The interpretation of these geothermometers led us to think in an initial assessment of the presence of a deep high temperature resource in a geothermal system, but it is necessary to consider the water rock interaction condition.
Higher temperature resources will produce more liquid and steam for natural pressure conditions.
This is especially true for the high-temperature resources needed for generating electricity.
Tapping for geothermal energy very often requires deep drilling in order to access high-temperature resources.
Drilling wells to reach high-temperature resources deep underground can cost millions of dollars, yet still be cost-effective because they're efficient for power generation, Richards says.
For high-temperature resources where two phase is dominated, the geothermal fluid is moved to the surface of the borehole as a mixture of steam and liquid (brine).
As in previous attempts in the 1980s, the goal is to characterize and test the deep high-temperature resource below the currently exploited reservoir horizons (which is expected to have a temperature of ≈450 °C, e.g., Büsing et al. 2016; Liotta and Ranalli 1999; Stamnes et al. 2016).
Geothermal electric plants were traditionally built exclusively on the edges of tectonic plates where high temperature geothermal resources are available near the surface.
Since the flight season is limited to the time of the year with sufficiently high temperatures and resource availability, every break reduces the potential for foraging and, thus, the productivity of a colony.
Stationary solar concentrators can be integrated with building façade and roof, which can reduce the area of solar cells and attain higher temperature heat resource, especially in winter for building application.
Flash steam plants, harnessing two-phase produced geofluids to drive condensing steam turbines or combined steam turbine/binary cycles, provide a reliable and economical method to harness higher-temperature geothermal resources.
