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He describes the bottom hole temperature will suddenly increase when the steam arrives at the producer.
The bottom hole temperature of this reservoir unit, which is about 30 ft thick, is approximately 250 °F.
Using bottom hole temperature measurements and/or temperature data from drillstem tests these interpolations were done using 3D kriging interpolation.
At that moment, the reservoir pore volume between wells whose temperature is above the bottom hole temperature of the producer is regarded as the heat invading volume.
Thermal stability results show that the fluid is stable up to 120 °C and can be utilized for the bottom hole temperature of 120 °C (Fig. 13).
If the new model is considered to be accurate, Li et al.'s (2015) model is expected to significantly underestimate the bottom hole temperature.
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Due to depths exceeding 4050 m, bottom hole temperatures exceeding 140 °C, and open hole section (dual zone), technically demanding and somewhat unprecedented conditions had to be managed.
High-pressure and high-temperature (HPHT) wells have bottom hole temperatures of 300 °F (150 °C) and bottom hole pressures of 10,000 psi (69 MPa) or higher (Saito et al. 1998, Saito and Sakuma 2000; Kjosnes et al. 2003).
In our earlier work, we documented its successful performance in different wells in systems with high bottom hole temperatures, high partial pressures of carbon dioxide, and some hydrogen sulfide and brines of different salinities (Ramachandran et al. 2006).
As illustrated in Fig. 6, 12 sites are showing temperature differences in a range of ±10 K, a value as high as the standard deviation of bottom hole temperatures and temperature logs (Hermanrud et al. 1990; Förster 2001; Noack et al. 2010; Agemar et al. 2012, 2014a).
The remaining average temperature misfit between the measured data (GeotIS, StMWIT 2010) and the model predictions of ±10 K lies in the range of the standard deviation of bottom hole temperatures and temperature logs (Hermanrud et al. 1990; Förster 2001; Noack et al. 2010; Agemar et al. 2012, 2014).
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