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Natural Science in Archaeology

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11.3 Cements and Mortars 261<br />

as alabaster. Gypsum is found <strong>in</strong> nodules <strong>in</strong> sedimentary rocks, and may be present <strong>in</strong><br />

dimensional stone as <strong>in</strong>clusions. Gypsum is often found as ch<strong>in</strong>k<strong>in</strong>g between blocks<br />

or <strong>in</strong> rubble fill of cavity walls. However, large nodules when plentiful were sometimes<br />

used <strong>in</strong> construction of desert cobble walls (Ashurst and Dimes 1998, p. 87).<br />

11.3 Cements and Mortars<br />

11.3.1 Lime<br />

S<strong>in</strong>ce at least the third millennium BCE, lime has been used as one of the most basic<br />

components of mortar (Dix 1982). Lime can be procured by burn<strong>in</strong>g limestone,<br />

marble, shell, coral, or bones (Mazzullo and Teal 1994). Limestone is the most common<br />

source, and both calcitic and dolomitic limestones can be used.<br />

Lime is simple and cheap to prepare. Limestone is heated <strong>in</strong> a kiln to over 900°C;<br />

the CO 2 is driven off and CaO rema<strong>in</strong>s. The result<strong>in</strong>g product (calcium oxide) is<br />

traditionally referred to as “quicklime” or “unslaked lime”. This slakes with water<br />

and, when mixed with sand, makes mortar or plaster; 100 kg of pure limestone yield<br />

56 kg of lime.<br />

The m<strong>in</strong>imum effective temperature for burn<strong>in</strong>g limestone is 880°C, but, <strong>in</strong><br />

order to achieve this temperature throughout the limestone, the overall surface temperature<br />

must be about 1000°C. Conversely, excessively high temperatures are also<br />

undesirable. “Excessive temperature produces ‘hard burned’ lime of high shr<strong>in</strong>kage,<br />

high density, and low chemical reactivity. In contrast, lower burn<strong>in</strong>g temperatures<br />

result <strong>in</strong> ‘soft burned’ lime of low shr<strong>in</strong>kage, low density, high porosity, and high<br />

chemical reactivity” (Adams et al. 1992).<br />

After burn<strong>in</strong>g, lime is further processed by “slak<strong>in</strong>g”, which refers to a hydration<br />

process. The result<strong>in</strong>g calcium hydroxide is traditionally referred to as “slaked”<br />

lime. There are four basic methods for slak<strong>in</strong>g lime (McKee 1973). These <strong>in</strong>clude:<br />

1. “Spr<strong>in</strong>kl<strong>in</strong>g” or “drown<strong>in</strong>g” <strong>in</strong> which the correct amount of water is spr<strong>in</strong>kled<br />

over the quicklime.<br />

2. “Immersion” <strong>in</strong> which the quicklime is placed <strong>in</strong> a basket and submerged <strong>in</strong>to<br />

water. The basket is drawn up after a time. The slak<strong>in</strong>g is completed by exposure<br />

to moisture <strong>in</strong> the air.<br />

3. “Exposure” <strong>in</strong> which quicklime is exposed to the air <strong>in</strong> a shelter. It absorbs<br />

moisture from the air, but may also absorb any unreacted calcium carbonate,<br />

thus result<strong>in</strong>g <strong>in</strong> an <strong>in</strong>ferior product.<br />

4. The “lime paste” method <strong>in</strong> which the lime is mixed with water <strong>in</strong> pits. The<br />

slaked lime is aged <strong>in</strong> the pits or clay jars for weeks, sometimes even months or<br />

years. This method produces the most satisfactory product.<br />

Due to the caustic nature of the lime and the potential for violent chemical reaction,<br />

slak<strong>in</strong>g can be a dangerous task. If not done carefully, the heat of the reaction

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