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Volume 1, 1868
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Fourth Meeting. August 3, 1868.
The Rev. James Buller, in the chair.

The following contributions were announced, viz:

Specimen of copper from Whangapurapura, Great Barrier Island—Mr. F. Whitaker. Two living specimens of Hatteria punctata from Karewa Island, near Tauranga—Mr. H. T. Clarke. Gold from Kapanga, gold from South Island, gold from South America, and arsenic from Kapanga—Mr. F. Whitaker. Gold from Paparata. Collection of Moa bones—Dr. Haast, Christchurch, per Captain Hutton. Fossil wood from the Portland beds, England—Dr. Purchas. Johnston's “Lectures on Agricultural Chemistry and Geology”—Mr. J. H. Crawford. Specimen of cement with gold (about four ounces to the ton), from Charleston, Nelson; specimen of quartz with gold, from Westport, Nelson—Mr. D. Murdoch. Trachytic rocks from Tokatoka, Kaipara—Captain Hutton. Specimen of wood (probably Leptospermum) taken from a depth of forty feet below the scoria, near Mount Eden—Mr. John Probert. Crystallised quartz and rock-casing from the “York” and “Devon” claims; quartz and bed-rock from the “Bendigo” claim; quartz from the “Pretty Jane” claim—Mr. Cartwright. Collection of thirty-nine coins and medals, chiefly silver—Mr. J. H. Crawford.

Papers read:

(1.) “On Arid Island,” by Captain Hutton and T. Kirk, Esq., read by the Honorary Secretary, Mr. Gillies. (See Transactions.)

At the conclusion of the paper, some discussion took place respecting what had been stated as to the subsidence of the island. Dr. Purchas, Mr. Gillies, Mr. Boardman, and Captain Hutton spoke on the subject.

(2.) “On Agricultural Chemistry,” by John Lowe, Esq., C.E.

(Extracts.)

The author commenced by observing that the fertility of a soil, as relates to the production of particular crops, may depend upon the presence or absence of very minute, and almost imperceptible, portions of inorganic substances—alkalies for instance—and salts of metals. The necessity, for example, of sulphate of lime to clover, silica to grapes, phosphorus to wheat, etc., was formerly quite disregarded; and it is only of late years that these matters have been more looked into: and we see, with satisfaction, the result of the joint labour of the farmer and the chemist.

Soils are made up of organic and inorganic constituents—he would

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confine himself to the latter,—and class them as those which constitute the bulk of the soil, on the mechanical texture of which, the growing crops depend, such as clay, sand, and lime; also those involving the fitness of soil for particular crops, such as sulphate and phosphate of lime, soda, ammonia, magnesia, etc.

The author described various mineral and chemical compounds, suitable for the different kinds of soils and crops; also the method for making and applying such. He described, at some length, the different kinds of clays and earths, and the properties peculiar to them, and recommended farmers to have their lands chemically tested or analyzed, so as to enable them, by applying the necessary compounds, to make the soil suitable for particular crops.

Captain Hutton said that in anticipation of the paper, he had prepared a map showing where limestone existed in the province. It would be seen that it occurred all over the north, in small patches, but the only great mass was in that part, from Raglan harbour, to Aotea, Kawhia, and Mokau. As to the value of limestone as a manure, he should like to ask Mr. Wark what was done with the refuse lime from the gas-works, which was a most valuable manure.

Mr. Wark said that when the gas-works were first started, lime was used to purify the gas; but it had been found expensive, and he (Mr. Wark) now used oxide of iron, which cost three farthings, while the lime had cost sixpence. While the lime was being used, it was readily bought by the farmers at two shillings and sixpence per load. A good deal of ammonia had been given to farmers gratuitously, but he had not heard of the results. Perhaps Mr. Gillies, who had got some, would inform them as to his experience.

Mr. Gillies said he was convinced that the ammonia was one of the most valuable manures for grass; it would increase the crop at least one-third, and was excellent as a destroyer of grubs, wire-worms, and slugs. He was sorry to see that the farmers pooh-poohed so much the idea of agricultural chemistry being of any benefit. He had conversed with many of them, and was sorry to hear their opinions on the subject. He observed, that Dr. Hector had done something to create an interest in the subject, by advertising that any person who sent a bag of soil to Wellington, would get an analysis free. It seemed to him (Mr. Gillies) that every farmer ought to send down a specimen of the soil of his farm, and have it analyzed. He was surprised, however, to hear from Dr. Hector, when he was last in Auckland, that he had not got half a dozen

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specimens of soils from the whole province. The Society might get specimens analyzed from every district in the province, and make out a map of soils, showing what their products might be. By this they would see, that, in one district wheat might advantageously be grown, in another clover, in another barley, and so on. Two years ago, he thought of growing vines at Mount Eden, which he thought would be admirably adapted for their growth. He found, however, that they produced too much wood, and did not succeed.

Dr. Fischer said that the soil upon which he had experimented, with reference to vines, was trachytic scoria, while Mount Eden was basaltic scoria. He (Dr. Fischer) had not yet succeeded very well with his vines. He believed that the Mount Eden soil would be too dry for the vines. Dr. Fischer remarked, that to have a map applied to such a purpose as that spoken of by Mr. Gillies, they would require to have the particulars of the climates of the different districts also.

Resolved, “That the Secretary be instructed to apply to Dr. Hector for forms respecting the analysis of soils.”