Update on subsidence at the Wairakei–Tauhara geothermal system, New Zealand
The total subsidence at the Wairakei field as a result of 50 years of geothermal fluid extraction is 15 +/- 0.5 m. Subsidence rates in the center of the subsidence bowl have decreased from over 450 mm/year during the 1970s to 80-90 mm/year during 2000-2007. The location of the bowl, adjacent to the...
Gespeichert in:
| Veröffentlicht in: | Geothermics 2009-03, Vol.38 (1), p.169-180 |
|---|---|
| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
Schreiben Sie den ersten Kommentar!