Talc Powder AL 40 is a premium-quality hydrated magnesium silicate, derived from the transformation of high magnesium rocks by siliceous hydrothermal fluids. With a distinct unique morphology and mineralogy, this talc is characterized by several properties that make it an invaluable additive across various industries. Its soft texture, water repellency, chemical inertness, platyness, and strong affinity for organic substances impart versatility to Talc Powder AL 40, allowing it to serve effectively as a multi-functional filler and process enabler in sectors such as plastics, paper, ceramics, and paints. The product boasts a high whiteness index of 92% ±2, along with the robust chemical specifications, which confer many benefits during the manufacturing processes. Explore the properties and technical specifications of Talc Powder AL 40 and see how it can enhance your production capabilities while improving product performance.

Key Features

Features Description
Whiteness Level 92% +/-2
Silica Content (SiO2) 50 - 52%
Magnesia Content (MgO) 26 - 28%
Alumina Content (AI2O3) 0.50 - 1.50%
Iron Content (Fe2O3) 0.5 - 0.8%
Calcium Oxide Content (CaO) 8 - 10%
Loss on Ignition 10 - 12%
Bulk Density 0.45 - 0.55 gm/ml
pH Level 8-9
Moisture Content 0.4 - 0.6%
Specific Gravity 2.7 - 2.8%
Retention on 500 Mesh 1.0%
Attributes Description
Chemical Composition Hydrated Magnesium Silicate
Physical State Powder
Application Industries Plastics, Paper, Ceramics, Paints
Unique Properties Softness, Water Repellency, Chemical Inertness, Platyness, Organic Affinity
Talc Origin Alteration of dolomite or ultramafic intrusive rocks
Associated Minerals Carbonates and Chlorite
Unique Morphology Depends on the particular deposit

*Disclaimer: The above description has been AI-generated and has not been audited or verified for accuracy. It is recommended to verify product details independently before making any purchasing decisions.

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Country Of Origin: India

Talc is a hydrated magnesium silicate. Talc deposits form from the transformation of high magnesium rocks by siliceous hydrothermal fluids. Most talc originates from the alteration of dolomite or ultramafic intrusive rocks. Following this process, talc is always found in combination with other mineral(s). Carbonates and chlorite are the most common associated minerals.

Each talc deposit has a unique morphology and mineralogy, but all talcs exhibit the following unique properties: softness, water repellency, chemical inertness, platyness, and an affinity for organic substances.

These properties make talc a highly prized multi-functional filler and process enabler in an array of applications from plastics to paper, ceramics to paint.

TECHNICAL DATA SPECIFICATION


WHITENESS : 92% +/-2

SILICA SiO2 : 50 - 52%

MAGNESIA MgO : 26 - 28%

ALUMINA AI2O3 : 0.50 - 1.50%

IRON Fe2O3 : 0.5 - 0.8%

CALCIUM OXIDE CaO : 8 - 10%

LOSS ON IGNITION : 10 - 12%

BULK DENSITY (gm/ml) : 0.45 - 0.55%

Ph : 8-9

MOISTURE : 0.4 - 0.6%

SPECIFIC GRAVITY : 2.7 - 2.8%

RETENTION ON 500 MESH : 1.0%



Non-metallic Mineral Deposits

Talc

Talc Powder AL 40

Hydrated Magnesium Silicate

Multi-functional Filler

Talc For Plastics

Talc For Ceramics

Talc For Paper

Talc Properties

High Whiteness Talc

TALC POWDER AL 40

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