Skip to content
Material World
Material · Engineered

Mineral wool

Rock or slag spun into fibres like candy floss — insulation that does not burn, in a market where most of the alternatives do.

Mineral wool is molten rock — basalt, dolomite, or blast furnace slag — spun or blown into fine fibres and bound into a mat. Like every bulk insulation it works by trapping air in spaces too small for convection to get going, and its thermal conductivity is consequently within a factor of two of glass wool, polyurethane foam and expanded polystyrene.

What distinguishes it is what happens in a fire. It is rock, so it does not burn, does not contribute fuel, and does not produce smoke — and the high-temperature grades hold together well above 1000 °C. Every organic foam insulation burns, and the flame retardants added to slow that down have their own history.

After the Grenfell Tower fire in 2017, regulation in several countries restricted combustible insulation on tall buildings regardless of its thermal performance, and mineral wool is the material that answer points to.

Processing

Rock is melted at around 1500 °C and the stream is thrown onto spinning wheels, which fling droplets that draw out into fibres as they fly — the same principle as candy floss, at ten times the temperature. A binder is sprayed on and cured, and the mat is cut into batts, rolls or boards.

Slag wool uses blast furnace slag instead of quarried rock, which is a genuine use for a large industrial by-product.

Uses

Building insulation in walls, roofs and floors. Acoustic insulation and studio treatment, where the same fibrous structure absorbs sound. Fire stopping and protection of structural steel. Industrial and marine pipe and vessel insulation. And, in a completely different application, as a hydroponic growing medium.

History

Observed in nature first: fibres form naturally around Hawaiian volcanoes and are called Pele's hair. Industrial production dates from the 1870s in Wales and the United States, and the material became a mass building product after the Second World War as insulation standards rose.

Environmental impact

Energy intensive to make — melting rock is not cheap — and it repays that many times over in a heated building, which is the clearest case of embodied energy being the wrong thing to optimise in isolation.

The health question has been examined thoroughly and the answer is reassuring in a specific way. Early concern arose by analogy with asbestos, since both are mineral fibres. The distinguishing property is biopersistence: asbestos fibres are durable and stay in lung tissue for decades, and modern mineral wool fibres dissolve in lung fluid within weeks. The International Agency for Research on Cancer moved glass and rock wool out of its possible-carcinogen category in 2001 on that basis. The fibres are still a mechanical irritant to skin and airways, and handling precautions are about that.

Medium confidence Weak evidence

How we know: checked recently · only one source, so there is nothing to cross-check it against · stated directly by the source.

How this connects

Where a connection has been confirmed by an outside reference, that reference is named beside it.

contains

  • Silicon element · as silicate, from the basalt or slag it was spun from
  • Iron element · from the rock, and the reason a slag wool exists at all

is sourced from

  • Basalt rock · melted at around 1500 °C and flung into fibres by spinning wheels

is used as

  • Thermal insulation application · and it does not burn, which after 2017 is the property regulation cares about most on a tall building
  • Flame retardancy application · it is rock: it contributes no fuel and produces no smoke, where every organic foam does both

is used in

  • Construction industry · insulation, fire stopping and the protection of structural steel

is an alternative to

  • Polyurethane material · as insulation: comparable per unit thickness, and it does not burn — which after 2017 is what decides it on a tall building
  • Polystyrene material · polystyrene is cheaper per unit of thermal resistance and combustible, and that trade is now largely made by regulation rather than by a designer

is commonly confused with

  • Asbestos material · both mineral fibres, and the distinguishing property is biopersistence: asbestos stays in lung tissue for decades and mineral wool fibres dissolve in weeks

is produced by

  • Glass melting process · spun off a rotating dish so the melt is thrown out as fibres — the same principle as candyfloss, at 1,400 °C

Sources

  • Material World
    Our own writing
  • Wikimedia Foundation · Creative Commons CC0 1.0 Universal (public domain dedication)

Questions this page answers

Where it comes from, and what it becomes

Follow Mineral wool back to what it starts as, and forward into what it becomes. Each step is a documented one — a real route material takes, not a chain of inference.

Upstream — what it comes from

  • Mineral wool → is produced by (spun off a rotating dish so the melt is thrown out as fibres — the same principle as candyfloss, at 1,400 °C) → Glass melting → takes as input (as the stabiliser, and without it a soda-silica glass would slowly dissolve in water) → Limestone → is sourced from (precipitated from it, mostly by organisms building shells and skeletons out of dissolved calcium and carbonate) → Seawater → is composed of (about 96.5 per cent by mass — seawater is 3.5 per cent dissolved solids and the rest of it is this) → Water
  • Mineral wool → is sourced from (melted at around 1500 °C and flung into fibres by spinning wheels) → Basalt → is sourced from (partial melting of mantle peridotite is what basalt magma is — the residue left behind stays peridotite, depleted of what went into the melt) → Peridotite → is composed of (the mineral that defines the rock and gives it its name — a peridotite is olivine-dominant by definition) → Olivine
  • Mineral wool → is produced by (spun off a rotating dish so the melt is thrown out as fibres — the same principle as candyfloss, at 1,400 °C) → Glass melting → takes as input (the largest ingredient by mass, and it must be low in iron because iron colours glass green) → Sand → is sourced from (the ultimate source of most of it — granite weathers, the feldspar becomes clay and washes out, and the quartz survives as grains) → Granite → is composed of (by volume, alongside feldspar and lesser mica) → Quartz
  • Mineral wool → is sourced from (melted at around 1500 °C and flung into fibres by spinning wheels) → Basalt → is composed of (an early-crystallising constituent of basaltic magma) → Olivine
  • Mineral wool → is sourced from (melted at around 1500 °C and flung into fibres by spinning wheels) → Basalt → is composed of (calcium-rich plagioclase is a defining constituent of basalt) → Plagioclase
  • Mineral wool → is sourced from (melted at around 1500 °C and flung into fibres by spinning wheels) → Basalt → is composed of (carried up as xenocrysts in alkali basalt and recovered from the gravels the basalt weathers into, rather than mined from the rock itself) → Sapphire

These are the most distinct paths back. Mineral wool can be traced through others besides.

Downstream — what it becomes