Introduction
Rock wool, also known as mineral wool or stone wool, is a highly efficient and versatile
insulation material made from volcanic rock, primarily basalt and diabase. It is widely used in
construction and industrial applications for its excellent thermal, acoustic, and fire-resistant
properties. As one of the most advanced and sustainable insulating materials available today,
rock wool plays a crucial role in improving building performance and energy efficiency.
The origins of rock wool date back to the early 20th century when researchers discovered a
method to melt volcanic rock and spin it into fibers. The process mimics a natural phenomenon
where volcanic eruptions produce fibrous ash when lava interacts with cool air or moisture.
Today, modern manufacturing methods use high-temperature furnaces to melt raw materials,
which are then spun into fine, interwoven fibers resembling wool.
The primary raw material for rock wool is basalt, a dense and hard volcanic rock. Other
materials like dolomite and recycled slag may also be included. These components are heated to
temperatures exceeding 1,500°C (2,732°F) until they melt into a lava-like consistency. This
molten rock is then rapidly spun and cooled to form thin, wool-like fibers. The resulting product
is lightweight, yet robust, with a complex, open structure that traps air and resists heat transfer.
One of the defining characteristics of rock wool is its outstanding thermal insulation. Its fibrous
structure creates countless tiny air pockets, which significantly reduce heat conduction. This
makes it an ideal material for insulating buildings, helping to maintain comfortable indoor
temperatures and reduce energy consumption for heating and cooling.
In addition to thermal performance, rock wool excels in sound insulation. Its dense, irregular
structure absorbs sound waves, reducing noise transmission between rooms and from external
sources. As a result, it is commonly used in offices, studios, homes, and industrial facilities to
improve acoustic comfort.
Another vital property of rock wool is its fire resistance. Because it is made from non-
combustible stone, rock wool can withstand temperatures above 1,000°C without melting or
releasing toxic fumes. This makes it a preferred material in fireproofing applications, especially
in high-rise buildings, tunnels, and industrial complexes where safety is paramount.
Rock wool is also resistant to moisture, mold, and mildew. Unlike organic materials, it does not
rot or decay when exposed to humidity. This ensures long-term performance and durability,
especially in damp or humid environments. It also contributes to healthier indoor air quality, as
it does not support microbial growth.
Environmentally, rock wool is considered a sustainable insulation choice. It is made from
abundant natural resources and often includes recycled industrial waste, such as slag.
Furthermore, rock wool insulation can significantly reduce energy use in buildings, thereby
cutting carbon emissions over the lifespan of a structure. It is also recyclable at the end of its
use.
The installation of rock wool is relatively straightforward. It is available in various forms, such
as batts, boards, rolls, and loose-fill. These products are easy to cut and fit between studs, joists,
and rafters in walls, roofs, and floors. Some variants are also faced with foil or other membranes
for specific vapor or thermal control requirements.
Compared to other insulation materials, such as fiberglass, polyurethane foam, and polystyrene,
rock wool offers superior fire resistance and sound insulation. While it may be heavier and
slightly more expensive, its durability and multi-functional performance often justify the
investment.
In industrial settings, rock wool is used for insulating pipes, boilers, storage tanks, and process
equipment. Its ability to maintain thermal performance at high temperatures makes it ideal for
power plants, chemical factories, and refineries.
In horticulture, a specialized form of rock wool is used as a growing medium in hydroponic
systems. The material provides excellent water retention and air circulation, helping plants grow
efficiently in soilless environments.
Architects and engineers appreciate rock wool for its design flexibility and its contribution to
energy-efficient building envelopes. It helps meet modern building codes and green building
certifications such as LEED and BREEAM. It also supports goals for net-zero energy buildings
and sustainable development.
Despite its many advantages, there are some considerations. Handling rock wool may cause
temporary skin or respiratory irritation due to loose fibers. Therefore, protective gear is
recommended during installation. However, modern formulations have improved fiber stability,
reducing these effects significantly.
Over the past decades, the demand for rock wool has grown significantly as awareness of energy
conservation and building safety has increased. Countries with strict energy efficiency
standards, such as those in the EU, promote the use of rock wool in both residential and
commercial construction.
Research and development continue to improve rock wool products, making them thinner,
lighter, and more efficient without compromising performance. Innovations include high-density
panels for façade insulation, acoustic ceiling tiles, and sandwich panels for prefabricated
buildings.
Rock wool manufacturers often emphasize closed-loop recycling in their operations. Waste rock
wool generated during production or construction is collected and reused, minimizing
environmental impact. This circular economic approach aligns with global efforts to reduce
waste and promote sustainable building practices.
In summary, rock wool is a high-performance insulation material with exceptional thermal,
acoustic, and fire-resistant qualities. Its durability, sustainability, and safety features make it a
top choice in both construction and industrial applications. As the world moves toward more
energy-efficient and resilient buildings, rock wool continues to play a central role in achieving
those goals.
The definitions of Wool Rock
Rock wool, or mineral wool, is an insulation material made by melting volcanic rock—usually
basalt or diabase—at around 1,500–1,600 °C, then spinning it into fine, wool-like fibers These
fibers are bonded (often with small amounts of resin) into batts, rolls, boards, or loose-fill
forms for versatile applications.
Thanks to its fibrous structure, rock wool excels in thermal insulation—its trapped air pockets
significantly reduce heat transfer. It also provides excellent acoustic insulation, absorbing and
dampening sound waves, ideal for quiet and comfortable spaces.
A major benefit is its outstanding fire resistance—being non-combustible, it can withstand
temperatures over 1,000 °C, making it a preferred choice for fire-safe constructions.
Rock wool is moisture-resistant and mold-proof, as it’s inorganic and doesn’t support
microbial growth—this ensures long-lasting performance even in damp environments.
It's also valued for being sustainable and recyclable: manufactured from abundant natural
minerals (and often recycled industrial slag), it’s eco-friendly and reusable.
Common forms include batts, rigid boards, and loose-fill, which are used in walls, roofs,
floors, industrial equipment, and even HVAC systems.
Comparatively, rock wool is more dimensionally stable over time—it doesn’t sag or lose R-
value and maintains insulation quality throughout its lifespan.
Although it can be slightly more expensive than alternatives like fiberglass, its durability, fire
safety, and acoustic performance often justify the cost
Due to fine fibers, protective gear (gloves, masks) is recommended during installation—
modern versions are designed to reduce irritation.
Today, rock wool is widely used in building envelopes, industrial insulation, acoustic
treatments, and fire protection systems—valued in residential, commercial, and industrial
settings alike.
MELTING THE RAW MATERIALS
Cupola furnace operation
The cupola furnace is an apparatus designed to melt magma rocks and their supplements,
utilizing coke as its fuel source. It is loaded from the top with pre-prepared bundles of magma
rocks and coke. Inside the furnace, various chemical and thermal reactions occur. The
melting process is affected by the composition and quantity of the materials fed into it, as
well as the under draft.
The under draft is essential for the optimal operation of the cupola furnace, acting as a
regulator for the melting speed and impacting the properties of the melt directly. It is
achieved through the use of concentric nozzles positioned around the furnace's periphery,
which deliver air in a precisely regulated manner regarding both volume and temperature.
This air can also be enriched with oxygen. The under draft enhances the combustion of coke,
generating extremely hot gases that ascend through the furnace, transferring heat energy to
the magma rocks and coke. The exhaust gases exit the cupola furnace at around 400°C.
Thanks to the heat transfer, the materials located above the nozzles start to melt and flow
downward toward the bottom of the cupola, where the melt level is controlled using a siphon.
The cupola furnace can be categorized into various zones based on its operation, as illustrated
in Fig. 2.1 [8]. The initial zone is known as the heating zone, where the raw materials are
heated, leading to the loss of moisture and gas. The indirect reduction of iron oxide begins at
temperatures between 300–400°C, and this zone operates within a temperature range of 200–
800°C. The second zone is referred to as the re-formation zone for the added materials, as
depicted in Fig. 2.1. The temperature in this zone ranges from 800°C to 1250°C. Here,
dolomite (CaC𝑂3 , MgC𝑂3) decomposes, releasing CO2. Amphibolite can be broken down as
it becomes more brittle at elevated temperatures. Additionally, iron oxide undergoes further
reduction. Casting coke remains inactive until it attains a temperature of 1000°C. The direct
reduction of iron oxide (FeO) is achievable.
The third zone is characterized by its thinness, resulting in the melting of the inserted
materials, as depicted in Fig. 2.1. Magma rocks and dolomite usually begin to melt at
temperatures ranging from 1250 to 1350°C. The melting process of magma rocks is
influenced by the types of minerals present and their granulation. At such elevated
temperatures, the solidity of amphibolite diminishes. The significant weight above the
furnace causes the material beneath to crush, making it easier to melt. A similar process
occurs with dolomite, which decomposes at approximately 800°C, releasing CO2. Grains of
CaO and MgO ignite at around 1200°C before melting at even higher temperatures. When
briquettes are melted, additional unknown quantities, including thin calcinated bauxite and
non-fiberized crushed melt, are produced. These substances combine, held together by
cement, to form a solid structure. Briquettes mainly consist of waste materials generated
during production, with a significant portion made up of previously fiberized mineral
materials and products from the fiberization process occurring within the furnace. Cement
phases bond with each other and sublimate at about 600°C.
The fourth zone, where coke burning occurs, is situated above the nozzles (illustrated in Fig.
2.1) and concludes at the melting bed. In this area, coke reaches the temperature required for
combustion with oxygen, around 600–700°C. The underdraft may be cold or heated, which
accelerates the coke burning process. It is understood that coke can burn to produce carbon
dioxide (CO2) and carbon monoxide (CO). The full oxidation release of heat energy is
substantially greater in the case of CO2, which occurs when there’s sufficient underdraft for
the coke. Above 600°C, thermodynamic conditions favor the generation of CO, which can
form from CO2 as it passes through the base coke. This reaction depends on temperature, the
contact surface area between CO2 and coke, and the duration the gases remain in contact with
the base coke. However, from a thermal perspective, this reaction is undesirable as it
consumes casting coke and is endothermic. An increase in CO promotes an atmosphere of
reduction, enhancing the ability of Fe2O3 to reduce into pig iron. Caster and mineral wool
manufacturers prefer using casting coke in cupola furnaces due to its reduced reactivity. CO
is generated more readily with casting coke, which also produces a greater thermal effect.
Within the fourth zone, temperatures reach their peak just above the melting bed,
distinguishing between the highest temperatures of gases, coke, and the incoming melt.
Research from Danish scientists [8] indicates peak temperatures of approximately 1500°C for
the melt, around 1800°C for the coke, and over 2000°C for the gas. It has been established
that the melt’s temperature elevates to between 1300–1500°C while traversing this zone and
maintains this temperature upon exiting the cupola furnace (as shown in Fig. 2.1)
The fifth zone, located at the bottom of the cupola furnace, is referred to as the separation
zone. In this area, due to physical principles, pig iron separates from the silicate melt (slag)
and sinks due to its higher density.
Processes and chemical reactions in the cupola furnace