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Boron in Soil Over Naike and Whitford Low-Enthalpy Geothermal Fields, New Zealand

Liu Wei and K. Nicholson

Location
Whitford, New Zealand; Naike Hot Springs, New Zealand
Conference
New Zealand Geothermal Workshop
Year
1990
Session
Geochemistry
Language
English

Full text

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Abstract

Mercury, arsenic, bismuth, antimony and boron soil surveys were conducted over two low-enthalpy, sedimentary-hosted, geothexmal fields, Naike and Whitford, in New Zealand. Analysis was by ICPAES following a leach. Appreciable amounts of boron (0.13 to 4.25 were found at both Whitford and Naike; As, Hg, Bi and Sb were not detected. A positive strong boron anomaly exists in the warm spring area of Naike. This was probably created by boron transported in water phase, a conclusion supported by the relatively high concentration of Na Mg and Li in soils of the same area. Weaker anomalies (1.1 to 2 were found at Naike and Whitford. These are problems caused by boron transported in the vapour phase and indicated more permeable areas and possible upflow zones. Boron in soils can be used as a pathfinder for enthalpy geothermalsystem and as a guide to upflow areas.

Copyright 1990, University of Auckland. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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