Conference Papers Database New search

Wairakei-Tauhara Pressure Regime Update

Sophie Frances Milloy and Yoong Wei Lim

Key words
Wairakei, Tauhara, Te Huka, Te Mihi, reservoir pressure, interference, isobars, pressure regime
Location
Wairakei, Tauhara, New Zealand
Conference
New Zealand Geothermal Workshop
Year
2012
Session
06. Geothermal Engineering - Production and Management
Language
English

Full text

1.2MB, opens in a new tab

Abstract

Information from wells drilled over the last five years at Wairakei and Tauhara, together with continuous pressure monitoring has provided new insights into the pressure regimes and interconnections between Wairakei and Tauhara. Continuous pressure monitoring using capillary tubing has allowed simultaneous observations of pressure responses in several wells. This information has significantly improved the understanding of both fields. This new information confirms the long-term pressure trends observed in both systems, with the Tauhara pressure regime approximately 5 bars higher than Wairakei. The new data was also used to develop isobar contours across both systems, which together with the information from the continuous pressure monitoring, indicates that the Tauhara pressure regime extends northwest as far as Karapiti. Wells that were once considered to be part of the Wairakei system can now be considered part of Tauhara based on their pressure regime. The results also suggest a connection between Karapiti South and Tauhara, and challenge the “traditional” concept of the two systems being separated by the Waikato River.

Copyright 2012, 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.

You have opened 0 records today from 216.73.217.128 (216.73.217.128).
Viewed 22 September 2026, 1:17 pm.