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Natural Science in Archaeology

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11.3 Cements and Mortars 267<br />

of several layers of calcium carbonate that resulted from the natural alteration of<br />

slaked lime. The Egyptians began us<strong>in</strong>g gypsum and lime mortars about 5000 BP.<br />

The Romans improved on lime mortar by add<strong>in</strong>g volcanic ash to make a pozzolana<br />

cement. Follow<strong>in</strong>g the fall of Rome the technology of cement manufacture was lost<br />

until the Middle Ages.<br />

11.3.6 Artifi cial “Pozzolana”<br />

Artificial pozzolanas are materials that produce a hydraulic reaction similar to the<br />

reaction produced by natural pozzolana. Artificial pozzolana can be organic or <strong>in</strong>organic<br />

material. Examples of <strong>in</strong>organic materials <strong>in</strong>clude calc<strong>in</strong>ed clays and shales, furnace<br />

slag, fly ash, and brick powder. Organic artificial pozzolanas <strong>in</strong>clude ashes from<br />

rice husks and coffee hulls. The use of rice husk ash is particularly well documented.<br />

After burn<strong>in</strong>g, the rema<strong>in</strong><strong>in</strong>g material is predom<strong>in</strong>antly reactive silica. Mix<strong>in</strong>g these<br />

f<strong>in</strong>e-gra<strong>in</strong>ed pozzolanic materials with wet lime develops a gel-like structure that<br />

expands as it sets, mak<strong>in</strong>g it a tight, essentially permanent bond<strong>in</strong>g agent.<br />

Pottery and brick dust are the most popular artificial pozzolanas. Their ma<strong>in</strong><br />

constituent is calc<strong>in</strong>ed clay. Clays are products of mechanical and chemical weather<strong>in</strong>g<br />

of igneous rocks. Microscopically, clays are flat plate-like crystall<strong>in</strong>e particles<br />

less than 2 µm <strong>in</strong> size. Clays can be considered active or <strong>in</strong>active depend<strong>in</strong>g on how<br />

much water they are capable of absorb<strong>in</strong>g. Thus, the amount of alternate swell<strong>in</strong>g,<br />

shr<strong>in</strong>kage, warp<strong>in</strong>g, and crack<strong>in</strong>g will depend on the type of clay. Clay m<strong>in</strong>eral particles<br />

will stack <strong>in</strong> layers and adhere to each other much the way two layers of wet<br />

plastic sheets sometimes do. When fired, the clay becomes vitrified or glassy.<br />

If fired at a high enough temperature, calc<strong>in</strong>ed clay may make an excellent<br />

pozzolana. High-fired brick and pottery dust makes a much better pozzolana than<br />

low-fired brick and pottery dust (Lea 1973). Research has shown that the size and<br />

distribution of the clay particles <strong>in</strong> the matrix of the cement can also have an impact<br />

on its strength.<br />

Fired clay <strong>in</strong> itself possesses “little or no cementitious value, but that <strong>in</strong> f<strong>in</strong>ely<br />

divided form and <strong>in</strong> the presence of moisture will chemically react with alkali<br />

or alkal<strong>in</strong>e earth hydroxides” (Adams et al. 1992). In other words, <strong>in</strong> order to be<br />

absorbed <strong>in</strong>to the chemical reaction, the clay product (usually crushed brick or pottery)<br />

must be crushed <strong>in</strong>to a f<strong>in</strong>e powder. “These reactions take place at ord<strong>in</strong>ary<br />

temperatures to form compounds possess<strong>in</strong>g cementitious properties” (Adams et al.<br />

1992). The nature of the pozzolanic reaction can be described as follows:<br />

“The so-called pozzolanic character of crushed brick mortar is attributed to the<br />

adhesion reactions of physicochemical character occurr<strong>in</strong>g at the ceramic-matrix<br />

<strong>in</strong>terface; their nature depends both on the type of ceramic and the calcium hydrate<br />

content of the mortar. The observed reactions could probably be attributed to calcium<br />

silicate formations at the <strong>in</strong>terface along the brick fragment, act<strong>in</strong>g as the<br />

silicate source and membrane and the lime, which makes the <strong>in</strong>terfacial surface<br />

alkal<strong>in</strong>e and causes the chemical reaction. The penetration of lime <strong>in</strong>to the ceramic

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