Battery graphite is the market that reached the news cycle first. It is not the only market for graphite. The second market is older, quieter, and defined by very different physics. The two share a name and almost nothing else.
The market you hear about
When lithium-ion batteries scaled, first through consumer electronics and then through electric vehicles, the anode side of the cell became a graphite story. Natural flake graphite is crushed, spheronized, coated, and in some cases blended with synthetic graphite to make anode active material. Depending on chemistry, a typical EV battery contains 50 to 100 kg of graphite anode material.
Anode-grade natural flake is generally sourced from concentrates with purity in the mid-to-high 90s (%Cg). The industry-standard purification step has been chemical: caustic bake followed by hydrofluoric acid, a multi-step process that removes silicate impurities to reach 99.95% purity or higher. Battery graphite is a commodity market with public price benchmarks from Fastmarkets, Argus, and Benchmark Mineral Intelligence.
The market you don't hear about
There is an older market for specialty graphite products that predates lithium-ion batteries by decades. Participants include nuclear industry suppliers, defence contractors, semiconductor equipment manufacturers, and refractory producers serving steel, aluminium, and specialty metals. Purity requirements are dramatically higher than for anode. Prices are dramatically higher too. The market is not benchmarked publicly. It clears through direct contracting, small tender rounds, and specification-driven qualification.
What decides which market you are in
Two properties of the source rock. First, crystallinity: well-formed, large, well-ordered graphite crystals are essential for the technical-ceramic market. Nuclear and defence buyers need graphite that behaves predictably under thermal and neutronic stress; that behaviour is set at the crystal scale. Second, purity ceiling: different deposits have different theoretical purity ceilings depending on how impurities sit inside the source ore. Geology strongly influences potential product pathways, while downstream processing and qualification determine whether commercial specifications can ultimately be achieved.
A useful rule of thumb. Anode graphite generally requires a 95%-plus concentrate purified to 99.95%. Nuclear-grade graphite requires a starting concentrate that can be purified to 5N (99.999%) and beyond, with specific limits on boron, sulphur, iron, and other neutron-absorbing impurities. Semiconductor-grade goes further still, into the 5N to 6N (99.999 to 99.9999%) territory with total metallics measured in ppb for the most demanding applications.
Albany's rock
Albany is hosted within a rare intrusion-related breccia-pipe vent system in northern Ontario. Unlike conventional flake graphite deposits, which typically originate from metamorphosed carbonaceous sediments, Albany is believed to have formed from carbon-rich fluids released during the degassing of an ascending magma. This distinct geological setting produced small graphite crystallites, with impurities concentrated primarily at crystal boundaries and surfaces rather than within the crystal lattice, a characteristic that may support efficient thermal purification.
That geological difference is what places Albany, in principle, in the second market rather than the first. Whether the potential is realised is a matter of processing route and qualification, which Chapters 2 through 4 address.