Material Research
Lime & Natural Plaster
Lime cycle from limestone to finish coat — the living chemistry of traditional plaster
Natural lime plaster has been applied to adobe, rammed earth, stone, and brick buildings for thousands of years — protecting earthen structures from water damage and producing interior surfaces of remarkable breath-ability, beauty, and durability. Unlike Portland cement plaster, lime plaster is a living material: it absorbs and releases moisture, continues to carbonate for years after application, and can be recycled.
The Lime Cycle
From The Material Way 2025 workshop notes:
- Limestone (석회석): Calcium carbonate (CaCO₃) — the raw material, mined from geological deposits
- Quick lime / burnt lime (생석회): Heat limestone to 900°C+ → calcium oxide (CaO) + CO₂ released. Highly reactive — exothermic, dangerous.
- Hydrated lime / slaked lime (소석회): Add water to quick lime → calcium hydroxide Ca(OH)₂. The hydration reaction produces significant heat (up to 300°C). This is the working form of lime for plaster.
- Lime putty: Excess water added to slaked lime → smooth paste that can be aged (pitted) for months or years. Older lime putty (aged 5–10+ years) produces finer, more workable plaster.
- Carbonation (hardening): Applied lime plaster absorbs CO₂ from the air and slowly reverts to calcium carbonate — essentially returning to limestone. This is why lime plaster "breathes" and continues to harden for years after application. The cycle is complete.
Natural Plaster Components
- Binder: Lime putty or hydraulic lime (NHL — natural hydraulic lime, sets faster in wet conditions)
- Aggregate: Sand — controls shrinkage and adds body. The particle size and type of sand determines the plaster's texture. Traditional adobe finish plasters use very fine-grained local sand.
- Fiber reinforcement: Animal hair (horsehair, goat hair) in the base coat — prevents cracking during drying. Same principle as organic fiber in adobe brick.
- Clay: Small amounts of clay can be added for working consistency and to improve adhesion to earthen substrates (clay-on-clay principle).
Plaster Layers
- Scratch coat: Coarsest mix, applied directly to substrate. Scratched with a comb tool to provide mechanical key for the next layer.
- Brown coat: Medium texture. Brings wall to flat. Applied when scratch coat has set but not fully cured.
- Finish coat: Finest mix. May be left as natural white, pigmented with earth pigments, or polished (marmorino technique).
Quartz / Silica
Quartz (SiO₂, silicon dioxide) is the primary mineral in most sands used for plaster aggregates. Pure quartz sand gives a very white, hard finish. Mixed with lime (calcium hydroxide), quartz can participate in a pozzolanic reaction (at elevated temperatures) — producing calcium silicate hydrates that add strength. Historical Roman concrete used volcanic pozzolans (silica-rich ash) for this reason.
Adobe Plaster Connection
In New Mexico and traditional adobe building, the earthen wall is plastered with successive layers of natural plaster — often combining clay-based earthen plasters (for interior) and lime plaster (for exterior weathering protection). The plastered surface is what gives traditional New Mexico adobe buildings their smooth, rounded appearance — the structural adobe brick beneath is hidden by plaster layers built up over decades.
Jay's Studio Note
The lime cycle is the slowest alchemy in this material library — limestone becoming plaster becoming stone again over years and decades. Working with lime plaster means working with a material that is still becoming. The surface applied today will be harder in five years, harder still in ten. In this way, lime plaster is the exact opposite of bioplastic: one material approaches permanence; the other approaches compost.
Related Materials
Related Materials
Rammed Earth
Compressed earth wall construction — 5cm layers, minimum binder, dense and water-resistant
Adobe — Sun-Dried Earthen Brick Building
How to make adobe bricks from clay, sand, and straw — one of the world's oldest building materials, still in use across arid climates from the Middle East to the American Southwest.
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