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The Pamphlet Collection of Sir Robert Stout: Volume 64

Artificial Cements

Artificial Cements.

When I began to investigate the subject of native cements and limes, I was under the impression that we had no stone capable of furnishing hydraulic limes, consequently some little time was devoted to the consideration of providing an artificial substitute; but the existence of natural cementing ingredients of a high character having been fully established, the necessity for adopting the latter expedient is removed, the subject will Wherefore be dismissed in a few words.

As you are probably aware, English Portland cement is made from two of the most common and abundant raw materials in the country—chalk and clay—and the manufacture is equally simple. The materials are mixed in the proportion of seven of the former to three of the latter, then burned in a kiln and pulverized as already described. In Germany, where there is no chalk, a substitute is found in hard limestone. This entails extra labour in pulverizing the raw material as well as the cement, but the result is practically the same.

Ordinary yellow clay does not make good cement; that in common use page 124 is a dark blue unctuous variety found in tidal estuaries and swamps. Blue clays, supposed to be suitable for the purpose, are abundant throughout the province. A sample from the railway cutting at Caversham was analyzed by Professor Black with the following results, which are shown alongside an English type:—
Otago Clay. English Clay.
Silica 65.28 68.45
Alumina 23.18 11.64
Iron 3.20 14.80
Lime and magnesia 2.58 0.75
Alkalies 1.04 4.00
Water 5.19
100.47 99.64

These figures are not near enough to prove that this clay is good for making cement, but they are sufficient to show that there is every chance of getting the proper kind if required.

Portland cement is a low-priced article, the value of which is more than doubled by the charges of importation, and it can be manufactured without much skilled labour, consequently it is an industry that might well be started in New Zealand if there were no hydraulic limes to compete with it. The best places in Otago for a factory are the Waihemo and Aparima districts, both of which furnish soft limestones and fuel, the main requisites. The soft marl found at Waikouaiti and Grey town, being supposed to contain the ingredients of raw cement, was analyzed and gave the following result:—
Clay 27.84 per cent
Iron 11.24 per cent
Lime 24.78 per cent
Sand 85.16 per cent
99.02

The last item neutralizes the good qualities of the others, so we pass it into the category of unsuitable materials.

The idea of utilising the rich limes induced me three years ago to mate an examination of volcanic clays to ascertain if they contained any of the properties of the Pozzuolanas of the old world that have been used from time immemorial to mix with lime in hydraulic works. About 40 specimens of all shades of colour imaginable were collected and tested by being made into mortar with an equal proportion of lime, then kept in water for two months. Four or five samples of drab and neutral tints gave indications of being feebly hydraulic, so possibly a more complete investigation would lead to the discovery of a material of considerable utility. The great objec- page 125 tion to Pozzuolanas is that, like the Moeraki boulders, uniformity of composition cannot be ensured.