Table 6: Geothermal resources with electricity generating.
Remarks: 1Reservoir temperature from quartz (maximum stream loss) equation
T = [1,522/(5.75 – log(SiO ))] – 273. .15 [35] SiO based on the study result of CMU [2].
 
2Q = ƞ
 
m. CpΔT, ƞ
 
is 10% [34], m is mass of flow rate, Cp is 4.18 KJ/Kg-K, ΔT is hot difference temperature at approximately 40°C [34] and density of hot string is
 
GS 2 2
 
ORC
1,000 Kg/m. 3.
 
ORC
.
 
3Q = ƞ
 
ORC
 
mCpΔT, m is 75% maximum hot spring flow rate which the minimum value is 10 times of the surface hot spring flow rate [34].