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Posted by Admin on June, 09, 2026

⬛ INDUSTRY TECHNICAL GUIDE | 2026 EDITION
L*, a*, b* Colour Values of Potash Feldspar
Understanding Whiteness, Colour Measurement & Quality Standards
A comprehensive technical and market intelligence guide covering CIELab colour science, global export data, market trends, production areas, technical specifications (HS Code, HSN, CAS, EC Number), and procurement guidance for ceramic raw material buyers worldwide.
Published by Aalok Overseas / FeldsparIndia.com | Rajasthan & Gujarat, India | www.feldsparindia.com
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L* 86–93 Whiteness Range Standard to Premium Grade K-Spar |
a* 0±0.8 Red/Green Axis Near-neutral: no green/red cast |
b* 0–3.5 Yellow/Blue Axis Slight warm tint in standard grades |
99.5% SiO₂ in Quartz Ultra-pure quartz L* 94–97 |
The CIELab colour space — standardised by the International Commission on Illumination (CIE) in 1976 — is the universally accepted system for measuring colour in minerals, ceramics, pigments, paints, and industrial raw materials. Unlike RGB or CMYK (which are device-dependent), CIELab is perceptually uniform and device-independent, making it the global standard for quality control in the ceramic industry.
For feldspar and quartz suppliers and buyers, L*, a*, and b* values are the primary quality indicators of whiteness, colour purity, and fired-body appearance.
|
Axis |
Name |
Range |
Mineral Significance |
|
L* |
Lightness / Whiteness |
0 (black) → 100 (white) |
Most critical: higher L* = whiter feldspar = brighter fired ceramic body and glaze |
|
a* |
Red (+) / Green (−) axis |
−128 → +128 |
Near zero is ideal; positive a* = reddish tint (Fe contamination); negative = greenish |
|
b* |
Yellow (+) / Blue (−) axis |
−128 → +128 |
Slight positive b* (0–3.5) is normal in feldspar; high b* = yellowish tint indicating iron/organic content |
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Key Formula: ΔE* (Total Colour Difference) |
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ΔE* = √[(ΔL*)² + (Δa*)² + (Δb*)²] |
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ΔE* < 1.0 = imperceptible difference | ΔE* 1–3 = slight difference | ΔE* > 3 = clearly visible difference |
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Ceramic manufacturers typically specify ΔE* < 1.5 between batches for consistent production. |
Potassium feldspar (K-Feldspar / Orthoclase / Microcline) from Rajasthan, India spans a range of L*, a*, b* values depending on the mine source, Fe₂O₃ content, and beneficiation level. The following specifications represent typical measured values from Indian export-grade potash feldspar.
|
Parameter |
Typical Value |
Range |
Quality Implication |
|
L* (Whiteness) |
88.5 |
86.0 – 90.5 |
Good whiteness; suitable for standard floor tile body and glaze applications |
|
a* (Red/Green) |
0.2 |
−0.2 → +0.5 |
Near-neutral; minor positive a* from trace iron; acceptable for most ceramics |
|
b* (Yellow/Blue) |
2.8 |
1.5 → 4.0 |
Slight warm yellow tone; normal for commercial-grade feldspar with Fe₂O₃ ~0.12–0.18% |
|
Fe₂O₃ (correlated) |
0.12–0.18% |
0.10–0.25% |
Direct relationship: higher Fe₂O₃ = lower L* and higher b* |
|
Parameter |
Typical Value |
Range |
Quality Implication |
|
L* (Whiteness) |
91.5 |
90.0 – 93.0 |
Excellent whiteness; preferred for premium tiles, sanitaryware glaze, and bone china |
|
a* |
0.1 |
−0.1 → +0.3 |
Virtually neutral; no perceptible colour cast |
|
b* |
1.8 |
1.0 → 2.5 |
Very low yellow tint; high-clarity fired surface |
|
Fe₂O₃ (correlated) |
0.06–0.10% |
0.04–0.12% |
Wet magnetic separation required to achieve this grade |
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The Iron-Whiteness Relationship — A Critical Correlation for QC Managers |
|
Fe₂O₃ 0.10% → L* ~91–93, b* ~1.5–2.0 | Fe₂O₃ 0.15% → L* ~88–90, b* ~2.5–3.5 | Fe₂O₃ 0.25% → L* ~84–87, b* ~4.0–6.0 |
|
Every 0.05% increase in Fe₂O₃ typically reduces L* by approximately 1.0–1.5 units and increases b* by ~0.8–1.2 units in potash feldspar. |
|
Mining Area |
Typical L* |
a* Range |
b* Range |
Fe₂O₃ % |
Grade Description |
|
Ajmer District |
90–93 |
0.0 to +0.3 |
1.2–2.2 |
0.06–0.10 |
Premium low-iron; best for frits, bone china, sanitaryware |
|
Bhilwara District |
88–91 |
0.1 to +0.4 |
2.0–3.0 |
0.10–0.15 |
Good standard grade; widely exported to ASEAN |
|
Sikar District |
87–90 |
0.1 to +0.5 |
2.5–3.8 |
0.12–0.18 |
Commercial grade; tile body and glaze applications |
|
Rajsamand District |
91–93 |
-0.1 to +0.2 |
1.0–2.0 |
0.05–0.09 |
Ultra-premium; selective mine extraction required |
|
Pali / Barmer |
85–88 |
0.2 to +0.6 |
3.0–4.5 |
0.18–0.28 |
Standard commercial; paint and filler applications |
Sodium feldspar (Albite, Na-Feldspar) from Gujarat typically achieves higher L* values than potash feldspar due to its lower natural iron content and distinct crystal chemistry. Albite is preferred for glass, fine porcelain, and wall tile glazes where extreme whiteness is required.
|
Grade |
L* |
a* |
b* |
Fe₂O₃ % |
Origin Area |
Primary Application |
|
Standard Albite |
90–92 |
0.0 to +0.3 |
1.5–2.8 |
0.08–0.12 |
Jamnagar, Gujarat |
Wall tile glaze, floor tile body |
|
Premium Albite |
92–94 |
−0.1 to +0.2 |
0.8–1.5 |
0.04–0.08 |
Porbandar, Gujarat |
Glass frit, bone china, fine porcelain |
|
Super Premium Albite |
93–95 |
−0.2 to +0.1 |
0.5–1.0 |
0.02–0.05 |
Saurashtra select mines |
Semiconductor glass, specialty ceramics |
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Why Soda Feldspar Achieves Higher L* Than Potash Feldspar |
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Albite (NaAlSi₃O₈) has a higher SiO₂ content (67–69% vs 64–66% in K-spar) and a different crystal structure that accommodates less iron substitution in the lattice. Gujarat's Saurashtra belt produces particularly clean albite with naturally low Fe₂O₃, making it the whitest naturally occurring feldspar commercially available from India. |
Quartz (SiO₂) from Rajasthan achieves the highest whiteness values of all industrial minerals — outperforming feldspar due to its near-pure silicon dioxide composition. For applications where maximum whiteness is critical (high-end tiles, white glass, electronics), quartz L* values are essential specifications.
|
Grade |
L* |
a* |
b* |
SiO₂ % |
Fe₂O₃ % |
Origin |
Application |
|
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