Clay-Based Lithium

Clay-based lithium refers to lithium contained within fine-grained clay minerals such as smectite, hectorite, and illite. Unlike hard-rock lithium ores or brine resources, lithium in clay deposits is adsorbed or structurally bound within layered clay lattices.

These deposits typically form through volcanic ash alteration, sedimentation, and hydrothermal processes over geological time. Clay-based lithium is increasingly regarded as a strategic resource due to its vast global reserves and importance in supporting future battery-grade lithium demand.

Lithium-Bearing Clay Minerals & Occurrence

Common Lithium-Bearing Clays:
• Hectorite – smectite clay with lithium incorporated into its structure
• Montmorillonite & illite – lithium substitutes within layered phyllosilicates

Occurrence:
• Formed through volcanic alteration, weathering, and sedimentation
• Major deposits in Nevada (USA), China, and other volcanic basins

Composition & Physical Characteristics

Lithium-bearing clays are lithium-rich silicates where Li⁺ ions occupy exchangeable or structural positions within layered matrices.

ComponentTypical Range
Li₂O~0.3 – 0.75% (varies widely)
SiO₂ / Al₂O₃Primary clay framework
Fe₂O₃, MgO, K₂OMinor constituents

Physical Traits

PropertyDescription
StructureLayered phyllosilicate (2:1 sheet structure)
DensityLower than hard rock ores
Mechanical BehaviorSoft, plastic, clay-like
Particle FormFine-grained, swells or disperses in water

Traditional mechanical strength properties are not applicable, as behavior is governed by particle size, plasticity, and swelling.

Strengthening & Metallurgical Behavior

Structural Features:
• Layered silicate sheets with interlayer spaces hosting lithium ions and water

Metallurgical Interaction:
• Lithium release depends on chemical accessibility rather than crushing
• Ion exchange: Li⁺ replaced by H⁺ or Fe³⁺ during leaching
• Thermal activation expands interlayers and disrupts bonds

Strengthening behavior is irrelevant; the focus is unlocking lithium from the clay lattice.

Refining & Processing Methods

Calcination + Acid Leaching:
• Roasting at ~500–600 °C to activate clay
• Sulfuric or oxalic acid leaching releases Li⁺
• Recovery can exceed ~90%

Ion-Exchange Leaching:
• Ferric or other salts replace lithium ions
• Reduced acid consumption

Mechanical Activation + Leaching:
• Intensive milling creates defects and exposes lithium sites
• Demonstrated recoveries ~90%+

Emerging Methods:
• Electrodialysis and electrochemical separation
• Lower reagent use and environmental footprint

Industrial Lithium Products from Clays

ProductUse
Lithium chloride (LiCl)Intermediate chemical
Lithium carbonate (Li₂CO₃)Battery-grade material
Lithium hydroxide (LiOH)EV battery cathodes
Technical-grade saltsCeramics, greases, specialty uses

Applications

CategoryUses
Energy StorageEV batteries, grid storage, electronics
IndustrialCeramics, glass, lubricants
SpecialtyPharmaceuticals, air treatment

Advantages of Clay-Based Lithium

✔ Extremely large global resource base
✔ Diversifies lithium supply beyond brines and hard rock
✔ Multiple extraction technology options
✔ Potential for lower environmental impact using advanced methods
✔ Feeds directly into standard lithium chemical supply chains

Challenges & Considerations

⚠ Lower lithium grades than brines or spodumene
⚠ Complex layered chemistry requires activation
⚠ Traditional acid leaching must be carefully managed
⚠ Economics depend on extraction efficiency and scale

Why Choose Clay-Based Lithium

Clay-based lithium is strategically important for the future of the global energy transition. As demand for electric vehicles and energy storage accelerates, clay deposits provide a scalable, geographically diverse lithium source. Continued technological innovation is rapidly improving extraction efficiency and sustainability, positioning clay-based lithium as a critical contributor to long-term supply security.