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dc.contributor.authorGray, George
dc.date.accessioned2008-05-19T03:58:42Z
dc.date.available2008-05-19T03:58:42Z
dc.date.issued1889
dc.identifier.citationGray, G. (1889). Note on the analysis of a mineral water from the Otira Gorge. Transactions and Proceedings of the New Zealand Institute, 22, 495-497.en
dc.identifier.urihttps://hdl.handle.net/10182/486
dc.description.abstractThe sample of water referred to in the present note was collected by the writer on the 21st January, 1889, in the Otira Gorge, from a spring which is stated to have been first discovered shortly after the earthquake of the 1st September, 1888. From the results obtained this water might be termed siliceous and sulphurous. It is essentially different from the water from the Hanmer Springs, and pertains more to the character of the waters of the Rotorua district. It differs, however, from these waters in having only a portion of its carbonic anhydride replaced by silica, and in containing less dissolved matter.en
dc.language.isoenen
dc.publisherNew Zealand Instituteen
dc.relationAlso available as part of a digitisation project carried out by the National Library of New Zealand in consultation with the Royal Society of New Zealand.en
dc.relation.urihttp://rsnz.natlib.govt.nz/volume/rsnz_22/rsnz_22_00_006150.htmlen
dc.subjectwateren
dc.subjectspringen
dc.subjectOtiraen
dc.titleNote on the analysis of a mineral water from the Otira Gorgeen
dc.typeJournal Articleen
dc.subject.marsdenFields of Research::300000 Agricultural, Veterinary and Environmental Sciences::300100 Soil and Water Sciencesen
lu.contributor.unitSoil and Physical Sciences Groupen


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