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"Some Chemical Observations on the Cuneiform Glassmaking Texts."

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Brill, R. H. "<str<strong>on</strong>g>Some</str<strong>on</strong>g> <str<strong>on</strong>g>Chemical</str<strong>on</strong>g> <str<strong>on</strong>g>Observati<strong>on</strong>s</str<strong>on</strong>g> <strong>on</strong> <strong>the</strong> <strong>Cuneiform</strong> <strong>Glassmaking</strong> <strong>Texts</strong>." Annales du 5e C<strong>on</strong>grès de<br />

l’Associati<strong>on</strong> Internati<strong>on</strong>ale pour l’Histoire du Verre. Liège: Editi<strong>on</strong> du Secrétariat Général, 1972, pp. 329-351.<br />

TABLE 1 (')<br />

Compositi<strong>on</strong> « Typical» Analyses Hypo<strong>the</strong>tical Compositi<strong>on</strong><br />

Assumed of Mesopotamian Mesopotamian Calculated<br />

fo r ahussu ( 2) Glasses (3) «Base Glass» (4) for zuki2 (5)<br />

Na20 34.5 % Si02 55 64% 68 56 66 '% 70 56.0 %<br />

KzO 5.20 Na20 13 16 19 14 17 20 23.8<br />

CaO 9 .20 CaO 4 6.5 8 4 7 10 6.6<br />

MgO 7.80<br />

Al 2 0 3 1.10 K20 1 1.5 3 1 1.5 3 3.8<br />

MgO 3 4.5 6 3 4.5 6 5.6<br />

24.0<br />

3.20 A lz0 3 1.5 2 3 1.5 2 3 2.2<br />

6.20 Fe Z0 3 0.5 1 1.5 0.5 1 1.5 0.7<br />

1.50 T i0 2 0.1 0. 1 0.05<br />

FezO3 0.6 MnO var. 0.02 0.05<br />

MnO<br />

Ti02<br />

0. 1<br />

0. 1<br />

Sb20 5<br />

PbO<br />

var.<br />

var.<br />

O.OOX( ?)<br />

O.OOOX( ?)<br />

nil<br />

nil<br />

Si0 2 3.0<br />

Li20 - BaO --,0.1 --,0.1 --,0.1<br />

BaO 0.2 SrO --,0.1 --,0.1 --,0.1<br />

SrO 0.2<br />

B20 3<br />

Zr02<br />

-<br />

--<br />

PZ0 5<br />

S03<br />

--,0.3<br />

--,0.3<br />

--,0.3<br />

--,0.3<br />

1.0<br />

--,0.5(?)<br />

PbO -- Cl --,0.3 --,0.3 --,0.5 (?)<br />

« Oth er» 3.1<br />

Na?O/ K2O 6.64<br />

lAsh Residue --' 37<br />

NOTES TO ACCOMPANY TABLE 1<br />

(1) Informati<strong>on</strong> taken from «The <str<strong>on</strong>g>Chemical</str<strong>on</strong>g> Interpretati<strong>on</strong> of <strong>the</strong> <strong>Texts</strong> », Glass and<br />

<strong>Glassmaking</strong> in Ancient Mesopotamia. (See complete reference in footnote no. 1.)<br />

(2) This is a composite of values estimated from analyses of specimens of plant ashes.<br />

( 3) The compositi<strong>on</strong>s of early Mesopotamian glasses valY c<strong>on</strong>siderably with period<br />

and color. The values given are meant to represent typical values and <strong>the</strong> approximate ranges<br />

found. var. indicates elements which are variable depending up<strong>on</strong> <strong>the</strong> color of <strong>the</strong> glasses.<br />

(4) This is a hypo<strong>the</strong>tical compositi<strong>on</strong> (typical values and ranges) for a colorless<br />

« base glass» to which could have been added various colorants and opacifiers in order<br />

to produce glasses having <strong>the</strong> analyzed compositi<strong>on</strong>s listed in <strong>the</strong> previous column. The<br />

nominal values in <strong>the</strong> previous column were used for calculating <strong>the</strong> values for <strong>the</strong> hypo<strong>the</strong>tical<br />

«base glass ». I<br />

(5) Calculated by assuming <strong>the</strong> proporti<strong>on</strong>s given in secti<strong>on</strong>s 1 and 4 of <strong>the</strong> cuneiform<br />

texts. (See note 1.) The immanakku mineral was assumed to have <strong>the</strong> following compositi<strong>on</strong><br />

Si02 = 95.0 percent, Alz0 3 = 2.5 percent, Fe Z0 3 , CaO, MgO, NazO and K 20<br />

= 0.5 percent each. The ahussu compositi<strong>on</strong> used was that given in <strong>the</strong> first column of<br />

th is table. The mineral:ash ratio was assumed to be 10:12.<br />

Rakow Research Library, The Corning Museum of Glass - http://www.cmog.org

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