid Consumption in Ilmenite Digestion?
Specific acid consumption is controlled mainly by the FeO content of the feedstock. Iron in the ilmenite lattice consumes acid stoichiometrically rather than catalytically. Each tonne of FeO reacts with 1.365 t H2SO4 to form FeSO4, while each tonne of Fe2O3 reacts with 1.843 t H2SO4 to form Fe2(SO4)3. For a rock ilmenite containing 35 wt% FeO and 45 wt% TiO2, the theoretical iron-related acid demand is approximately 0.478 t H2SO4 per tonne of ore, equivalent to 1.06 t H2SO4 per tonne of contained TiO2. This stoichiometric base is amplified by free acid retained in filter cake, acid mist loss, and purge neutralization.
Carbonate gangue also consumes acid. Calcite in the ore reacts with H2SO4 to form calcium sulfate, consuming 0.98 t H2SO4 per tonne CaCO3. This gangue-related demand is frequently underestimated in acid-sourcing models because ore blends change between shipments. Batch-to-batch variance in acid demand can be observed when the carbonate content of the feed shifts by a few percentage points.
| Parameter | Rock ilmenite | Sulfate slag |
|---|---|---|
| TiO2 content | 45–50 wt% | 70–78 wt% |
| FeO content | 30–40 wt% | 8–14 wt% |
| Acid-to-ore mass ratio | 1.5:1–1.8:1 | 1.2:1–1.5:1 |
| Fresh H2SO4 demand | 2.8–4.0 t/t TiO2 | 1.6–2.2 t/t TiO2 |
| Digestion temperature | 150–180 °C | 160–200 °C |
| By-product load | High FeSO4·7H2O crystallization | Reduced iron sulfate bleed |
Because hydrolysis produces weak acid, purchased acid demand is not equal to fresh acid demand. Clarified titanyl sulfate liquor at 180–230 g/L TiO2 equivalent is hydrolyzed at 95–110 °C after seeding. The filtered weak acid contains 18–25 wt% H2SO4 and is returned to digestion after clarification. Recycle efficiency is bounded by impurity buildup, especially magnesium, aluminum, and colored transition metals. A continuous liquor bleed is required. Weak-acid return can reduce fresh 96 wt% acid consumption by 20–30% in operations designed for high water recovery, although published data for specific plants is limited by proprietary water balance.
Water balance governs the lower limit of acid concentration in recycle. Hydrolysis requires controlled dilution of titanyl sulfate liquor; if recycled acid concentration falls below 18 wt%, evaporation load increases and the titanium hydrolysis rate can shift. Conversely, recycle above 25 wt% may increase liquor viscosity and salt precipitation in transfer lines. These boundaries are operational, not thermodynamic phase limits, and are managed by controlling steam addition and evaporator duty.
When Sulfate Slag Replaces Rock Ilmenite, Fresh Acid Demand Declines
Switching from rock ilmenite to sulfate slag changes the consumption profile because slag contains 8–14 wt% FeO rather than 30–40 wt% FeO. The acid-to-ore ratio in slag-based digestion is typically reduced to 1.2:1–1.5:1, and fresh acid demand falls to 1.6–2.2 t H2SO4 per tonne TiO2. Lower iron content reduces self-heating from iron sulfate formation, so the digestion batch requires more direct steam to hold 160–200 °C. The sulfate-route demand therefore shifts from acid volume toward energy and water balance.
Ferrous sulfate heptahydrate crystallization is the main acid-retaining by-product. In ilmenite-based operations, clarified liquor is cooled in forced-circulation crystallizers to below 15 °C to precipitate FeSO4·7H2O. Interstitial acid in the crystal cake must be washed, and washing losses add to total H2SO4 demand. Slag-based operations generate less ferrous sulfate, which reduces crystallizer throughput but removes a natural acid sink from the recovery loop.
Digestion vessels in sulfate-route plants are typically brick-lined carbon steel with acid-resistant mortar, while weak-acid recycle lines use rubber-lined steel or high-density polyethylene. Agitator shafts and impellers are specified from alloys resistant to dilute boiling sulfuric acid and abrasive ore solids. Manual charging lines have shown acid-to-ore ratio variance of ±0.05 t/t; automated weigh hoppers and mass-flow acid totalizers reduce this variance. Digestion blow tanks and air sparges control foam generated by carbonate minerals, and off-gas scrubbers remove acid mist before atmospheric discharge.
Acid Quality and Handling Standards for Sulfate-Route Procurement
| Standard or code | Application |
|---|---|
| ASTM E223-23e1 | Test methods for total acidity, nonvolatile matter, and reducing substances in sulfuric acid |
| ISO 910:1977 | Titrimetric determination of total acidity for industrial sulfuric acid and oleum |
| UN 1830 | Transport classification for sulfuric acid |
Acid purity constraints for sulfate-route titanium dioxide are set by corrosion and pigment brightness rather than digestion yield alone. Iron in purchased acid adds to the sulfate load, but its concentration is normally small relative to iron in the ore. Chloride, nitrate, and organic impurities can affect heat exchanger corrosion and off-gas composition. Published threshold values vary by plant metallurgy and emission permit, so qualification programs rely on corrosion coupon testing and full acid assay rather than single-element limits. Fresh makeup acid is commonly specified at ≥96.0 wt% H2SO4, with lower-strength streams used only as recycle.
Storage and unloading systems for sulfate-route acid demand are designed around the corrosive and hygroscopic properties of concentrated H2SO4. Dilution is performed by adding acid to water, never water to acid, to avoid localized boiling at the interface. Bulk tanks are vented through scrubbers or drying media because sulfuric acid absorbs atmospheric moisture, which reduces strength and increases corrosion risk. The material is incompatible with reducing agents, chlorates, carbides, and alkaline materials; segregation under UN 1830 and local fire codes is mandatory in tank farms serving TiO2 plants.