Wairakei Power Station

Wairakei Power Station

The Wairakei Power Station, with the main two blocks at the left rear. The binary plant is in front.
Location of Wairakei Power Station in New Zealand
Country New Zealand
Location Wairakei, north of Taupo
Coordinates 38°37′37″S 176°06′19″E / 38.62694°S 176.10528°E / -38.62694; 176.10528Coordinates: 38°37′37″S 176°06′19″E / 38.62694°S 176.10528°E / -38.62694; 176.10528
Status Operational
Commission date November 1958 (November 1958)
Owner(s) Contact Energy
Geothermal power station
Type Flash steam with binary cycle[1]
Wells 55 production
6 reinjection
50 monitoring[1]
Max. well depth 660 m (2,170 ft)[1]
Thermal power station
Cogeneration? No
Power generation
Units operational 6× 11.2 MW
3× 30 MW
1× 4 MW
1×14 MW binary
Nameplate capacity 175 MW
Capacity factor 89.0%
Average generation 1365 GWh[1]

The Wairakei Power Station is a geothermal power station near the Wairakei Geothermal Field in New Zealand. Wairakei lies in the Taupo Volcanic Zone.

History

The power station was built in 1958, the first of its type (wet steam) in the world, and it is currently owned and operated by Contact Energy. A binary cycle power plant was constructed in 2005 to use lower-temperature steam that had already gone through the main plant.[2][3] This increased the total capacity of the power station to 181MW.[1] The Wairakei power station is due to be phased out from 2013, replaced by the Te Mihi geothermal power station. The Poihipi Power Station was built in 1996 at a nearby site in the same field.[2]

Recent Electricity Generation at Wairakei.

Units

Wairakei A station

Units 2, 3, 5 and 6 were decommissioned in 1984.

Wairakei B station

Wairakei Unit 14 – 4 MW intermediate/low pressure

Wairakei Binary Plant – 14 MW binary

Effects

Pipes running from the Power station

The use of steam from the field has had a number of visible effects on the local environment. Visible geothermal activity has increased (due to changes in the water table / water pressure allowing more steam to be created underground, upsurging at places like Craters of the Moon), while there has also been some land subsidence and reduction in steam volumes from the field after some decades of use. Recent total electrical production has been sustained or increased with the investment in additional power stations such as the binary plant of 2005 designed for lower-temperature generation, but the total still does not reach the early power levels such as the 192MW reported in 1965 (NZED Annual Statistics), for instance. Some power stations in the field are now capped in their extraction capacities and a substantial part of the water / steam is being reinjected after use.[2]

The hot geothermal fluid that is extracted is originally cold rainwater that had percolated downwards and been heated by hot rock; pumping back the warm water that emerges from the exhaust of the generator system thus reduces the heat drawn from the ground. Also, the Waikato river water is already too high in arsenic content to be safe to drink without special treatment, so reinjection of the facility's water does not exacerbate this problem.[4][5]

Transmission

Also at Wairakei is a major electrical substation, owned by the national grid operator Transpower. The substation is a major switching point for the Central North Island, and is responsible for connecting more than half the country's geothermal power stations, several hydroelectric power stations, the electricity supply to the entire Hawke's Bay and Gisborne regions and half of the Bay of Plenty region. A 33 kV connection at the substation supplies Unison Networks' Taupo distribution network.[6]

See also

References

  1. 1 2 3 4 5 "Geothermal" (PDF). Contact Energy. Retrieved 2008-10-23.
  2. 1 2 3 "Geothermal Fields". New Zealand Geothermal Association. Retrieved 13 March 2011.
  3. ↑ "Geothermal Energy and Electricity Generation". New Zealand Geothermal Association. Retrieved 13 March 2011.
  4. ↑ Arsenic in the New Zealand environment - Brett Robinson, Brent Clothier, Nanthi S. Bolan, Santiago Mahimairaja, Marc Greven, Christopher Moni, Monica Marchetti, Carlo van den Dijssel and Georgina Milne - Institute of Natural Resources, Massey University, Palmerston North, New Zealand
  5. ↑ Inflows of geothermal fluid chemicals to the Waikato River catchment, New Zealand - M.H. Timperley and B.A. Hauser, New Zealand Journal of Marine and Freshwater Research, 1996: Vol 30: 525-535.
  6. ↑ "Chapter 11: Central North Island Regional Plan - Annual Planning Report 2012" (PDF). Transpower New Zealand Limited. March 2012. Retrieved 1 July 2012.

Further reading

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