Limonite, Alunite, Jarosite, Phoenicochroite, Pyromorphite, Wulfenite
Iran
9th Century
Source: Holakooei, P., de Lapérouse, J. F., Rugiadi, M., & Carò, F. (2018). Early Islamic pigments at Nishapur, north-eastern Iran: studies on the painted fragments preserved at The Metropolitan Museum of Art. Archaeological and Anthropological Sciences, 10(1), 175-195.
Recipe Details
Ingredients
limonite, alunite, jarosite, phoenicochroite, pyromorphite, wulfenite, kaolinite, calcite, gypsum, quartz
Preparation Steps
Clay-based yellow pigments such as limonite and jarosite were likely locally sourced from the Arghash area in south-western Nishapur (p. 185). In contrast, the rare lead-bearing yellow pigments including phoenicochroite, pyromorphite, and wulfenite are suggested to be imported, potentially from mines like Seh-Changi, Chah Khuni, or the Gologa mine in Afghanistan (p. 187). Historical texts like Tabari’s Tohfat al-Gharayeb (ca. 1093) mention that slaked lime should be mixed and heated with water and pigments in a big pan before use as a paint layer (p. 182).
Original Recipe Text
Clay-based yellow pigments such as limonite and jarosite were likely locally sourced from the Arghash area in south-western Nishapur (p. 185). In contrast, the rare lead-bearing yellow pigments including phoenicochroite, pyromorphite, and wulfenite are suggested to be imported, potentially from mines like Seh-Changi, Chah Khuni, or the Gologa mine in Afghanistan (p. 187). Historical texts like Tabari’s Tohfat al-Gharayeb (ca. 1093) mention that slaked lime should be mixed and heated with water and pigments in a big pan before use as a paint layer (p. 182).
Evidence
"The main coloring agent of this group of yellow pigments was limonite, iron hydroxide (FeOOH), as suggested by μ-Raman bands at 300, 399, and 687 cm−1 (p. 184)."
Remarks
The association of kaolinite and alunite with limonite points to a local provenance for these pigments (p. 175). These findings suggest that pigment use and manufacturing during the 9th to 11th centuries in Nishapur was still in a trial-and-error stage (p. 175). Some lead-based yellows (phoenicochroite) were found precipitated on gypsum crystals (p. 187).
Scientific Analysis
Chemical CompositionFeOOH; KAl3(SO4)2(OH)6; NaFe3(SO4)2(OH)6; Pb2O(CrO4); Pb5(PO4)3Cl; PbMoO4
Analytical Techniques
XRF
Raman
XRD
optical reflectance spectroscopy
scanning electron microscopy (SEM)
Certainty Level
Confirmed
Instrumentally Verified
Verified
Metadata
Material Type
pigment
ColorYellow
RegionIran
Approx. Year850
Source Information
AuthorHolakooei, P., de Lapérouse, J. F., Rugiadi, M., & Carò, F.
CollectionNishapur; Arghash area; Seh-Changi and the Chah Khuni mines; Gologa mine (Afghanistan)
Language
N/A
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