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Hydroelectricity is the primary source of renewable energy in New Zealand. Power is generated the most in the South Island and is used most in the North Island. [1] Early schemes such as the Waipori scheme commissioned in 1903 and the Lake Coleridge power station commissioned in 1914 established New Zealand's use of renewable hydro energy. By ...
The institute was formed on 1 December 2008 by merging existing CRIs HortResearch and Crop and Food Research. [3] Plant & Food has over 900 staff based at sites throughout New Zealand as well as science and business development staff working in the United States, Europe, Asia and Australia.
The Institute for Crop and Food Research was formed in 1992 as a New Zealand-based biological science Crown Research Institute researching new knowledge in five main areas: sustainable water and land use; high performance plants; personalised foods; high value marine products; biomolecules and biomaterials
Graph of New Zealand electricity generation capacity by year. This is a list of power stations in New Zealand. The list is not exhaustive – only power stations over 0.5 MW and significant power stations below 0.5 MW are listed. Power plants in New Zealand have different generating roles – for baseload, intermediate or peaking.
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Walls for Water: Pioneer Dam Building in New Zealand. Palmerston North: The Dunmore Press Ltd. ISBN 0-86469-313-3 . Retired civil engineer and dam inspector examines the development of New Zealand dam construction techniques and uses from the 1860s to the 1950s for municipal water supply, mining, kauri logging and development of the Lake ...
The first surveyors mapping out this corner of New Zealand noted the potential for hydro generation in the 178-metre drop from the lake to the Tasman Sea at Doubtful Sound. The idea of building a power station was first formulated by Peter Hay, the Superintending Engineer of the Public Works Department, and Lemuel Morris Hancock, the Electrical ...
The dam is the largest earth-fill (zoned embankment dam) water-retaining structure in New Zealand. Its core is low permeability clay material, supported by two massive shoulders of river gravel. Lake Benmore has a volume of 1.25 billion cubic metres, about 1.5 times as much water as Wellington Harbour .