Interference Tests at Kawerau, New Zealand
Conference
·
OSTI ID:888531
Analysis of interference tests at the Kawerau geothermal field in New Zealand has indicated that the reservoir may be viewed on a coarse scale as a two-layer structure. While these layers have high permeabilities, they are in poor hydrological communication with each other. The shallower layer is modelled as a finite cylindrical reservoir. The deeper layer is modelled as a larger cylindrical reservoir with recharge from the sides. The fitted permeabilities and storativities suggest the importance of flow in fractures at Kawerau. 2 tabs., 14 figs., 8 refs.
- Research Organization:
- Applied Mathematics Division, DSIR, Wellington, New Zealand
- Sponsoring Organization:
- USDOE
- DOE Contract Number:
- AT03-80SF11459; AS07-84ID12529
- OSTI ID:
- 888531
- Report Number(s):
- SGP-TR-109-25
- Country of Publication:
- United States
- Language:
- English
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