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sources of energy for geothermal direct heat use - GNS Science

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Estimated temperatures in the coal mines range from 18 o to 24 o C, with a mean <strong>of</strong> 18 o C.Temperatures are higher in gold mines at 19 o to 35 o C with a mean <strong>of</strong> 23 o C mainly beca<strong>use</strong>the mines could be as deep as 700 to 850m and are also located in high <strong>heat</strong> flux areas inthe Coromandel and the South Island where the thermal gradient is about 35-40 o C/km(Table 6).The volume <strong>of</strong> the underground coal mines are calculated from the total mass extracteddivided by the mean density <strong>of</strong> coal at about 1260 kg/m 3 . For the gold and copper mines thearea covered by the underground mines and the depth <strong>of</strong> the deepest stopes are included inthe calculation. The estimated potential <strong>heat</strong> <strong>energy</strong> from the warm waters is about 0.64 PJ<strong>for</strong> the 22 coal mines and 13.6 PJ <strong>for</strong> the gold and copper mines.5.0 PROJECTED USE OF UNCONVENTIONAL GEOTHERMAL RESOURCES5.1 SHALLOW CONDUCTIVE HEAT FLOW AND GROUND SOURCE HEAT PUMPSIn calculating the attainable <strong>use</strong> <strong>of</strong> <strong>heat</strong> <strong>for</strong> ground source <strong>heat</strong> pumps in New Zealand <strong>for</strong>the next 10 years, it is assumed that about 5% <strong>of</strong> the buildings in New Zealand will have atleast 6 kW installed.According to New Zealand Statistics, there are 1,961,290 buildings in New Zealand <strong>of</strong> which309,750 are business buildings and 1,651,540 dwellings. About 18.6 PJ will be harnessed if5% <strong>of</strong> the buildings (98,065) will have a 6 kW ground source <strong>heat</strong> pump installed within thenext 10 years (Table 7).5.2 ABANDONED HYDROCARBON WELLSIn the next 10 years about 20 <strong>of</strong> the 140 abandoned wells in Taranaki could be exploited <strong>for</strong><strong>geothermal</strong> <strong>direct</strong> <strong>heat</strong> <strong>use</strong>s, approximately amounting to 25 MWt or 0.5 PJ on an annualbasis. Another 20 could probably be harnessed <strong>for</strong> <strong>use</strong> with 6 kW ground source <strong>heat</strong> pumpsamounting to an additional 0.004 PJ. Hence <strong>for</strong> the next 10 years, at least 0.504 PJ may beexploited from these wells.5.3 ABANDONED UNDERGROUND MINESWithin the next 10 years two mines could probably be installed with 6 kW ground source <strong>heat</strong>pumps yielding an <strong>energy</strong> <strong>of</strong> 0.0004 PJ. Access to abandoned underground mines may,however, be hampered by several factors such as high concentrations <strong>of</strong> combustible gas insome coal mines, cave-ins, highly polluted environment as in the Tui mine and distance frompopulated areas. In some cases the abandoned mines may be filled-in and secured.6.0 SUMMARY AND CONCLUSIONSPotential <strong>sources</strong> <strong>of</strong> <strong>geothermal</strong> <strong>energy</strong> in New Zealand are widespread and are not onlyconfined to active volcanic regions such as the TVZ and Ngawha in Northland (Figure 14).The <strong>sources</strong> <strong>of</strong> <strong>geothermal</strong> <strong>energy</strong> include (1) more than 100 hot spring systems occurring allover New Zealand, ranging in temperatures from 17 o C to 100 o C, (2) <strong>heat</strong>ed waters inabandoned hydrocarbon wells and flooded underground coal and mineral mines and (3)conductive <strong>heat</strong> in rock below 15m that can be harnessed by ground source <strong>heat</strong> pumps andin the future, by using the wellbore <strong>heat</strong> exchangers.<strong>GNS</strong> <strong>Science</strong> Report 2007/16 20

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