2002
DOI: 10.1111/1475-4754.00042
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Estimation of the Production Parameters of Very Large Medieval Bricks from St. Urban, Switzerland

Abstract: The aim of the present study is to determine the production technology of a particular type of large medieval brick. The firing temperature and their soak times are estimated using a combination of colour and fabric, as well as mineralogical, microstructural and open porosity analysis. A replication experiment was carried out in order to validate the estimated predictions, and to give a realistic idea of the time needed to dry and fire each large brick. The experiment also suggests the temperature distribution… Show more

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Cited by 40 publications
(38 citation statements)
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References 9 publications
(14 reference statements)
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“…If sufficient amounts of calcium are available in the reaction, anorthite is formed either consuming the existing gehlenite together with amorphous clay mineral breakdown products or only by reaction of decomposed clay minerals and lime [70] in the rims of the grains [61]. The breakdown of anorthite is, however, occurred in the range of 900-1,000°C and its progressive disappearance is slightly higher than 1,100°C [72]. On the other hand, wollastonite is another phase which was detected two bodies of this group (I.C.6 and I. E.1).…”
Section: Resultsmentioning
confidence: 99%
“…If sufficient amounts of calcium are available in the reaction, anorthite is formed either consuming the existing gehlenite together with amorphous clay mineral breakdown products or only by reaction of decomposed clay minerals and lime [70] in the rims of the grains [61]. The breakdown of anorthite is, however, occurred in the range of 900-1,000°C and its progressive disappearance is slightly higher than 1,100°C [72]. On the other hand, wollastonite is another phase which was detected two bodies of this group (I.C.6 and I. E.1).…”
Section: Resultsmentioning
confidence: 99%
“…Images of surface texture and internal morphology produced by the secondary electron detector (SE) served to determine the extent of vitrification, reflecting the temperature at which the pottery was fired (Maniatis and Tite, 1981;Tite and Maniatis, 1975;Tite et al, 1982;Wolf, 2002). Images of compositional variability produced by the backscattered electron detector (BSE), coupled with the analysis by the EDS, allowed us to identify the presence and the composition of the slip of the samples.…”
Section: Archaeological Contextmentioning
confidence: 99%
“…Según (29), el color de la materia prima arcillosa sin carbonatos y en condiciones oxidantes varía en función de la temperatura de cocción: naranja claro (Munsell 5YR) entre 500 ºC y 900 ºC, naranja rojizo (2,5 YR) entre 900 ºC y 1.100 ºC y marrón rojizo (10R) a temperaturas superiores a 1.100 ºC. El color rojizo va ligado igualmente, como ya se ha comentado, a la hematites Differences in brick colour may be the result of both blending (presence of carbonate and Fe-oxy-hydroxides) and firing conditions (kiln temperature and oxidizing/reducing atmosphere), which determine the (ferrous or ferric) form of the Fe ion (24,25).…”
Section: Figura 2 Grupos Seleccionados (Ver Texto) Figure 2 Selectunclassified
“…According to (29), under oxidizing conditions, the colour of carbonate-free clayey raw materials may depend on the firing temperature: 500-900 °C (light orange = Munsell 5YR), 900-1,100 °C (orange-red = 2.5 YR) and >1,100 °C (red-brown = 10R). Red hues can be attributed to hematite neoformation, whereas shades of duskyblack are indicative of the presence of maghemite neoformada, en tanto que la maghemita (γ-Fe 2 O 3 ) da lugar a tonalidades negruzco-oscuras.…”
Section: Figura 2 Grupos Seleccionados (Ver Texto) Figure 2 Selectmentioning
confidence: 99%
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